Fluid Pressure Changes Recorded by Trace Elements in Quartz
Abstract Fluid pressure is a key parameter in earthquake mechanics, controlling seismic failure and plate coupling in convergent zones. Yet fluid pressure is also extremely difficult to quantify at seismogenic depth, which limits our knowledge of the stress state in accretionary prisms. Here, we sho...
Gorde:
| Egile Nagusiak: | , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Wiley
2022-10-01
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| Saila: | Geochemistry, Geophysics, Geosystems |
| Gaiak: | |
| Sarrera elektronikoa: | https://doi.org/10.1029/2022GC010346 |
| Etiketak: |
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