scholarly journals New constraints on fault architecture, slip rates, and strain partitioning beneath Pyramid Lake, Nevada

Geosphere ◽  
2015 ◽  
Vol 11 (3) ◽  
pp. 683-704 ◽  
Author(s):  
A. K. Eisses ◽  
A. Kell ◽  
G. M. Kent ◽  
N. W. Driscoll ◽  
R. LeRoy Baskin ◽  
...  
Keyword(s):  
Strain Partitioning ◽  
Slip Rates ◽  
Pyramid Lake ◽  
Fault Architecture

scholarly journals Strain partitioning and fault slip rates in the northeastern Caribbean from GPS measurements

2002 ◽  
Vol 29 (18) ◽  
pp. 3-1-3-4 ◽  
Author(s):  
Eric Calais ◽  
Yves Mazabraud ◽  
Bernard Mercier de Lépinay ◽  
Paul Mann ◽  
Glen Mattioli ◽  
...  
Keyword(s):  
Fault Slip ◽  
Strain Partitioning ◽  
Gps Measurements ◽  
Slip Rates ◽  
Fault Slip Rates

Slip-rates along the Chaman fault: Implication for transient strain accumulation and strain partitioning along the western Indian plate margin

2013 ◽  
Vol 608 ◽  
pp. 389-400 ◽  
Author(s):  
Shams Ul-Hadi ◽  
Shuhab D. Khan ◽  
Lewis A. Owen ◽  
Abdul S. Khan ◽  
Kathryn A. Hedrick ◽  
...  
Keyword(s):  
Indian Plate ◽  
Strain Accumulation ◽  
Strain Partitioning ◽  
Slip Rates ◽  
Transient Strain ◽  
Plate Margin

Fault interaction and strain partitioning in southeastern Tibetan Plateau: from kinematics to geodynamics

2020 ◽  
Author(s):  
Li Yin
Keyword(s):  
Tibetan Plateau ◽  
Fault Slip ◽  
Fault System ◽  
Strain Partitioning ◽  
Fault Interaction ◽  
Slip Rates ◽  
Southeastern Tibetan Plateau ◽  
Fault Systems ◽  
Fault Strength ◽  
Fault Slip Rates

<p>In southeastern Tibetan Plateau, the Xianshuihe-Xiaojiang fault system (XXFS) and its neighboring fault systems collectively accommodates the material extrusion of the Tibetan Plateau. However we do not mechanically understand how these faults interact with each other and how the fault interaction impacts strain partitioning, fault slip rates, and seismicity in this region. We develop and use a three-dimensional viscoelastoplastic finite element model to simulate regional deformation, fault slip rates, and fault interaction in the fault system of southeastern Tibetan Plateau. We investigate the effects of inception and activity of faults, fault strength, lithospheric rheology, and topography on partitioning of strain and fault slip rates. Model results show that fault strength, lithospheric rheology, and topography all significantly influence the strain partitioning and slip rates on faults. The initiation of the Daliangshan fault results mainly from the non-smooth fault geometry of the main trace of the XXFS. Our model results support the hypothesis of codependent slip rate between fault systems. For the present fault configuration, our model predicts localized strain in the Daliangshan faults, Yingjing-Mabian faults, and Lianfeng-Zhaotong faults, where numerous earthquakes occurred in recent years.</p>

Estimating the slip rates of normal faults in the Great Basin, USA

2000 ◽  
Vol 12 (3-4) ◽  
pp. 227-240 ◽  
Author(s):  
C. M. dePolo ◽  
J. G. Anderson
Keyword(s):  
Great Basin ◽  
Normal Faults ◽  
Slip Rates

SLIP RATES OF CHAMAN FAULT SYSTEM, PAKISTAN

2016 ◽  
Author(s):  
Jingqiu Huang ◽  
◽  
Shuhab Khan ◽  
Abdul Salam Khan
Keyword(s):  
Fault System ◽  
Slip Rates
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