Present-day Crustal Deformation in Arc-Continent Collision Zone of the Southeastern Eurasia Plate

WU Xiaolong; YANG Zhiqiang; GONG Yun

doi:10.13203/j.whugis20170081

Volume 44 Issue 2

Feb. 2019

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Geomatics and Information Science of Wuhan University > 2019 > 44(2): 240-245, 253. > DOI: 10.13203/j.whugis20170081

WU Xiaolong, YANG Zhiqiang, GONG Yun. Present-day Crustal Deformation in Arc-Continent Collision Zone of the Southeastern Eurasia Plate[J]. Geomatics and Information Science of Wuhan University, 2019, 44(2): 240-245, 253. DOI: 10.13203/j.whugis20170081

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Present-day Crustal Deformation in Arc-Continent Collision Zone of the Southeastern Eurasia Plate

1.
College of Geomatics, Xi'an University of Science and Technology, Xi'an 710054, China
2.
School of Geology and Geomatics, Chang'an University, Xi'an 710054, China

Funds:

The National Natural Science Foundation of China 51674195

the PhD Startup Foundation of Xi'an University of Science and Technology 2016QDJ049

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Author Bio:
WU Xiaolong, PhD, lecturer, specializes in the crustal deformation monitoring and analysis based on geodetic surveying technologies. E-mail: xlong_wu@126.com
Received Date: November 06, 2017
Published Date: February 04, 2019

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Abstract

Abstract

Based on the systematic collection of the GPS observations in China:Fujian, China:Taiwan and Philippine:Luzon, this paper obtains the current crustal horizontal velocity field of the arc-continent collision zone. Targeting the specific areas whose super-long span is more than 1000 km, this paper builds the least squares collocation model on the basis of ellipsoidal coordinates, uniformly calculating current GPS strain distribution of this collision zone. The results show that china:Taiwan province has the strongest crustal deformation, followed by Philippine:Luzon and China:Fujian regions respectively. The Philippine sea plate at the east Taiwan, China collides intensively with the Eurasia plate, and the collision is severely consumed through the central mountain's uplifting, the thrust napping and the tectonic escaping. The overall deformation characteristics is closely related to the structural variation of the Philippine sea plate. While the relative deformation in Luzon region is mainly involved with the relative sliding of the Philippine fault.
- arc-continental collision zone,
- Eurasia plate,
- the Philippine sea plate,
- GPS strain field,
- the Luzon arc volcanic

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