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《SEISMOLOGY AND GEOLOGY》 2000-01
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THE FISSION TRACK EVIDENCE OF HUASHAN BATHOLITH UPLIFTING IN MESOZOIC-CENOZOIC

Wan Jinglin Li Qi Wang Yu ( Institute of Geology, China Seismological Bureau, Beijing 100029 )  
Apatite minerals separated from samples that were collected from elevations of 520m to 1 950m on the Huashan batholith, yielded fission track ages of (20 59±3 6)Ma to (29 26±3 3)Ma. The data suggest an uplift rate of 0 019 to 0 189mm/a. One zircon mean fission track age of (43 45±2 7) Ma also suggests that the Huashan batholith started to uplift in early E 2. We infer that there is a sub normal fault developed in north part of the Huashan batholith.
【CateGory Index】: P542.2
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