DOI: 10.1306/11051212103
Scopus记录号: 2-s2.0-84880349498
论文题名: Arabian carbonate reservoirs: A depositional model of the Arab-D reservoir in Khurais field, Saudi Arabia
作者: Al-Awwad S.F. ; Collins L.B.
刊名: AAPG Bulletin
ISSN: 0149-1668
EISSN: 1558-9398
出版年: 2013
发表日期: 2013
卷: 97, 期: 7 起始页码: 1099
结束页码: 1119
语种: 英语
Scopus关键词: Carbonate reservoir
; Depositional environment
; Depositional models
; Kingdom of Saudi Arabia
; Lithofacies
; Onshore oil fields
; Ooid grainstone
; Saudi Arabia
; Deposition
; Oil fields
; Petroleum reservoir evaluation
; Reefs
; Stratigraphy
; abrasion
; carbonate platform
; depositional environment
; dolomite
; Jurassic
; lime
; lithofacies
; mudstone
; reservoir
; storm
; succession
; turbidity
; Arabian Peninsula
; Saudi Arabia
; Cladocoropsis
; Stromatoporoida
Scopus学科分类: Energy
; Earth and Planetary Sciences
英文摘要: The Upper Jurassic Arab Formation in the Arabian Peninsula, the most prolific oil-bearing interval of the world, is a succession of interbedded thick carbonates and evaporites that are defined stratigraphically upsection as the Arab-D, Arab-C, Arab-B, and Arab-A. The Arab-D reservoir is the main reservoir in Khurais field, one of the largest onshore oil fields of the Kingdom of Saudi Arabia. In Khurais field, the Arab-D reservoir is composed of the overlying evaporitic Arab-D Member of the Arab Formation and the underlying upper part of the Jubaila Formation. It contains 11 lithofacies, listed from deepest to shallowest: (1) hardground-capped skeletal wackestone and lime mudstone; (2] intraclast floatstone and rudstone; (3) pelletai wackestone and packstone; (4) stromatoporoid wackestone, packstone, and floatstone; (5) Cladocoropsis wackestone, packstone, and floatstone; (6) Clypeina and Thaumatoporella wackestone and packstone; (7) peloidal packstone and grainstone; (8) ooid grainstone; (9) crypt-microbial laminites; (10) evaporites; and (11) stratigraphically reoccurring dolomite. The Arab-D reservoir lithofacies succession represents shallowing-upward deposition, which, from deepest to shallowest, reflects the following depositional environments: offshore submarine turbidity fans (lithofacies 1 and 2); lower shoreface settings (lithofacies 3); stromatoporoid reef (lithofacies 4); lagoon (lithofacies 5 and 6); shallow subtidal settings (lithofacies 7 and 8); peritidal settings (lithofacies 9); and sabkhas and salinas (lithofacies 10). The depositional succession of the reservoir represents a prograding, shallow-marine, reef-rimmed carbonate shelf that was subjected to common storm abrasion, which triggered turbidites. Copyright © 2013. The American Assodation of Petroleum Geologists. All rights reseived. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84880349498&doi=10.1306%2f11051212103&partnerID=40&md5=e05ad7277a968221b6d56ece26e24a4e
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13238
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:
Al-Awwad S.F.,Collins L.B.. Arabian carbonate reservoirs: A depositional model of the Arab-D reservoir in Khurais field, Saudi Arabia[J]. AAPG Bulletin,2013-01-01,97(7)