临汾盆地北起韩侯岭，向南至侯马折而向西直至黄河岸，盆地东西两侧分别以霍山大断层、罗云山，韩城大断层与山地相接，南部与峨嵋台地相接。
本研究选择的三个全新世黄土剖面位于临汾盆地中部陶寺地区，其中DPG剖面位于塔儿山古洪积扇前沿，TSC剖面和LGK剖面位于与古洪积扇相连的汾河4级阶地。
DPG profile lies in the front of the palaeo-alluvial-pluvial fans of Ta'ershan hill, and TSC and LGK profiles on the 4th terrace of Fenhe River.
本文首先运用卫星影像，对临汾—运城盆地中主要活动断层的平面展布状况进行了解译。
In this paper, at first, the plane distribution of main active faults in the Basin of Linfen-Yuncheng are interpreted by satellite imagery.
东亢矿泉水处于临汾断陷盆地边缘山前地带。
Dongkang mineral water is Located at the edge of Linfen faulted basins.
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