This study is supported by grants from the National Basic Research Program of China (973 Program, No.2007CB411301) and the Natural Science Foundations of China (No. 40573038 and No. 40472112).
Although many authors have emphasized the Cenozoic history of deformation, exhumation and cooling in the Tianshan area related to the India-Asia collision, very little is known about the Mesozoic history of compression and uplift within the Tianshan. In order to obtain information about the Mesozoic exhumation history and processes of cooling in eastern Tianshan, fission track methods on apatite were used. Sampling was made in the Jueluotage Range. Three samples (Z001–Z003) were taken from granite in borehole ZK6301 of Yandong pluton; the ages range from 97.0 to 87.6 Ma that are much younger than the pluton age which was dated by U-Pb zircon at 334±2 Ma. Two samples in northern piedmont of the Jueluotage Range were collected from Jurassic strata in Dikaner (DK001) and Dananhu (D001) whose ages are 91.5 and 93.4 Ma respectively. The average apparent exhumation rate is 0.039 mm/a calculated by extrapolation on the basis of Yandong samples, indicating an extremely slow exhumation in the Jueluotage Range since the Late Cretaceous. Two Jurassic samples reached the maximum depths after deposition and experienced the maximum temperatures of ca. 105 and 108°C until the late Early Cretaceous before a period of cooling and exhumation occurred at 114 and 106 Ma.
Although many authors have emphasized the Cenozoic history of deformation, exhumation and cooling in the Tianshan area related to the India-Asia collision, very little is known about the Mesozoic history of compression and uplift within the Tianshan. In order to obtain information about the Mesozoic exhumation history and processes of cooling in eastern Tianshan, fission track methods on apatite were used. Sampling was made in the Jueluotage Range. Three samples (Z001–Z003) were taken from granite in borehole ZK6301 of Yandong pluton; the ages range from 97.0 to 87.6 Ma that are much younger than the pluton age which was dated by U-Pb zircon at 334±2 Ma. Two samples in northern piedmont of the Jueluotage Range were collected from Jurassic strata in Dikaner (DK001) and Dananhu (D001) whose ages are 91.5 and 93.4 Ma respectively. The average apparent exhumation rate is 0.039 mm/a calculated by extrapolation on the basis of Yandong samples, indicating an extremely slow exhumation in the Jueluotage Range since the Late Cretaceous. Two Jurassic samples reached the maximum depths after deposition and experienced the maximum temperatures of ca. 105 and 108°C until the late Early Cretaceous before a period of cooling and exhumation occurred at 114 and 106 Ma.
ZHU Wenbin, WAN Jinglin, SHU Liangshu, ZHANG Zhiyong, SU Jinbao, SUN Yan, GUO Jichun, ZHANG Xueyun.2008. Late Mesozoic Thermotectonic Evolution of the Jueluotage Range, Eastern Xinjiang, Northwest China: Evidence from Apatite Fission Track Data[J]. ACTA GEOLOGICA SINICA(English edition),82(2):348~357
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