000 02339nam a22004575i 4500
001 u375074
003 SIRSI
005 20160812084306.0
007 cr nn 008mamaa
008 101029s2010 gw | s |||| 0|eng d
020 _a9783642155888
_9978-3-642-15588-8
040 _cMX-MeUAM
050 4 _aQE351-399.2
082 0 4 _a549
_223
100 1 _aGrapes, Rodney.
_eauthor.
245 1 0 _aPyrometamorphism
_h[recurso electrónico] /
_cby Rodney Grapes.
250 _a2.
264 1 _aBerlin, Heidelberg :
_bSpringer Berlin Heidelberg :
_bImprint: Springer,
_c2010.
300 _aXI, 365 p.
_bonline resource.
336 _atext
_btxt
_2rdacontent
337 _acomputer
_bc
_2rdamedia
338 _aonline resource
_bcr
_2rdacarrier
347 _atext file
_bPDF
_2rda
505 0 _aThermal Regimes and Effects -- Quartzofeldspathic Rocks -- Calc-Silicates and Evaporates -- Mafic Rocks -- Anthropogenic and Biomass Pyrometamorphism -- Metastable Mineral Reactions.
520 _a1000 °C) and low pressures (< 2 kb) and typically results in the formation of "burnt" and fused rocks termed buchites, paralavas, clinkers and fulgarites. It is typically associated with shallow basaltic intrusions (contact aureoles, xenoliths,) combustion of carbonaceous matter, lightning strikes, and is also found in meteorites. During pyrometamorphism, the sequence of heating and cooling is greatly condensed favouring the preservation of a variety of stranded reaction microstructures that reflect disequilibrium reaction kinetics with metastable and mineral crystallisation. This second edition includes the latest developments in the study of pyrometamorphism derived from over 60 new references and accompanied with over 20 new illustrations.
650 0 _aGeography.
650 0 _aGeochemistry.
650 0 _aMines and mineral resources.
650 0 _aMineralogy.
650 1 4 _aEarth Sciences.
650 2 4 _aMineralogy.
650 2 4 _aMineral Resources.
650 2 4 _aGeochemistry.
710 2 _aSpringerLink (Online service)
773 0 _tSpringer eBooks
776 0 8 _iPrinted edition:
_z9783642155871
856 4 0 _zLibro electrónico
_uhttp://148.231.10.114:2048/login?url=http://link.springer.com/book/10.1007/978-3-642-15588-8
596 _a19
942 _cLIBRO_ELEC
999 _c202954
_d202954