获得了相应地区断层陡坎的一些资料和距今2700年左右形成的断层陡坎回归方程。

And some relevant geologic data regression equations for fault scarp formed in the past 2700 years have been obtained.

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这些被称为“叶状陡坡”的有趣的地貌特点是在月球一度融化的内核开端冷却的进程中形成的断层，这一进程使得月球表面产生压缩，并呈现褶皱。

The intriguing features, called lobate scarps, are faults created when the Moon's once-molten interior began to cool, causing the lunar surface to contract and then crinkle, they said.

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矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。

The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.

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