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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F11%3A10107986%21RIV12-GA0-11310___
rdf:type
skos:Concept n5:Vysledek
rdfs:seeAlso
http://www.elsevierdirect.com/ISBN/9780123851444/UltrahighPressure-Metamorphism
dcterms:description
Since the first discovery of coesite (Chopin, 1984; Smith, 1984) and microdiamond (Sobolev & Shatsky, 1990) within eclogite-bearing metamorphic belts, extensive progress has been achieved in understanding the origin of ultrahigh-pressure metamorphic (UHPM) rocks in the context of global tectonics operating through continental subduction, collision, exhumation, mantlelithospheric slab interactions, and geochemical recycling of subducted/exhumed rocks. Comprehensive review articles and special issues related to UHP metamorphism and plate tectonics are published almost every year (Ernst & Liou, 2000, 2008; Chopin, 2003; Liou et al., 2004; Green, 2005; Ernst et al., 2007; Zhang et al., 2007; Guillot et al., 2008; Liou et al., 2009a; Beltrando et al., 2010). They provide valuable summaries of existing knowledge, outline future directions, and discuss controversial concepts. These papers also summarized recent progress in experimental determination of PT stability fields of new phases, phase transformations of those minerals which were known before to be stable only at shallow depths of the continental crust, and they reported that the exsolution products of UHPM minerals indicate that continental rocks were subducted to depths exceeding 100250 km. Extensive research in UHP metamorphic rocks led to new constraints and the improvement of many geotectonic models developed for very deep subduction of continental rocks and their exhumation within many well-known orogenic belts. Numerical geodynamic modeling of subduction and exhumation became a powerful tool for understanding mantle dynamics and global continental subduction (Gerya, 2010). Since the first discovery of coesite (Chopin, 1984; Smith, 1984) and microdiamond (Sobolev & Shatsky, 1990) within eclogite-bearing metamorphic belts, extensive progress has been achieved in understanding the origin of ultrahigh-pressure metamorphic (UHPM) rocks in the context of global tectonics operating through continental subduction, collision, exhumation, mantlelithospheric slab interactions, and geochemical recycling of subducted/exhumed rocks. Comprehensive review articles and special issues related to UHP metamorphism and plate tectonics are published almost every year (Ernst & Liou, 2000, 2008; Chopin, 2003; Liou et al., 2004; Green, 2005; Ernst et al., 2007; Zhang et al., 2007; Guillot et al., 2008; Liou et al., 2009a; Beltrando et al., 2010). They provide valuable summaries of existing knowledge, outline future directions, and discuss controversial concepts. These papers also summarized recent progress in experimental determination of PT stability fields of new phases, phase transformations of those minerals which were known before to be stable only at shallow depths of the continental crust, and they reported that the exsolution products of UHPM minerals indicate that continental rocks were subducted to depths exceeding 100250 km. Extensive research in UHP metamorphic rocks led to new constraints and the improvement of many geotectonic models developed for very deep subduction of continental rocks and their exhumation within many well-known orogenic belts. Numerical geodynamic modeling of subduction and exhumation became a powerful tool for understanding mantle dynamics and global continental subduction (Gerya, 2010).
dcterms:title
Frontiers of Ultrahigh-Pressure Metamorphism: View from Field and Laboratory Frontiers of Ultrahigh-Pressure Metamorphism: View from Field and Laboratory
skos:prefLabel
Frontiers of Ultrahigh-Pressure Metamorphism: View from Field and Laboratory Frontiers of Ultrahigh-Pressure Metamorphism: View from Field and Laboratory
skos:notation
RIV/00216208:11310/11:10107986!RIV12-GA0-11310___
n5:predkladatel
n6:orjk%3A11310
n3:aktivita
n10:Z n10:P
n3:aktivity
P(GAP210/10/0249), Z(MSM0021620855)
n3:dodaniDat
n4:2012
n3:domaciTvurceVysledku
n24:6555470
n3:druhVysledku
n22:C
n3:duvernostUdaju
n12:S
n3:entitaPredkladatele
n11:predkladatel
n3:idSjednocenehoVysledku
200456
n3:idVysledku
RIV/00216208:11310/11:10107986
n3:jazykVysledku
n21:eng
n3:klicovaSlova
Laboratory; Field; View; Metamorphism; Ultrahigh-Pressure; Frontiers
n3:klicoveSlovo
n15:Frontiers n15:Metamorphism n15:Field n15:Laboratory n15:View n15:Ultrahigh-Pressure
n3:kontrolniKodProRIV
[047F3E454047]
n3:mistoVydani
USA
n3:nazevEdiceCisloSvazku
Neuveden
n3:nazevZdroje
Ultrahigh-Pressure Metamorphism 25 Years After the Discovery of Coesite and Diamond
n3:obor
n19:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetStranKnihy
670
n3:pocetTvurcuVysledku
2
n3:projekt
n23:GAP210%2F10%2F0249
n3:rokUplatneniVysledku
n4:2011
n3:tvurceVysledku
Faryad, Shah Wali Dobrzhinetskaya, Larissa
n3:zamer
n8:MSM0021620855
s:numberOfPages
40
n20:doi
10.1016/B978-0-12-385144-4.00020-5
n16:hasPublisher
Elsevier
n18:isbn
978-0-12-385144-4
n13:organizacniJednotka
11310