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    中国百强科技报刊

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    Volume 43 Issue 6
    Jun.  2018
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    Pang Yumao, Guo Xingwei, Han Zuozhen, Zhang Xunhua, Zhu Xiaoqing, 2018. Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin. Earth Science, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602
    Citation: Pang Yumao, Guo Xingwei, Han Zuozhen, Zhang Xunhua, Zhu Xiaoqing, 2018. Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin. Earth Science, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602

    Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin

    doi: 10.3799/dqkx.2018.602
    • Received Date: 2017-11-30
    • Publish Date: 2018-06-15
    • Significant tectonic uplift and denudation occurred in central uplift of the South Yellow Sea basin (SYSB) since Late Cretaceous. Based on the drilling cores of CSDP-2 well which is supported and carried out by the Continental Scientific Drilling Project (CSDP) of China Geological Survey (CGS), the denudation and related characteristics of thermal history since Late Cretaceous in central uplift of SYSB were analyzed by apatite fission track (AFT) technique. The eight AFT ages obtained show two age groups, with one at (38±3) Ma, and the others ranging from (52±4) Ma to (65±5) Ma which all are much younger than the age of Permian where all samples locate, indicating that the samples were completely annealed and recorded the thermal history since Late Cretaceous. Modeling results of thermal history show that the peak paleo-geotemperature calculated by testing data of vitrinite reflectance (Ro) is within the range of the temperature interval of annealing zone of AFT. All samples suffered continuous cooling processes from the early stage of Late Cretaceous (ca.100 Ma) and started to enter into partial annealing zone (PAZ) at about 80-75 Ma. The first rapid cooling process began at the end of Late Cretaceous, and continued to the Early Paleocene, then was followed by a stage of slow cooling process during Paleogene. Some samples show the other rapid cooling process which is weaker than the first that occurred from the Late Oligocene to Early Miocene. The AFT ages and modeling results of thermal history significantly show the denudation and related characteristics since Late Cretaceous in central uplift of SYSB.

       

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