首页|Experimental investigation on the origin of carbonaceous materials in the fault zone of the Wenchuan earthquake
Experimental investigation on the origin of carbonaceous materials in the fault zone of the Wenchuan earthquake
扫码查看
点击上方二维码区域，可以放大扫码查看
原文链接
万方数据
维普
Carbonaceous materials in seismic fault zones may considerably influence seismic fault slip;however,the formation mechanism of carbonaceous materials remains unclear.In this study,we proposed a novel hypothesis for the formation of carbonaceous materials in fault gouge.Thus,we conducted a CO2 hydrogenation experiment in a high-temperature reactor at a co-seismic temperature,with fault gouge formed during the Wenchuan earthquake as the catalyst.Our experimental results demonstrate that carbonaceous materials in fault zones are formed on the fault gouge during the chemical reaction process,suggesting that the carbonaceous materials are possibly generated from the catalytic hydrogenation of CO2,followed by thermal cracking of its products.The results of this study provide a theoretical basis for understanding fault behavior and earthquake physics.
carbon dioxide hydrogenationcarbonaceous mineral formationco-seismic temperaturefault weakeningfault gouge
Deyang Shi、Yaowei Liu、Jin Shi
展开 >
Institute of Geophysics,China Earthquake Administration,Beijing 10081,China
National Institute of Natural Hazards,Ministry of Emergency Management of People's Republic of China,Beijing 10085,China
College of Metallurgy and Energy Engineering,Kunming University of Science and Technology,Kunming 650093,China
万方数据
维普
