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A Mesoproterozoic continental flood rhyolite province, the Gawler Ranges, Australia: the end member example of the Large Igneous Province clan
Mesoproterozoic continental fl ood rhyolite province Gawler Ranges
2014/12/31
Rhyolite and dacite lavas of the Mesoproterozoic upper Gawler Range Volcanics (GRV) (>30 000 km3
preserved), South Australia, represent the remnants of one
of the most voluminous felsic magmatic eve...
Thermochemistry and the enthalpy of formation of synthetic end-member (CaTiSiO5) titanite
Thermochemistry formation synthetic end-member CaTiSiO5 titanite
2012/4/5
Theenthalpyofdropsolutionofaquicklyquenched,clear,titaniteglasssampleandseveralsynthetic,polycrystalline,sampleswasmeasuredinaCalvet-typecalorimeterin2PbO!/
O solventat702C.Theenthalpyofformationofst...
Synthesis methods and unit-cell volume of end-member titanite (CaTiOSiO4)
Synthesis methods unit-cell volume end-member titanite CaTiOSiO4
2012/4/5
Unit-cellparametersofsynthetic,end-membertitanite(CaTiOSiO )criticallydependonthesynthesisconditions,asisshownforstudiesreportedintheliteratureandfornew
samplesreportedhere.Ourstudysuggeststhatphase-...
Parameterization of energy and interactions in garnets: End-member properties
Parameterization of energy interactions garnets End-member properties
2012/4/5
Wepresent results ofstatic lattice energy and vibrational energy calculations for the 12 garnet end-members in the system (Ca,Mg,Mn,FeMAl,Cr,Fe)2Si3012' The structure ofthe end-member phases wasfirst ...
The crystal structure of nanpingite-2M2, the CS end-member of muscovite
crystal structure nanpingite-2M2 CS end-member of muscovite
2012/4/5
Nanpingite, ideally CsA12(AlSi3)OIO(OH)2,is a Csend-member dioctahedral mica,crys-tallizing in C21c,witha =9.076(3), b= 5.226(2), c =21.41(5) A,and (3
=99.48(6)°. The crystal structure of type nanpin...
Chemistry of Illite/Smectite and End-Member Illite
Bentonite Chemical composition Diagenesis Illite Illite/smectite Smectite
2012/1/12
Chemical data from three different series of diagenetic illite/smectites (I/S), analyzed statistically by two regresion techniques, indicate that the content of fixed-K per illite layer is not constan...