PPT-SEISMICITY ( M>3.0) IN

THE PERIOD 20022014 AND ACTIVE TECTONICS IN THE GULF OF CALIFORNIA MEXICO Raúl R Castro 1 Joann Stock 2 Egill Hauksson 2 and Robert Clayton 2 1 CICESE División Ciencias de la Tierra Departamento de Sismología Ensenada Baja California 22860 México . The Great California . ShakeOut. . NO. Caused by sudden release of energy. Tectonic earthquakes are focused on a fault. Induced seismicity. Volcanism. The Great California . ShakeOut. . Earthquakes caused by the movement of magma through the earth’s crust. UCERF2. and . Plans for UCERF3. Andy Michael. Historical Earthquake Catalog: 1850 – 1932. Primary compilation: . Toppozada. and . Branum. (2003). 1769-1999, M≥5.5, magnitude based on area with MMI V, VI, VIII,. Properties of aftershocks and foreshocks . and implications for earthquake forecasting. Agnès. . Helmstetter. , . ISTerre. , CNRS, University Grenoble 1 . Earthquake triggering. When? Where? What size?. Emma Myers. IRIS Internship. Advisors: Dr. Rick Aster, CSU. Harley Benz, USGS/NEIC. http://www.huffingtonpost.com/2013/12/09/antarctica-record-cold-_n_4415564.html. Antarctic Seismic Network. Guiding Research. Seismicity and Geologic Structures Indubitable in Wadi Hagul, North Eastern Desert, Egypt Tarek A. Seleem, Hamdy A. AboulelaGeology Department Faculty of Science T. A. SELEEM ET ALCopyright of significant seismic quiescence in the Pacific Mexican . coast. A. . Muñoz-. Diosdado. , A. H. Rudolf-Navarro, . A. Barrera-Ferrer, F. Angulo-Brown. National . Polytechnic Institute, . Mexico . City, . Hazard . Prediction Based on Seismicity . Simulation. . Shiyong. Zhou Russell Robinson . Xiaofei. Chen . M. Jiang . X. . Jin. . B. Gao . Karen Felzer. USGS. Decision points #1: Which smoothing algorithm to use?. National Hazard Map smoothing method (. Frankel. , 1996. )?. Helmstetter. et al.. (2007) smoothing. method down to M 2, back to 1981?. Jeremy Douglas Zechar. Lamont-Doherty Earth Observatory. Smoothed seismicity. Physical intuition. : Earthquakes do not occur at a point, they affect some (unknown) region around the hypocenter/rupture surface.. Volcano Monitoring: Deformation, Seismicity & Gas* Animations: Seismic Signature(See “Rock break earthquake”)GPS—Measuring Plate Motion Some techniques used for monitoring volcanoes. De Petroleum Geologists. Distinguished Lecturer. Sponsored by. Investigating The Induced Seismicity Potential In Energy Technologies To Understand How To Limit The Occurrence Of Felt Seismicity And Its Impacts. Dept. Earth and Space Sciences, UCLA, Los Angeles,. CA 90095-1567, . kagan@moho.ess.ucla.edu. , http://eq.ess.ucla.edu/~kagan.html. http://moho.ess.ucla.edu/~. kagan/Potsdam2. .pptx. GLOBAL EARTHQUAKE FORECAST. No major . tectonism. , . magmatism. , basement metamorphism or . anorogenic. intrusion since . t. he Cretaceous. No rifting, major extension or . transtension. since the . Paleogene. Schulte and Mooney (2005). subducting. plate has been detected in a majority of . subduction. zones.. LVZ may be a . hydrated layer of oceanic crust . caused by dehydration reactions as the plate . subducts. .. LVZ has interesting consequences for imaging the .