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    WANG Guo-can, XIANG Shu-yuan, WANG An, Garver John I., Wintsch Robert P., ZHANG Ke-xin, 2007. Thermochronological Constraint to the Processes of the East Kunlun and Adjacent Areas in Mesozoic-Early Cenozoic. Earth Science, 32(5): 605-614.
    Citation: WANG Guo-can, XIANG Shu-yuan, WANG An, Garver John I., Wintsch Robert P., ZHANG Ke-xin, 2007. Thermochronological Constraint to the Processes of the East Kunlun and Adjacent Areas in Mesozoic-Early Cenozoic. Earth Science, 32(5): 605-614.

    Thermochronological Constraint to the Processes of the East Kunlun and Adjacent Areas in Mesozoic-Early Cenozoic

    • Received Date: 2007-06-16
    • Publish Date: 2007-09-25
    • This paper displays some new thermochronological data on the tectonic processes of the East Kunlun and its adjacent areas in Mesozoic-Early Cenozoic, which were less investigated before. Three thermal events are revealed by different thermochronological methods. The first thermal event, which was a regional tectonic thermal event and established regional tectonic framework, started-up at about 200 Ma and lasted to the interim of the early-middle Jurassic. Its dynamics can be related to the closure of the Songpan-Ganzi-Bayan Har Triassic turbilite basin and the collision between the Qiangtang block and the Kumlun block. The second thermal event, mainly shows a series of NWW-SEE regional faults activity, occurred at about 130-150 Ma and lasted to about 100 Ma, the end of Early Cretaceous. The dynamics of this thermal event can be correspond to the collision between the Lhasa block and the Eurasia plate alone the Bangong-Nujiang suture zone. The last one happened at about 56-45 Ma, showing a extension-coursed uplift. The thermochronological records match well to the geological records which fragmentaryrily presented in the study area and provide a more certain constraint to the tectonic processes.

       

    • 致谢: 野外工作中得到朱云海、李德威、林启祥、 贾春兴、魏启荣和袁晏明等多位同志的协助, 在此对 给予帮助的提及和未提及有关人员表示衷心感谢!
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