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- W2044042886 abstract "An unexpected microstructure, with important implications for melt distribution in the upper mantle, has been found in a 70% olivine +30% orthopyroxene rock experimentally deformed at 1500K, 300 MPa, where incipient partial melting occurred. As found in previous studies of comparable systems, most melt in the olivine-orthopyroxene sample resided in a network of grain-edge tubes and occasional thick (50–500 nm) layers. We infer, using electron microscopy at its highest resolution, that melt also existed in another form as glass films 1.0–1.5 nm thick, along all grain boundaries, with total film fraction (F) of 0.0002. All of these melts are unusually SiO2-rich. Further work is needed to confirm that the thin films are not transient, although their coexistence with smoothly curved solid-melt interfaces and flat crystal faces suggests they are stable. If thin high-silica melt films are stable they might influence physical properties and melt extraction processes in regions of incipient melting and metasomatism in the upper mantle." @default.
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- W2044042886 date "1996-04-01" @default.
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- W2044042886 title "Grain boundary melt films in an experimentally deformed olivine-orthopyroxene rock: Implications for melt distribution in upper mantle rocks" @default.
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- W2044042886 doi "https://doi.org/10.1029/96gl00702" @default.
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