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dc.contributor.author Wilding, Martin C.
dc.contributor.author Benmore, C. J.
dc.date.accessioned 2008-12-09T14:57:42Z
dc.date.available 2008-12-09T14:57:42Z
dc.date.issued 2006-01
dc.identifier.citation Wilding , M C & Benmore , C J 2006 , ' Structure of glasses and melts ' Reviews in Mineralogy and Geochemistry , vol 63 , no. 1 , pp. 275-311 . , 10.2138/rmg.2006.63.12 en
dc.identifier.issn 1529-6466
dc.identifier.other PURE: 89508
dc.identifier.other dspace: 2160/1488
dc.identifier.uri http://hdl.handle.net/2160/1488
dc.identifier.uri http://www.minsocam.org/MSA/Rim/RiM63_Ch_12_Wilding.pdf en
dc.description Wilding, M. C., Benmore, C. J. (2006). Structure and Glasses and Melts. reviews in Mineralogy and Geochemistry, 63 (1), 275-311 RAE2008 en
dc.description.abstract The liquid state dominates terrestrial and planetary processes. The history of the early solar system for example involved the accretion of primarily molten bodies. In cooler temperature regimes, interplanetary dust, comets and the moons and planets in the outer part of the solar system are dominated by ices which may be present in liquid or amorphous forms (Cernicharo and Crovisier 2005; Porco et al. 2005a,b). The interior of the Earth and terrestrial planets are dominated by magnesium silicate minerals, a reflection of separation of iron dominated liquids from chondrite composition planetesimals (Poirier 2000). Subsequently planets evolved through segregation, crystallization and volcanic activity; all dominated by liquid state processes. The oceanic and continental crust, while compositionally distinct form the mantle is dominated by liquid state processes, the oceanic crust resulting from basaltic volcanism. Hydrothermal processes are important agents for geochemical processes in the Earth’s crust and also, according to recent surveys on Mars (Neukum et al. 2004; Bullock 2005; Newsom 2005). en
dc.format.extent 37 en
dc.language.iso eng
dc.relation.ispartof Reviews in Mineralogy and Geochemistry en
dc.title Structure of glasses and melts en
dc.type Text en
dc.type.publicationtype Article (Journal) en
dc.identifier.doi http://dx.doi.org/10.2138/rmg.2006.63.12
dc.contributor.institution Institute of Mathematics & Physics (ADT) en
dc.contributor.institution Materials Research en
dc.description.status Peer reviewed en


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