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Thiviers-Payzac Unit : ウィキペディア英語版 | Thiviers-Payzac Unit The Thiviers-Payzac Unit is a metasedimentary succession of late Neoproterozoic and Cambrian age outcropping in the southern Limousin in France. The unit geologically forms part of the Variscan basement of the northwestern Massif Central. == Terminology == The Thiviers-Payzac Unit, sometimes still called ''Thiviers-Payzac Nappe'' or ''Bas-Limousin Group'', was named after Thiviers and Payzac, two small towns in the northeastern Dordogne situated within the unit's outcrop area. The term nappe is somewhat misleading.
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「Thiviers-Payzac Unit」の詳細全文を読む
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