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Regional geological structure

2015-03-23 11:49 | Author:gzzjd | Reading:amount |


 Regional geological structure
The geopark is located in the north side of Nanling tectonic zone that strikes EW. Within the area,the tectonic line and stratum generally strike NE, the structural deformation of stratum mainly occurred in Yanshan Epoch, and the intermittent bulge
is the overall reflection of Neotectonic movement.
Within the geopark area, anticline distributes with syncline in an alternative mode.From Chenjiazhai syncline in the northwest boundary to SE direction,there are Zhijin anticline, Taoshuwan syncline, Diaobian anticline and Lujiadu syncline, etc. Their axis all strike NE-SW, and they are dominant structures and control the movement and direction of regional underground rivers and surface rivers. For example, upstream and downstream of Qijiehe River are respectively controlled by
Diaobian syncline and Zhijin syncline.
Faults develop intensively in the geopark area, and many faults,like Qijiehe River fault, belong to primary structure.They are distributed over limbs of Taoshuwan anticline, belong to compressoshear and piezotropy reverse fault, and their strike is in consistent with the folds.Areas of bare rock, fissures are found everywhere, and they primarily strike NEE, NWW, NNE and near SN. Meanwhile, the effluent fissures
mainly strike SN, NE and NW.
 


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