塔里木盆地麦盖提斜坡奥陶系储层成因与分布

doi:10.7623/syxb201404005

石油学报 ›› 2014, Vol. 35 ›› Issue (4): 654-663.DOI: 10.7623/syxb201404005

塔里木盆地麦盖提斜坡奥陶系储层成因与分布

刘忠宝¹, 高山林¹, 岳勇², 黄秀仁³, 刘士林¹, 吴仕强¹, 张仲培¹, 杨圣彬¹

1. 中国石油化工股份有限公司石油勘探开发研究院北京 100083;
2. 中国石油化工股份有限公司西北油田分公司勘探开发研究院新疆乌鲁木齐 830011;
3. 中国石油大学地球科学学院北京 102249

收稿日期:2014-02-14 修回日期:2014-05-10 出版日期:2014-07-25 发布日期:2014-08-05
通讯作者: 刘忠宝，男，1978年12月生，2001年获中国地质大学（北京）学士学位，2006年获中国地质大学（北京）博士学位，现为中国石油化工股份有限公司石油勘探开发研究院高级工程师，主要从事碳酸盐岩沉积储层方面研究。Email：liuzb.syky@sinopec.com
作者简介:刘忠宝，男，1978年12月生，2001年获中国地质大学（北京）学士学位，2006年获中国地质大学（北京）博士学位，现为中国石油化工股份有限公司石油勘探开发研究院高级工程师，主要从事碳酸盐岩沉积储层方面研究。Email：liuzb.syky@sinopec.com
基金资助:
国家重点基础研究发展计划（973）项目（2012CB214802）、国家重大科技专项（2011ZX05005）及中国石油化工股份有限公司科技部项目（P11083）资助。

Formation and distribution of the Ordovician reservoir in Maigaiti slope, Tarim Basin

Liu Zhongbao¹, Gao Shanlin¹, Yue Yong², Huang Xiuren³, Liu Shilin¹, Wu Shiqiang¹, Zhang Zhongpei¹, Yang Shengbin¹

1. Sinopec Research Institute of Petroleum Exploration & Production, Beijing 100083, China;
2. Exploration and Development Research Institute, Sinopec Northwest Oilfield Company, Xinjiang Urumqi 830011, China;
3. College of Geosciences, China University of Petroleum, Beijing 102249, China

Received:2014-02-14 Revised:2014-05-10 Online:2014-07-25 Published:2014-08-05

摘要/Abstract

摘要：

岩心、薄片、钻井及成像测井资料综合研究表明，塔里木盆地麦盖提斜坡奥陶系储集空间以裂缝、孔洞为主，不同区带储层发育程度差异大，玉北地区东部储层最好，发育2套优质储层。按成因将储层类型划分为3种：潜山缝洞型、不整合面岩溶型、顺层深潜流岩溶型。鹰山组缝洞型储层受古地貌与裂缝控制，蓬莱坝组具备发育顺层深潜流带岩溶条件，建立了不同类型储层发育的地质模式。以此为指导，结合地震储层预测成果，预测了麦盖提斜坡不同类型储层分布，指出玉北地区东部断褶翼部及断洼区、中西部岩溶残丘带为有利储层勘探区。

关键词: 麦盖提斜坡, 奥陶系, 碳酸盐岩, 储层类型, 储层模式

Abstract:

A comprehensive study of cores, thin sections, drilling, and imaging logging data indicates that fractures and caves are dominating in the Ordovician reservoir in the Maigaiti slope of Tarim Basin. The Ordovician reservoir is developed to varying degrees in different zones of the slope area, with the best quality (including two sets of high quality reservoir) found in the east area of Yubei. The Ordovician reservoir can be classified into three types according to its genesis, i.e., burial and epidiagenetic fracture-cave reservoir, unconformity karst reservoir, and bedding deep-underflow karst reservoir. The fracture-cave reservoir of Yingshan Formation is controlled by ancient landform and fractures, whereas the geological conditions of Penglaiba Formation support the development of bedding deep-underflow karst reservoir. A geological development model for different types of Ordovician reservoirs is established and then used in combination with seismic reservoir prediction data for predicting the distribution patterns of different types of reservoirs in the Maigaiti slope. The eastern fault-fold wing and fault-depression areas as well as the mid-western karst hill-belt are identified as favorable zones for reservoir exploration in Yubei area.

Key words: Maigaiti slope, Ordovician, carbonate rock, reservoir type, reservoir model

中图分类号:

TE112.2

刘忠宝, 高山林, 岳勇, 黄秀仁, 刘士林, 吴仕强, 张仲培, 杨圣彬. 塔里木盆地麦盖提斜坡奥陶系储层成因与分布[J]. 石油学报, 2014, 35(4): 654-663.

Liu Zhongbao, Gao Shanlin, Yue Yong, Huang Xiuren, Liu Shilin, Wu Shiqiang, Zhang Zhongpei, Yang Shengbin. Formation and distribution of the Ordovician reservoir in Maigaiti slope, Tarim Basin[J]. ACTA PETROLEI SINICA, 2014, 35(4): 654-663.

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塔里木盆地麦盖提斜坡奥陶系储层成因与分布

Formation and distribution of the Ordovician reservoir in Maigaiti slope, Tarim Basin

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