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

OriginalPaper | Updated：2023-05-16

- A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone
- A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone
- 海洋湖沼学报（英文） 1995年13卷第3期页码：226-232
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 2589 from the Institute of Oceanology, Chinese Academy of Sciences.;The project was supported by NSFC (No. 49472148).
- DOI：10.1007/BF02850523
  中图分类号：
- 纸质出版：1995
- Accepted：
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A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone[J]. 海洋湖沼学报（英文）, 1995,13(3):226-232.

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
A preliminary study on the tectonics and evolution of the Fujian Coast Changle—Nanao metamorphism zone[J]. 海洋湖沼学报（英文）, 1995,13(3):226-232. DOI： 10.1007/BF02850523.

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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Keywords

references

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