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逆冲断层The Thrust Fault
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逆冲断层The Thrust Fault

晚古生代灰白色中厚层状灰岩逆冲在三叠纪薄板状灰岩(植被掩盖)之上。断层面倾向南,倾角40°±。大约距今2.99亿年至2.52亿年。

  In late Paleozoic gray thick bedded limestone thrustedon Triassic laminated limestone (vegetation cover). The tendency of fault is south and the dip is 40°of thrust plane. Approximately 299 to 252 million years ago.

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