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机构地区:[1]Institute of High Energy Physics, Academia Sinica, Beijing 100080, PRC
出 处:《Chinese Science Bulletin》1991年第8期666-669,共4页
基 金:Project supported by the National Natural Science Foundation of China.
摘 要:At present, the study of Cretaceous-Tertiary (K-T) boundary event is focused on its formation mechanism. Two main models to interpret the K-T event are extraterrestrial impact and volcanic eruption. Unfortunately, until now none of the experimental results, even iridium anomaly and shock-metamorphic quartz, give exclusive evidence. They support
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