这种应力场特征与上述阶段形成的盆地原型、盆地反转、构造变形相匹配。
This tectonic stress field feature is consistent with the basin prototype, basin reversal and tectonization forming in the relevant period.
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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