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000752027 020__ $$a9783662484791$$q(electronic book)
000752027 020__ $$a366248479X$$q(electronic book)
000752027 020__ $$z9783662484777
000752027 0247_ $$a10.1007/978-3-662-48479-1$$2doi
000752027 035__ $$aSP(OCoLC)ocn922640356
000752027 035__ $$aSP(OCoLC)922640356
000752027 040__ $$aN$T$$beng$$erda$$epn$$cN$T$$dN$T$$dYDXCP$$dIDEBK$$dOCLCF$$dAZU$$dCOO$$dGW5XE$$dOCLCQ$$dOCLCA
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000752027 049__ $$aISEA
000752027 050_4 $$aQB755
000752027 08204 $$a523.5/1$$223
000752027 1001_ $$aXie, Xiande,$$eauthor.
000752027 24510 $$aSuizhou meteorite$$h[electronic resource] :$$bmineralogy and shock metamorphism /$$cXiande Xie, Ming Chen.
000752027 264_1 $$aGuangzhou, China :$$bGuangdong Science & Technology Press Co., Ltd. ;$$aHeidelberg :$$bSpringer,$$c[2016]
000752027 300__ $$a1 online resource.
000752027 336__ $$atext$$btxt$$2rdacontent
000752027 337__ $$acomputer$$bc$$2rdamedia
000752027 338__ $$aonline resource$$bcr$$2rdacarrier
000752027 4901_ $$aSpringer geochemistry/mineralogy
000752027 504__ $$aIncludes bibliographical references.
000752027 5050_ $$aGeneral introduction of the Suizhou meteorite -- Micro-mineralogical investigative techniques -- Mineralogy of unmelted chondritic rock -- Distinct morphological and petrological features of the Suizhou shock veins.- Mineralogy of Suizhou shock veins -- Shock-induced redistribution of trace elements.- Evaluation of shock stage for Suizhou meteorite -- P-T history of the Suizhou meteorite.
000752027 506__ $$aAccess limited to authorized users.
000752027 520__ $$aThis book introduces the unusual shock-related mineralogical features of the shocked Suizhou L6 (S5) meteorite. The olivine and pyroxene in Suizhou display a mosaic shock feature, while most of plagioclase grains have transformed to glassy maskelynite. A few of the shock-induced melt veins in the meteorite are the simplest, straightest and thinnest ones among all shock-vein-bearing meteorites, and contain the most abundant high-pressure mineral species. Among the 11 identified species, tuite, xieite, and the post-spinel CF-phase of chromite are new minerals. The meteorite experienced a peak shock pressure up to 24 GPa and temperatures of up to 1000° C. Locally developed shock veins were formed at the same pressure, but at an elevated temperature of about 2000° C that was produced by localized shear-friction stress. The rapid cooling of the extremely thin shock veins is the main reason why 11 shock-induced high-pressure mineral phases could be preserved in them so well. This book offers a helpful guide for meteoritics researchers and mineralogists and invaluable resource for specialists working in high-pressure and high-temperature mineralophysics.
000752027 650_0 $$aMeteorites$$zChina$$zSuizhou Shi.
000752027 650_0 $$aMineralogical chemistry.
000752027 650_0 $$aGeochemistry.
000752027 650_0 $$aAstrogeology.
000752027 7001_ $$aChen, Ming$$c(Geochemist),$$eauthor.
000752027 77608 $$iPrint version:$$z9783662484777
000752027 830_0 $$aSpringer geochemistry/mineralogy.
000752027 852__ $$bebk
000752027 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-662-48479-1$$zOnline Access$$91397441.1
000752027 909CO $$ooai:library.usi.edu:752027$$pGLOBAL_SET
000752027 980__ $$aEBOOK
000752027 980__ $$aBIB
000752027 982__ $$aEbook
000752027 983__ $$aOnline
000752027 994__ $$a92$$bISE