Crustal deformation measurements by global positioning system (GPS) along NSL, western India

被引:14
|
作者
Dumka, Rakesh K. [1 ]
SuriBabu, D. [1 ,3 ]
Kotlia, B. S. [2 ]
Kothyari, Girish Ch. [1 ]
Prajapati, Sandip [1 ]
机构
[1] Inst Seismol Res, Gandhinagar 382009, Gujarat, India
[2] Kumaun Univ, Ctr Adv Study Geol, Naini Tal 263002, India
[3] Adikavi Nannaya Univ, Rajahmundary, Andhra Pradesh, India
关键词
GPS; Intra-plate deformation; Strain accumulation; Seismic moment; Seismic activity; NARMADA-SON LINEAMENT; JABALPUR EARTHQUAKE; SOURCE PARAMETERS; BROACH EARTHQUAKE; PENINSULAR INDIA; NAGAR HAVELI; MARCH; 23; EVOLUTION; ZONE; KACHCHH;
D O I
10.1016/j.geog.2021.05.004
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Narmada Son Lineament (NSL) is a major palaeo-rift system and seismically active intra-plate region. In this paper, we processed and analyzed the GPS data from 2009 to 2016 to study the geodynamic characteristics of NSL. The velocities derived from GPS were used to calculate the associated deformation and crustal strain, while the slip deficit was estimated using the horizontal motion of GPS sites. The investigation reveals that the maximum deformation of western NSL is 1.6 mm per year, and the upper bound of the seismic moment (M-0) is 2.0 x 10(24) dyn/cm, corresponding to an earthquake of about 6.0 magnitude. The study highlights the significance of Aravalli and Satpura mobile belts. The estimated strain of 0.03 mu strain/yr is low but comparable to the stable continental region, and a close association of factors (the fragility, crustal conductors, and compressive tectonics) is considered responsible for seismogenic activities in western NSL. (C) 2022 Editorial office of Geodesy and Geodynamics. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd.
引用
收藏
页码:254 / 260
页数:7
相关论文
共 50 条
  • [21] Global Positioning System measurements from eastern Tibet and their implications for India/Eurasia intercontinental deformation
    Chen, Z
    Burchfiel, BC
    Liu, Y
    King, RW
    Royden, LH
    Tang, W
    Wang, E
    Zhao, J
    Zhang, X
    JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2000, 105 (B7) : 16215 - 16227
  • [23] Optimal GPS positioning solutions interval for a crustal deformation estimation
    Dong-Seob Song
    Hong-Sic Yun
    KSCE Journal of Civil Engineering, 2007, 11 (4) : 193 - 198
  • [24] Crustal Deformation Revealed by GPS in Kumaun Himalaya,India
    Rakesh K.DUMKA
    Bahadur S.KOTLIA
    Kireet KUMAR
    Gokul S.SATYAL
    Lalit M.JOSHI
    Journal of Mountain Science, 2014, 11 (01) : 41 - 50
  • [25] Crustal deformation revealed by GPS in Kumaun Himalaya, India
    Dumka, Rakesh K.
    Kotlia, Bahadur S.
    Kumar, Kireet
    Satyal, Gokul S.
    Joshi, Lalit M.
    JOURNAL OF MOUNTAIN SCIENCE, 2014, 11 (01) : 41 - 50
  • [26] Crustal deformation revealed by GPS in Kumaun Himalaya, India
    Rakesh K. Dumka
    Bahadur S. Kotlia
    Kireet Kumar
    Gokul S. Satyal
    Lalit M. Joshi
    Journal of Mountain Science, 2014, 11 : 41 - 50
  • [27] Crustal deformation in the Baikal rift from GPS measurements
    Géosciences Azur UMR 6526, CNRS, UPMC, Valbonne and Villefranche/Mer, France
    不详
    不详
    不详
    不详
    不详
    不详
    不详
    Geophys. Res. Lett., 21 (4003-4006):
  • [28] Crustal deformation in the Baikal rift from GPS measurements
    Calais, E
    Lesne, O
    Deverchere, J
    San'kov, V
    Lukhnev, A
    Miroshnitchenko, A
    Buddo, V
    Levi, K
    Zalutzky, V
    Bashkuev, Y
    GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (21) : 4003 - 4006
  • [29] Application of global positioning system (GPS) to displacement measurements of cut slopes
    Sakurai, Shunsuke
    Shimizu, Norikazu
    Saragai, Akio
    Furutani, Shigeya
    Doboku Gakkai Rombun-Hokokushu/Proceedings of the Japan Society of Civil Engineers, 1993, (475 pt 3-24): : 137 - 142
  • [30] Crustal strain field in the Deccan trap region, western India, derived from GPS measurements
    Reddy, CD
    El-Fiky, G
    Kato, T
    Shimada, S
    Kumar, KV
    EARTH PLANETS AND SPACE, 2000, 52 (11): : 965 - 969