中国石油勘探 ›› 2021, Vol. 26 ›› Issue (1): 86-98.DOI: 10.3969/j.issn.1672-7703.2021.01.007

• 石油地质 • 上一篇    下一篇

湘中坳陷涟源凹陷湘页1井大隆组页岩气地质特征

汪凯明,何希鹏,许玉萍,金伟   

  1. 中国石化华东油气分公司勘探开发研究院
  • 出版日期:2021-01-13 发布日期:2021-01-13
  • 基金资助:
     

Geological characteristics of shale gas in the Dalong Formation in Well Xiangye 1 in the Lianyuan Sag, Xiangzhong Depression#br#

Wang Kaiming, He Xipeng, Xu Yuping, Jin Wei   

  1. Research Institute of Exploration and Development, Sinopec East China Oil & Gas Company
  • Online:2021-01-13 Published:2021-01-13
  • Supported by:
     

摘要: 为评价湘中坳陷涟源凹陷二叠系大隆组页岩气成藏地质条件,部署实施了该区首口以大隆组为目的层 的页岩气参数井——湘页1 井。充分利用湘页1 井钻井、岩心、测井及分析测试资料,开展大隆组岩石矿物组成特 征、沉积特征、有机地球化学特征、储集物性特征、含气性等地质条件分析。研究结果表明:湘页1 井大隆组页岩 形成于缺氧的较深水台盆相沉积环境,有利于页岩发育和有机质保存,优质页岩厚度大(TOC 大于2% 的页岩厚 92.8m)、有机质丰度高(TOC 为0.41%~10.47%,平均为3.91%)、热演化程度适中(R o 为1.50%~ 1.72%, 平均为1.58%),微观孔隙结构以中孔和大孔为主,微裂缝发育,页岩脆性指数高,两向水平主应力差值小,有利于 压裂形成复杂网络裂缝,具备形成页岩气藏的基本地质条件;保存条件是影响页岩含气性的关键因素,湘页1 井大隆 组页岩进入生烃期以后,经历了3 期明显的构造抬升剥蚀,以致现今埋藏浅,距离剥蚀区近,向斜构造页岩气易横向 逸散,同时腐殖型干酪根产烃率相对较低也影响其含气性。构造形态宽缓、埋深较大、远离剥蚀区、翼部发育反向逆 断层有利于残留向斜型页岩气富集。

 

关键词: 涟源凹陷, 湘页1 井, 大隆组, 常压页岩气

Abstract: In the Lianyuan Sag of the Xiangzhong Depression, Well Xiangye 1 was deployed and implemented to evaluate the geological conditions for accumulation of shale gas in the Permian Dalong Formation. It was the first shale gas parameter well with the Dalong Formation as the target layer. In this study, the geological conditions of shale targets in the Dalong Formation are
analyzed using data from drilling, cores, well logging, and lab test results from Well Xiangye 1, including the sedimentary characteristics,rock minerals composition, organic geochemical characteristics, reservoir physical properties, and gas-bearing properties of the Dalong Formation. The results show that the Dalong Formation shale in Well Xiangye 1 is developed in an anoxic and deep-water platform-basin sedimentary environment, which is conducive to the development of shale and the preservation of organic matter. The thickness of high-quality shale is great (shale thickness is 92.8 m with TOC greater than 2%), there is a high
abundance of organic matter (TOC ranges from 0.41% to 10.47%, with an average of 3.91%), and the thermal evolution degree is moderate (Ro ranges from 1.50% to 1.72%, with an average of 1.58%). The pore structure of the shale reservoir is dominated by mesopores and macropores, with micro-fractures developed. The brittleness index of the shale is high, and the difference in
two-dimensional principal stress is small, which is conducive to the formation of a complex fracture network by hydraulic fracturing.The combination of these parameters indicates that the basic geological conditions are favorable for accumulation of shale gas. However, the preservation conditions are the key factor affecting the gas-bearing properties of the shale. After entering the period of hydrocarbon generation, the Dalong Formation shale in Well Xiangye 1 experienced three distinct phases of tectonic uplift and denudation, which resulted in the current shallow burial depth of the shale and its proximity to the denudation area. Shale gas in synclinal structures was easily able to escape laterally, and the hydrocarbon generation rate of humic kerogen was relatively low; both factors affected the gas-bearing properties of shale in the Dalong Formation. The area far away from the denudation zone, with a wide and gentle structure and great burial depth, and with reverse faults developed in the wings, is more favorable for the accumulation of residual syncline type shale gas.

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