福建泉州晚中生代伸展构造变形特征与年代学制约

徐先兵; 李源; 薛德杰; 谢明阳; 汤帅; 崔建军; 张岳桥

doi:10.3799/dqkx.2014.005

Volume 39 Issue 1

Jan. 2014

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Article Navigation > Earth Science > 2014 > 39(1): 45-63

Xu Xianbing, Li Yuan, Xue Dejie, Xie Mingyang, Tang Shuai, Cui Jianjun, Zhang Yueqiao, 2014. Deformation Characteristics and Geochronological Constraints of Late Mesozoic Extensional Structures in Quanzhou, Fujian Province. Earth Science, 39(1): 45-63. doi: 10.3799/dqkx.2014.005

Citation:

Xu Xianbing, Li Yuan, Xue Dejie, Xie Mingyang, Tang Shuai, Cui Jianjun, Zhang Yueqiao, 2014. Deformation Characteristics and Geochronological Constraints of Late Mesozoic Extensional Structures in Quanzhou, Fujian Province. Earth Science, 39(1): 45-63. doi: 10.3799/dqkx.2014.005

Citation:

Xu Xianbing, Li Yuan, Xue Dejie, Xie Mingyang, Tang Shuai, Cui Jianjun, Zhang Yueqiao, 2014. Deformation Characteristics and Geochronological Constraints of Late Mesozoic Extensional Structures in Quanzhou, Fujian Province. Earth Science, 39(1): 45-63. doi: 10.3799/dqkx.2014.005

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Deformation Characteristics and Geochronological Constraints of Late Mesozoic Extensional Structures in Quanzhou, Fujian Province

doi: 10.3799/dqkx.2014.005

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
3.
Fujian Institute of Geological Survey, Fuzhou 350013, China
4.
Southeastern Fujian Geology Party of Fujian Province, Quanzhou 362021, China
5.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 2013-03-15
Publish Date: 2014-01-01

Abstract

Abstract

Multi-stage Late Mesozoic magmatism and structural deformation related to the subduction of Paleo-Pacific plate occurred in the coast of Fujian Province, southeastern China. Extensional deformation in Quanzhou area presents high-angular normal faults and low-angular normal faults or detachment faults. The extensional deformation developed in NW-striking extensional setting. Zircon U-Pb geochronological data in this study suggest that Late Jurassic (~155 Ma), middle Early Cretaceous (130-125 Ma), late Early Cretaceous (~109 Ma) and early Late Cretaceous magmatic rocks outcrop in Quanzhou area. The comprehensive analyses of cutting relations and geochronological data of magmatic rocks show that the sinistral ductile strike-slip of the Changle-Nan'ao shear zone occurred in 130-120 Ma, whereas the dextral brittle shear developed between 120 Ma and 100 Ma. The angular variations of subduction for the Paleo-Pacific plate underneath the South China led to the development of the Late Mesozoic orogenic belt in the coast of Fujian Province. This orogen commenced at the beginning of Early Cretaceous and terminated in the latest Early Cretaceous, which is marked by the extensive NW-striking extensional structures. The transform from syn-orogen compression to post-orogen extension occurred at ~120 Ma.
- Late Mesozoic,
- orogeny,
- tectonics,
- extensional deformation,
- zircon U-Pb,
- geochronology

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References(71)

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