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The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China

Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong

Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China[J]. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
引用本文: Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China[J]. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
Citation: Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z

The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China

doi: 10.1007/s12583-013-0352-z

The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China

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出版历程
  • 收稿日期:  2013-12-19
  • 修回日期:  2013-12-19
  • 刊出日期:  2013-12-19

The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China

doi: 10.1007/s12583-013-0352-z

摘要: This article reports 21 AFT (apatite fission track) data from the West Shandong (山东) rise (WSR) and Jiyang (济阳) depression, and mainly studies their Cenozoic uplifting/subsidence history and the relationship between them. Furthermore, we improve our insights into the Bohai Bay Basin (BBB). Our AFT analysis and AFT T-t modeling indicates that the WSR was uplifted at ca. 65 Ma with apparent uplift rate of 0.019 mm/a; it underwent two relatively rapid uplifting events at 43–33 and 16–0 Ma with rates of 0.097 and 0.052 mm/a, respectively. Meanwhile, the Jiyang depression subsided at rate of 0.032 mm/a at 52–43 Ma, and the rate increased to 0.13 mm/a at ca. 42–33 Ma; finally the subsidence rate increased to 0.053 mm/a in 16–0 Ma. They all underwent a uplift in time of 23–16 Ma with rate of 0.04–0.07 mm/a. A careful comparison shows that the Cenozoic uplifting of the WSR coupled well with the subsidence of the Jiyang depression. Our research also suggests that the uplift- basin coupling events are part of the couplings between the Bohai Bay Basin and its peripheral mountains. This intraplate mountain-basin coupling is a reflection of global tectonic events.

English Abstract

Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China[J]. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
引用本文: Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China[J]. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z
Citation: Li Li; Dalai Zhong; Changchun Yang; Xiupeng Shi; Li Zhao; Dawei Dong. The Coupling Relationship between the West Shandong Rise and the Jiyang Depression, China. Journal of Earth Science, 2013, 15(4). doi: 10.1007/s12583-013-0352-z

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