1、
银根 - 额济纳旗盆地是中新生界陆相盆地, 前中生界构成盆地基底.
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2、
Weibei Basin is a Mesozoic Cenozoic basin developed in the Tanlu fault zone.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地.
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3、
Cenozoic tectonic activities are controlled by the eastward propagation of Tibetan Plateau uplift.
新生代的构造活动受制于青藏高原抬升作用向东扩展的影响.
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4、
Through long terms of tectonic evolutions, it changed into a transform fault in the Cenozoic Era.
经长期构造演化于新生代转变为转换断层.
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5、
讨论了黄骅坳陷横向变换带的构造特征和成因.
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