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• W2023044218 endingPage "188" @default.
• W2023044218 startingPage "171" @default.
• W2023044218 abstract "The effects of collision between three major plates define the geological development of eastern Indonesia. Garnet peridotite and associated granulite-facies contact rocks are described from two sites within the valley of the active Palu-Koro left-lateral, strike-slip fault crossing central Sulawesi. Disrupted parts of a medium- to low-grade metamorphic complex intruded by Neogene granite occur on both sides of the fault. Thermobarometry on minerals and fluids in the garnet peridotite reveals a re-equilibration path from a depth of 60 km upward. Chemistry points to metasomatic effects — isolated trace-element enrichment — by a CO2-rich liquid and fluid in a peridotite of oceanic affiliation. The granulite shows an increase in T and incipient melting at the arrival of peridotite. The sequence of fluid inclusions of an evolving CO2CH4(N2)H2O-bearing fluid defines a concave decompression path suggesting rapid uplift. Trace element chemistry of granulite with basaltic to peraluminious rhyolitic composition indicates island-arc affinity. The described history may well reflect the processes beneath a mantled gneiss dome, present as a coeval metamorphic aureole around the garnet peridotite outcrops." @default.
• W2023044218 created "2016-06-24" @default.
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• W2023044218 date "1990-11-01" @default.
• W2023044218 modified "2023-09-26" @default.
• W2023044218 title "Garnet peridotite and associated high-grade rocks from Sulawesi, Indonesia" @default.
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• W2023044218 doi "https://doi.org/10.1016/0024-4937(90)90013-q" @default.
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