作者: Andrew C. Morton , Claire Hallsworth
DOI: 10.1016/S0070-4571(07)58007-6
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摘要: Detrital heavy-mineral assemblages respond to increasing burial diagenesis by progressive dissolution of unstable components. Case studies from sedimentary basins worldwide show a uniform pattern of relative stability. The order of stability during burial diagenesis is olivine (least stable)< orthopyroxene, clinopyroxene< sodic pyroxene< calcic amphibole, andalusite, sillimanite< epidote< titanite< kyanite< sodic amphibole< staurolite< allanite< garnet, chloritoid< tourmaline, monazite, spinel< rutile, anatase, brookite, zircon, apatite …