scholarly journals Reply to comment by J. C. Savage on “Aseismic slip and fault-normal strain along the creeping section of the San Andreas Fault”

2009 ◽  
Vol 36 (13) ◽  
Author(s):  
F. Rolandone ◽  
R. Bürgmann ◽  
D. C. Agnew ◽  
I. A. Johanson ◽  
D. C. Templeton ◽  
...  
Keyword(s):  
San Andreas Fault ◽  
Normal Strain ◽  
Aseismic Slip ◽  
San Andreas

scholarly journals Aseismic slip and fault-normal strain along the central creeping section of the San Andreas fault

2008 ◽  
Vol 35 (14) ◽  
Author(s):  
F. Rolandone ◽  
R. Bürgmann ◽  
D. C. Agnew ◽  
I. A. Johanson ◽  
D. C. Templeton ◽  
...  
Keyword(s):  
San Andreas Fault ◽  
Normal Strain ◽  
Aseismic Slip ◽  
San Andreas

scholarly journals Aseismic slip and seismogenic coupling along the central San Andreas Fault

2015 ◽  
Vol 42 (2) ◽  
pp. 297-306 ◽  
Author(s):  
R. Jolivet ◽  
M. Simons ◽  
P. S. Agram ◽  
Z. Duputel ◽  
Z.-K. Shen
Keyword(s):  
San Andreas Fault ◽  
Aseismic Slip ◽  
San Andreas

Aseismic slip on the San Andreas Fault south of Loma Prieta

1990 ◽  
Vol 17 (9) ◽  
pp. 1445-1448 ◽  
Author(s):  
J. Behr ◽  
R. Bilham ◽  
P. Bodin ◽  
R. O. Burfoid ◽  
R. Bürgmann
Keyword(s):  
San Andreas Fault ◽  
Aseismic Slip ◽  
San Andreas ◽  
Loma Prieta

Reconstructing 10 years of spatio-temporal aseismic slip history along the San Andreas Fault

2020 ◽  
Author(s):  
Sylvain Michel ◽  
Romain Jolivet ◽  
Adriano Gualandi ◽  
Blandine Guardonio ◽  
Olivier Lengliné ◽  
...  
Keyword(s):  
San Andreas Fault ◽  
Slip Rate ◽  
Temporal Variations ◽  
Independent Component ◽  
Tectonic Activity ◽  
Aseismic Slip ◽  
Linear Inversion ◽  
San Andreas ◽  
Acceleration And Deceleration ◽  
Spatio Temporal

<p>The San Andreas Fault creeping section is generally considered as slipping continuously and aseismically, at a rate of about 35 mm/yr. However, recent studies, using either Global Positioning System (GPS) network or Interferometric Synthetic Aperture Radar (InSAR) data, have highlighted spatial and temporal variations of slip rate. Here, we combine GPS, InSAR, creepmeter and seismicity data over the 2008-2018 period, taking advantage of their complementary spatial and temporal resolutions, to detail a comprehensive picture of episodic acceleration and deceleration slip patterns. For this purpose, we use a variational Bayesian Independent Component Analysis (vbICA) decomposition to separate geodetic deformation due to non-tectonic sources from signals of tectonic origin. The fault slip kinematics is reconstructed by linear inversion of each Independent Component related to transient tectonic activity. We document aseismic slip acceleration transients and discuss their origin.</p>

scholarly journals Seismic and aseismic slip on the San Andreas Fault

1969 ◽  
Vol 74 (8) ◽  
pp. 2049-2069 ◽  
Author(s):  
C. H. Scholz ◽  
M. Wyss ◽  
S. W. Smith
Keyword(s):  
San Andreas Fault ◽  
Aseismic Slip ◽  
San Andreas
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