SCG66-08

JpGU-AGU Joint Meeting 2017

Constraint on the yield strength envelope of subducting oceanic platefrom stress neutral surface depth and bending moment*篠島 僚平1、伊藤 武男1*Ryohei Sasajima1, Takeo Ito1
1. 名古屋大学大学院 環境学研究科
1. Graduate School of Environmental Studies, Nagoya University

1. Introduction
Many previous studies attempted to estimate the yield strength envelope (brittle strength and ductile flowlaw) of the oceanic plate from flexural topography and gravity anomalies in outer rise [e.g., Goetze andEvans, 1979; Hunter and Watts, 2016]. Their approaches can constrain the bending moment, whichreflects depth-integrated yield strength envelope. Estimated bending moments of world outer rise areconsistent with the standard yield strength envelope estimated from rock experiments [Hunter and Watts,2016].
In addition, recent seismic studies succeeded to constrain stress neutral surface depth (SNSD) in theoceanic plate around the trench and double seismic zone in intermediate depth slab, in few km ofprecision. The SNSD reflects relative strength between shallower-half brittle part and deeper-half ductile
part, while bending moment reflects integrated absolute strength. Thus, combining these two
independent observed parameters enables us to constrain the yield strength envelope in more detail,which will contribute to understand rheology, magnitude of stress, and pore-fluid pressure in the oceanic
plate and slab.
This study attempted to constrain the yield strength envelope of the oceanic plate around outer rise andintermediate depth slab from observed SNSD and bending moment. The target is the Pacific platesubducting from the Japan Trench and the Kuril Trench.
2. Bending moment
We estimated the bending moment at the outer rise from topography and gravity anomalies following thestudy of Hunter and Watts [2016]. In addition to their study, we considered the effect of thermal stress on
estimating the bending moment. We estimated the bending moment of subducting, intermediate depth
slab from gravity anomalies [Sasajima and Ito, 2016, SSJ fall-meeting] and corner flow stress in the mantlewedge.
3. Stress neutral surface depth (SNSD)
We used observed SNSD around the Japan Trench that is 30-35 km from the plate upper surface basedon Hino et al. [2009] and Obana et al. [2012]. We used observed SNSDs of intermediate-depth double
seismic zone that are 22 km from the slab upper surface under the Tohoku region, and 10 km from theslab upper surface under the Hokkaido region based on Kita et al. [2010b].
4. Modeling stress evolution in subducting oceanic plate
In order to connect observed SNSDs and the bending moment to the yield strength envelope, we
conducted a model simulation of stress evolution of the oceanic plate. The model describes differential
stress of 1D column of the oceanic plate in the Lagrangian description by time integral of elastic stresschanging, brittle stress release, and ductile stress relaxation.
The factors controlling SNSD are (1) brittle strength, (2) ductile flow law, (3) thermal structure, and (4)net-horizontal force. We tested to change them within conceivable range and compared the resulting©2017. Japan Geoscience Union. All Right Reserved.

- SCG66-08 -SCG66-08

JpGU-AGU Joint Meeting 2017

modeled SNSD and bending moment with observed them.
5. Results
Observed SNSD (30-35 km) and bending moment around the trench are explained by standard ductileflow law with moderate pore-fluid pressure for brittle strength. On the other hand, observed SNSD (22 km)
at intermediate depth under the Tohoku region requires further higher pore-fluid pressure than aroundthe trench. This is because the compressional brittle strength in the intermediate depth without highpore-fluid pressure is extremely strong and it shifts the SNSD to too shallow. This high pore-fluid pressurein the intermediate depth slab is consistent with many previous studies. On the other hand, muchshallower SNSD (10 km) at intermediate depth under the Hokkaido region may be caused by both ofrelatively low pore-fluid pressure than Tohoku region [Shiina et al., 2017] and extensional net-horizontalforce [Kita et al., 2010b].
キーワード：応力中立面、強度プロファイル
Keywords: Stress neutral surface depth, Yield strength envelope©2017. Japan Geoscience Union. All Right Reserved.

- SCG66-08 -