日本地球惑星科学連合2019年大会

講演情報

[E] ポスター発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS06] Nankai Trough Seismogenic Zone Experiment: Logging and sampling the seismogenic megathrust

2019年5月28日(火) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 8ホール)

コンビーナ:金川 久一(千葉大学大学院理学研究科)、Demian M Saffer(Pennsylvania State University)、木下 正高(東京大学地震研究所)

[SSS06-P06] Modelling thermal maturity of an accretionary wedge

Mannu Utsav2、*木下 正高1Gerya Taras3 (1.東京大学地震研究所、2.Department of Earth and Climate Science, IISER Pune、3.Institute of Geophysics, ETH Zürich)

キーワード:thermal maturity、accretionary wedge、numerical simulation

In accretionary margins, the estimation of peak heating through the thermal maturity of organic material reveals differentiated deformational pathways in the adjoining sections of the wedge. As the thermal maturity of the deformed structures is a function of both the geothermal gradient and the duration of time it has been exposed to different gradients, the distribution of vitrinite reflectance (the measure of thermal maturity) in the wedge does not necessarily reveal the temporal deformational pathway of the individual pockets. As a result, the different portions of the accretionary wedge exhibit different correlations between the thermal maturity and a unique deformational pathway. These different correlations can be explored through the means of geodynamic modelling which can then be used in the field to ascertain a more holistic picture of deformation in an accretionary wedge. Therefore, in this study, we use a 2D plate subduction thermomechanical model, to simulate formation of accretionary wedge and the track the evolution of the vitrinite reflectance in the accretionary wedge.