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机构地区:[1]Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
出 处:《Chinese Science Bulletin》1995年第5期395-399,共5页
基 金:Project supported by the National Natural Science Foundation of China
摘 要:Anomalies of content of Ir, noble metals and other trace elements are usually regarded as crucial evidence of impact event. A large number of microtektites have been found in deep-sea sediments since the 1960s, but analyses of trace elements in microtektitebearing layers have seldom been reported, with the exception that Asaro et al. stated that microtektite-bearing layers in Caribbean Gulf exhibited anomaly of Ir (?). The
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