前述各种特征则可能是此类构造反转盆地所具有的特殊的地质构造现象。
The above mentioned characteristics may be the special geotectonic phenomena which only this kind of inversion basin has.
以地表地质和勘探地震资料为基础，对洛阳盆地的负反转构造进行了研究。
The negative inverted structure in Luoyang basin is studied on the basis of geological data and prospecting seismic data.
早—中侏罗世研究区处于一种张扭构造环境之中，晚侏罗世盆地发生明显抬升和反转。
The study area was in a tectonic setting of transtension during Early and Middle Jurassic, and the basins were reversed and uplifted in Late Jurassic.
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