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    Volume 38 Issue 4
    Jul.  2013
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    Article Navigation >  Earth Science  > 2013  >  38(4): 725-744
    ZHANG Yuan-ze, WANG Guo-can, WANG An, ZHANG Ke-xin, 2013. Coupling Processes of Xunhua-Hualong Basin-Orogenic Belt Since Late Cretaceous: Evidence from Apatite Fission Track Geochronology and Source Analysis. Earth Science, 38(4): 725-744. doi: 10.3799/dqkx.2013.071
    Citation: ZHANG Yuan-ze, WANG Guo-can, WANG An, ZHANG Ke-xin, 2013. Coupling Processes of Xunhua-Hualong Basin-Orogenic Belt Since Late Cretaceous: Evidence from Apatite Fission Track Geochronology and Source Analysis. Earth Science, 38(4): 725-744. doi: 10.3799/dqkx.2013.071
    shu

    Coupling Processes of Xunhua-Hualong Basin-Orogenic Belt Since Late Cretaceous: Evidence from Apatite Fission Track Geochronology and Source Analysis

    doi: 10.3799/dqkx.2013.071
    • 1.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • 2.

      Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 3.

      State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

    • Received Date: 2013-01-28
    • Publish Date: 2013-07-01
      Abstract
    • Xunhua-Hualong basin Cenozoic sedimentary strata, basement and surrounding mountains analysis of apatite fission track geochronology reveals the Northeast margin of Qinghai-Tibet plateau experienced three periods of uplift and exhumation events since Late Cretaceous: (1) Basin basement, Laji mountain and West Qinling orogenic belt apatite fission track ages generally record a Late Cretaceous-Eocene relatively rapid regional uplift and exhumation event. Northern margin of West Qinling rapidly uplift at 84Ma, which was controlled by the uplift of the northward thrust; to the North Lamu Gorge in central of Xunhua-Hualong basin uplift at 69Ma; further north rapid uplift stages along Laji mountain is mainly between 40-50Ma, reflecting Paleocene-Eocene rapid uplift gradually extending from south to north. This tectonic uplift event resulted in Xunhua-Hualong basin and Linxia basin missing Paleogene Xining group sedimentary strata that deposits in northern Xining-Minhe basin. The first period of uplift and exhumation ended at about 31Ma, when Xunhua-Hualong basin connected with eastern Linxia basin to a large unified foreland basin of West Qinling, both experience the same tectonic and sedimentary evolution history, therefore Cenozoic oldest Tala group sedimentary strata age in Xunhua-Hualong basin won't exceed the oldest sedimentary strata with Paleomagnetic age of 29Ma in Linxia basin. (2) Late Oligocene about 26Ma Laji mountain began bi-directionally thrust-uplift and may have continued to Early Miocene about 21Ma, and uplifting made Xunhua-Hualong basin become piedmont extrusion foreland basin between Laji mountain and West Qinling, when Xunhua-Hualong basin began to deposit Tala group alluvial fan of thick coarse clastic rocks. By analyzing sedimentary facies, the ancient flow direction and gravel composition of Xianshuihe group and Linxia group sedimentary strata in Xunhua-Hualong basin, it is concluded that Laji mountains experienced the largest bi-directional thrust-uplift event in the Miocene about 8Ma, which led directly to the event of Xunhua-Hualong piedmont extrusion foreland basin turning into mountain basin, which formed basic pattern of basin-mountain landform in northeastern margin of Qinghai-Tibet plateau nowadays.

       

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