鄂尔多斯盆地海相碳酸盐岩规模优质储层分布与勘探方向

作    者:范立勇1,吴东旭2,任军峰1,王永骁2,魏柳斌1, 张 豪2,李维岭2 ,鲁慧丽2,朱文博2,3,4
单    位:1 中国石油长庆油田公司;2 中国石油杭州地质研究院;3 国家能源碳酸盐岩油气重点实验室; 4 中国石油碳酸盐岩储层重点实验室
基金项目:
摘    要:
鄂尔多斯盆地下古生界海相碳酸盐岩是我国重要的天然气勘探领域,但储层非均质性强、成藏主控因素 复杂等问题,严重制约了规模效益勘探开发。综合应用最新勘探成果及区域格架剖面地震资料,从岩相古地理演 化、储层成因类型与主控因素、源储配置关系等基础地质问题入手,揭示了盆地海相碳酸盐岩规模优质储层分布规 律与勘探潜力。主要取得以下成果认识:①盆地早古生代沉积环境经历了混积陆棚→碳酸盐缓坡→镶边台地的完 整演化序列,其中环古隆起及海盆周缘发育的内缓坡颗粒滩相带具有最优异的储集性能。②储层发育受沉积微 相、准同生溶蚀、表生溶蚀及白云石化作用等多因素控制。寒武系—奥陶系发育颗粒滩型、藻丘型、生物扰动型、溶 模孔型和溶蚀孔洞型 5类储层,平面上主要沿古隆起周缘和海盆边缘及坡折带分布。③基于构造-沉积格局、源储 配置关系及封盖条件综合分析,优选出 3 个最具勘探潜力的区带:乌银海盆东侧有利区、宜铜海盆两侧有利区和神 木—米脂台洼西侧有利区,总面积达 10.5×104 km2。研究成果为鄂尔多斯盆地海相碳酸盐岩天然气勘探提供了重 要的理论支撑和勘探方向。
关键词:海相碳酸盐岩;储层分布;天然气成藏;勘探方向;寒武系;奥陶系;鄂尔多斯盆地

Distribution of large-scale high-quality carbonate reservoirs and exploration directions in the Ordos Basin

Author's Name: FAN Liyong1, WU Dongxu2, REN Junfeng1, WANG Yongxiao2, WEI Liubin1, ZHANG Hao2, LI Weiling2, LU Huili2, ZHU Wenbo2,3,4
Institution: 1. PetroChina Changqing Oilfield Company; 2. PetroChina Hangzhou Research Institute of Geology; 3. State Energy Key Laboratory for Carbonate Oil and Gas; 4. Key Laboratory of Carbonate Reservoirs, CNPC
Abstract:
The Lower Paleozoic marine carbonate rocks in the Ordos Basin represent a critical natural gas exploration target in China. However, problems such as strong reservoir heterogeneity and complex hydrocarbon accumulation controlling factors have severely restricted large-scale and efficient exploration and development. This study integrates the latest exploration results with regional seismic profiles, focusing on key scientific issues such as lithofacies paleogeographic evolution, genetic types and controlling factors of reservoirs, and source-reservoir configurations, to systematically investigate the distribution patterns of high-quality carbonate reservoirs and evaluate their exploration potential. The main findings are as follows: (1) The Early Paleozoic sedimentary environment underwent a complete evolutionary sequence from mixed sedimentary shelf (Mantou to Xuzhuang Formation) to carbonate ramps (Zhangxia to Majiagou Formation) and finally to rimmed platforms (Upper Majiagou Formation). Among these, the inner ramp grain shoal facies belts around paleo-uplifts and marine basins exhibit the most favorable reservoir properties. (2) Reservoir development is jointly controlled by depositional microfacies, penecontemporaneous dissolution, supergene karstification, and dolomitization. Five types of reservoirs are identified in the Cambrian-Ordovician succession: grain shoal, algal mound, bioturbated, moldic pore, and dissolution vug types. These reservoirs are predominantly distributed along paleouplifts, basin margins and slope breaks. (3) Based on comprehensive analysis of tectonic-sedimentary framework, sourcereservoir relationships, and sealing conditions, three highly prospective exploration zones are delineated: the eastern Wuyin marine basin, both flanks of the Yitong marine basin, and the western Shenmu-Mizhi platform depression, with a total area of 10.5×104 km2. This study provides critical theoretical support and practical guidance for gas exploration in marine carbonate rocks of the Ordos Basin.
Keywords: marine carbonate rock; reservoir distribution; natural gas accumulation; exploration direction; Cambrian; Or⁃ dovician; Ordos Basin
投稿时间: 2025-11-10  
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