Variable In Situ Stress Orientations Across the Northern Hikurangi Subduction Margin
| Autor: | P. Barnes, H. Lee, Effat Behboudi, M. Paganoni, Katerina Petronotis, Leah J. LeVay, David D. McNamara, Ake Fagereng, Ingo Pecher, Heather M. Savage, Laura M. Wallace, Demian M. Saffer, Hung Yu Wu, Ann E. Cook, G. Kim |
|---|---|
| Rok vydání: | 2021 |
| Předmět: |
Accretionary wedge
010504 meteorology & atmospheric sciences Subduction Slip (materials science) 010502 geochemistry & geophysics 01 natural sciences Tectonics Geophysics 13. Climate action Trench General Earth and Planetary Sciences Submarine pipeline Thrust fault Forearc Seismology Geology 0105 earth and related environmental sciences |
| Zdroj: | Geophysical Research Letters |
| ISSN: | 0094-8276 |
| DOI: | 10.1029/2020gl091707 |
| Popis: | 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. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|
Plný text