Geochemical characteristics and genesis of hydrocarbons in superficial soil in continental permafrost regions in China
YANG Zhi-Bin1,2,3(), ZHOU Ya-Long1, ZHANG Fu-Gui1, ZHANG Shun-Yao1, SUN Zhong-Jun1
1. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China 2. State Research Center of Modern Geological Exploration Engineering Technology, Langfang 065000, China 3. Tibet Institute of Geological Survey, Lhasa 850000, China
This study analyses the geochemical characteristics, genesis, and properties of hydrocarbon components using data of surface soil samples collected from the permafrost regions in the Qiangtang Basin, the Qilian Mountains, and the Mohe Basin. The results revealed that the hydrocarbon gases in the superficial soils in the permafrost regions mainly comprise methane, as well as a small amount of ethane, ethylene, propane, butane, and pentane. The hydrocarbon gases in the Qiangtang and Mohe basins are mainly of pyrolytic genesis and their types include soil-formed gas and the mixed gas of soil-formed gas and coalbed methane. In contrast, hydrocarbon gases in the superficial soil in the permafrost zone in the Qilian Mountains are of pyrolytic and biogenic genesis and their types include soil-formed gas, coalbed methane, and biogenetic gas. The study provides a basis for exploring oil and gas resources such as natural gas hydrates in the continental permafrost regions in China.
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YANG Zhi-Bin, ZHOU Ya-Long, ZHANG Fu-Gui, ZHANG Shun-Yao, SUN Zhong-Jun. Geochemical characteristics and genesis of hydrocarbons in superficial soil in continental permafrost regions in China. Geophysical and Geochemical Exploration, 2022, 46(3): 628-636.
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