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Penninic thrustfront : ウィキペディア英語版 | Penninic thrustfront
The Penninic thrustfront is a major tectonic thrustfront in the French Alps. The thrustfront moves over a developing decollement horizon, and separates the (internal) high grade metamorphic rocks of the Penninic nappes from the (external) sedimentary rocks and crystalline basement of the Helvetic nappes. The last are in France often called ''zone Dauphiné'' or ''Dauphinois''. Thrusting over the decollement horizon continues today, as the Apulian tectonic plate moves westward, converging with the European plate.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Penninic thrustfront」の詳細全文を読む
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