PPT-Slip-dependent weakening revealed for a shallow megasplay fault in the Nankai subduction

A Roesner MJ Ikari A Huepers AJ Kopf s tudy site Japan PLEASE CLICK ON ME EGU 2020 Session Understanding large subduction earthquakes and tsunamigenesis 2. PUBLIC SWIM FEES ARE LISTED BELOW 1145 AM 115 PM Rec Fitness 1145 AM115 PM WHOLE POOL Rec Fitness 1145 AM115 PM WHOLE POOL Rec Fitness 1145 AM115 PM WHOLE POOL Rec Fitness 1145 AM115 PM WHOLE POOL Longcourse Rec Fitness 1145 AM115 PM WHOLE POOL Strike slip systems are relatively narrow and subvertical wrench zones along which two adjacent blocks move sideways horizontally parallel to the strike of the fault zone For example they are produced at transform plate boundaries where plates hori for . Crustal Deformation. (including seismicity of optimal locking depth, shallow surface creep . and geological constraints). . Yuehua. Zeng and . Steve Ward. John Rundle. Jim Dieterich. Keith Richards-Dinger. Fred . Pollitz. Generic Description of . Earthquake Simulators. Olaf . Zielke. Outline. What are Earthquake Simulators?. Inputs. Rheology. Structures. ( . Folds, Faults and Joints) . Instructor: . Dr. Attaullah Shah . . Lecture # 6. . Department of Civil Engineering. Swedish College of Engineering and Technology-Wah Cantt. . . 3. The wavy undulations in the rock beds are called . Sarah Minson. California Institute of Technology. Real-time . finite fault slip models for . earthquake early warning. Sarah E. . Minson. . California Institute of Technology. Jessica R. Murray, John O. . Reporters:. Alconera. , P.P.. Villacampa. , E.. Mangaway. , . Cris. A scientific theory which describes the large scale motions of Earth's lithosphere. . Plate tectonics is the study of how the Earth's plates are driven and shaped by geological forces that keep them in constant motion. . Ben Valentino. 1. , Eduardo Toledo. 2. , Eduardo Nobre. 2. , Luciana Vieira. 2. , . Diogo. Cintura. 2. 1. Department of Earth Sciences, SUNY Oswego. 2. Department of Civil Engineering, . Federal University of . Right Lateral. Fault Plane. Auxiliary Plane. How are . focal mechanisms . determined by seismic data?. The Great California . ShakeOut. . Focal mechanisms . are. . visualization models that show:. direction. 114The long partially preserved record of civilization in Myanmar Burma provides an unusual opportunity to understand the recent behavior of some of its active faults In particular inscriptions on som M. Bruzzi. 1. , R. Mori. 1. , M. Scaringella. 1. , Z. Li. 2. 1. INFN and University of Florence, Florence (Italy). 2. BNL, Upton New York (US). M. . Bruzzi. , R. Mori, M. . Scaringella. , Z. Li . Shallow levels analysis in n-type MCZ Si detectors after mixed irradiation, . An international multi-disciplinary observatory along a . subduction. zone plate boundary (. ies. ?). “. subduction. . collaboratory. ”. 2014 Fall AGU meeting, San Francisco. EarthScope. Beyond 2018. weakenings. of the stratospheric polar vortex . Lim E.-P., H.H. Hendon, G. . Boschat. , D. Hudson, D.W.J. Thompson, A.J. Dowdy and . J.M. Arblaster. , 2019, Australian hot and dry extremes induced by . 36. Cl cosmogenic exposure dating and decadal GPS strain-rate.. Francesco Iezzi. (francesco.iezzi.15@ucl.ac.uk). ,. G. Roberts, J. Faure Walker, I. Papanikolaou, A. . Ganas. , G. . Deligiannakis. , J. Beck, S. Wolfers, D. .