WAN Jinglin1, 2 WANG Yu3 LI Qi1 ZHENG Dewen1 LI Daming1 1. Apatite fission track study of Taibai Mountain uplift in the Mesozoic-Cenozoic[J]. Nuclear techniques, 2005, (9): 712-716.
WAN Jinglin1, 2 WANG Yu3 LI Qi1 ZHENG Dewen1 LI Daming1 1. Apatite fission track study of Taibai Mountain uplift in the Mesozoic-Cenozoic[J]. Nuclear techniques, 2005, (9): 712-716.DOI:
Apatite fission track study of Taibai Mountain uplift in the Mesozoic-Cenozoic
The apatite fission track results of 14 samples from Taibai Mountain suggest that Taibai Mountain underwent two episodic uplifts. These two uplifts occurred at about 100-80Ma and 40Ma
respectively. These are consistent with the conclusion that Qinling Mountain changed to a new tectonic evolution phase since about late Cretaceous
and this evolution resulted in the basic tectonic geomorphologic pattern of Qinling Mountain.