Estimation of crustal strength in Izu collision zone
スポンサーリンク
概要
- 論文の詳細を見る
We used 2D finite element method (FEM) to investigate the crustal strength of the Izu collision zone. Our model primarily based on the crustal structure given by Aoike et al. (2001). We set up standard rock layer properties for simulation. During simulation, cohesion was varied systematically. Simulation results show that failure zone decreases with increasing the convergent displacement in both cases i.e. before and after increasing cohesion. We used Mohr-Coulomb failure criterion and Mohr's circle to understand the reason. It is reasonable that rock layers do not break but flow below more than 30km depth. Further we compared simulated results with the focal mechanism data. Our models show only normal faulting which is not consistent with focal mechanism data. Thus our simulation models probably reveal the crustal strength of Izu collision zone.
- 琉球大学理学部の論文
著者
関連論文
- Shortening rate at frontal part of Hidaka thrust system by elastic plastic finite element method
- Simulation of role of decollement slope and surface slope angles to the stress field in accretionary wedge
- Estimation of crustal strength in Izu collision zone
- FEM simulation to clarify the Himalayan thrusts system
- Fault analysis around Himalaya by means of 2 dimensional finite element method.
- FE modeling of contemporary tectonic stress in the India-Eurasia collision zone
- Fault development in the Thakkhola half graben : insights from numerical simulation
- Geology, structure and metamorphism of the Mai khola area, southwestern part of Ilam Bazaar, eastern Nepal
- Paleostress transition by fault-striation analysis in the northern and central Ryukyu arc, southwest Japan
- Paleostress analysis around southern area of Okinawa-jima, Central Ryukyu, Japan
- Stress distribution and seismic faulting in the Nepal Himalaya : insights from finite element modeling
- Stress Distribution and Fault Development Around Nepal Himalaya by Means of Finite Element Method
- Numerical fault simulation in Himalayas with 2D finite element method
- Miocene to Pleistocene stress field transitions, around the Miyako-jima Island, South Ryukyu, Japan
- Neotectonics in Southern Ryukyu arc by means of paleostress analysis
- Geology and Three Dimensional Finite Strain Analysis around Annapurna Himal, Central Nepal
- Genesis of Okinawa Trough and thrust development within accretionary prism by means of 2D finite element method
- The technique that constructs strain ellipsoid from three strain ellipses measured on non-parallel sections based on the least square method and the factors that control precision of strain
- Strain Analysis of Kayo Formation around Teniya-zaki, Okinawa-jima
- Fault development around the Red Sea rift system : A finite element approach
- Numerical fault simulation in Himalayas with 2D finite element method