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鄂尔多斯盆地西缘麻黄山地区中生界油藏富集规律
引用本文:丁晓琪,张哨楠,谢世文,冯一波.鄂尔多斯盆地西缘麻黄山地区中生界油藏富集规律[J].石油与天然气地质,2009,30(6):726-731.
作者姓名:丁晓琪  张哨楠  谢世文  冯一波
作者单位:成都理工大学, 油气藏地质及开发工程国家重点实验室, 四川, 成都, 610059
基金项目:国家自然科学基金青年基金 
摘    要:断裂特征、典型油藏解剖和剩余压力分布特征研究结果表明,鄂尔多斯盆地西缘麻黄山地区中生界油气分布和成藏组合在不同构造带有较大的差别,油藏受构造影响明显。西缘冲断带主要发育源外成藏组合和远源成藏组合,油藏主要为断块油藏和断背(鼻)油藏,油藏面积小、油柱高度大、储量小、产量高;中央凹陷带主要发育源内成藏组合,主要为致密低渗岩性油藏,油藏面积大、油柱高度小、产量低;而东部凸起带,源内、源外和远源成藏组合均发育,油藏则主要为背斜-岩性油藏。

关 键 词:致密砂岩  源外成藏组合  远源成藏组合  油气分布规律  中生界  麻黄山  鄂尔多斯盆地  
收稿时间:2009-03-09

Hydrocarbon accumulation pattern in the Mesozoic of Mahuangshan area in the western margin of the Ordos Basin
Ding Xiaoqi,Zhang Shaonan,Xie Shiwen,Feng Yibo.Hydrocarbon accumulation pattern in the Mesozoic of Mahuangshan area in the western margin of the Ordos Basin[J].Oil & Gas Geology,2009,30(6):726-731.
Authors:Ding Xiaoqi  Zhang Shaonan  Xie Shiwen  Feng Yibo
Affiliation:State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan 610059, China
Abstract:An analysis is performed on the fault characteristics,typical reservoirs,and residual pressure distribution in the Mesozoic of the Mahuangshan area in the western margin of Ordos Basin.The results show that the hydrocarbon distribution and plays there vary greatly in different structural belts and structural control on reservoirs is significant.In the thrust belt in the western margin,proximal plays and distal plays are predominant.The re-servoir types here are mainly fault-block and faulted anticlinal(nose) reservoirs,featuring in small area but high oil column and small reserve but high production.While in the central depression,the indigenous plays are predominant.The reservoirs here are tight low-permeability type featuring in large area,low oil column,and low production.In the eastern uplift belt,proximal,distal and indigenous plays all occur.The reservoirs are dominated by anticline-lithologic reservoirs.
Keywords:tight sand  proximal play  distal play  hydrocarbon distribution pattern  Mesozoic  Mahuangshan  Ordos Basin
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