搜索结果: 1-10 共查到“矿床学与矿相学 Melt”相关记录10条 . 查询时间(0.093 秒)
High-pressure X-ray diffraction study on the structure of NaCl melt using synchrotron radiation
NaCl high-pressure X-ray synchrotron radiation
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2012/3/30
MoltenNaClwasanalyzedbyhigh-pressureX-raydiffractionexperimentsusingsyn-
chrotronradiationupto5GPaand1600Calongthemeltingcurve.Theinterference
function Qi(Q)andthecorrelationfunction g(r)werederived...
Systematics of Ni and Co in olivine from planetary melt systems: Lunar mare basalts
planetary melt systems:Luna rmare basalts Co Ni
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2012/3/31
ThesystematicsofCoandNiinolivinefromsixApollo12olivinebasaltswerestudied
bySIMStechniquesandcorrelatedwithmajorandminorelementdataobtainedwiththe
electronmicroprobe.Ourresults,togetherwithpreviousst...
Melt viscosities in the system Na-Fe-Si-O-F-Cl: Contrasting effects of F and Cl in alkaline melts
Melt viscosities Na-Fe-Si-O-F-Cl alkaline melts
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2012/4/1
The shear viscosities of melts in the system Na-Fe-Si-O-F-Cl were determined over a wide range of temperatures (400–1200 8 C) at 1 atm pressure in air. The compositions are based on the addition of Fe...
Heterogeneous crystal nucleation on bubbles in silicate melt
Heterogeneous crystal nucleation bubbles silicate melt
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2012/4/1
Experiments reported herein document heterogeneous crystal nucleation on bubbles in supercooled lithium disilicate melt. Crystalline lithium disilicate (Li2Si2O5) nucleated and grew on small bubb...
Temperature dependence of the OH- absorption in the SiO2 glass and melt to 1975 K
Temperature dependence OH- absorption SiO2 glass
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2012/3/31
FTIR absorbance spectra of SiO2 glass containing 1200 ppm OH2 groups were recorded in situ to 1975 K. There are only minor changes in peak height to 1700 K, indicating that the molar extinction coeffi...
Minor and trace element partitioning between pyroxene and melt in rapidly cooled chondrules
Minor trace element partitioning pyroxene melt rapidly cooled chondrules
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2012/4/5
Wepresentminorandtraceelement(REE,Sr,Y,andZr)dataforpyroxenesandme-
sostasesinfourporphyriticchondrulesfromtheSemarkonaordinarychondrite.Apparent
partitioncoef?cientsforclinoenstatite,orthoenstatite...
The influence of H2O on the viscosity of a haplogranitic melt
H2O haplogranitic melt
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2012/4/6
The viscosity T/of dry and hydrous haplogranitic melts(anhydrous normative compo-sition: QZ28Ab340r38)has been determined between 3and 10kbar and 800 and 1400 DC using the falling-sphere method. The H...
Morphology and maturation of melt inclusions in quartz phenocrysts in afrom the Badlands rhyolite lava flow, southwestern Idaho
Morphology maturation of melt inclusions phenocrysts Badlands rhyolite lava flow southwestern Idaho
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2012/4/5
Morphologiesofprimary rhyolitic meltinclusions in three successive populations of quartz phenocrysts in asinglevolcanic unit illustrate the changeofinclusion shape after trapping. The 14MaBadlandslava...
Granitic melt viscosities: Empirical and configurational entropy models for their calculation
Granitic melt viscosities entropy models calculation
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2012/4/5
Newly measured viscosities ofa low H20-content granitic meltand a low H20-content albitic melthave been combined withviscosity data from the literature to create two new modelsfor the calculation ofgr...
Cooling Rate Dependency of the Formation of Smectite Crystals from a High-Pressure and High-Temperature Hydrous Melt
High pressure experiment Quenching rate Smectite crystals
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2011/12/28
The effect of cooling rate on the formation of smectite crystals with high crystallinity was investigated using two different types of high-pressure and high-temperature apparatus, a modified belt typ...