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Seismo-stratigraphy and numerical basin modeling of the southern
Brazilian continental margin (Campos, Santos, and Pelotas basins) (PhD thesis)
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Kiang Chang, Hung; Assine, Mario Luis; Santos Corrêa, Fernando; Setsuo Tinen, Julio; Campane Vidal, Alexandre; Koike, Luzia (2008),
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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
Marambaia Formation is between 261 and 2,000 metres (856 and 6,562 ft) thick, and consists of grey
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period and has a maximum thickness of 2,700 metres (8,900 ft). The formation is a
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582:"Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos"
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sandstones. The
Marambaia Formation is the deeper lateral equivalent of the
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394:. This formation in places can be found cropping out at sea bottom. The
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basin. Biostratigraphic data indicate a
Tertiary age.
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in the
Atlanta and Oliva Fields of the Santos Basin.
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of the
Atlanta and Oliva Fields in the Santos Basin.
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16:Geological formation of the Santos Basin offshore
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621:: CS1 maint: DOI inactive as of July 2024 (
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567:Ruprecht-Karls-Universität Heidelberg
739:Geography of Santa Catarina (state)
734:Geography of Rio de Janeiro (state)
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161:up to 2,700 m (8,900 ft)
14:
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689:Paleogene System of South America
590:Revista Brasileira de Geociências
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423:
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684:Neogene System of South America
603:10.25249/0375-7536.2008382S2946
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744:Geography of São Paulo (state)
470:Kiang Chang et al., 2008, p.32
386:interbedded with fine-grained
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1:
664:Geologic formations of Brazil
633:Brazil Round 9 - Santos Basin
543:Danmarks Tekniske Universitet
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366:The formation is named after
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292:Location of the Santos Basin
7:
729:Geography of Paraná (state)
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398:is thought to be talus and
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556:Contreras, Jorham (2011),
719:Reservoir rock formations
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630:Vieira, Juliana (2007),
535:Clemente, Pilar (2013),
396:depositional environment
346:formation dates to the
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605:(inactive 2024-07-08)
508:"Santos Basin Fields"
488:Contreras, 2011, p.77
368:Restinga da Marambaia
280:Restinga da Marambaia
709:Deep marine deposits
704:Sandstone formations
479:Clemente, 2013, p.24
338:. The predominantly
312:geological formation
118:Geological formation
724:Petroleum in Brazil
405:The formation is a
300:Marambaia Formation
219: /
28:Stratigraphic range
22:Marambaia Formation
714:Turbidite deposits
497:Vieira, 2007, p.10
370:, Rio de Janeiro.
308:Formacão Marambaia
138:Sepetiba Formation
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223:26.100°S 43.717°W
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694:Shale formations
679:Paleogene Brazil
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510:. Archived from
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392:Iguape Formation
318:offshore of the
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228:-26.100; -43.717
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128:Itamambuca Group
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699:Marl formations
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445:Geology portal
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411:reservoir rock
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356:reservoir rock
336:Santa Catarina
324:Rio de Janeiro
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514:on 2017-09-07
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669:Santos Basin
645:, retrieved
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607:, retrieved
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571:, retrieved
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547:, retrieved
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529:Bibliography
516:. Retrieved
512:the original
502:
493:
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453:Campos Basin
404:
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365:
316:Santos Basin
299:
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271:Type section
243:Santos Basin
42:65–2.6
400:open marine
374:Description
226: /
201:Coordinates
658:Categories
647:2017-09-04
609:2017-09-04
573:2017-09-04
549:2017-09-04
518:2017-09-07
459:References
388:turbiditic
322:states of
304:Portuguese
152:Juréia Fm.
597:: 29–46,
362:Etymology
328:São Paulo
320:Brazilian
276:Named for
189:Sandstone
166:Lithology
158:Thickness
134:Underlies
32:Paleocene
617:citation
417:See also
348:Tertiary
195:Location
144:Overlies
36:Pliocene
314:of the
310:) is a
253:Country
214:43°43′W
171:Primary
124:Unit of
409:, and
380:shales
332:Paraná
265:Brazil
262:
239:Region
211:26°6′S
637:(PDF)
585:(PDF)
563:(PDF)
384:marls
340:shale
185:Other
175:Shale
623:link
407:seal
354:and
352:seal
344:marl
342:and
334:and
298:The
179:marl
114:Type
50:PreꞒ
641:ANP
599:doi
660::
639:,
619:}}
615:{{
595:38
593:,
587:,
565:,
541:,
330:,
326:,
306::
245:,
177:,
150:,
100:Pg
44:Ma
30::
625:)
601::
521:.
302:(
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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