MARC Record from harvard_bibliographic_metadata

LEADER: 02291nam a22004695a 4500
001 013835247-X
005 20131206200326.0
008 121227s1994 ne | s ||0| 0|eng d
020 $a9789401111065
020 $a9789401111065
020 $a9789401044837
024 7 $a10.1007/978-94-011-1106-5$2doi
035 $a(Springer)9789401111065
040 $aSpringer
050 4 $aQE351-399.2
072 7 $aPNV$2bicssc
072 7 $aSCI048000$2bisacsh
082 04 $a549$223
100 1 $aParsons, Ian,$eeditor.
245 10 $aFeldspars and their Reactions /$cedited by Ian Parsons.
264 1 $aDordrecht :$bSpringer Netherlands :$bImprint: Springer,$c1994.
300 $aXXX, 650 p.$bonline resource.
336 $atext$btxt$2rdacontent
337 $acomputer$bc$2rdamedia
338 $aonline resource$bcr$2rdacarrier
347 $atext file$bPDF$2rda
490 1 $aNATO ASI Series, Series C: Mathematical and Physical Sciences,$x1389-2185 ;$v421
520 $aFeldspar minerals make up 60% of the crust of the Earth. They are stable in the upper mantle, and are so abundant in the crust that they form the basis of the classification of igneous rocks. At the surface, feldspars weather to form clay minerals which are the most important mineral constituent of soils. The articles in this book review the chemical reactions of feldspars over the whole sweep of pressure and temperature regimes in the outer Earth, and describe the fundamental aspects of crystal structure which underlie their properties. The book covers intracrystalline reactions, such as order-disorder transformations and exsolution, and transfer of stable and radiogenic isotopes, which can be interpreted to provide insights into the thermal history of rocks. It is suitable for final year undergraduates or research workers.
650 20 $aChemistry, Inorganic.
650 20 $aCrystallography.
650 20 $aGeochemistry.
650 20 $aMineralogy.
650 10 $aEarth sciences.
650 0 $aGeography.
650 0 $aChemistry, inorganic.
650 0 $aGeochemistry.
650 0 $aMineralogy.
650 0 $aCrystallography.
776 08 $iPrinted edition:$z9789401044837
830 0 $aNATO ASI Series, Series C: Mathematical and Physical Sciences ;$v421.
988 $a20131114
906 $0VEN