SPINMELT-2.0: Simulation of Spinel-Melt Equilibrium in Basaltic Systems under Pressures up to 15 Kbar: I. Model Formulation, Calibration, and Tests

被引:16
|
作者
Nikolaev, G. S. [1 ]
Ariskin, A. A. [1 ,2 ]
Barmina, G. S. [1 ]
机构
[1] Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem GEOKHI, Moscow 119991, Russia
[2] Moscow MV Lomonosov State Univ, Geol Fac, Moscow 119234, Russia
基金
俄罗斯科学基金会; 俄罗斯基础研究基金会;
关键词
Cr-spinel-melt equilibrium; geothermometer; MELTS; SPINMELT; MELT-CHROMITE; basalt; MEDICINE LAKE VOLCANO; IRON-RICH MANTLE; PHASE-EQUILIBRIA; OXYGEN FUGACITY; EXPERIMENTAL CONSTRAINTS; MIDOCEAN RIDGE; ORTHO-PYROXENE; PETROGENETIC INDICATORS; CHROME-SPINEL; H2O CONTENTS;
D O I
10.1134/S0016702918010044
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The paper presents results of testing currently used models proposed to describe Cr-spinel-melt equilibrium: models of the MELTS family by M.S. Ghiorso with colleagues, the SPINMELT program by A.A. Ariskin and G.S. Nikolaev, and the "MELT-CHROMITE spinel calculator" by A.A. Pustovetov and R.L. Roeder. The new calibration of the SPINMELT model presented in this publication enables calculating a six-component (Mg, Fe2+, Cr, Al, Fe3+, and Ti) composition of Cr-spinel and the T-fo(2) parameters of its stability on the liquidus of basaltic melts under pressures up to 15 kbar. The model is based on results of 392 runs from 43 experimental studies, including systems of normal alkalinity fo(2) <= QFM + 2. The experimental dataset (which was extended compared to that used for the previous calibration) allowed us not only to estimate the pressure effect, but also apply the model to aluminous and hydrous systems. Tests of the SPINMELT-2.0 model show that the errors of the calculated temperature of the spinel-melt equilibrium increase with pressure from 16 degrees C at 1 atm to 50 degrees C at 15 kbar. Experimental spinel compositions are reproduced by the model accurate to < 3 at % Al and Cr, and no worse 1 at % for the other cations.
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页码:24 / 45
页数:22
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