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Join Prof. J. Ramon Arrowsmith from Arizona State University (ASU) for a training workshop on active tectonic study techniques. The workshop will include lectures, field trips, and hands-on activities around the Lembang Fault in West Java. Don't miss this opportunity to expand your knowledge in earthquake cycle exploration using 2D dislocations.
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Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US Tempat Pelaksanaan: Ruang Pangea, Laboratorium Gempabumi (LabEarth) – Puslit Geoteknologi LIPI dan Kuliah lapangan akan dilakukan disekitar Sesar Lembang, Jawa Barat. * Lebih jelas baca TOR/KAK dan daftar acara
Earthquake cycle exploration using 2D dislocations: strike-slipOutline of this lecture • Motivations from the San Andreas Fault • Basic ideas of dislocations • Strike-slip parallel displacements from simple screw dislocation model (Thatcher, 1990) • A few examples • Application to Izmit Earthquake
Areas of contrasting behavior along the San Andreas Fault (from Allen, 1968) Carrizo Plain
1906 M7.8 San Francisco EarthquakeBeginning of modern earthquake science
1906 earthquake surface rupture. 8’ fence offset above http://mnw.eas.slu.edu/Earthquake_Center/1906EQ/1906thumb.html And http://quake.wr.usgs.gov/info/1906/images/fenceoffset_big.html
“Reid’s elastic rebound hypothesis http://quake.wr.usgs.gov/info/1906/reid.html
http://www.matter.org.uk/matscicdrom/manual/di.html Edge dislocation Screw dislocation Dislocation: simple idealization of displacement discontinuity in continuous body
Idealization of brittle crust with embedded strike slip fault (Thatcher, 1990)
Strike-slip parallel displacements from simple screw dislocation model (Thatcher, 1990)
Interseismic motion along the San Andreas Fault System (max arrow length=~50mm/yr relative to stable North America) Thatcher, 1990 Noriega, et al. 2006; see also Schmalzle, et al., 2006 Plate Boundary Observatory velocity field