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Suizhou Meteorite: Mineralogy and Shock Metamorphism

Record Type:	Language materials, printed : Monograph/item
Title/Author:	Suizhou Meteorite: Mineralogy and Shock Metamorphism/ by Xiande Xie, Ming Chen.
Author:	Xie, Xiande.
other author:	Chen, Ming.
Description:	XIV, 258 p. 168 illus., 17 illus. in color.online resource. :
Contained By:	Springer Nature eBook
Subject:	Mineralogy. -
Online resource:	https://doi.org/10.1007/978-3-662-48479-1
ISBN:	9783662484791

Suizhou Meteorite: Mineralogy and Shock Metamorphism
Xie, Xiande.

Suizhou Meteorite: Mineralogy and Shock Metamorphism[electronic resource] /by Xiande Xie, Ming Chen. - 1st ed. 2016. - XIV, 258 p. 168 illus., 17 illus. in color.online resource. - Springer Geochemistry/Mineralogy,2194-3176. - Springer Geochemistry/Mineralogy,.

General introduction of the Suizhou meteorite -- Micro-mineralogical investigative techniques -- Mineralogy of unmelted chondritic rock -- Distinct morphological and petrological features of the Suizhou shock veins.- Mineralogy of Suizhou shock veins -- Shock-induced redistribution of trace elements.- Evaluation of shock stage for Suizhou meteorite -- P-T history of the Suizhou meteorite.

This book introduces the unusual shock-related mineralogical features of the shocked Suizhou L6 (S5) meteorite. The olivine and pyroxene in Suizhou display a mosaic shock feature, while most of plagioclase grains have transformed to glassy maskelynite. A few of the shock-induced melt veins in the meteorite are the simplest, straightest and thinnest ones among all shock-vein-bearing meteorites, and contain the most abundant high-pressure mineral species. Among the 11 identified species, tuite, xieite, and the post-spinel CF-phase of chromite are new minerals. The meteorite experienced a peak shock pressure up to 24 GPa and temperatures of up to 1000° C. Locally developed shock veins were formed at the same pressure, but at an elevated temperature of about 2000° C that was produced by localized shear-friction stress. The rapid cooling of the extremely thin shock veins is the main reason why 11 shock-induced high-pressure mineral phases could be preserved in them so well. This book offers a helpful guide for meteoritics researchers and mineralogists and invaluable resource for specialists working in high-pressure and high-temperature mineralophysics.

ISBN: 9783662484791

Standard No.: 10.1007/978-3-662-48479-1doiSubjects--Topical Terms:

670562
Mineralogy.

LC Class. No.: QE351-399.2

Dewey Class. No.: 549

Suizhou Meteorite: Mineralogy and Shock Metamorphism
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520 $a This book introduces the unusual shock-related mineralogical features of the shocked Suizhou L6 (S5) meteorite. The olivine and pyroxene in Suizhou display a mosaic shock feature, while most of plagioclase grains have transformed to glassy maskelynite. A few of the shock-induced melt veins in the meteorite are the simplest, straightest and thinnest ones among all shock-vein-bearing meteorites, and contain the most abundant high-pressure mineral species. Among the 11 identified species, tuite, xieite, and the post-spinel CF-phase of chromite are new minerals. The meteorite experienced a peak shock pressure up to 24 GPa and temperatures of up to 1000° C. Locally developed shock veins were formed at the same pressure, but at an elevated temperature of about 2000° C that was produced by localized shear-friction stress. The rapid cooling of the extremely thin shock veins is the main reason why 11 shock-induced high-pressure mineral phases could be preserved in them so well. This book offers a helpful guide for meteoritics researchers and mineralogists and invaluable resource for specialists working in high-pressure and high-temperature mineralophysics.
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