398:
735:
1254:
723:
40:
4569:
2113:, whereas the western half is in the late oil/wet gas generation window. In terms of transformation ratio, the Barremian and Aptian source rock systems in the area reached 70% to 80% today where the main depocentres are. The charge and accumulation simulation model for the pre-salt province suggests a potential reserve in the Cluster area of Santos Basin much larger than that reported, getting numbers to 60 billion barrels of oil reserves.
1056:
963:
1500:
570:
5001:
1322:
390:
5013:
62:
47:
4711:
4702:
4693:
4684:
4675:
4666:
4657:
4648:
4639:
4630:
151:
4747:
4738:
4729:
4720:
4621:
4612:
4603:
4594:
4585:
4576:
1390:
4873:
4864:
4855:
4846:
4837:
4828:
4819:
4810:
4801:
4792:
4783:
4774:
4765:
4756:
1281:, which laterally grade to greyish ochre and brownish grey calcilutites and grey marls. These facies are interbedded with the alluvial clastics of the Florianópolis Formation. The Guarujá name is restricted to the lowest limestone intercalation, previously named Lower Guarujá by Ojeda and Ahranha in Pereira and Feijó (1994). The microfacies indicate a
1178:
2122:
1005:
1381:
is 1,545 metres (5,069 ft) thick and comprises a thick interval of dark grey clayey rocks, interbedded with the clastics of the Santos and Juréia
Formations. Within this formation, the Ilhabela Member includes the turbiditic sandstones occurring along the section. The sedimentary environment is
1249:
shales and siltstones. These clastic units are thought to represent alluvial environments distributed along the western
Brazilian basin margin, along the Santos Hinge Line. These alluvial environments were gradational towards the east, with the shallow marine carbonates of the Guarujá Formation, and
1520:
is 261 metres (856 ft) thick and consists of grey shales and light grey marls interbedded with fine-grained turbiditic sandstones. This formation in places can be found cropping out at sea bottom. The depositional environment is thought to be talus and open marine basin. Biostratigraphic data
910:
along the
Brazilian and southwestern African continental margins, a process continuing towards the north later in the Cretaceous. The deposition of the lowermost 600 metres (2,000 ft) of salt in the Aptian would have taken approximately 20,000 to 30,000 years. With the continental break-up of
1132:
and silicified. In more distal sections, the formation consists of dark organic matter rich shales. In the well 1-RSJ-625, the formation includes 110 metres (360 ft) of radioactive shales interbedded with carbonates. These facies are thought to represent a lacustrine environment. The organic
656:
in the south of the basin. Within the basin, several highs are located. The Outer High, in the distal part of the Santos Basin, is the most prominent and extensive intra-basinal high with an approximate area of 12,000 square kilometres (4,600 sq mi). The Outer High is likely a segmented
1312:
is 517 metres (1,696 ft) thick and consists of dark grey shales, silts and light grey marls, ochre-brown calcisilts and subordinated sandstones. These facies change laterally into the coarse clastics of the
Florianópolis Formation. Facies analysis indicates a marine environment ranging from
1410:
is 952 metres (3,123 ft) thick and includes a succession of clastics between the coarse facies of the Santos
Formation in the west and the fine-grained clastics of the Itajai-Açu Formation in the east. The formation is characterized by dark grey to greenish and brown shales, dark grey
2129:
Exploration in the Santos Basin started in the 1970s. Between 1970 and 1987, 59 dry wells were drilled, with one discovery in
Santonian turbidites in 1979, Merluza Field. From 1988 to 1998, 45 wells were drilled in the basin providing small discoveries, with the 30 million barrels
2166: m/d) in April 2016. The Lapa Field, originally named Carioca, was taken in production in December 2016. In 2017, the Santos Basin accounted for 35% of Brazil's oil, with the Campos Basin at 55%. In the same year, 76 blocks were open for bidding in the Santos Basin.
1364:
and sandstones, interbedded with grey shales and reddish clays. These facies are interbedded and change laterally into the Itajai-Açu and Juréia
Formations. The sedimentary environment is thought to be transitional continental to marginal marine, ranging from alluvial to
2104:
study performed in 2008 and 2009, a detailed facies model from the pre-salt section was built based on well data and conceptual models from seismic interpretation associated with previous knowledge of the tectono-sedimentary sequences of the Santos Basin. The predicted
1496:. The depositional environment is thought to be a marine carbonate platform, influenced by the arrival of alluvial clastics in the most proximal areas. Biostratigraphic data from planktonic foraminifera, calcareous nanofossils and palynomorphs indicate a Tertiary age.
1411:
siltstones, fine-very fine sandstones and light ochre calcisilts. The depositional environment is thought to be of a marine platform setting. The age based on palynomorphs and calcareous nanofossils is Late
Cretaceous (Santonian-Maastrichtian). Two new
954:, several areas of the now deep water distal part of the Santos Basin were exposed to subaerial conditions and suffered erosion. The distal parts of the basin were affected by E-W to NW-SE oriented shortening, sub-perpendicular to the Brazilian margin.
1114:
of the Campos Basin, the sandstones, stevensite-bearing siltstones and shales represent an alkaline lacustrine environment affected by volcanic activity. The shales represent deeper lacustrine waters in more distal areas. The alternation of the two
1492:, foraminifera, fragmented shells, and algae remains. They are interbedded with grey-greenish clays, siltstones, marls and variegated grey fine-to-medium grained conglomerates. These facies are interbedded with and change laterally to the
531:, the Albian limestones of the Guarujá Formation and the Late Cretaceous to Paleogene turbiditic sandstones of the Itanhaém, Juréia, Itajaí-Açu, Florianópolis and Marambaia Formations. The mobile salt of the Ariri Formation forms regional
1119:
implies a series of alluvial progradation-retractions into the
Cretaceous carbonate lakes. The low textural and compositional maturity of conglomerates and sandstones implies the basin was supplied from areas close to the basin margins.
919:, oceanic circulation returned during the post-rift stage. The drift phase since the Late Cretaceous produced a thick sequence of clastic and carbonate deposits. Differential thermal regimes and sediment loading of these units produced
1459:
The Ponta Aguda
Formation is up to 2,200 metres (7,200 ft) thick and consists of conglomerates, coarse to fine-grained sandstones interbedded with siltstones and shales. The dominant facies are coarse to fine-grained
1533:
is the uppermost formation in the Santos Basin. It has a variable thickness due to the proximal erosion of the uppermost part. The formation consists of whitish grey fine to coarse grained carbonitic sands. They are
1325:
The Itajaí-Açu and Juréia Formations consist mainly of turbidites, formed at the base of the Brazilian marginal continental slopes. The sands of these formations have proven to be excellent reservoirs worldwide.
2134:
Tubarão Field discovered in 1988. Eighty-one wells were drilled from 1999 to 2005, leading to the discovery of the Mexilhão Field. Exploration boomed between 2006 and 2012, with 166 wells and the giant
1128:
The Itapema Formation is several hundreds of metres thick and consists of calcirudites (limestones) and dark shales. The calcirudite limestones consist of fragmented bivalve shells, frequently
4388:
2156: m/d). Thanks to the pre-salt production, compensating for the declining post-salt production, the total oil production of Brazil rose above 2,500 thousand barrels per day (400
4355:
535:, as well as the shales of the post-salt sedimentary infill. In 2014, the total production of only the sub-salt reservoirs accumulated to more than 250 thousand barrels per day (40
3780:
Beasley, Craig J.; Fiduk, Joseph Carl; Bize, Emmanuel; Boyd, Austin; Frydman, Marcelo; Zerilli, Andrea; Dribus, John R.; Moreira, Jobel L.P.; Capeleiro Pinto, Antonio C. (2010),
996:
The total stratigraphic thickness of the sediments in the Santos Basin has been estimated at 23,170 metres (76,020 ft) and has been described in detail by Clemente in 2013.
2139:(8 BBOE), discovered at the Tupi prospect in 2006. In 2013, the Sagitário Field was discovered in the sub-salt carbonates at a water depth of 1,871 metres (6,138 ft) and a
445:
formed on both sides of the South Atlantic; the Pelotas, Santos, Campos and Espírito Santo Basins in Brazil, and the Namibia, Kwanza and Congo Basins in southwestern Africa.
3997:
902:
with relatively uniform water depths, ranging from 600 to 950 metres (1,970 to 3,120 ft). The Late Aptian climate was arid with high evaporation rates which triggered
1250:
further to the open basin with the siltstones of the Itanhaém Formation. Biostratigraphical data and its relations with the Guarujá Formation point towards an Albian age.
4050:"The Outer High of the Santos Basin, Southern São Paulo Plateau, Brazil: Pre-Salt Exploration Outbreak, Paleogeographic Setting, and Evolution of the Syn-Rift Structures"
4116:
3808:
Bryant, Ian; Herbst, Nora; Dailly, Paul; Dribus, John R.; Fainstein, Roberto; Harvey, Nick; McCoss, Angus; Montaron, Bernard; Quirk, Paul Tapponnier, David (2012),
1044:
rocks with a basin–wide distribution. The basalts are dark green to dark grey, holocrystalline, medium grained, with an ophiolitic texture. The main components are
1161:
clasts and bioclasts (fragmented ostracods). The carbonates frequently are partly or completely dolomitized. These facies represent a transitional continental and
1169:
in the Campos Basin, as both are typified by laminated microbialites and stromatolites. These limestones are one of the sub-salt reservoirs in the Santos Basin.
3574:
1464:
sandstones. They range from reddish to grey, usually with calcite cements. Intercalated are reddish to light grey claystones and siltstones. They represent a
1145:
The Barra Velha Formation is approximately 300 to 350 metres (980 to 1,150 ft) thick. In the proximal sections, the formation comprises limestones of
3884:
Geological Origins Of Sugarloaf Mountains In Eastern Brazil And Their Environmental Significance As Refugia For The Mata Atlantica Rainforest (PhD thesis)
1181:
The Ariri Formation, originally deposited as flat evaporite layers, has undergone extensive diapirism and canpoy formation during the Albian to Paleocene.
4381:
1313:
sub-littoral (inner neritic) and more rarely to pelagic (outer bathyal) conditions. The age based on planktonic foraminifera and pollen is Early Albian.
472:. The rift stage of the basin evolution combined with the arid Aptian climate of the southern latitudes resulted in the deposition of evaporites in the
452:
to the north by the Cabo Frio High and the Pelotas Basin in the south by the Florianópolis High and the northwestern boundary onshore is formed by the
3938:
Alves, Tiago M.; Fetter, Marcos; Lima, Cláudio; Cartwright, Joseph A.; Cosgrove, John; Gangá, Adriana; Queiroz, Cláudia L.; Strugale, Michael (2017),
1149:
and laminated microbialites. In the distal sections, it is composed of shales. Interbedded with the laminated microbialites there are limestones with
989:
of the Araçuarí Belt that formed at the western boundary of the Congo Craton. The erosion resistant metamorphic and magmatic rocks are exposed in the
3428:
1193:
581 metres (1,906 ft) thick and may be up to 4,000 metres (13,000 ft) thick in other areas of the basin. It is predominantly composed of
1072:
The Piçarras Formation is 990 metres (3,250 ft) thick and consists of clastic and carbonate rocks. The formation includes reddish polymictic
4125:
1245:
is 343 metres (1,125 ft) thick in the type oil well, and consists of reddish, fine to coarse-grained sandstones with a clay matrix, reddish
4359:
4027:
Seismo-stratigraphy and numerical basin modeling of the southern Brazilian continental margin (Campos, Santos, and Pelotas basins) (PhD thesis)
3552:
1063:
where rift shoulders were exposed and eroded, providing various sediment sources for the deposition in the lacustrine to shallow marine parts.
5004:
4374:
711:
3940:"An incomplete correlation between pre-salt topography, top reservoir erosion, and salt deformation in deep-water Santos Basin (SE Brazil)"
4300:
3491:
480:. This process led to the deposition of a more than 20 kilometres (66,000 ft) thick succession of clastic and carbonate sediments.
5008:
476:, approximately 112 million years ago. The phase of rifting was followed by a thermal sag phase and drift stage in the widening of the
4333:
4309:
4221:
4124:
Mello, Marcio R.; Azambuja Filho, Nilo C.; De Mio, Eduardo; Bender, André A.; De Jesus, Carlos Luciano C.; Schmitt, Priscila (2009),
3652:
714:
The break-up of Pangaea characterised the start of formation of the Santos Basin in the South Atlantic, forming at the same time the
39:
4074:
Kiang Chang, Hung; Assine, Mario Luis; Santos Corrêa, Fernando; Setsuo Tinen, Julio; Campane Vidal, Alexandre; Koike, Luzia (2008),
2100:, hydrocarbon generation and charge, timing of migration, oil origin, quality, and volume of petroleum in the main reservoirs. In a
1012:, Canada. These organic build-up structures are the reservoir of the giant pre-salt Tupi field, holding 8000 million barrels of oil.
597:. The basin covers an area of approximately 352,000 square kilometres (136,000 sq mi), and is bounded in the north by the
4436:
3742:
4075:
3982:
4568:
4280:
3585:
1257:
The depositional environment of the Guarujá Formation has been interpreted as a tidal flat, like this present-day example in
3809:
1213:, evolving under an arid climate. The ostracod assemblages of this formation indicate a neo-Algoas age (local time scale).
5037:
3858:
2746:
545: m/d). In 2017, the Santos Basin accounted for 35% of Brazil's oil, with the northern neighbour Campos Basin at 55%.
4190:
4158:
3781:
4083:
3947:
795:
677:
72:
397:
4150:
3731:
669:
483:
One of the largest Brazilian sedimentary basins, it is the site of several recently (2007 and later) discovered giant
4025:
3688:
3632:
1165:
environment. The age of this formation has been estimated to be Late Barremian to Aptian. It is correlative with the
2109:, integrated with all data, indicates that the Coquinas source rock in most of the eastern half area is in the main
393:
The northern edge of the basin is formed by the Cabo Frio High, extending southeastward from Cabo Frio at the coast.
79:
4665:
4005:
3867:
2836:
2811:
2786:
2715:
2690:
2667:
2619:
2354:
2331:
2085:
1834:
1725:
1378:
1334:
1242:
1222:
685:
4324:
3007:
3978:
Petroleum geology of the Campos and Santos basins, Lower Cretaceous Brazilian sector of the South Atlantic margin
695:
673:
610:
4186:"Tectono-stratigraphic evolution of Lapa Field pre-salt section, Santos Basin (SE Brazilian continental margin)"
1133:
matter-rich shales are one of the main source rocks of the Santos Basin. This formation is correlative with the
4049:
1107:
665:
661:
134:
4917:
4467:
3563:
3511:
653:
208:
4611:
3596:
2211:
4230:
3891:
1383:
284:
4892:
4477:
4457:
1480:
is 1,103 metres (3,619 ft) thick and consists of bioclastic calcarenites and calcirudites, containing
1253:
4942:
4185:
2097:
1361:
1073:
734:
594:
582:
178:
166:
4932:
4927:
4897:
4800:
4764:
4482:
3432:
1134:
5032:
4937:
4922:
4902:
4130:
4034:
3607:
2146:
In 2014, the pre-salt reservoirs of the Santos Basin produced more than 250 thousand barrels per day (40
2106:
1992:
1037:
1021:
1008:
The Guaratiba Group is characterised by the presence of microbialites, like this present-day example in
692:
606:
239:
2642:
2476:
1839:
1552:
The stratigraphy following the classifications by Vieira 2007, Kiang Chang 2008 and Contreras 2011 is:
1309:
1230:
1111:
2088:
of the Santos Basin has revealed insights about the interplay among the elements and processes of the
1166:
1025:
1004:
4629:
4508:
3956:
3817:
3789:
2974:
2951:
2928:
2905:
2882:
2761:
1897:
1873:
1271:
1226:
1186:
637:
586:
558:
554:
426:
317:
200:
170:
138:
114:
4912:
4845:
4534:
4529:
4426:
2781:
1421:
722:
598:
235:
4674:
4647:
4551:
4462:
4421:
2999:
2994:
2859:
2738:
2283:
2140:
2053:
1964:
1888:
1859:
1774:
1720:
1668:
1625:
1563:
1517:
1493:
1440:
1439:
Itamambuca Group is 4,200 metres (13,800 ft) thick and includes four formations, Ponta Aguda,
1427:
1407:
1338:
944:
912:
787:
578:
512:
410:
4513:
4503:
4441:
4431:
916:
763:
715:
4907:
3843:
3041:
2069:
1591:
1530:
1448:
966:
940:
895:
791:
771:
336:
4416:
417:) is an approximately 352,000 square kilometres (136,000 sq mi) large mostly offshore
4809:
4755:
4265:
657:
series of rift fault-block shoulders which were uplifted and eroded during the Late Barremian.
4472:
4110:
2867:
2421:
1576:
1221:
The Camburi Group is up to 6,100 metres (20,000 ft) thick and includes three formations,
906:
conditions in these marginal sag basins. This resulted in the accumulation of thick layers of
806:
590:
418:
174:
5012:
4701:
4256:
3939:
3618:
1369:
and deltas. Biostratigraphic data indicate a Late Cretaceous age (Cenomanian-Maastrichtian).
511:
of the pre-salt Guaratiba Group and the marine shales of the post-salt Itajaí-Açu Formation.
4827:
4818:
4719:
4656:
4593:
4584:
4167:
4092:
3964:
3906:
2447:
2089:
1715:
1620:
1477:
1444:
1358:
1354:
1330:
821:
803:
755:
629:
438:
296:
212:
4836:
4773:
4746:
1055:
1020:
is 4,200 metres (13,800 ft) thick and includes four formations, from old to young the
962:
2576:
2549:
2482:
2453:
2427:
2400:
2289:
2262:
2256:
2236:
2101:
1933:
1499:
1017:
810:
681:
496:
373:
312:
4737:
4692:
4620:
4539:
3036:
2096:
potential (vertical and horizontal distribution), thermal evolution of the source rocks,
836:
bordering the present-day South Atlantic. The Pelotas-Namibia spreading commenced in the
799:
401:
Itajaí (left) and Balneario Camboriú (right) at the southern edge of onshore Santos Basin
4782:
3960:
569:
4048:
Gomes, Paulo Otávio; Kilsdonk, Bill; Minken, Jon; Grow, Tim; Barragan, Roberto (2009),
2570:
2543:
2394:
2136:
2131:
1386:
and planktonic foraminifera indicate a Late Cretaceous age (Cenomanian-Maastrichtian).
1162:
1129:
974:
751:
743:
633:
516:
488:
477:
422:
369:
301:
274:
192:
1329:
The Frade Group is 4,000 metres (13,000 ft) thick and includes three formations:
5026:
4957:
4791:
4728:
4498:
4076:"Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos"
3976:
2675:
2662:
2217:
1710:
1366:
1009:
932:
614:
528:
492:
377:
124:
4872:
4683:
4638:
4282:
Brazilian Pre-Salt & Libra: Overview, Initial Results & Remaining Challenges
4096:
3968:
3732:
Coral Field: Case History in Oil Producing Albian Carbonates in Santos Basin, Brazil
4947:
4863:
4854:
4710:
4602:
3031:
3026:
1558:
1549:
fragments and foraminifera. The depositional environment is thought to be coastal.
1503:
The uppermost sedimentary layer is formed by coquinas (similar to this sample from
1382:
thought to be marine talus to open basin. Biostratigraphic data from palynomorphs,
1321:
1293:
1146:
990:
936:
814:
727:
710:
621:
602:
465:
453:
449:
389:
352:
243:
3996:
Constantino, Renata Regina; Cassola Molina, Eder; Anderson de Souza, Iata (2016),
3839:
South Atlantic Pre-Salt Play Elements, Play Potential and Continental Margin Types
2275:
8,000–12,000 million bbl (1,300–1,900 million m) (recoverable)
433:. The basin is one of the Brazilian basins to have resulted from the break-up of
4575:
4544:
3998:"Study of salt structures from gravity and seismic data in Santos Basin, Brazil"
2221:
2093:
2048:
2011:
1987:
1968:
1780:
1586:
1278:
1060:
1045:
928:
920:
903:
866:
860:
840:, around 133 million years ago and reached the Santos Basin to the north in the
837:
759:
573:
Outline of the Serra do Mar coastal forest ecoregion, bordering the Santos Basin
500:
461:
4366:
4149:
Piovesan, Enelise Katia; Trescastro Bergue, Cristianini; Fauth, Gerson (2010),
3882:
1209:. The sedimentary environment probably was restricted marine including mudflat
1024:, Piçarras, Itapema and Barra Velha Formations. The group is equivalent to the
61:
3837:
2110:
1822:
1606:
1539:
1282:
1154:
1137:
in the Campos Basin. The age of the Itapema Formation is Barremian to Aptian.
1104:
1089:
970:
947:
for hydrocarbon accumulation in the Brazilian and southwest African offshore.
924:
899:
833:
641:
504:
469:
442:
305:
196:
4973:
4151:"New ostracode species from the Upper Cretaceous of the Santos Basin, Brazil"
1059:
The syn-rift stage of the Santos Basin was characterised by the formation of
94:
81:
2982:
2959:
2936:
2913:
2890:
2844:
2819:
2794:
2769:
2723:
2698:
2650:
2627:
2584:
2557:
2530:
2510:
2490:
2461:
2435:
2408:
2362:
2317:
2297:
2270:
2244:
2040:
1980:
1960:
1942:
1938:
1912:
1902:
1878:
1844:
1808:
1801:
1794:
1768:
1748:
1739:
1734:
1703:
1689:
1662:
1647:
1638:
1634:
1568:
1461:
1394:
1342:
1202:
1194:
1150:
1085:
951:
907:
870:
841:
767:
726:
The Santos Basin formed with the rifting of Brazil and Africa splitting the
636:
is located at the coastal edge of the Santos Basin in the northern portion,
625:
532:
524:
520:
508:
484:
364:
341:
188:
1099:
The conglomerates and sandstones of the formation are representative of an
649:
204:
4171:
3492:
Brazil Draws Auctions Calendar, Confirms Santos Basin Most Attractive Area
1397:
commonly used to identify paleo-environments and for age dating formations
1389:
2031:
2022:
1950:
1815:
1615:
1535:
1485:
1412:
1290:
1100:
1093:
888:
856:
825:
783:
775:
689:
645:
434:
345:
329:
2058:
1682:
1596:
1546:
1542:
1481:
1465:
1416:
1289:
and open carbonate platform depositional environment. The age based on
1081:
982:
779:
324:
738:
Schematic diagram of the formation of a passive margin on a rift basin
2382:
2339:
2062:
1997:
1928:
1921:
1868:
1829:
1696:
1504:
1297:
1286:
1275:
1258:
1210:
1198:
1116:
1077:
1049:
1041:
986:
882:
876:
845:
844:. Seafloor spreading continued northwards to the Campos Basin in the
829:
774:
is the most iconic. The ancient rocks consist of a Neoproterozoic to
747:
499:, with an estimated 8 to 12 billion barrels of recoverable oil. Main
473:
457:
430:
156:
1317:
IV - Frade Group (Turonian-Maastrichtian, middle post-salt sequence)
977:
are the onshore representatives of the basement of the Santos Basin.
1177:
1080:
in a clay-sandy matrix. It also includes white, reddish lacustrine
851:
Five tectonic stages have been identified in the Brazilian basins:
577:
The Santos Basin is a mostly offshore sedimentary basin across the
4356:"Pre-Salt Reservoirs Offshore Brazil: Perspectives and Challenges"
2120:
1946:
1849:
1744:
1730:
1643:
1630:
1498:
1489:
1388:
1320:
1252:
1176:
1158:
1054:
1003:
993:, forming the edge of the Santos Basin along the Brazilian coast.
961:
733:
721:
709:
568:
464:. The basin started forming in the Early Cretaceous on top of the
396:
388:
4231:"Santos Basin: 40 Years from Shallow to Deep to Ultra-Deep Water"
1217:
III - Camburi Group (Albian-Cenomanian, lower post-salt sequence)
1246:
1206:
4370:
4184:
Ribeiro da Silva, Suzana Faria Chula; Pereira, Egberto (2017),
2495:
1,100–2,000 million bbl (170–320 million m)
2413:
3,000–4,000 million bbl (480–640 million m)
2121:
2604:
1357:
is 1,275 metres (4,183 ft) thick and consists of reddish
3012:
0.074 trillion cu ft (2.1 billion m)
2680:
0.173 trillion cu ft (4.9 billion m)
1197:. The formation is characterized by thick intervals of white
660:
The climate of the onshore stretch of the basin ranges from
3860:
The Petroleum Potential of the Brazilian Sedimentary Basins
1507:
in Europe); carbonitic sandstones composed of broken shells
1000:
I - Guaratiba Group (Hauterivian-Aptian, pre-salt sequence)
381:
4258:
The Santos Basin, Brazil: Unlocking the Pre-Salt Potential
3653:
Petrobras BS-400 gas find confirms E&P expansion plans
2826:
2.5 trillion cu ft (71 billion m)
2801:
3.4 trillion cu ft (96 billion m)
2655:
1.6 trillion cu ft (45 billion m)
2468:
17 trillion cu ft (480 billion m)
456:
coastal range. The basin is known for its thick layers of
1435:
V - Itamambuca Group (Cenozoic, upper post-salt sequence)
950:
During the phases of halokinesis, dated to the Albian to
813:, is considered the driver behind the formation of these
750:
consisting of hard and resistant rocks and partly on the
676:(Cfa). The onshore portion of the Santos Basin is in the
2705:
1 trillion cu ft (28 billion m)
581:, bordering from north to south the Brazilian states of
2849:
212.8 million bbl (33.83 million m)
2799:
532.23 million bbl (84.6 million m)
2751:
231.16 million bbl (36.8 million m)
2703:
174.27 million bbl (27.7 million m)
2589:
8,000 million bbl (1,300 million m)
1554:
1419:
of wells drilled into the Santonian-Campanian section,
894:
The sag phase in the Santos Basin was characterised by
620:
Along the Brazilian coast, the basin is bounded by the
2964:
15.16 million bbl (2.41 million m)
2941:
22.57 million bbl (3.59 million m)
2895:
48.81 million bbl (7.76 million m)
2872:
92.64 million bbl (14.7 million m)
2824:
54.24 million bbl (8.62 million m)
2774:
25.04 million bbl (3.98 million m)
2728:
63.52 million bbl (10.1 million m)
2632:
95.76 million bbl (15.2 million m)
2609:
158.4 million bbl (25.2 million m)
2367:
321.4 million bbl (51.1 million m)
4972:
Souza Lima, Wagner; Hamsi Junior, Gilvan Pio (2003).
2466:
1,600 million bbl (250 million m)
2302:
3,058 million bbl (486 million m)
939:
and various salt-related structures produced several
460:
that have formed structures in the subsurface due to
4218:
Oil, natural gas and biofuels - Statistical Yearbook
3347:
3345:
3343:
3317:
3315:
3313:
3311:
3309:
3307:
3305:
2562:
459 million bbl (73.0 million m)
2515:
113 million bbl (18.0 million m)
2344:
176 million bbl (28.0 million m)
1274:
is 832 metres (2,730 ft) thick and consists of
553:
The Santos Basin is named after the coastal city of
4966:
4885:
4522:
4491:
4450:
4409:
4402:
3478:
3476:
3260:
3258:
3256:
3254:
3235:
3233:
3231:
3229:
3227:
3217:
3215:
3213:
3211:
3201:
3199:
3197:
3195:
3185:
3183:
3181:
3179:
3151:
3149:
2535:
83 million bbl (13.2 million m)
832:, starting to break-up, resulting in a sequence of
802:, have been found underlying the Santos Basin. The
730:
from the Araçuaí Belt, shown as a thin brown strip.
363:
351:
335:
323:
311:
295:
290:
280:
270:
265:
257:
249:
231:
223:
218:
184:
162:
144:
130:
120:
110:
71:
21:
4126:"3D modeling illuminates Brazil's presalt geology"
2987:30 million bbl (4.8 million m)
2918:5 million bbl (0.79 million m)
1040:is 40 metres (130 ft) thick and includes the
3743:Estrela do Mar, Cavalo Marinho oil output by 2007
3700:
3698:
3696:
3521:
3519:
3359:
3357:
3333:
3331:
3329:
3327:
1173:II - Ariri Formation (Late Aptian, salt sequence)
786:, formed during the collision of Gondwana in the
425:, some 300 kilometres (190 mi) southeast of
3842:, Houston Geological Society, pp. 1:06:49,
3810:"Basin to Basin: Plate Tectonics in Exploration"
3672:
3670:
3668:
3666:
3664:
3662:
3660:
3628:
3626:
3286:
3284:
3282:
3280:
3278:
3276:
3274:
3272:
3270:
981:The basement of the Santos Basin is composed of
911:the Santos and Campos Basins from the opposite
766:along the Brazilian coast, most notably in the
762:basement of the Santos Basin is exposed as the
487:, including the first large pre-salt discovery
3423:
3421:
3419:
3417:
3415:
3413:
3411:
3409:
3407:
3112:
3110:
1103:environment. The coquinas represent a shallow
4382:
4354:Lyrra, Gustavsyn Alpherline (November 2007).
3405:
3403:
3401:
3399:
3397:
3395:
3393:
3391:
3389:
3387:
495:(1.6 billion barrels and 17 tcf of gas), and
16:Sedimentary basin in the south Atlantic Ocean
8:
4115:: CS1 maint: DOI inactive as of July 2024 (
3482:Ribeiro da Silva & Pereira, 2017, p.136
2193:Reserves (in place unless otherwise noted)
4406:
4389:
4375:
4367:
3684:
3682:
3608:Brazil Confirms Massive Offshore Oil Field
2173:
261:~352,000 km (136,000 sq mi)
60:
4288:, KIVI Engineering Society, pp. 1–80
1205:, ochre greyish calcilutites, shales and
1415:species were identified in the drilling
754:mobile belts composed of less resistant
3052:
2195:
1580:
1096:assemblages, is Hauterivian to Aptian.
945:combined stratigraphic-structural traps
613:, separating the Santos Basin from the
4108:
2170:Oil and gas fields in the Santos Basin
2016:
18:
4035:Ruprecht-Karls-Universität Heidelberg
1954:
1937:
1932:
1906:
1901:
1896:
1651:
1642:
1624:
66:Location of the basin offshore Brazil
7:
1084:(shelly limestones) and sandstones,
46:
4191:Journal of Sedimentary Environments
4159:Revista Brasileira de Paleontologia
2130:(4.8 million cubic metres) of
1092:composition. Its age, based on the
746:margin developed on Archean stable
448:Santos Basin is separated from the
2143:of 6,150 metres (20,180 ft).
14:
4974:"Bacias sedimentares brasileiras"
4084:Revista Brasileira de Geociências
357:
5011:
5000:
4999:
4871:
4862:
4853:
4844:
4835:
4826:
4817:
4808:
4799:
4790:
4781:
4772:
4763:
4754:
4745:
4736:
4727:
4718:
4709:
4700:
4691:
4682:
4673:
4664:
4655:
4646:
4637:
4628:
4619:
4610:
4601:
4592:
4583:
4574:
4567:
1525:Sepetiba Formation (Pleistocene)
601:, separating the basin from the
253:Brazilian Atlantic margin basins
149:
45:
38:
4097:10.25249/0375-7536.2008382S2946
3969:10.1016/j.marpetgeo.2016.10.015
3846:from the original on 2021-12-21
3059:Constantino et el., 2016, p.200
1468:to shallow marine environment.
778:high-grade metamorphic core of
3907:"The Paraná-Etendeka Province"
3299:Kiang Chang et al., 2008, p.34
3290:Kiang Chang et al., 2008, p.32
1341:. They predominantly comprise
1052:, usually fresh, non-altered.
875:Sag stage - Late Barremian to
702:) has its restricted habitat.
632:in the southwest. The city of
1:
4326:Brazil Round 9 - Santos Basin
3983:Danmarks Tekniske Universitet
3881:Owen, Sarah Caroline (2014),
3868:Brazilian Geophysical Society
2125:Location of the Tupi prospect
1956:~1,500 m (4,900 ft)
887:Drift stage - Late Albian to
798:, exposed to the west in the
684:biome. On the islands of the
421:. It is located in the south
4397:Sedimentary basins of Brazil
4229:Juarez Feijó, Fávio (2013),
3948:Marine and Petroleum Geology
3870:& EXPOGEf, pp. 1–44
1908:2,500 m (8,200 ft)
1884:2,500 m (8,200 ft)
1855:1,500 m (4,900 ft)
1764:2,000 m (6,600 ft)
1759:2,000 m (6,600 ft)
1754:2,700 m (8,900 ft)
1658:2,700 m (8,900 ft)
1653:2,200 m (7,200 ft)
1076:, with clasts of basalt and
770:of Rio de Janeiro, of which
678:Serra do Mar coastal forests
4279:Moczydlower, Bruno (2014),
848:, at approximately 112 Ma.
670:tropical rainforest climate
5054:
4302:Brazil Bidding Rounds 2017
4299:Petersohn, Eliane (2017),
4024:Contreras, Jorham (2011),
3134:Beasley et al., 2010, p.31
1602:570 m (1,870 ft)
4997:
4562:
3633:Baúna and Piracaba Fields
3164:Bryant et al., 2012, p.51
2205:"Paleocene-Maastrichtian"
2066:
2057:
2052:
2001:
1996:
1991:
1972:
1959:
1916:
1911:
1882:
1877:
1872:
1867:
1853:
1848:
1843:
1838:
1833:
1786:
1767:
1762:
1757:
1752:
1743:
1738:
1729:
1724:
1719:
1714:
1674:
1661:
1656:
1629:
1619:
1600:
1595:
1590:
1572:
1567:
1562:
1521:indicate a Tertiary age.
898:and generated restricted
796:Paraná and Etendeka traps
794:. Basalts similar to the
688:in the Santos Basin, the
674:humid subtropical climate
59:
33:
26:
4918:Pernambuco-Paraíba Basin
4468:Parecis-Alto Xingu Basin
4323:Vieira, Juliana (2007),
4210:Santos Basin exploration
3975:Clemente, Pilar (2013),
3782:"Brazil's Pre-Salt Play"
3722:ANP Yearbook, 2014, p.30
3381:Mello et al., 2009, p.47
3173:Alves et al, 2017, p.319
1422:?Afrocytheridea cretacea
1201:, associated with white
666:tropical monsoon climate
662:tropical savanna climate
648:in the central area and
4255:Mann, Jaswiner (2013),
4006:Geofísica Internacional
3905:Peate, David W (1997),
3892:University of Leicester
3543:Moczydlower, 2014, p.52
3534:Moczydlower, 2014, p.42
3461:Moczydlower, 2014, p.34
3086:Gomes et al., 2009, p.3
2212:Karoon Energy Australia
2117:Oil and gas exploration
1384:calcareous nannofossils
1243:Florianópolis Formation
1237:Florianópolis Formation
923:; salt movement in the
824:, the former continent
700:Leontopithecus caissara
686:Superagüi National Park
3857:Oddone, Décio (2017),
2812:Florianópolis Fm.
2126:
1835:Florianópolis Fm.
1508:
1398:
1326:
1262:
1182:
1064:
1013:
978:
883:Early to Middle Albian
828:, as southern part of
739:
731:
719:
696:Superagüi lion tamarin
574:
441:, where a sequence of
414:
402:
394:
4923:Sergipe-Alagoas Basin
4893:Foz do Amazonas Basin
4478:São Luís-Grajaú Basin
4458:Alto do Tapajós Basin
4172:10.4072/rbp.2010.3.02
4099:(inactive 2024-07-19)
3914:Geophysical Monograph
3502:Petersohn, 2017, p.18
3429:"Santos Basin Fields"
3351:Contreras, 2011, p.77
3321:Contreras, 2011, p.22
3248:Piovesan, 2010, p.177
2124:
1502:
1455:Ponta Aguda Formation
1428:Pelecocythere dinglei
1392:
1324:
1256:
1180:
1141:Barra Velha Formation
1058:
1028:of the Campos Basin.
1007:
965:
737:
725:
713:
693:critically endangered
572:
491:(8 billion barrels),
400:
392:
227:Both, mostly offshore
95:26.10611°S 43.72917°W
5038:Oil fields of Brazil
4943:Espírito Santo Basin
4238:Search and Discovery
4057:Search and Discovery
3932:Santos Basin geology
3836:Love, Frank (2013),
3264:Clemente, 2013, p.24
3239:Clemente, 2013, p.23
3221:Clemente, 2013, p.22
3205:Clemente, 2013, p.21
3189:Clemente, 2013, p.20
3155:Contreras, 2011, p.8
3143:Contreras, 2011, p.7
3077:Contreras, 2011, p.1
3068:Clemente, 2013, p.18
2098:transformation ratio
1778:(Itajaí-Açu, Juréia)
1393:Ostracods are small
1379:Itajaí-Açu Formation
1373:Itajaí-Açu Formation
1157:textures made up of
628:in the northeast to
478:South Atlantic Ocean
330:Break-up of Gondwana
275:South Atlantic Ocean
100:-26.10611; -43.72917
4933:Jequitinhonha Basin
4928:Camamu-Almada Basin
4898:Pará-Maranhão Basin
4483:São Francisco Basin
4422:Madre de Deus Basin
3961:2017MarPG..79..300A
3104:Clemente, 2013, p.3
2837:Itajaí-Açu Fm.
2787:Itajaí-Açu Fm.
2716:Itajaí-Açu Fm.
2691:Itajaí-Açu Fm.
2668:Itajaí-Açu Fm.
2620:Itajaí-Açu Fm.
2355:Itajaí-Açu Fm.
2332:Itajaí-Açu Fm.
2220:(11.9 million
2141:true vertical depth
1726:Itajaí-Açu Fm.
1518:Marambaia Formation
1512:Marambaia Formation
1494:Marambaia Formation
1135:Coqueiros Formation
644:and the islands of
624:and stretches from
579:Tropic of Capricorn
240:Florianópolis Highs
91: /
4938:Cumuruxatiba Basin
4903:Barreirinhas Basin
3753:Juarez, 2013, p.11
3704:Juarez, 2013, p.14
3643:Juarez, 2013, p.24
3525:Juarez, 2013, p.44
3372:Vieira, 2007, p.24
3363:Vieira, 2007, p.18
3337:Vieira, 2007, p.19
3125:Peate, 1997, p.220
3042:Geology of Namibia
2860:Marambaia Fm.
2739:Marambaia Fm.
2577:Guaratiba Gp.
2550:Guaratiba Gp.
2483:Guaratiba Gp.
2454:Guaratiba Gp.
2428:Guaratiba Gp.
2401:Guaratiba Gp.
2290:Guaratiba Gp.
2263:Guaratiba Gp.
2237:Guaratiba Gp.
2127:
1934:Guaratiba Gp.
1626:Marambaia Fm.
1573:Maximum thickness
1531:Sepetiba Formation
1509:
1399:
1327:
1310:Itanhaém Formation
1304:Itanhaém Formation
1263:
1183:
1068:Piçarras Formation
1065:
1038:Camboriú Formation
1032:Camboriú Formation
1014:
979:
967:Sugarloaf Mountain
896:thermal subsidence
881:Post-rift stage -
792:Brasiliano orogeny
772:Sugarloaf Mountain
740:
732:
720:
654:Balneário Camboriú
607:Florianópolis High
575:
515:are formed by the
485:oil and gas fields
403:
395:
209:Balneário Camboriú
5020:
5019:
4560:
4559:
3762:Juarez, 2013, p.7
3713:Vieira, 2007, p.8
3676:Vieira, 2007, p.9
3564:Iracema Sul Field
3470:Oddone, 2017, p.5
3452:Juarez, 2013, p.1
3095:Love, 2015, 16:16
3018:
3017:
2643:Itanhaém Fm.
2077:
2076:
1993:Camboriú Fm.
1840:Itanhaém Fm.
1592:Sepetiba Fm.
1577:Petroleum geology
1300:is Early Albian.
1272:Guarujá Formation
1266:Guarujá Formation
1124:Itapema Formation
1112:Atafona Formation
1110:. Similar to the
865:Syn-rift stage -
855:Pre-rift stage -
756:metamorphic rocks
680:ecoregion of the
419:sedimentary basin
387:
386:
285:Ribeira de Iguape
5045:
5015:
5003:
5002:
4992:
4990:
4989:
4875:
4866:
4857:
4848:
4839:
4830:
4821:
4812:
4803:
4794:
4785:
4776:
4767:
4758:
4749:
4740:
4731:
4722:
4713:
4704:
4695:
4686:
4677:
4668:
4659:
4650:
4641:
4632:
4623:
4614:
4605:
4596:
4587:
4578:
4571:
4407:
4391:
4384:
4377:
4368:
4363:
4358:. Archived from
4343:
4342:
4341:
4331:
4319:
4318:
4317:
4307:
4295:
4294:
4293:
4287:
4275:
4274:
4273:
4263:
4251:
4250:
4249:
4235:
4225:
4205:
4204:
4203:
4180:
4179:
4178:
4155:
4145:
4144:
4143:
4120:
4114:
4106:
4105:
4104:
4080:
4070:
4069:
4068:
4054:
4044:
4043:
4042:
4037:, pp. 1–171
4032:
4020:
4019:
4018:
4002:
3992:
3991:
3990:
3971:
3944:
3927:
3926:
3925:
3911:
3901:
3900:
3899:
3894:, pp. 1–337
3889:
3877:
3876:
3875:
3865:
3853:
3852:
3851:
3832:
3831:
3830:
3814:
3804:
3803:
3802:
3786:
3763:
3760:
3754:
3751:
3745:
3740:
3734:
3729:
3723:
3720:
3714:
3711:
3705:
3702:
3691:
3686:
3677:
3674:
3655:
3650:
3644:
3641:
3635:
3630:
3621:
3616:
3610:
3605:
3599:
3594:
3588:
3583:
3577:
3572:
3566:
3561:
3555:
3550:
3544:
3541:
3535:
3532:
3526:
3523:
3514:
3509:
3503:
3500:
3494:
3489:
3483:
3480:
3471:
3468:
3462:
3459:
3453:
3450:
3444:
3443:
3441:
3440:
3431:. Archived from
3425:
3382:
3379:
3373:
3370:
3364:
3361:
3352:
3349:
3338:
3335:
3322:
3319:
3300:
3297:
3291:
3288:
3265:
3262:
3249:
3246:
3240:
3237:
3222:
3219:
3206:
3203:
3190:
3187:
3174:
3171:
3165:
3162:
3156:
3153:
3144:
3141:
3135:
3132:
3126:
3123:
3117:
3116:Owen, 2014, p.36
3114:
3105:
3102:
3096:
3093:
3087:
3084:
3078:
3075:
3069:
3066:
3060:
3057:
2975:Guarujá Fm.
2952:Guarujá Fm.
2929:Guarujá Fm.
2906:Guarujá Fm.
2883:Guarujá Fm.
2762:Guarujá Fm.
2216:75 million
2181:
2180:bold is pre-salt
2174:
2162:
2161:
2152:
2151:
2090:petroleum system
2043:
2034:
2025:
2014:
1874:Guarujá Fm.
1555:
1478:Iguape Formation
1472:Iguape Formation
1408:Juréia Formation
1402:Juréia Formation
1355:Santos Formation
1349:Santos Formation
1261:, United States.
1192:
1167:Macabu Formation
1026:Lagoa Feia Group
927:. The resulting
822:Early Cretaceous
804:Tristan da Cunha
706:Tectonic history
557:in the state of
541:
540:
439:Early Cretaceous
155:
153:
152:
106:
105:
103:
102:
101:
96:
92:
89:
88:
87:
84:
64:
49:
48:
42:
19:
5053:
5052:
5048:
5047:
5046:
5044:
5043:
5042:
5023:
5022:
5021:
5016:
4993:
4987:
4985:
4971:
4962:
4881:
4880:
4879:
4878:
4877:
4876:
4868:
4867:
4859:
4858:
4850:
4849:
4841:
4840:
4832:
4831:
4823:
4822:
4814:
4813:
4805:
4804:
4796:
4795:
4787:
4786:
4778:
4777:
4769:
4768:
4760:
4759:
4751:
4750:
4742:
4741:
4733:
4732:
4724:
4723:
4715:
4714:
4706:
4705:
4697:
4696:
4688:
4687:
4679:
4678:
4670:
4669:
4661:
4660:
4652:
4651:
4643:
4642:
4634:
4633:
4625:
4624:
4616:
4615:
4607:
4606:
4598:
4597:
4589:
4588:
4580:
4579:
4556:
4518:
4509:Recôncavo Basin
4487:
4446:
4398:
4395:
4353:
4350:
4339:
4337:
4336:, pp. 1–73
4329:
4322:
4315:
4313:
4312:, pp. 1–45
4305:
4298:
4291:
4289:
4285:
4278:
4271:
4269:
4261:
4254:
4247:
4245:
4233:
4228:
4224:, pp. 1–73
4215:
4212:
4201:
4199:
4183:
4176:
4174:
4153:
4148:
4141:
4139:
4123:
4107:
4102:
4100:
4078:
4073:
4066:
4064:
4052:
4047:
4040:
4038:
4030:
4023:
4016:
4014:
4000:
3995:
3988:
3986:
3985:, pp. 1–33
3974:
3942:
3937:
3934:
3923:
3921:
3909:
3904:
3897:
3895:
3887:
3880:
3873:
3871:
3863:
3856:
3849:
3847:
3835:
3828:
3826:
3818:Oilfield Review
3812:
3807:
3800:
3798:
3790:Oilfield Review
3784:
3779:
3776:
3771:
3766:
3761:
3757:
3752:
3748:
3741:
3737:
3730:
3726:
3721:
3717:
3712:
3708:
3703:
3694:
3687:
3680:
3675:
3658:
3651:
3647:
3642:
3638:
3631:
3624:
3617:
3613:
3606:
3602:
3595:
3591:
3584:
3580:
3573:
3569:
3562:
3558:
3551:
3547:
3542:
3538:
3533:
3529:
3524:
3517:
3510:
3506:
3501:
3497:
3490:
3486:
3481:
3474:
3469:
3465:
3460:
3456:
3451:
3447:
3438:
3436:
3427:
3426:
3385:
3380:
3376:
3371:
3367:
3362:
3355:
3350:
3341:
3336:
3325:
3320:
3303:
3298:
3294:
3289:
3268:
3263:
3252:
3247:
3243:
3238:
3225:
3220:
3209:
3204:
3193:
3188:
3177:
3172:
3168:
3163:
3159:
3154:
3147:
3142:
3138:
3133:
3129:
3124:
3120:
3115:
3108:
3103:
3099:
3094:
3090:
3085:
3081:
3076:
3072:
3067:
3063:
3058:
3054:
3050:
3023:
3000:Juréia Fm.
2825:
2800:
2704:
2467:
2196:
2179:
2178:
2172:
2159:
2157:
2149:
2147:
2119:
2082:
2039:
2030:
2021:
2010:
1975:
1974:
1957:
1909:
1885:
1856:
1789:
1788:
1783:
1779:
1777:
1773:
1771:
1765:
1760:
1755:
1721:Juréia Fm.
1716:Santos Fm.
1677:
1676:
1671:
1667:
1665:
1659:
1654:
1621:Iguape Fm.
1603:
1437:
1319:
1219:
1190:
1187:Ariri Formation
1175:
1018:Guaratiba Group
1002:
960:
811:Tristan hotspot
809:, known as the
708:
682:Atlantic Forest
567:
551:
538:
536:
513:Reservoir rocks
415:Bacia de Santos
219:Characteristics
150:
148:
99:
97:
93:
90:
85:
82:
80:
78:
77:
67:
55:
54:
53:
52:
51:
50:
28:Bacia de Santos
17:
12:
11:
5:
5051:
5049:
5041:
5040:
5035:
5025:
5024:
5018:
5017:
4998:
4995:
4994:
4970:
4968:
4964:
4963:
4961:
4960:
4955:
4950:
4945:
4940:
4935:
4930:
4925:
4920:
4915:
4913:Potiguar Basin
4910:
4905:
4900:
4895:
4889:
4887:
4883:
4882:
4870:
4869:
4861:
4860:
4852:
4851:
4843:
4842:
4834:
4833:
4825:
4824:
4816:
4815:
4807:
4806:
4798:
4797:
4789:
4788:
4780:
4779:
4771:
4770:
4762:
4761:
4753:
4752:
4744:
4743:
4735:
4734:
4726:
4725:
4717:
4716:
4708:
4707:
4699:
4698:
4690:
4689:
4681:
4680:
4672:
4671:
4663:
4662:
4654:
4653:
4645:
4644:
4636:
4635:
4627:
4626:
4618:
4617:
4609:
4608:
4600:
4599:
4591:
4590:
4582:
4581:
4573:
4572:
4566:
4565:
4564:
4563:
4561:
4558:
4557:
4555:
4554:
4549:
4548:
4547:
4537:
4535:Pantanal Basin
4532:
4530:Itaboraí Basin
4526:
4524:
4520:
4519:
4517:
4516:
4511:
4506:
4501:
4495:
4493:
4489:
4488:
4486:
4485:
4480:
4475:
4473:Parnaíba Basin
4470:
4465:
4460:
4454:
4452:
4448:
4447:
4445:
4444:
4439:
4434:
4429:
4427:Solimões Basin
4424:
4419:
4413:
4411:
4404:
4400:
4399:
4396:
4394:
4393:
4386:
4379:
4371:
4365:
4364:
4362:on 2013-10-24.
4349:
4348:External links
4346:
4345:
4344:
4320:
4296:
4276:
4268:, pp. 1–2
4252:
4226:
4211:
4208:
4207:
4206:
4181:
4166:(3): 175–180,
4146:
4121:
4071:
4045:
4021:
3993:
3972:
3933:
3930:
3929:
3928:
3902:
3878:
3854:
3833:
3805:
3775:
3774:Brazil general
3772:
3770:
3767:
3765:
3764:
3755:
3746:
3735:
3724:
3715:
3706:
3692:
3678:
3656:
3645:
3636:
3622:
3619:Sapinhoá Field
3611:
3600:
3589:
3578:
3575:Piracucá Field
3567:
3556:
3545:
3536:
3527:
3515:
3504:
3495:
3484:
3472:
3463:
3454:
3445:
3383:
3374:
3365:
3353:
3339:
3323:
3301:
3292:
3266:
3250:
3241:
3223:
3207:
3191:
3175:
3166:
3157:
3145:
3136:
3127:
3118:
3106:
3097:
3088:
3079:
3070:
3061:
3051:
3049:
3046:
3045:
3044:
3039:
3034:
3029:
3022:
3019:
3016:
3015:
3013:
3010:
3005:
3002:
2997:
2991:
2990:
2988:
2985:
2980:
2977:
2972:
2968:
2967:
2965:
2962:
2957:
2954:
2949:
2948:Estrela do Mar
2945:
2944:
2942:
2939:
2934:
2931:
2926:
2922:
2921:
2919:
2916:
2911:
2908:
2903:
2899:
2898:
2896:
2893:
2888:
2885:
2880:
2876:
2875:
2873:
2870:
2865:
2862:
2857:
2853:
2852:
2850:
2847:
2842:
2839:
2834:
2830:
2829:
2827:
2822:
2817:
2814:
2809:
2805:
2804:
2802:
2797:
2792:
2789:
2784:
2778:
2777:
2775:
2772:
2767:
2764:
2759:
2758:Cavalo Marinho
2755:
2754:
2752:
2749:
2744:
2741:
2736:
2732:
2731:
2729:
2726:
2721:
2718:
2713:
2709:
2708:
2706:
2701:
2696:
2693:
2688:
2684:
2683:
2681:
2678:
2673:
2670:
2665:
2659:
2658:
2656:
2653:
2648:
2645:
2640:
2636:
2635:
2633:
2630:
2625:
2622:
2617:
2613:
2612:
2610:
2607:
2602:
2599:
2597:
2593:
2592:
2590:
2587:
2582:
2579:
2574:
2566:
2565:
2563:
2560:
2555:
2552:
2547:
2539:
2538:
2536:
2533:
2528:
2525:
2523:
2519:
2518:
2516:
2513:
2508:
2505:
2503:
2499:
2498:
2496:
2493:
2488:
2485:
2480:
2472:
2471:
2469:
2464:
2459:
2456:
2451:
2443:
2442:
2440:
2438:
2433:
2430:
2425:
2417:
2416:
2414:
2411:
2406:
2403:
2398:
2390:
2389:
2387:
2385:
2380:
2377:
2375:
2371:
2370:
2368:
2365:
2360:
2357:
2352:
2348:
2347:
2345:
2342:
2337:
2334:
2329:
2325:
2324:
2322:
2320:
2315:
2312:
2310:
2306:
2305:
2303:
2300:
2295:
2292:
2287:
2279:
2278:
2276:
2273:
2268:
2265:
2260:
2252:
2251:
2249:
2247:
2242:
2239:
2234:
2228:
2227:
2225:
2214:
2209:
2206:
2203:
2199:
2198:
2194:
2191:
2188:
2185:
2182:
2171:
2168:
2132:oil equivalent
2118:
2115:
2102:basin modeling
2086:Basin analysis
2081:
2080:Basin analysis
2078:
2075:
2074:
2072:
2067:
2065:
2056:
2051:
2045:
2044:
2036:
2035:
2027:
2026:
2018:
2017:
2015:
2007:
2006:
2004:
2002:
2000:
1995:
1990:
1984:
1983:
1977:
1976:
1973:
1971:
1958:
1955:
1953:
1936:
1931:
1925:
1924:
1918:
1917:
1915:
1910:
1907:
1905:
1900:
1898:Ariri Fm.
1894:
1893:
1891:
1886:
1883:
1881:
1876:
1871:
1865:
1864:
1862:
1857:
1854:
1852:
1847:
1842:
1837:
1832:
1826:
1825:
1819:
1818:
1812:
1811:
1805:
1804:
1798:
1797:
1791:
1790:
1787:
1785:
1766:
1763:
1761:
1758:
1756:
1753:
1751:
1742:
1737:
1728:
1723:
1718:
1713:
1707:
1706:
1700:
1699:
1693:
1692:
1686:
1685:
1679:
1678:
1675:
1673:
1660:
1657:
1655:
1652:
1650:
1641:
1628:
1623:
1618:
1612:
1611:
1609:
1604:
1601:
1599:
1594:
1589:
1583:
1582:
1579:
1574:
1571:
1566:
1561:
1545:consisting of
1527:
1526:
1514:
1513:
1474:
1473:
1457:
1456:
1436:
1433:
1404:
1403:
1375:
1374:
1367:braided rivers
1351:
1350:
1318:
1315:
1306:
1305:
1268:
1267:
1239:
1238:
1218:
1215:
1174:
1171:
1163:shallow marine
1143:
1142:
1126:
1125:
1088:and shales of
1070:
1069:
1034:
1033:
1001:
998:
975:Rio de Janeiro
969:and the other
959:
956:
892:
891:
885:
879:
873:
871:Late Barremian
863:
752:Neoproterozoic
744:South Atlantic
707:
704:
634:Rio de Janeiro
599:Cabo Frio High
595:Santa Catarina
583:Rio de Janeiro
566:
563:
550:
547:
423:Atlantic Ocean
385:
384:
367:
361:
360:
355:
349:
348:
339:
333:
332:
327:
321:
320:
318:South American
315:
309:
308:
302:Passive margin
299:
293:
292:
288:
287:
282:
278:
277:
272:
268:
267:
263:
262:
259:
255:
254:
251:
247:
246:
233:
229:
228:
225:
221:
220:
216:
215:
193:Rio de Janeiro
186:
182:
181:
179:Santa Catarina
167:Rio de Janeiro
164:
160:
159:
146:
142:
141:
132:
128:
127:
122:
118:
117:
112:
108:
107:
75:
69:
68:
65:
57:
56:
44:
43:
37:
36:
35:
34:
31:
30:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
5050:
5039:
5036:
5034:
5031:
5030:
5028:
5014:
5010:
5006:
4996:
4983:
4979:
4975:
4969:
4965:
4959:
4958:Pelotas Basin
4956:
4954:
4951:
4949:
4946:
4944:
4941:
4939:
4936:
4934:
4931:
4929:
4926:
4924:
4921:
4919:
4916:
4914:
4911:
4909:
4906:
4904:
4901:
4899:
4896:
4894:
4891:
4890:
4888:
4884:
4874:
4865:
4856:
4847:
4838:
4829:
4820:
4811:
4802:
4793:
4784:
4775:
4766:
4757:
4748:
4739:
4730:
4721:
4712:
4703:
4694:
4685:
4676:
4667:
4658:
4649:
4640:
4631:
4622:
4613:
4604:
4595:
4586:
4577:
4570:
4553:
4552:Taubaté Basin
4550:
4546:
4543:
4542:
4541:
4538:
4536:
4533:
4531:
4528:
4527:
4525:
4521:
4515:
4512:
4510:
4507:
4505:
4502:
4500:
4499:Araripe Basin
4497:
4496:
4494:
4490:
4484:
4481:
4479:
4476:
4474:
4471:
4469:
4466:
4464:
4463:Bananal Basin
4461:
4459:
4456:
4455:
4453:
4449:
4443:
4440:
4438:
4435:
4433:
4430:
4428:
4425:
4423:
4420:
4418:
4415:
4414:
4412:
4408:
4405:
4401:
4392:
4387:
4385:
4380:
4378:
4373:
4372:
4369:
4361:
4357:
4352:
4351:
4347:
4335:
4328:
4327:
4321:
4311:
4304:
4303:
4297:
4284:
4283:
4277:
4267:
4260:
4259:
4253:
4243:
4239:
4232:
4227:
4223:
4219:
4214:
4213:
4209:
4197:
4193:
4192:
4187:
4182:
4173:
4169:
4165:
4161:
4160:
4152:
4147:
4137:
4133:
4132:
4127:
4122:
4118:
4112:
4098:
4094:
4090:
4086:
4085:
4077:
4072:
4062:
4058:
4051:
4046:
4036:
4029:
4028:
4022:
4012:
4008:
4007:
3999:
3994:
3984:
3980:
3979:
3973:
3970:
3966:
3962:
3958:
3954:
3950:
3949:
3941:
3936:
3935:
3931:
3919:
3915:
3908:
3903:
3893:
3886:
3885:
3879:
3869:
3862:
3861:
3855:
3845:
3841:
3840:
3834:
3824:
3820:
3819:
3811:
3806:
3796:
3792:
3791:
3783:
3778:
3777:
3773:
3768:
3759:
3756:
3750:
3747:
3744:
3739:
3736:
3733:
3728:
3725:
3719:
3716:
3710:
3707:
3701:
3699:
3697:
3693:
3690:
3689:Atlanta Field
3685:
3683:
3679:
3673:
3671:
3669:
3667:
3665:
3663:
3661:
3657:
3654:
3649:
3646:
3640:
3637:
3634:
3629:
3627:
3623:
3620:
3615:
3612:
3609:
3604:
3601:
3598:
3593:
3590:
3587:
3586:Vampira Field
3582:
3579:
3576:
3571:
3568:
3565:
3560:
3557:
3554:
3549:
3546:
3540:
3537:
3531:
3528:
3522:
3520:
3516:
3513:
3512:Echidna Field
3508:
3505:
3499:
3496:
3493:
3488:
3485:
3479:
3477:
3473:
3467:
3464:
3458:
3455:
3449:
3446:
3435:on 2017-09-07
3434:
3430:
3424:
3422:
3420:
3418:
3416:
3414:
3412:
3410:
3408:
3406:
3404:
3402:
3400:
3398:
3396:
3394:
3392:
3390:
3388:
3384:
3378:
3375:
3369:
3366:
3360:
3358:
3354:
3348:
3346:
3344:
3340:
3334:
3332:
3330:
3328:
3324:
3318:
3316:
3314:
3312:
3310:
3308:
3306:
3302:
3296:
3293:
3287:
3285:
3283:
3281:
3279:
3277:
3275:
3273:
3271:
3267:
3261:
3259:
3257:
3255:
3251:
3245:
3242:
3236:
3234:
3232:
3230:
3228:
3224:
3218:
3216:
3214:
3212:
3208:
3202:
3200:
3198:
3196:
3192:
3186:
3184:
3182:
3180:
3176:
3170:
3167:
3161:
3158:
3152:
3150:
3146:
3140:
3137:
3131:
3128:
3122:
3119:
3113:
3111:
3107:
3101:
3098:
3092:
3089:
3083:
3080:
3074:
3071:
3065:
3062:
3056:
3053:
3047:
3043:
3040:
3038:
3035:
3033:
3030:
3028:
3025:
3024:
3020:
3014:
3011:
3009:
3006:
3003:
3001:
2998:
2996:
2993:
2992:
2989:
2986:
2984:
2981:
2978:
2976:
2973:
2970:
2969:
2966:
2963:
2961:
2958:
2955:
2953:
2950:
2947:
2946:
2943:
2940:
2938:
2935:
2932:
2930:
2927:
2924:
2923:
2920:
2917:
2915:
2912:
2909:
2907:
2904:
2901:
2900:
2897:
2894:
2892:
2889:
2886:
2884:
2881:
2878:
2877:
2874:
2871:
2869:
2866:
2863:
2861:
2858:
2855:
2854:
2851:
2848:
2846:
2843:
2840:
2838:
2835:
2832:
2831:
2828:
2823:
2821:
2818:
2815:
2813:
2810:
2807:
2806:
2803:
2798:
2796:
2793:
2790:
2788:
2785:
2783:
2780:
2779:
2776:
2773:
2771:
2768:
2765:
2763:
2760:
2757:
2756:
2753:
2750:
2748:
2745:
2742:
2740:
2737:
2734:
2733:
2730:
2727:
2725:
2722:
2719:
2717:
2714:
2711:
2710:
2707:
2702:
2700:
2697:
2694:
2692:
2689:
2686:
2685:
2682:
2679:
2677:
2676:El Paso Corp.
2674:
2671:
2669:
2666:
2664:
2661:
2660:
2657:
2654:
2652:
2649:
2646:
2644:
2641:
2638:
2637:
2634:
2631:
2629:
2626:
2623:
2621:
2618:
2615:
2614:
2611:
2608:
2606:
2603:
2600:
2598:
2595:
2594:
2591:
2588:
2586:
2583:
2580:
2578:
2575:
2573:
2572:
2568:
2567:
2564:
2561:
2559:
2556:
2553:
2551:
2548:
2546:
2545:
2541:
2540:
2537:
2534:
2532:
2529:
2526:
2524:
2521:
2520:
2517:
2514:
2512:
2509:
2506:
2504:
2501:
2500:
2497:
2494:
2492:
2489:
2486:
2484:
2481:
2479:
2478:
2474:
2473:
2470:
2465:
2463:
2460:
2457:
2455:
2452:
2450:
2449:
2445:
2444:
2441:
2439:
2437:
2434:
2431:
2429:
2426:
2424:
2423:
2419:
2418:
2415:
2412:
2410:
2407:
2404:
2402:
2399:
2397:
2396:
2392:
2391:
2388:
2386:
2384:
2381:
2378:
2376:
2373:
2372:
2369:
2366:
2364:
2361:
2358:
2356:
2353:
2350:
2349:
2346:
2343:
2341:
2338:
2335:
2333:
2330:
2327:
2326:
2323:
2321:
2319:
2316:
2313:
2311:
2308:
2307:
2304:
2301:
2299:
2296:
2293:
2291:
2288:
2286:
2285:
2281:
2280:
2277:
2274:
2272:
2269:
2266:
2264:
2261:
2259:
2258:
2254:
2253:
2250:
2248:
2246:
2243:
2240:
2238:
2235:
2233:
2230:
2229:
2226:
2223:
2219:
2215:
2213:
2210:
2207:
2204:
2201:
2200:
2192:
2189:
2186:
2183:
2176:
2175:
2169:
2167:
2165:
2155:
2144:
2142:
2138:
2133:
2123:
2116:
2114:
2112:
2108:
2107:vitrinite map
2103:
2099:
2095:
2091:
2087:
2079:
2073:
2071:
2068:
2064:
2060:
2055:
2054:Araçuarí Belt
2050:
2047:
2046:
2042:
2038:
2037:
2033:
2029:
2028:
2024:
2020:
2019:
2013:
2009:
2008:
2005:
2003:
1999:
1994:
1989:
1986:
1985:
1982:
1979:
1978:
1970:
1966:
1962:
1952:
1948:
1944:
1940:
1935:
1930:
1927:
1926:
1923:
1920:
1919:
1914:
1904:
1899:
1895:
1892:
1890:
1887:
1880:
1875:
1870:
1866:
1863:
1861:
1858:
1851:
1846:
1841:
1836:
1831:
1828:
1827:
1824:
1821:
1820:
1817:
1814:
1813:
1810:
1807:
1806:
1803:
1800:
1799:
1796:
1793:
1792:
1782:
1776:
1770:
1750:
1746:
1741:
1736:
1732:
1727:
1722:
1717:
1712:
1711:Maastrichtian
1709:
1708:
1705:
1702:
1701:
1698:
1695:
1694:
1691:
1688:
1687:
1684:
1681:
1680:
1670:
1664:
1649:
1645:
1640:
1636:
1632:
1627:
1622:
1617:
1614:
1613:
1610:
1608:
1605:
1598:
1593:
1588:
1585:
1584:
1578:
1575:
1570:
1565:
1560:
1557:
1556:
1553:
1550:
1548:
1544:
1541:
1537:
1532:
1524:
1523:
1522:
1519:
1511:
1510:
1506:
1501:
1497:
1495:
1491:
1487:
1483:
1479:
1471:
1470:
1469:
1467:
1463:
1454:
1453:
1452:
1450:
1446:
1442:
1434:
1432:
1430:
1429:
1424:
1423:
1418:
1414:
1409:
1401:
1400:
1396:
1391:
1387:
1385:
1380:
1372:
1371:
1370:
1368:
1363:
1362:conglomerates
1360:
1356:
1348:
1347:
1346:
1344:
1340:
1336:
1332:
1323:
1316:
1314:
1311:
1303:
1302:
1301:
1299:
1295:
1292:
1288:
1284:
1280:
1277:
1273:
1265:
1264:
1260:
1255:
1251:
1248:
1244:
1236:
1235:
1234:
1232:
1228:
1224:
1223:Florianópolis
1216:
1214:
1212:
1208:
1204:
1200:
1196:
1191:type oil well
1188:
1179:
1172:
1170:
1168:
1164:
1160:
1156:
1152:
1148:
1147:stromatolites
1140:
1139:
1138:
1136:
1131:
1123:
1122:
1121:
1118:
1113:
1109:
1106:
1102:
1097:
1095:
1091:
1087:
1083:
1079:
1075:
1074:conglomerates
1067:
1066:
1062:
1057:
1053:
1051:
1047:
1043:
1039:
1031:
1030:
1029:
1027:
1023:
1019:
1011:
1010:Pavilion Lake
1006:
999:
997:
994:
992:
988:
984:
976:
972:
968:
964:
957:
955:
953:
948:
946:
942:
941:stratigraphic
938:
937:thrust faults
934:
930:
926:
922:
918:
917:Kwanza Basins
914:
909:
905:
901:
897:
890:
886:
884:
880:
878:
874:
872:
868:
864:
862:
858:
854:
853:
852:
849:
847:
843:
839:
835:
831:
827:
823:
818:
816:
815:flood basalts
812:
808:
805:
801:
797:
793:
789:
785:
781:
777:
773:
769:
765:
761:
757:
753:
749:
745:
736:
729:
724:
717:
712:
705:
703:
701:
697:
694:
691:
687:
683:
679:
675:
671:
667:
663:
658:
655:
651:
647:
643:
639:
635:
631:
630:Florianópolis
627:
623:
618:
616:
615:Pelotas Basin
612:
611:Fracture Zone
608:
604:
600:
596:
592:
588:
584:
580:
571:
564:
562:
560:
556:
548:
546:
544:
534:
530:
529:microbialites
526:
522:
518:
514:
510:
506:
502:
498:
494:
490:
486:
481:
479:
475:
471:
467:
463:
459:
455:
451:
446:
444:
440:
436:
432:
428:
424:
420:
416:
412:
408:
399:
391:
383:
379:
375:
371:
368:
366:
362:
359:
356:
354:
350:
347:
343:
340:
338:
334:
331:
328:
326:
322:
319:
316:
314:
310:
307:
303:
300:
298:
294:
289:
286:
283:
279:
276:
273:
269:
264:
260:
256:
252:
248:
245:
241:
237:
234:
230:
226:
222:
217:
214:
213:Florianópolis
210:
206:
202:
198:
194:
190:
187:
183:
180:
176:
172:
168:
165:
161:
158:
147:
143:
140:
136:
133:
129:
126:
125:South America
123:
119:
116:
113:
109:
104:
76:
74:
70:
63:
58:
41:
32:
29:
25:
20:
5033:Santos Basin
4986:. Retrieved
4981:
4977:
4953:Santos Basin
4952:
4948:Campos Basin
4540:Paraná Basin
4514:Tucano Basin
4504:Jatobá Basin
4492:Northeastern
4442:Marajó Basin
4437:Amazon Basin
4432:Tacutu Basin
4360:the original
4338:, retrieved
4325:
4314:, retrieved
4301:
4290:, retrieved
4281:
4270:, retrieved
4257:
4246:, retrieved
4241:
4237:
4217:
4216:ANP (2014),
4200:, retrieved
4195:
4189:
4175:, retrieved
4163:
4157:
4140:, retrieved
4135:
4129:
4101:, retrieved
4088:
4082:
4065:, retrieved
4060:
4056:
4039:, retrieved
4026:
4015:, retrieved
4010:
4004:
3987:, retrieved
3977:
3952:
3946:
3922:, retrieved
3917:
3913:
3896:, retrieved
3883:
3872:, retrieved
3859:
3848:, retrieved
3838:
3827:, retrieved
3822:
3816:
3799:, retrieved
3794:
3788:
3769:Bibliography
3758:
3749:
3738:
3727:
3718:
3709:
3648:
3639:
3614:
3603:
3592:
3581:
3570:
3559:
3553:Búzios Field
3548:
3539:
3530:
3507:
3498:
3487:
3466:
3457:
3448:
3437:. Retrieved
3433:the original
3377:
3368:
3295:
3244:
3169:
3160:
3139:
3130:
3121:
3100:
3091:
3082:
3073:
3064:
3055:
3037:Paraná Basin
3032:Campos Basin
3027:Angola Basin
2902:Caravela Sul
2569:
2542:
2475:
2446:
2420:
2393:
2282:
2255:
2231:
2222:cubic metres
2163:
2153:
2145:
2128:
2083:
1929:Early Aptian
1869:Early Albian
1784:(Itajaí-Açu)
1772:(Itajaí-Açu)
1551:
1528:
1515:
1475:
1458:
1438:
1426:
1420:
1405:
1376:
1352:
1328:
1307:
1294:foraminifera
1279:calcarenites
1269:
1240:
1220:
1184:
1144:
1127:
1098:
1071:
1061:half-grabens
1035:
1015:
995:
991:Serra do Mar
980:
958:Stratigraphy
949:
929:salt diapirs
893:
850:
846:Early Albian
819:
800:Paraná Basin
764:Araçuaí Belt
741:
728:Congo Craton
716:Kwanza Basin
699:
659:
622:Serra do Mar
619:
603:Campos Basin
576:
552:
542:
501:source rocks
482:
466:Congo Craton
454:Serra Do Mar
450:Campos Basin
447:
407:Santos Basin
406:
404:
358:Stratigraphy
353:Stratigraphy
244:Serra do Mar
27:
22:Santos Basin
4908:Ceará Basin
4545:Bauru Basin
3955:: 300–320,
2808:Pirapitanga
2309:Iracema Sul
2094:source rock
2049:Precambrian
2012:Valanginian
1988:Hauterivian
1922:Late Aptian
1830:Late Albian
1672:(Marambaia)
1666:(Marambaia)
1587:Pleistocene
1569:Lithologies
1540:glauconitic
1395:crustaceans
1285:to shallow
1130:dolomitized
1108:environment
1046:plagioclase
921:halokinesis
904:hypersaline
900:depocentres
877:Late Aptian
867:Hauterivian
861:Valanginian
838:Hauterivian
834:rift basins
820:During the
788:Pan-African
760:Precambrian
565:Description
507:shales and
474:Late Aptian
462:halokinesis
443:rift basins
224:On/Offshore
98: /
73:Coordinates
5027:Categories
4988:2017-09-04
4417:Acre Basin
4340:2017-09-04
4316:2017-09-04
4292:2017-09-04
4272:2017-09-04
4248:2017-09-04
4202:2017-09-04
4177:2017-09-04
4142:2017-09-04
4103:2017-09-04
4067:2017-09-04
4041:2017-09-04
4017:2017-09-04
3989:2017-09-04
3924:2017-09-04
3898:2017-09-04
3874:2017-09-04
3850:2017-09-04
3829:2017-09-04
3801:2017-09-04
3597:Iara Field
3439:2017-09-07
3048:References
2184:Reservoir
2137:Tupi field
2111:oil window
2092:to assess
1943:sandstones
1939:Carbonates
1903:Evaporites
1879:Limestones
1845:Sandstones
1823:Cenomanian
1749:sandstones
1740:Sandstones
1735:sandstones
1648:sandstones
1639:sandstones
1635:limestones
1607:Overburden
1564:Formations
1462:quartzitic
1343:turbidites
1335:Itajaí-Açu
1291:planktonic
1283:tidal flat
1195:evaporites
1189:is in the
1155:grainstone
1105:lacustrine
1090:stevensite
1086:siltstones
971:inselbergs
925:subsurface
908:evaporites
768:inselbergs
718:in Africa.
672:(Af) to a
525:limestones
521:sandstones
519:Guaratiba
509:carbonates
505:lacustrine
470:rift basin
437:since the
411:Portuguese
306:rift basin
297:Basin type
232:Boundaries
86:43°43′45″W
4266:GEO Expro
4198:: 133–148
4091:: 29–46,
4013:: 199–214
3920:: 217–245
2983:Petrobras
2960:Petrobras
2937:Petrobras
2914:Petrobras
2891:Petrobras
2845:Petrobras
2820:Petrobras
2795:Petrobras
2770:Petrobras
2724:Petrobras
2699:Petrobras
2651:Petrobras
2628:Petrobras
2585:Petrobras
2558:Petrobras
2531:Petrobras
2511:Petrobras
2491:Petrobras
2462:Petrobras
2436:Petrobras
2409:Petrobras
2363:Petrobras
2328:Panoramix
2318:Petrobras
2298:Petrobras
2271:Petrobras
2245:Petrobras
2232:Sagitário
2190:Operator
2041:Paleozoic
1981:Barremian
1951:volcanics
1809:Coniacian
1802:Santonian
1795:Campanian
1704:Paleocene
1690:Oligocene
1486:echinoids
1441:Marambaia
1247:micaceous
1203:anhydrite
1151:packstone
952:Paleocene
842:Barremian
668:(Am) and
626:Cabo Frio
587:Sáo Paulo
559:São Paulo
549:Etymology
342:Barremian
266:Hydrology
236:Cabo Frio
189:Cabo Frio
171:São Paulo
135:Southeast
111:Etymology
83:26°6′22″S
5005:Category
4886:Offshore
4523:Southern
4131:Offshore
4111:citation
3844:archived
3021:See also
2879:Caravela
2833:Tambuatá
2782:Mexilhão
2596:Belmonte
2522:Piracaba
2477:Sapinhoá
2351:Piracucá
2070:Basement
2063:gneisses
2059:Granites
2032:Triassic
2023:Jurassic
1816:Turonian
1616:Pliocene
1597:Coquinas
1543:coquinas
1536:feldspar
1449:Sepetiba
1417:cuttings
1413:ostracod
1231:Itanhaém
1101:alluvial
1094:ostracod
1082:coquinas
1042:basaltic
1022:Camboriú
987:gneisses
983:granites
889:Holocene
857:Jurassic
826:Gondwana
784:gneisses
780:granites
776:Cambrian
646:Ilhabela
605:and the
517:pre-salt
503:are the
435:Gondwana
365:Field(s)
281:River(s)
163:State(s)
121:Location
4978:Phoenix
4451:Central
4403:Onshore
4138:: 46–47
3957:Bibcode
3825:: 38–57
3797:: 28–37
2995:Merluza
2971:Tubarão
2735:Atlanta
2712:Carapiá
2663:Lagosta
2448:Júpiter
2422:Iracema
2374:Vampira
2218:barrels
2202:Echidna
1683:Miocene
1547:bivalve
1538:-rich,
1482:bryozoa
1466:fluvial
1276:oolitic
1227:Guarujá
1211:sabkhas
933:listric
913:Namibia
807:hotspot
748:cratons
690:endemic
642:Guarujá
493:Júpiter
378:Júpiter
325:Orogeny
291:Geology
250:Part of
197:Guarujá
145:Country
5009:Images
4967:Source
4410:Amazon
4244:: 1–49
4063:: 1–13
3008:Pecten
2687:Uruguá
2639:Tambaú
2383:Repsol
2340:Repsol
2284:Búzios
2197:Notes
1998:Basalt
1947:shales
1850:Shales
1745:Shales
1731:Shales
1697:Eocene
1644:Shales
1631:Shales
1581:Notes
1505:Crimea
1490:corals
1445:Iguape
1359:lithic
1339:Juréia
1331:Santos
1298:pollen
1287:lagoon
1259:Oregon
1199:halite
1117:facies
1078:quartz
1050:augite
830:Pangea
758:. The
664:(Aw),
650:Itajaí
638:Santos
591:Paraná
555:Santos
431:Brazil
427:Santos
382:others
346:recent
271:Sea(s)
205:Itajaí
201:Santos
185:Cities
175:Paraná
157:Brazil
154:
131:Region
115:Santos
4330:(PDF)
4306:(PDF)
4286:(PDF)
4262:(PDF)
4242:10553
4234:(PDF)
4154:(PDF)
4079:(PDF)
4061:10193
4053:(PDF)
4031:(PDF)
4001:(PDF)
3943:(PDF)
3910:(PDF)
3888:(PDF)
3864:(PDF)
3813:(PDF)
3785:(PDF)
2925:Coral
2868:Shell
2856:Oliva
2616:Cedro
2502:Baúna
2257:Libra
2187:Year
2177:Field
1207:marls
1159:algal
533:seals
497:Libra
468:as a
374:Libra
313:Plate
139:South
4117:link
3004:1979
2979:1988
2956:1990
2933:1990
2910:1991
2887:1992
2864:1993
2841:1999
2816:2001
2791:2001
2766:2001
2747:QGEP
2743:2001
2720:2002
2695:2003
2672:2003
2647:2005
2624:2005
2601:2005
2581:2006
2571:Tupi
2554:2007
2544:Lapa
2527:2008
2507:2008
2487:2008
2458:2008
2432:2008
2405:2008
2395:Iara
2379:2009
2359:2009
2336:2009
2314:2009
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