Contemporary movement of the Earth's crust in the Northwestern Vietnam by continuous GPS data

被引:3
|
作者
Le Huy Minh [1 ,5 ]
Vu Tuan Hung [2 ]
Hui, Jyr-Ching [3 ]
Nguyen Le Minh [1 ,5 ]
Huang, Bor-Shouh [4 ]
Chen, Horng-Yue [4 ]
Nguyen Chien Thang [1 ]
Nguyen Ha Thanh [1 ]
Le Truong Thanh [1 ]
Nguyen Thi Mai [1 ]
Pham Thi Thu Hong [1 ,5 ]
机构
[1] VAST, Inst Geophys, Hanoi, Vietnam
[2] VAST, Inst Geol Sci, Hanoi, Vietnam
[3] Natl Taiwan Univ, Taipei, Taiwan
[4] SINICA, Inst Earth Sci, Taipei, Taiwan
[5] VAST, Grad Univ Sci & Technol, Hanoi, Vietnam
来源
VIETNAM JOURNAL OF EARTH SCIENCES | 2020年 / 42卷 / 04期
关键词
Crustal movement; GPS continuous data; IGS14; Northwestern Vietnam; GAMIT/GLOBK; BIEN-PHU FAULT; SE-ASIA; TECTONICS; MOTION;
D O I
10.15625/0866-7187/42/4/15282
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The paper presents an estimation of the Earth's crustal motion from the continuous GPS data at 6 stations (MTEV, MLAY, DBIV, TGIV, SMAV and SLAV) in the Northwestern and at PHUT (Hanoi) station using GAMIT/GLOBK software. The absolute horizontal displacements of the Earth's crust at 7 stations in the IGS14 frame are respectively: 34.10 +/- 0.71 mm/yr (DBIV), 34.31 +/- 0.65 mm/yr (PHUT), 34.51 +/- 0.75 mm/yr (SMAV), 34.55 +/- 0.80 mm/yr (MLAY), 34.80 +/- 0.72 mm/yr (TGIV), 34.93 +/- 0.99 mm/yr (SLAV) and 35.59 +/- 0.73 mm/yr (MTEV), in the southeastward with the azimuth range 104-108 degrees. The Son La fault is a right-lateral slip fault with a shear amplitude of similar to 1.5 mm/yr. The Lai Chau - Dien Bien fault is a left-lateral slip fault with a shear amplitude of similar to 1.9 mm/yr. Although the absolute velocities at the DBIV, SMAV, SLAV, TGIV and MLAY stations are evaluated with the error < 1 mm/yr, the relative displacement on the Ma River fault is of similar to 0.5 mm/yr, and it seems that we still do not have a reliable assessment of the slip rate on the Ma River right-lateral slip fault.
引用
收藏
页码:334 / 350
页数:17
相关论文
共 50 条
  • [31] Estimating the stress and strain fields of the Earth's crust on the basis of seismotectonic data
    L. A. Nazarova
    Journal of Mining Science, 1999, 35 : 26 - 35
  • [32] Estimation of the orientation of stress in the Earth’s crust without earthquake or borehole data
    Andrew A. Delorey
    Götz H. R. Bokelmann
    Christopher W. Johnson
    Paul A. Johnson
    Communications Earth & Environment, 2
  • [33] New data on the possibility of catalytic abiogenic synthesis of hydrocarbons in the earth's crust
    Ione, KG
    Mysov, VM
    Stepanov, VG
    Parmon, VN
    PETROLEUM CHEMISTRY, 2001, 41 (03) : 159 - 165
  • [34] The inhomogeneity of the Earth's crust in the Central Indian basin on seismic tomography data
    Neprochnov, YP
    Bezverbnaya, VV
    El'nikov, IN
    DOKLADY AKADEMII NAUK, 1997, 357 (04) : 519 - 523
  • [35] Modeling of the Earth's crust from seismic and gravity data: Tectonic implications
    Kozlenko, VG
    Starostenko, VI
    Baranova, EP
    Gurova, IY
    FIZIKA ZEMLI, 1997, (08): : 20 - 30
  • [36] Rigidity of the fault zones in the Earth’s crust estimated from seismic data
    A. A. Spivak
    Izvestiya, Physics of the Solid Earth, 2011, 47 : 600 - 609
  • [37] Correction on Effect of Earth's Oblateness in Inversion of GPS Occultation Data
    Xu Xiaohua
    Li Zhenghang
    Luo Jia
    GEO-SPATIAL INFORMATION SCIENCE, 2005, 8 (04) : 247 - +
  • [38] Correction on Effect of Earth’s Oblateness in Inversion of GPS Occultation Data
    XU Xiaohua LI Zhenghang LUO Jia
    Geo-Spatial Information Science, 2005, (04) : 247 - 250
  • [39] Quality Evaluation of the Earth's Crust Height Movement Kinematic Model in the Northern Part of the Republic of Croatia
    Radanovic, Marko
    Rozic, Nevio
    Razumovic, Ivan
    WORLD MULTIDISCIPLINARY EARTH SCIENCES SYMPOSIUM (WMESS 2018), 2019, 221
  • [40] Analysis of Current Movements and Deformations of the Earth's Crust in Fennoscandia from GNSS Data
    Steblov, G. M.
    Agibalov, A. O.
    Mel'nik, G. E.
    Perederin, V. P.
    Perederin, F., V
    Sentsov, A. A.
    IZVESTIYA-PHYSICS OF THE SOLID EARTH, 2022, 58 (04) : 459 - 468