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DOI | 10.1126/science.248.4957.843 |
Proximal cretaceous-tertiary boundary impact deposits in the Caribbean | |
Hildebrand A.R.; Boynton W.V. | |
发表日期 | 1990 |
ISSN | 0036-8075 |
起始页码 | 843 |
结束页码 | 847 |
卷号 | 248期号:4957 |
英文摘要 | Trace element, isotopic, and mineralogic studies indicate that the proposed impact at the Cretaceous-Tertiary (K-T) boundary occurred in an ocean basin, although a minor component of continental material is required. The size and abundance of shocked minerals and the restricted geographic occurrence of the ejecta layer and impact-wave deposits suggest an impact between the Americas. Coarse boundary sediments at sites 151 and 153 in the Colombian Basin and 5- to 450-meter-thick boundary sediments in Cuba may be deposits of a giant wave produced by a nearby oceanic impact. On the southern peninsula of Haiti, a ∼50-centimeter-thick ejecta layer occurs at the K-T boundary. This ejecta layer is ∼25 times as thick as that at any known K-T site and suggests an impact site within ∼1000 kilometers. Seismic reflection profiles suggest that a buried ∼300-km-diameter candidate structure occurs in the Colombian Basin. |
英文关键词 | Cretaceous/Tertiary boundary; ejecta layer; impact deposit; tsunami deposit; Caribbean; Cuba; Haiti |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/244010 |
作者单位 | Department of Planetary Sciences, University of Arizona, Tucson, AZ 85721 |
推荐引用方式 GB/T 7714 | Hildebrand A.R.,Boynton W.V.. Proximal cretaceous-tertiary boundary impact deposits in the Caribbean[J],1990,248(4957). |
APA | Hildebrand A.R.,&Boynton W.V..(1990).Proximal cretaceous-tertiary boundary impact deposits in the Caribbean.Science,248(4957). |
MLA | Hildebrand A.R.,et al."Proximal cretaceous-tertiary boundary impact deposits in the Caribbean".Science 248.4957(1990). |
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