Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-CG Complex & General

[S-CG66_30AM1] Toward the integrated understanding of crustal deformation in plate convergence zones

Wed. Apr 30, 2014 9:00 AM - 10:45 AM 414 (4F)

Convener:*Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Yuji Yagi(Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba), Takeshi Sagiya(Disaster Mitigation Research Center, Nagoya University), Manabu Hashimoto(Disaster Prevention Research Institute, Kyoto University), Masanobu Shishikura(Active Fault and Earthquake Research Center, GSJ/AIST), Shoichi Yoshioka(Research Center for Urban Safety and Security, Kobe University), Yasutaka Ikeda(Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo), Gaku Kimura(Department of Earth and Planetary Science of the Graduate School of Science, The University of Tokyo), Mitsuhiro Matsu'ura(The Institute of Statistical Mathematics), Chair:Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Saeko Kita(National Research Institute for Earth Science and Disaster Prevention)

10:30 AM - 10:45 AM

[SCG66-P01_PG] Spatial relationship between the volcanic chain and high gravity anomalies in subduction zones

3-min talk in an oral session

*Yukitoshi FUKAHATA1 (1.DPRI, Kyoto University)

Keywords:island arc, subduction zone, gravity anomaly, volcanic front

The most conspicuous features of arc-trench systems are active seismicity, characteristic topography and gravity anomalies, and volcanism. The topography and gravity anomalies are low in the trench and high in the arc, which can be theoretically explained by mechanical interaction between the subducting oceanic plate and the overriding plate (Sato & Matsu'ura, 1993, GJI; Hashimoto et al, 2004, PAGEOPH). Because the topography is more complicated to be understood, free-air gravity anomaly is more suitable to be compared to the theoretical model. Free-air gravity anomalies with long wave length basically represent the effect of tectonic force, which disturbs gravity equilibrium. Volcanoes align along the volcanic front in most arcs. Since both of the high free-air gravity anomalies and volcanic front have a subparellel strike to the trench, it should be possible to classify arc-trench systems according to the spatial relationship between them. Based on such an idea, Fukahata (2008, JPGU meeing) classified arc-trench systems, but there was a problem that the recognition of the location of high gravity anomalies was quite subjective. So, in this study, I improved this process.; the location of high gravity anomalies were more quantitatively recognized. As a result, the location of high gravity anomalies relative to the volcanic front did not change for most arcs, but I found that it was difficult to define its location in some arcs (mostly tensile). Using the result, I discuss the spatial relationship between the volcanic chain and high gravity anomalies in subduction zones and consider causes of topographic evolution of island arcs.