Melting in the Sub-Arc Mantle: The Effects of H2O on Primary Magmas and the Spinel-to-Garnet Transition
Melting in the Sub-Arc Mantle: The Effects of H2O on Primary Magmas and the Spinel-to-Garnet Transition
复制标题
弧下地幔的熔化:H2O 对原生岩浆和尖晶石到石榴石转变的影响
DOI:
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发表时间:
1994
期刊:
影响因子:
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通讯作者:
G. Gaetani
中科院分区:
文献类型:
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作者:
G. Gaetani
In subduction zone settings H20 plays an important role in the melt generation process. The effects of H20 are likely to be complex in a dynamic melting environment, because H20 contents will vary continuously with increasing degree of melting. In order to model the melting process, a quantitative understanding of the role of variable H20 content and variable mantle residue composition must be developed. The model must be capable of recovering liquidus temperatures and compositions of melts saturated with a mantle residual assemblage of olivine + orthopyroxene + clinopyroxene _ spinel _.+ amphibole _ garnet (primary magmas) as a function of pressure and H20 content. Equally important is understanding the effect of H20 on the stability of mantle phases under various pressure-temperature conditions. Recent experimental work indicates that the presence of H20 stabilizes garnet to lower pressures in mantle peridotlte (Gaetani and Grove, 1993). Here we report the results of H20-undersaturated melting experiments performed at 10-16 kbar. These experiments were designed to determine the temperature of the H20-undersaturated liquidus of primary maLmaas over a range of pressures, and the compositions of mantle melts containing 6 wt% H20. Further, the results can be used to constrain the pressure at which the spinel-togarnet transition occurs in the mantle under hydrous conditions.