Solid Earth Sciences (S)
Session Sub-categoryCG
Session IDS-CG62
Title Structure, evolution, and deformation of island arcs associated with subduction processes
Short Title Structure and evolution of island arcs
Date & Time
Oral
session
AM1, AM2 Thu, 25 MAY
On-site
poster
coretime
PM3 Fri, 26 MAY
Online
Poster
session
PM1 Thursday, 25 MAY
Main ConvenerName Tatsuya Ishiyama
Affiliation Earthquake Research Institute, University of Tokyo
Co-Convener 1Name Masahiro Ishikawa
Affiliation Graduate School of Environment and Information Sciences, Yokohama National University
Co-Convener 2Name Masanao Shinohara
Affiliation Earthquake Research Institute, University of Tokyo
Co-Convener 3Name Makoto MATSUBARA
Affiliation National Research Institute for Earth Science and Disaster Resilience
Session Language J
Scope Subduction processes such as accretion, back-arc-spreading, and arc-arc collisions have created overall architectures of the Japanese island arc through geologic time. Recent advances in seismic imaging of crust and mantle by both passive and controlled source have successfully provided plenty of new information on their structural, mechanical, rheological and thermal properties that have presumably strong controls on tectonic activities in the overriding plate including faulting, seismicity and crustal deformation in various timescales. Our goal of this session is to advance the understanding of overriding plate deformation in various timescales based on state-of-the-art results of observational, experimental and modeling studies encompassing both earthquake cycles and tectonic evolution of the Japanese island arc and other plate convergent margins. We welcome contributions from seismology, exploration geophysics, geodesy, tectonic geomorphology, physical geology, petrology, geochemistry, geochronology, rheology and numerical/analogue modeling on deformation processes associated with plate subduction processes and related feedbacks.
Presentation Format Oral and Poster
Collaboration Joint with -
Co-sponsoring
Society
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