Geochemical Partitioning in Till

نویسنده

  • W. W. Shilts
چکیده

and Vagners (1971, 1972) expressed this phenomenon elegantly by introducing the concept of "terminal mode" for the optimum grain size to which a mineral can be reduced, given the force and energy typically available in the glacial environment. Thus, hard, uncleaved or poorly cleaved minerals such as quartz, fcldspar, garnet, pyrite and magnetite dominate either the medium or the fine sand fraction of glacial sediments, depending on their grain size in the source rocks; calcite, dolomite and gypsum have their terminal modes in the silt sizes because of their softness or good clcavage; clay minerals, micas and other phyllosilicates, serpentine, and hematite, because of their excellent cleav-

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تاریخ انتشار 2002