| DOI: | 10.1306/01031110106
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| Scopus记录号: | 2-s2.0-80051960749
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| 论文题名: | Tectonostratigraphic evolution of the Guyana Basin |
| 作者: | Yang W.; Escalona A.
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| 刊名: | AAPG Bulletin
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| ISSN: | 0149-1837
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| EISSN: | 1558-9567
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| 出版年: | 2011
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| 发表日期: | 2011
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| 卷: | 95, 期:8 | | 起始页码: | 1339
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| 结束页码: | 1368
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| 语种: | 英语
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| Scopus关键词: | Carbonate platforms
; Hydrocarbon potential
; Incised valley
; Jurassic
; Late Miocene
; Listric fault
; Middle Miocene
; Offshore wells
; Oil discoveries
; Paleodrainage
; Paleogene
; Pattern change
; Plate convergence
; Pliocene
; Progradation
; Seismic datas
; Shelf edges
; Siliciclastics
; South America
; Stratigraphic sequences
; Submarine fans
; System change
; Trinidad
; U.s. geological surveys
; Hydrocarbons
; Offshore oil wells
; Seismology
; Stratigraphy
; Tectonics
; basin evolution
; carbonate
; Cretaceous
; deposition
; hydrocarbon
; Jurassic
; Miocene
; paleoenvironment
; Paleogene
; Pliocene
; sedimentation
; seismic data
; submarine fan
; survey
; tectonostratigraphy
; turbidity
; two-dimensional modeling
; Atlantic Ocean
; Guyana Basin
; Trinidad [Trinidad and Tobago]
; Trinidad and Tobago
|
| Scopus学科分类: | Energy
; Earth and Planetary Sciences
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| 英文摘要: | The Guyana Basin is located along the passive margin of northeastern South America. With no major oil discoveries, the region is considered by the U.S. Geological Survey the second least explored basin in the world. We integrated approximately 3000 km (∼ 1870 mi) of industry two-dimensional seismic data and 16 offshore wells in offshore Guyana to provide a regional framework and its hydrocarbon potential. Four main stratigraphic sequences from the Cretaceous to the Pliocene were recognized. Sequence 1 of the Cretaceous consists of shelfal sedimentation and submarine fan systems. The main Cretaceous depocenter is located in the southeastern part of the area, which coincides with a free-air gravity low, suggesting a basement depression inherited from Jurassic rifting. Sequence 2 of the Paleogene consists of shelfal clastic and carbonate deposits. Listric faults affect the shelf edge and slope, resulting in large turbidites down the slope. The west-southwesteast-northeast-oriented Waini arch developed along the northern shelf, and it may reflect a flexural long-distance effect of the Caribbean plate convergence with the northwestern South American plate. Sequence 3 of the early to middle Miocene consists of isolated carbonate platforms at the shelf edge surrounded by siliciclastics. On the sequence top, a regional unconformity was identified by large incised valleys. We suggest that this unconformity was caused by the peak of the Caribbean orogeny in the Trinidad area. Sequence 4 of the late Miocene to Pliocene shows the largest terrigenous progradational event in the shelf, which was built up by clear sigmoidal clinoforms. We suggest that the large progradation pattern change is caused by paleodrainage system changes in northern South America since the middle Miocene and by glacioeustasy. Copyright © 2011. The American Association of Petroleum Geologists. |
| URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-80051960749&doi=10.1306%2f01031110106&partnerID=40&md5=07615d1aeb148540a674bbd46a1c0eaf
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| Citation statistics: |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/13406
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| Appears in Collections: | 过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响
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| Recommended Citation: | |
Yang W.,Escalona A.. Tectonostratigraphic evolution of the Guyana Basin[J]. AAPG Bulletin,2011-01-01,95(8)
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