| 河南牟页1井山西组—太原组页岩含气性控制因素 |
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| 引用本文： | 刘家橙,刘家橘,张栋,王晓燕.河南牟页1井山西组—太原组页岩含气性控制因素[J].地质找矿论丛,2019,34(2):219-224. |
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| 作者姓名： | 刘家橙 刘家橘 张栋 王晓燕 |
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| 作者单位： | 河南省地质调查院,郑州450001;地下清洁能源勘查开发产业技术创新战略联盟,郑州450001;地下清洁能源勘查开发产业技术创新战略联盟,郑州450001;河南省地质矿产勘查开发局第二地质矿产调查院,郑州450001 |
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| 基金项目： | 国土资源部第二轮页岩气探矿权项目"河南中牟页岩气勘查"（编号：GT2012YQTKQCR0020）、河南省重大科技专项项目"河南页岩气勘查开发及示范应用研究"（编号：151100311000）、河南省国土资源厅科技攻关项目"河南省平原区晚古生代页岩气层岩相古地理研究"（编号：2015-1992-20）联合资助。 |
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| 摘 要： | 目前页岩含气性控制因素是页岩气勘探研究的一个关键问题。基于中牟区块及周边研究资料,在太原组—山西组海陆过渡相的泥炭沼泽亚相和潟湖亚相沉积岩是页岩气发育最有利相带,对岩芯进行含气量测试研究。结果表明:1)山西组泥页岩平均含气量为1.82m~3/t,累计厚度20～25m;太原组泥页岩平均含气量为2.64m~3/t,累计厚度26～30m。2)太原组泥岩的有机碳含量要高于山西组;随着埋藏深度的加大,有机碳含量具有逐渐增加的趋势,且非均质性较强。3)地层垂向岩性变化、厚度、有机质含量、有机质生烃能力影响页岩含气性。4)现场解吸气量、有机质丰度、厚度、埋深、裂缝、孔隙结构是牟页1井山西组—太原组页岩含气性控制因素。
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| 关 键 词： | 中牟区块 牟页1井 太原组 山西组 页岩气 主控因素 河南省 |
| 收稿时间： | 2018/3/7 0:00:00 |
Controlling factors of shale gas content in Taiyuan and Shanxi Formations determined by data from well Mouye 1 in Henan province |
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| LIU Jiacheng,LIU Jiaju,ZHANG Dong and WANG Xiaoyan.Controlling factors of shale gas content in Taiyuan and Shanxi Formations determined by data from well Mouye 1 in Henan province[J].Contributions to Geology and Mineral Resources Research,2019,34(2):219-224. |
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| Authors: | LIU Jiacheng LIU Jiaju ZHANG Dong and WANG Xiaoyan |
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| Institution: | Henan provincial institute of geological survey, Zhengzhou 450001, China;Innovation Strategy Alliance of Underground Clean Energy Exploration and Development, Zhengzhou 450001, China,Henan provincial institute of geological survey, Zhengzhou 450001, China;Innovation Strategy Alliance of Underground Clean Energy Exploration and Development, Zhengzhou 450001, China,Henan provincial institute of geological survey, Zhengzhou 450001, China;Innovation Strategy Alliance of Underground Clean Energy Exploration and Development, Zhengzhou 450001, China and Innovation Strategy Alliance of Underground Clean Energy Exploration and Development, Zhengzhou 450001, China;The second geological and mineral survey institute of Henan bureau of Geological & Mineral Resources Exploration, Zhengzhou 45001, China |
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| Abstract: | At present, the controlling factors of shale gas content are a key issue in shale gas exploration and study. According to the data of Zhongmou block and nearby regions sedimentary rock of peat swamp sub-facies and laggo0n sub-facies of the sea-continent transitional facies in Taiyuan Formation-Shanxi Formation is the most favorable facies belt of shale gas. The gas content of the rock core was tested and studied. The result shows that the average gas content of the argillutite (cumulative thickness (20 to 25 m), in Shanxi Formation was 1.82 m3 and the average gas content of argillutite (thickness 26 to 30 m) in Taiyuan Formation was 2.64 m3/t; the organic carbon content of argillutite in Taiyuan Formation was higher than that in Shanxi Formation and the organic carbon content gradually increases with stronger heterogeneity to depth; vertical lithologic variation, thickness, organic matter content and ability of the organic matter to generate hydrocarbon affect the shale gas content and the on-site desorption gas amount, organic matter abundance, thickness, burial depth, fracture, pore structure are the main control factors. |
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| Keywords: | Zhongmou block well Mouye 1 Taiyuan Formation Shanxi Formation shale gas main controlling factor Henan province |
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