长白山天池周围地热活动中CO2的来源探讨
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本文为国土资源部岩溶地质研究所岩溶动力学开放研究实验室资助课题(编号9705)


A Discussion on the Genesis of CO2 Outgassed in Geothermal Processes around the Tianchi Lake on Changbai Mountains
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  • 国土资源部环境地质研究所,北京,100081    
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  • Institute of Environmental Geology, MLR, Beijing,100081    
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    摘要:

    碳循环是目前国内外环境地学界研究的重大课题。笔者认为,在长白山地区,以天池为中心,存在着强烈的地热活动,受断裂控制的温泉为地热活动的主要形式。温泉具有深循环特征,温泉气体和泉水中碳质含量高,碳质主要来自上地幔,并与上地幔的挤压流动有关。

    Abstract:

    Carbon circulation is a very important subject in recent studies of the env ironmental geology. It is pointed out in this paper that there existed strong ge othermal ac tivity with a lot of hot springs controlled by deep faults around the Tianchi L a k e, Changbai Mountains, and the plentiful CO2 outgassed from the h ots prings meanly came from the upper mantle. Also the CO2 had a connection with t he thrust and flow in the upper mantle.

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张加桂,胡海涛.1999.长白山天池周围地热活动中CO2的来源探讨[J].地质论评,45(7):231-235,[DOI].
Zhang Jiagui, Hu Haitao.1999. A Discussion on the Genesis of CO2 Outgassed in Geothermal Processes around the Tianchi Lake on Changbai Mountains[J]. Geological Review,45(7):231-235.

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