506:
398:
295:
492:
266:
796:
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425:
and light ochre calcisilts. The depositional environment is thought to be of a marine platform setting as pro-delta facies on the shelf edge. The age based on
856:
851:
762:
861:
574:
405:
The Jureia
Formation is 952 to 2,000 metres (3,123 to 6,562 ft) thick, and includes a succession of clastics between the coarse facies of the
846:
781:
635:
Seismo-stratigraphy and numerical basin modeling of the southern
Brazilian continental margin (Campos, Santos, and Pelotas basins) (PhD thesis)
836:
751:
656:
Kiang Chang, Hung; Assine, Mario Luis; Santos Corrêa, Fernando; Setsuo Tinen, Julio; Campane Vidal, Alexandre; Koike, Luzia (2008),
386:
286:
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618:
826:
821:
715:
841:
665:
207:
831:
707:
633:
791:
742:
413:
in the eastern distal part of the Santos Basin. The formation is characterized by dark grey to greenish and brown
214:
816:
614:
Petroleum geology of the Campos and Santos basins, Lower
Cretaceous Brazilian sector of the South Atlantic margin
811:
806:
430:
401:
The turbidites of the Jureia
Formation were deposited at the shelf edge of the Brazilian continental margin
410:
342:
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692:
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epochs and has a maximum thickness of 2,000 metres (6,600 ft). The formation is a
253:
775:
658:"Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos"
612:
497:
442:
366:
85:
46:
38:
678:
519:
505:
397:
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138:
426:
60:
17:
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Piovesan, Enelise Katia; Trescastro Bergue, Cristianini; Fauth, Gerson (2010),
294:
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105:
70:
708:"New ostracode species from the Upper Cretaceous of the Santos Basin, Brazil"
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in the western proximal part and the fine-grained clastics of the
396:
346:
181:
27:
Geological formation of the Santos Basin near Brazil
480:, the first discovery in 1979 of the Santos Basin.
282:
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172:
164:
154:
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124:
32:
8:
697:: CS1 maint: DOI inactive as of July 2024 (
377:, the first discovery in the Santos Basin.
293:
29:
797:Upper Cretaceous Series of South America
449:species were identified in the drilling
530:
690:
643:Ruprecht-Karls-Universität Heidelberg
7:
802:Maastrichtian Stage of South America
453:of wells drilled into the Santonian-
857:Geography of Santa Catarina (state)
852:Geography of Rio de Janeiro (state)
716:Revista Brasileira de Paleontologia
168:up to 2,000 m (6,600 ft)
25:
666:Revista Brasileira de Geociências
387:Jureia-Itatins Ecological Station
385:The formation is named after the
287:Jureia-Itatins Ecological Station
504:
490:
264:
679:10.25249/0375-7536.2008382S2946
862:Geography of São Paulo (state)
537:Kiang Chang et al., 2008, p.32
1:
782:Geologic formations of Brazil
744:Brazil Round 9 - Santos Basin
619:Danmarks Tekniske Universitet
299:Location of the Santos Basin
847:Geography of Paraná (state)
878:
632:Contreras, Jorham (2011),
837:Reservoir rock formations
292:
37:
741:Vieira, Juliana (2007),
611:Clemente, Pilar (2013),
460:?Afrocytheridea cretacea
431:calcareous nannofossils
357:formation dates to the
546:Contreras, 2011, p.104
402:
314:
729:10.4072/rbp.2010.3.02
681:(inactive 2024-07-08)
575:"Santos Basin Fields"
564:Piovesan, 2010, p.177
472:The formation is the
466:Pelecocythere dinglei
400:
827:Sandstone formations
822:Siltstone formations
555:Clemente, 2013, p.23
411:Itajai-Açu Formation
345:. The predominantly
319:geological formation
129:Geological formation
842:Petroleum in Brazil
226: /
149:Marambaia Formation
39:Stratigraphic range
832:Turbidite deposits
765:2017-02-03 at the
598:Vieira, 2007, p.19
403:
159:Itanhaém Formation
792:Cretaceous Brazil
421:, fine-very fine
349:with interbedded
303:
302:
230:26.100°S 43.717°W
16:(Redirected from
869:
817:Shale formations
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645:, pp. 1–171
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577:. Archived from
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407:Santos Formation
325:offshore of the
307:Jureia Formation
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235:-26.100; -43.717
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33:Jureia Formation
30:
21:
18:Juréia Formation
877:
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868:
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812:Santonian Stage
807:Campanian Stage
772:
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767:Wayback Machine
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754:, pp. 1–73
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435:Late Cretaceous
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359:Late Cretaceous
315:Formacão Jureia
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723:(3): 175–180,
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512:Geology portal
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474:reservoir rock
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371:reservoir rock
343:Santa Catarina
331:Rio de Janeiro
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581:on 2017-09-07
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498:Brazil portal
488:
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479:
478:Merluza Field
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443:Maastrichtian
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389:, São Paulo.
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375:Merluza Field
372:
368:
367:Maastrichtian
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47:Maastrichtian
44:
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36:
31:
19:
787:Santos Basin
756:, retrieved
743:
732:, retrieved
720:
714:
683:, retrieved
670:
664:
647:, retrieved
634:
623:, retrieved
613:
605:Bibliography
594:
583:. Retrieved
579:the original
569:
560:
551:
542:
533:
520:Campos Basin
471:
464:
458:
427:palynomorphs
417:, dark grey
404:
384:
323:Santos Basin
306:
304:
278:Type section
250:Santos Basin
445:). Two new
393:Description
233: /
208:Coordinates
139:Frade Group
53:86–66
776:Categories
758:2017-09-04
734:2017-09-04
685:2017-09-04
649:2017-09-04
625:2017-09-04
585:2017-09-07
526:References
423:sandstones
419:siltstones
355:sandstones
351:siltstones
329:states of
311:Portuguese
673:: 29–46,
457:section,
455:Campanian
439:Santonian
381:Etymology
363:Santonian
353:and fine
335:São Paulo
327:Brazilian
283:Named for
196:sandstone
192:Siltstone
173:Lithology
165:Thickness
145:Underlies
43:Santonian
763:Archived
693:citation
484:See also
451:cuttings
447:ostracod
361:period;
202:Location
155:Overlies
476:of the
373:of the
321:of the
317:) is a
260:Country
221:43°43′W
178:Primary
135:Unit of
415:shales
339:Paraná
272:Brazil
269:
246:Region
218:26°6′S
748:(PDF)
711:(PDF)
661:(PDF)
639:(PDF)
347:shale
188:Other
182:Shale
699:link
463:and
429:and
341:and
305:The
125:Type
61:PreꞒ
752:ANP
725:doi
675:doi
433:is
778::
750:,
721:13
719:,
713:,
695:}}
691:{{
671:38
669:,
663:,
641:,
617:,
469:.
337:,
333:,
313::
252:,
194:,
111:Pg
55:Ma
41::
727::
701:)
677::
588:.
441:-
437:(
365:-
309:(
116:N
106:K
101:J
96:T
91:P
86:C
81:D
76:S
71:O
66:Ꞓ
50:~
45:-
20:)
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