Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2020GL091707 |
Variable in‐situ stress orientations across the northern Hikurangi Subduction Margin | |
D. D. McNamara; E. Behboudi; L. Wallace; D. Saffer; A. E. Cook; A. Fagereng; M Paganoni; W Hung‐; Yu; G Kim; H. Lee; H. M. Savage; P. Barnes; I Pecher; L. J. LeVay; K. E. Petronotis | |
2021-02-24 | |
发表期刊 | Geophysical Research Letters |
出版年 | 2021 |
英文摘要 | We constrain orientations of the horizontal stress field from borehole image data in a transect across the Hikurangi Subduction Margin. This region experiences NW‐SE convergence and is the site of recurrent slow slip events. The direction of the horizontal maximum stress is E‐W at an active splay thrust fault near the subduction margin trench. This trend changes to NNW‐SSE in a forearc trench slope basin on the offshore accretionary wedge, and to NE‐SW in the onshore forearc. Multiple, tectonic and geological processes, either individually or in concert, may explain this variability. The observed offshore to onshore stress rotation may reflect a change from dominantly compressional tectonics at the deformation front, to a strike‐slip and/or extensional tectonic regime closer to the Taupo Volcanic Zone, further inland. In addition, the offshore stress may be affected by topography and/or stress rotation around subducting seamounts, and/or temporal stress changes during the slow slip cycle. |
领域 | 气候变化 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/315839 |
专题 | 气候变化 |
推荐引用方式 GB/T 7714 | D. D. McNamara,E. Behboudi,L. Wallace,等. Variable in‐situ stress orientations across the northern Hikurangi Subduction Margin[J]. Geophysical Research Letters,2021. |
APA | D. D. McNamara.,E. Behboudi.,L. Wallace.,D. Saffer.,A. E. Cook.,...&K. E. Petronotis.(2021).Variable in‐situ stress orientations across the northern Hikurangi Subduction Margin.Geophysical Research Letters. |
MLA | D. D. McNamara,et al."Variable in‐situ stress orientations across the northern Hikurangi Subduction Margin".Geophysical Research Letters (2021). |
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