New Red Sandstone
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The Triassic system was deposited inside the mountains of Central Europe during the Variscan orogeny. It is mainly composed of continental deposits characterized by red sandstone and pebble rocks formed in an arid climate, and is sandwiched between shallow marine deposits. It is called the New Red Sandstone in contrast to the Old Red Sandstone from the Devonian Caledonian orogeny. In a broad sense, it is also used to refer to similar deposits from the same period in various places. Source : Heibonsha Encyclopedia About MyPedia Information |
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中部ヨーロッパのバリスカン造山運動による山脈の内側に堆積した三畳系。乾燥気候のもとで形成された赤色の砂岩・レキ岩を特徴とする陸成層を主とし，浅海成層をはさむ。デボン紀のカレドニア造山運動による旧赤色砂岩に対し新赤色砂岩と呼ばれる。広義には各地の同じ時期の同様の堆積層に対しても使用。
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