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青海木里三露天冻土区天然气水合物钻孔岩心顶空气组成及指示意义
引用本文:唐世琪,卢振权,王伟超,谭盼盼,李清海,刘文进,李永红.青海木里三露天冻土区天然气水合物钻孔岩心顶空气组成及指示意义[J].现代地质,2015,29(5):1201-1213.
作者姓名:唐世琪  卢振权  王伟超  谭盼盼  李清海  刘文进  李永红
作者单位:(1.中国地质大学(北京)地球科学与资源学院,北京100083; 2.中国地质调查局 油气资源调查中心,北京100029; 3.中国地质科学院 矿产资源研究所,北京100037; 4.青海煤炭地质一0五勘探队,青海 西宁810007)
基金项目:神华青海能源开发有限责任公司“青海省天峻县聚乎更煤矿区三露天天然气水合物调查评价”项目(SHQHNY201307001);中国地质调查局“祁连山冻土区天然气水合物资源勘查”项 目(GZH201400302);中国地质调查局“陆域天然气水合物环境监测及效应研究“项目(GZH201400308);中国地质调查局“南祁连盆地油气资源战略调查”项目(1211302108021-3)。
摘    要:对青海木里三露天地区DK8-19、DK10-16、DK10-17、DK11-14、DK12-13、DK13-11共6个天然气水合物钻孔岩心顶空气气体组分进行分析测试,并 将获得的各孔岩心顶空气组分含量变化与天然气水合物及其异常层段、油气显示层段、断层或破碎带分布之间的空间关系进行对比分析。结果显示:6个钻孔岩心顶空气中烃类气体高含量区间 均与天然气水合物及其异常层段、油气显示层段具较好的对应关系,其高值区间可作为天然气水合物、油气显示的一种指示;距断层或破碎带产出位置不同的岩心顶空气组分含量变化特征显 示,不同级次的断裂系统为烃类气体向上运移提供通道,部分可为天然气水合物提供赋存空间。研究结果说明顶空气组成对天然气水合物及其异常现象、油气显示现象、烃类气体运移作用有 重要指示意义。

关 键 词:青海木里  三露天  冻土  天然气水合物  顶空气组成  指示意义  

The Indicative Significance of Gas Composition of Headspace Gases from the Gas Hydrate Drilling Holes in the Sanlutian Mine of the Muli Mining Area,Qinghai
Affiliation:(1. School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China; 2.Oil & Gas Survey, China Geological Survey, Beijing100029, China;3.Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing100037, China; 4.Qinghai No.105 Coal Geological Exploration Team, Xining, Qinghai810007,China)
Abstract:Through the analysis on hydrocarbon gas components at different depths in headspace gases from the cores in DK8-19, DK10-16, DK10-17, DK11-14, DK12-13, DK13-11 in Sanlutian area of Muli, the distribution relationship of the sections with anomalistic gas component content, gas hydrate output layers, oil and gas output layers, faults or fracture zones output layers was discussed. The results show that the anomalistic gas component content sections can be compared with those of gas hydrate and its major anomaly output layers, and oil and gas output layers; the abnormal section can be used as an indication of gas hydrate and its major anomalies and oil and gas. The relationship between variation of hydrocarbon gas content in headspace gases and the location of faults or fracture zones shows that different levels of fault system from the deep can provide a channel for deep hydrocarbon gas migration or existing space for the formation of gas hydrate.The results show that the gas component of headspace gas has important significance for gas hydrate and its major anomalies, the oil and gas and the migration of hydrocarbon.
Keywords:Muli  Qinghai  Sanlutian  permafrost  gas hydrate  headspace gas composition  indicative significance  
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