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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
845:
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751:
850:
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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
835:
770:
624:
Seismo-stratigraphy and numerical basin modeling of the southern
Brazilian continental margin (Campos, Santos, and Pelotas basins) (PhD thesis)
825:
740:
645:
Kiang Chang, Hung; Assine, Mario Luis; Santos Corrêa, Fernando; Setsuo Tinen, Julio; Campane Vidal, Alexandre; Koike, Luzia (2008),
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in the eastern distal part of the Santos Basin. The formation is characterized by dark grey to greenish and brown
203:
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Petroleum geology of the Campos and Santos basins, Lower
Cretaceous Brazilian sector of the South Atlantic margin
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The turbidites of the Jureia
Formation were deposited at the shelf edge of the Brazilian continental margin
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epochs and has a maximum thickness of 2,000 metres (6,600 ft). The formation is a
242:
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647:"Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos"
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Piovesan, Enelise Katia; Trescastro Bergue, Cristianini; Fauth, Gerson (2010),
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697:"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
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Geological formation of the Santos Basin near Brazil
469:, the first discovery in 1979 of the Santos Basin.
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8:
686:: CS1 maint: DOI inactive as of July 2024 (
366:, the first discovery in the Santos Basin.
282:
18:
786:Upper Cretaceous Series of South America
438:species were identified in the drilling
519:
679:
632:Ruprecht-Karls-Universität Heidelberg
7:
791:Maastrichtian Stage of South America
442:of wells drilled into the Santonian-
846:Geography of Santa Catarina (state)
841:Geography of Rio de Janeiro (state)
705:Revista Brasileira de Paleontologia
157:up to 2,000 m (6,600 ft)
14:
655:Revista Brasileira de Geociências
376:Jureia-Itatins Ecological Station
374:The formation is named after the
276:Jureia-Itatins Ecological Station
493:
479:
253:
668:10.25249/0375-7536.2008382S2946
851:Geography of São Paulo (state)
526:Kiang Chang et al., 2008, p.32
1:
771:Geologic formations of Brazil
733:Brazil Round 9 - Santos Basin
608:Danmarks Tekniske Universitet
288:Location of the Santos Basin
836:Geography of Paraná (state)
867:
621:Contreras, Jorham (2011),
826:Reservoir rock formations
281:
26:
730:Vieira, Juliana (2007),
600:Clemente, Pilar (2013),
449:?Afrocytheridea cretacea
420:calcareous nannofossils
346:formation dates to the
535:Contreras, 2011, p.104
391:
303:
718:10.4072/rbp.2010.3.02
670:(inactive 2024-07-08)
564:"Santos Basin Fields"
553:Piovesan, 2010, p.177
461:The formation is the
455:Pelecocythere dinglei
389:
816:Sandstone formations
811:Siltstone formations
544:Clemente, 2013, p.23
400:Itajai-Açu Formation
334:. The predominantly
308:geological formation
118:Geological formation
831:Petroleum in Brazil
215: /
138:Marambaia Formation
28:Stratigraphic range
821:Turbidite deposits
754:2017-02-03 at the
587:Vieira, 2007, p.19
392:
148:Itanhaém Formation
781:Cretaceous Brazil
410:, fine-very fine
338:with interbedded
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219:26.100°S 43.717°W
858:
806:Shale formations
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566:. Archived from
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396:Santos Formation
314:offshore of the
296:Jureia Formation
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224:-26.100; -43.717
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22:Jureia Formation
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801:Santonian Stage
796:Campanian Stage
761:
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756:Wayback Machine
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743:, pp. 1–73
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424:Late Cretaceous
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348:Late Cretaceous
304:Formacão Jureia
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712:(3): 175–180,
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501:Geology portal
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463:reservoir rock
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360:reservoir rock
332:Santa Catarina
320:Rio de Janeiro
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570:on 2017-09-07
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487:Brazil portal
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467:Merluza Field
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432:Maastrichtian
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364:Merluza Field
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356:Maastrichtian
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36:Maastrichtian
33:
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776:Santos Basin
745:, retrieved
732:
721:, retrieved
709:
703:
672:, retrieved
659:
653:
636:, retrieved
623:
612:, retrieved
602:
594:Bibliography
583:
572:. Retrieved
568:the original
558:
549:
540:
531:
522:
509:Campos Basin
460:
453:
447:
416:palynomorphs
406:, dark grey
393:
373:
312:Santos Basin
295:
293:
267:Type section
239:Santos Basin
434:). Two new
382:Description
222: /
197:Coordinates
128:Frade Group
42:86–66
765:Categories
747:2017-09-04
723:2017-09-04
674:2017-09-04
638:2017-09-04
614:2017-09-04
574:2017-09-07
515:References
412:sandstones
408:siltstones
344:sandstones
340:siltstones
318:states of
300:Portuguese
662:: 29–46,
446:section,
444:Campanian
428:Santonian
370:Etymology
352:Santonian
342:and fine
324:São Paulo
316:Brazilian
272:Named for
185:sandstone
181:Siltstone
162:Lithology
154:Thickness
134:Underlies
32:Santonian
752:Archived
682:citation
473:See also
440:cuttings
436:ostracod
350:period;
191:Location
144:Overlies
465:of the
362:of the
310:of the
306:) is a
249:Country
210:43°43′W
167:Primary
124:Unit of
404:shales
328:Paraná
261:Brazil
258:
235:Region
207:26°6′S
737:(PDF)
700:(PDF)
650:(PDF)
628:(PDF)
336:shale
177:Other
171:Shale
688:link
452:and
418:and
330:and
294:The
114:Type
50:PreꞒ
741:ANP
714:doi
664:doi
422:is
767::
739:,
710:13
708:,
702:,
684:}}
680:{{
660:38
658:,
652:,
630:,
606:,
458:.
326:,
322:,
302::
241:,
183:,
100:Pg
44:Ma
30::
716::
690:)
666::
577:.
430:-
426:(
354:-
298:(
105:N
95:K
90:J
85:T
80:P
75:C
70:D
65:S
60:O
55:Ꞓ
39:~
34:-
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