上新世-中新世地层 Plio-Miocene beds
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本区具有出露良好的中新世地层。
Miocene formations (better: strata) are well-exposed in this area.
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中新世以来,双河组(N1s)地层的褶皱走向为NE向,此期间盆缘主断裂变为左旋逆推性质;
Since the Miocene, the fold in the Shuanghe group (N1s) stroke in NE when the main fault on the basin rim changed into sinistral thrust.
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