S11A:
Ambient Field Seismology: Theoretical and Methodological Innovations I


Submit an Abstract to this Session


Session ID#: 58687

Session Description:
The ambient seismic field (noise) is now widely used to assess a variety of features such as seismic velocities, medium stiffness, ground motion and attenuation. Recently, we have seen more attempts to gain spatial resolution and to extract body waves from noise correlations. Deep-phase extraction also offers global seismologists new opportunities to map Earth’s structures and to perform time-lapse studies. However, all these research topics strongly depend on the accurate estimation of the Green’s function, thus relying on, for example, microseism sources distribution, receiver coverage, and appropriate signal processing. In this session, we would like to cover most theoretical and methodological aspects of ambient-field seismology. We invite abstracts related to all the aforementioned research lines but also encourage innovative studies exploring the source distribution, the importance of scattering, and imaging applications involving novel processing such as higher-order correlations, double beam forming, or multi-dimensional deconvolution.
Primary Convener:  Zack Spica, University of Michigan, Ann Arbor, MI, United States
Conveners:  Nori Nakata, University of Oklahoma, ConocoPhillips School of Geology and Geophysics, Norman, OK, United States and Lise Retailleau, Stanford University, Department of Geophysics, Stanford, United States
Primary Liaison:  Zack Spica, University of Michigan, Ann Arbor, United States
Chairs:  Zack Spica, University of Michigan, Ann Arbor, United States and Nori Nakata, Lawrence Berkeley National Laboratory, Earth and Environmental Sciences Area, Berkeley, United States
OSPA Liaison:  Zack Spica, University of Michigan, Ann Arbor, United States
Index Terms:

7203 Body waves [SEISMOLOGY]
7255 Surface waves and free oscillations [SEISMOLOGY]
7260 Theory [SEISMOLOGY]
7270 Tomography [SEISMOLOGY]

Abstracts Submitted to this Session:

Zhengbo Li1,2 and Xiaofei Chen2, (1)University of Science and Technology of China, School of Earth and Space Sciences, Shenzhen, China, (2)Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China
Zhang Gong Heng, Southern University of Science and Technology of China, Shenzhen, China; HIT Harbin Institute of Technology, Harbin, China and Xiaofei Chen, Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China
Yadong Wang1, Kevin Michael Ward2,3 and Fan-Chi Lin3, (1)University of Utah, Department of Geology & Geophysics, Salt Lake City, UT, United States, (2)South Dakota School of Mines and Technology, Rapid City, SD, United States, (3)University of Utah, Salt Lake City, UT, United States
Yang LU1, Laurent Stehly2, Romain Brossier1, Anne Paul1, Ludovic Metivier1 and AlpArray Working Group, (1)ISTerre, CNRS, Université Grenoble Alpes, Grenoble, France, (2)Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, IRD, Univ. Gustave Eiffel, ISTerre, Grenoble, France
Hrvoje Tkalčić, Australian National University, Research School of Earth Sciences, Canberra, ACT, Australia and Thanh-Son Pham, Australian National University, Research School of Earth Sciences, Canberra, Australia
Jorge C. Castellanos, California Institute of Technology, Seismological Laboratory, Pasadena, CA, United States and Robert W Clayton, California Institute of Technology, Pasadena, CA, United States
Raphael S.M. De Plaen1,2, Ernesto Leon3, Francisco J Nuñez-Cornu2 and Diana Núñez4, (1)University of Guadalajara, SisVOc, Guadalajara, Mexico, (2)Universidad de Guadalajara, SisVOc, Puerto Vallarta, Mexico, (3)Universidad de Guadalajara, Guadalajara, Mexico, (4)Universidad Complutense de Madrid, Física de la Tierra y Astrofísica, Madrid, Spain
Josiah Ensing, University of Auckland, Auckland, New Zealand and Kasper van Wijk, The University of Auckland, Physics Department, Auckland, New Zealand

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