A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone

Wang Xin; Zhang Yue-hong; Chen Wen-shan; Yang Xiao-qing; Huang Hui

doi:10.1007/BF02850523

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A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone

Updated：2023-05-16

- A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone
- Journal of Oceanology and Limnology Vol. 13, Issue 3, Pages: 226-232(1995)
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
- DOI：10.1007/BF02850523
  CLC：
- Published：1995
- Accepted：
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Xin, W., Yue-hong, Z., Wen-shan, C. et al. A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone., Chin. J. Ocean. Limnol. 13, 226–232 (1995). https://doi.org/10.1007/BF02850523
DOI：

Xin, W., Yue-hong, Z., Wen-shan, C. et al. A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone., Chin. J. Ocean. Limnol. 13, 226–232 (1995). https://doi.org/10.1007/BF02850523 DOI：

摘要

Abstract

The Fujian coast Changle—Nanao metamorphism zone rocks are composed of gneiss

schist and hornblendite which had gone through metamorphism of amphilbolite facies

and followed the large-scale intrusive mass of gneissic granite. The zone was originally composed of Early Palaeozoic continental margin and island arc volcanic and sedimentary rocks. In 180-150 Ma

the zone underwent ductile shear deformation and amphibolite facies metamorphism; and in 130-80 Ma

rose rapidly and collided with the Southeastern China continental margin volcanic rocks along the NE trending ductile shear belt. The above geologic setting laid the present Fujian coast tectonic foundation whose formation and evolution are known to be interrelated with the subduction and collision of the Taiwan. Central Range.

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references

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