000 02375nam a22004695i 4500
001 978-3-642-15588-8
003 DE-He213
005 20140220084546.0
007 cr nn 008mamaa
008 101029s2010 gw | s |||| 0|eng d
020 _a9783642155888
_9978-3-642-15588-8
024 7 _a10.1007/978-3-642-15588-8
_2doi
050 4 _aQE351-399.2
072 7 _aPNV
_2bicssc
072 7 _aSCI048000
_2bisacsh
082 0 4 _a549
_223
100 1 _aGrapes, Rodney.
_eauthor.
245 1 0 _aPyrometamorphism
_h[electronic resource] /
_cby Rodney Grapes.
250 _a2.
264 1 _aBerlin, Heidelberg :
_bSpringer Berlin Heidelberg :
_bImprint: Springer,
_c2010.
300 _aXI, 365p. 269 illus.
_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 _uhttp://dx.doi.org/10.1007/978-3-642-15588-8
912 _aZDB-2-EES
999 _c112675
_d112675