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- W2327673847 abstract "Sequences of ancient end moraines are evidence that successively smaller ice sheets centred on the Patagonian Andes developed during successive Quaternary glaciations. At Torres del Paine (51°S, 73..." @default.
- W2327673847 created "2016-06-24" @default.
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- W2327673847 date "1994-12-01" @default.
- W2327673847 modified "2023-09-28" @default.
- W2327673847 title "Factors Affecting the Volume of Quaternary Glacial Deposits in Southern Patagonia" @default.
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- W2327673847 doi "https://doi.org/10.1080/04353676.1994.11880423" @default.
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