中国可能的煤层气高产走廊:中亚造山带北缘中-新生代含煤盆地群  

A Probable High Production Coalbed Methane Belt in China:the Mesozoic Basins along the Northern Edge of the Central Asian Orogenic Belt

作　　者：方爱民[1,2] 侯泉林[3] 张俊敏[1] 谢峰震[1] 帕尔哈提[1] 陈飞[1] FANG Aimin HOU Quanlin ZHANG Juanmin XIE Fengzheng PA Erhati CHENG Fei(Mining Department, Xinjiang Engineering College, Xinjiang 450016 Institute of Geology and Geophysics Chinese Academy of Sciences, Beijing 100029 College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049)

机构地区：[1]新疆工程学院采矿工程系,新疆450016 [2]中国科学院地质与地球物理研究所,北京100029 [3]中国科学院大学地球科学学院,北京100049

出　　处：《中国煤层气》2017年第1期7-10,31,共5页China Coalbed Methane

基　　金：国家自然科学基金项目(41562007和41030422)

摘　　要：本文通过对中亚造山带和煤层气中亚聚集域与北美落基山造山带及其煤层气高产走廊的主要地质特征(包括含煤盆地性质、造山带构造活动特点、煤变质程度、煤储层渗透率等方面)的对比,分析了我国中亚煤层气聚集域煤层气富集成藏的基本条件,提出中亚造山带北缘的中亚煤层气聚集域有望成为我国煤层气高产走廊带,为中国煤层气产业化进程中所面临的宏观部署和决策调整提供理论依据。In this article,a comparative study has been conducted on the basic geological backgrounds such as the properties of the coal basins,the coal ranks and the permeability of the coal-layers to analysis the basic conditions of the enrichment of the coalbed methane of the central Asian coalbed methane belt,and to provide theoretical support of the change of the national strategies of the coal gas exploration.

关 键 词：煤层气 高产走廊 中亚造山带 中亚煤层气聚集域 

分 类 号：P618.13[天文地球—矿床学]