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机构地区:[1]Institute of Geochemistry, Academia Sinica, Guiyang 550002, PRC [2]Southwest Institute of Fluid Physics, Mianyang 610003, PRC
出 处:《Chinese Science Bulletin》1991年第23期1984-1988,共5页
基 金:Project supported by the National Natural Science Foundation of China
摘 要:Ⅰ. INTRODUCTION A wide variety of shock effects in meteorites were generated by hypervelocity impacts between their parent bodies. According to study results of shocked meteorite samples loaded by shock wave produced by the dynamic high pressure device, it is possible to determine the pressure or temperature ranges of important shock features and to predict the dynamic condition and the impact environment of their parent bodies. An artificially shockloaded meteorite (Kernouve chondrite, H6)has been studied by Sears et al., who
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