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This document summarizes research on geochemical indicators of source lithology and weathering intensity in fine-grained Permian sediments from the central Transantarctic Mountains. Aluminum oxide to titanium oxide ratios indicate source rocks ranging from diorite to granodiorite on average. Chemical alteration indices show increasing weathering upward from glacial to chemical regimes. Both proxies vary spatially, suggesting changing source area compositions and weathering styles over time and space during

Author

Amritzal Nur

Language

EN