| 塔里木盆地中央隆起带演化与奥陶系礁滩储集体 |
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| 引用本文： | 张聪,于炳松,张迪.塔里木盆地中央隆起带演化与奥陶系礁滩储集体[J].新疆石油地质,2010,31(1). |
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| 作者姓名： | 张聪 于炳松 张迪 |
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| 作者单位： | 1. 中国地质大学,地球科学与资源学院,北京,100083
2. 吉林大学,地球科学学院,长春,130061 |
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| 基金项目： | 科技部科研项目，国家自然科学基金 |
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| 摘 要： | 奥陶系生物礁滩是塔里木盆地碳酸盐岩中十分有利的油气储集体。目前已发现的礁滩主要发育在台地边缘相带、台内凸起的缓坡带。巴楚地区生物礁滩沿北东-南西向成群成带分布,总体平行于巴楚断隆与柯坪断隆的构造分界线;塔中地区生物礁滩主要集中于塔中Ⅰ号断裂带的台地边缘带,具有随台缘迁移而变迁的特征;总体上,塔里木盆地奥陶系生物礁滩主要围绕古隆起分布,以台地边缘相为主,随着构造升降,台地边缘相带逐渐向西迁移,礁滩相也随之向西迁移,说明古隆起的演化对礁滩储集体的发育具有明显的控制作用。
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| 关 键 词： | 塔里木盆地 古隆起 奥陶系礁滩 台地边缘相 控制 |
Central Uplift Belt Evolution and Ordovician Reef Bank Reservoir in Tarim Basin |
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| ZHANG Cong,YU Bing-song,ZHANG Di.Central Uplift Belt Evolution and Ordovician Reef Bank Reservoir in Tarim Basin[J].Xinjiang Petroleum Geology,2010,31(1). |
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| Authors: | ZHANG Cong YU Bing-song ZHANG Di |
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| Affiliation: | ZHANG Cong1,YU Bing-song1,ZHANG Di2 (1.Iinstitute of Earth Science , Resource,China University of Geosciences,Beijing 100083,China,2.College of Earth Sciences,Jilin University,Changchun,Jilin 130061,China) |
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| Abstract: | The Ordovician reef bank developed in Tarim basin is the quite favorable carbonate reservoir for petroleum exploration. The reef bank in this basin is found mainly in platform margin zone and inner-platform arch ramp zone. The reef bank in Bachu area develops in group along NE-SW,parallel to the tectonic boundary between Bachu uplift and Keping uplift; in Tazhong area it is mainly distributed in platform margin zone in Tazhong No.1 fault belt,with the feature of shifting with the platform margin migration. ... |
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| Keywords: | Tarim basin ancient uplift Ordovician reef bank platform margin zone control |
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