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- W2362863912 abstract "There occur Cenozoic volcanic rocks of two ages in the Canmei Mountain area, northern Tibet: Pliocene granite-porphyry or rhyolitic-porphyry with a muscovite K-Ar age of 3.65±0.31 Ma and Miocene trachydacite, trachyandesite and basaltic trachyandesite with whole-rock K-Ar ages of 12.81±0.4, 12.85±0.56 and 14.51±0.23 Ma respectively. The Miocene surface morphology during volcanic eruption is recovered according to the altitude of the overlying surface around the various volcanic lavas and the altitude of the top of the highest local mountain made up of non-volcanic rocks. It may be completely correlated with the modern planation surface morphology. On that basis, combined with the development of the paleo-crust of weathering below the volcanic lavas, it is thought that the surface below the volcanic lavas in the Canmei Mountain area is the paleo-planation surface and that the study area is a remnant area of paleo-planation surface." @default.
- W2362863912 created "2016-06-24" @default.
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- W2362863912 date "2004-01-01" @default.
- W2362863912 modified "2023-09-23" @default.
- W2362863912 title "Ages of volcanic rocks and planation surface in the Canmei Mountain area, northern Tibet" @default.
- W2362863912 hasPublicationYear "2004" @default.
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