Major Alpine overthrust in the Tschingelhorner in the Grison Alps, Switzerland. The rocks above the prominent thrust fault are conglomerates of Permian age, whereas below is highly deformed limestone of Mesozoic age and flysch of Cenozoic age. The rock window is the famous Martinsloch between the towns of Flims and Elm.
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Creative#:
TOP25487949
Source:
達志影像
Authorization Type:
RM
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須由TPG 完整授權
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No
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