Abstract:By means of the field geological and geomorphological investigation combined with UAV aerial photography survey, geological radar exploration and shallow seismic exploration, we comprehensively reckon that the eastern margin fault of Jinshan uplift extends with the strike of 40° in a whole, starting from the northern Xinkou village, extending to the southwest through the western Jinshanpu village and western Qianyuni village, and turning to the SWS and into the basin area around northern Buluo village. Through trenching and chronology tests, we think the fault latestly misplaced the early Late Pleistocene strata.
HU Guirang,YAN Xiaobing,LIANG Ruiping et al. The Extension and Latest Activity characteristic in Late Quaternary of the Eastern Margin Fault of Jinshan Uplift in Xinding Basin[J]. jgg, 2024, 44(6): 606-610.