STUDY OF CHEMICAL SPECIES OF ANOMALOUS IRIDIUM IN CRETACEOUS-TERTIARY (K-T) BOUNDARY CLAY LAYER  

STUDY OF CHEMICAL SPECIES OF ANOMALOUS IRIDIUM IN CRETACEOUS-TERTIARY (K-T) BOUNDARY CLAY LAYER~*

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作  者:柴之芳 孔屏 毛雪瑛 马建国 马淑兰 

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

关 键 词:IRIDIUM SPECIES K-T boundary. 

分 类 号:N[自然科学总论]

 

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