地学前缘 ›› 2012, Vol. 19 ›› Issue (3): 264-279.

• 论文 • 上一篇    下一篇

羌塘盆地中生界海相黑色泥页岩特征及页岩气远景区预测

王丽波，苏爱国，郑有业，李超，久凯   

  1. 1. 中国地质大学（武汉） 资源学院， 湖北 武汉 430074 2. 东北石油大学, 黑龙江 大庆 163318 3. 中国石油勘探开发研究院， 北京 100083 4. 中国地质大学（北京） 海相储层演化与油气富集机理教育部重点实验室， 北京 100083  
  • 收稿日期:2011-11-18 修回日期:2012-02-18 出版日期:2012-05-25 发布日期:2012-05-25
  • 作者简介:王丽波（1966—），女，博士研究生，副教授，主要从事资源管理与评价工作。E-mail：Libowang2008@126.com
  • 基金资助:

    国家自然科学基金项目（41072098）；国家科技重大专项（2011ZX05018-001-002）；全国油气资源战略选区调查与评价国家专项（2009GYXQ-15）

Characteristics of Mesozoic marine black shales and prediction of shale gas prospective area in Qiangtang Basin, Tibet.

  1. 1. Faculty of Earth Resources, China University of Geosciences(Wuhan), Wuhan 430074, China 2. Northeast Petroleum University, Daqing 163318, China 3. Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing 100083, China 4. Key Laboratory for Marine Reservoir Evolution and Hydrocarbon Abundance Mechanism, Ministry of Education, China University of Geosciences(Beijing), Beijing 100083, China
  • Received:2011-11-18 Revised:2012-02-18 Online:2012-05-25 Published:2012-05-25

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摘要：

青藏高原羌塘盆地中生界发育上三叠统肖茶卡组（T3x）、中侏罗统布曲组（J2b）和上侏罗统索瓦组（J3s）3套海相黑色泥页岩，形成于有机质比较丰富且易于保存的营养型还原性沉积环境，以台地相为主，其次为盆地相和三角洲相；厚度在41～474 m范围内，有机碳（TOC）含量平均值为0.25%～8.34%，有机质类型主要为Ⅱ型干酪根，镜质体反射率（Ro）平均值为1.21%～3.0%，处于高—过成熟生气阶段，脆性矿物以石英、长石为主，含量为65%～70%，页岩孔隙度约2%。与美国主要盆地产气页岩各项指标相比较，羌塘盆地中生界海相黑色泥页岩具有厚度大、有机质丰度低、热演化熟度高、脆性矿物种类多、石英含量较低、长石和粘土矿物含量较高及孔隙度低的特征，具备了形成页岩气基本地质条件，是我国海相页岩气勘探的沉积盆地之一，综合评价预测的页岩气远景区以上三叠统肖茶卡组（T3x）分布范围大，其次是布曲组（J2b）和索瓦组（J3s）。

关键词: 羌塘盆地, 中生界, 海相页岩, 页岩气, 形成条件, 远景区

Abstract:

Mesozoic marine black shales are mainly distributed in the Qiangtang Basin, QinghaiTibet plateau, in the Upper Triassic Xiaochaka Formation（T3x）， the Jurassic Buqu Formation (J2b) and the Suowa Formation (J3x).  They are formed in the reducing sedimentary environment which is abundant in organics that are easily preserved. The sedimentary facies are mainly platform facies, followed by basinal facies and delta facies. The thickness is 41474 m; TOC is 0.25%8.34％; organic matter is typeⅡ; the average value of Ro is 1.21%3.0％, showing in the gas stage of highover mature. The brittle minerals are mainly quartz and feldspar, total contents are 65%70%, and the shale porosity is about 2%. Compared with each index of gas shales in the main basins of American, we can consider that the Mesozoic marine black shales in Qiangtang Basin have the features of large deposition thickness, low organic abundance, high maturity of thermal evolution, numerous species of brittle minerals, low content of quartz, high content of feldspar and clay minerals, and low porosity. It means that the shales have the condition of producing shale gas and the basin is one of the sedimentary basins, in which the marine shale gas could be explored. From the comprehensive evaluation of the shale gas prospective areas, it can be predicted that in the Upper Triassic Xiaochaka Formation shale gas is widely distributed, followed by the Buqu Formation and the Suowa Formation.

Key words:  Qiangtang Basin, Mesozoic, marine shale, shale gas, formation conditions, prospective area

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