Shock metamorphism in meteorites
Shock metamorphism resulting from hypervelocity collisions between planetary bodies, is a fundamental processes in the solar system. The term "shock metamorphism" is used to describe all changes in rocks and minerals resulting from the passage of shock waves. Most meteorites have experienc...
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Polar Research Institute of China - PRIC
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ftarcticportal:oai:generic.eprints.org:2382 2023-10-09T21:44:08+02:00 Shock metamorphism in meteorites Zhidong, Xie 2009-12 application/pdf http://library.arcticportal.org/2382/ http://library.arcticportal.org/2382/1/A0090206.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2382/1/A0090206.pdf Zhidong, Xie (2009) Shock metamorphism in meteorites. Advances in Polar Science, 20 (2). pp. 172-186. Space Article PeerReviewed 2009 ftarcticportal 2023-09-13T22:54:14Z Shock metamorphism resulting from hypervelocity collisions between planetary bodies, is a fundamental processes in the solar system. The term "shock metamorphism" is used to describe all changes in rocks and minerals resulting from the passage of shock waves. Most meteorites have experienced collisions and have a record of shock metamorphism, which includes brecciation, deformation, phase transformation, local melting and crystallization. The key to reading this record is to use the shock features to estimate the pressure and duration of shock event. In this paper, the history of the study of shock metamorphism is reviewed; basic knowledge of shock physics is discussed; recent 10 years! studies of shock-induced melt veins are summarized; and finally a short note to the shock metamorphism in general is given. Article in Journal/Newspaper Advances in Polar Science Polar Science Polar Science Arctic Portal Library |
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Open Polar |
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Arctic Portal Library |
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ftarcticportal |
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English |
topic |
Space |
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Space Zhidong, Xie Shock metamorphism in meteorites |
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Space |
description |
Shock metamorphism resulting from hypervelocity collisions between planetary bodies, is a fundamental processes in the solar system. The term "shock metamorphism" is used to describe all changes in rocks and minerals resulting from the passage of shock waves. Most meteorites have experienced collisions and have a record of shock metamorphism, which includes brecciation, deformation, phase transformation, local melting and crystallization. The key to reading this record is to use the shock features to estimate the pressure and duration of shock event. In this paper, the history of the study of shock metamorphism is reviewed; basic knowledge of shock physics is discussed; recent 10 years! studies of shock-induced melt veins are summarized; and finally a short note to the shock metamorphism in general is given. |
format |
Article in Journal/Newspaper |
author |
Zhidong, Xie |
author_facet |
Zhidong, Xie |
author_sort |
Zhidong, Xie |
title |
Shock metamorphism in meteorites |
title_short |
Shock metamorphism in meteorites |
title_full |
Shock metamorphism in meteorites |
title_fullStr |
Shock metamorphism in meteorites |
title_full_unstemmed |
Shock metamorphism in meteorites |
title_sort |
shock metamorphism in meteorites |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
2009 |
url |
http://library.arcticportal.org/2382/ http://library.arcticportal.org/2382/1/A0090206.pdf |
genre |
Advances in Polar Science Polar Science Polar Science |
genre_facet |
Advances in Polar Science Polar Science Polar Science |
op_relation |
http://library.arcticportal.org/2382/1/A0090206.pdf Zhidong, Xie (2009) Shock metamorphism in meteorites. Advances in Polar Science, 20 (2). pp. 172-186. |
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1779317447158923264 |