The DOI matches its Crossref record; 93 of the 93 references it cites were found in a registry or an index.
Fluid Processes in Subduction Zones
Abstract
Fluids play a critical role in subduction zones and arc magmatism. At shallow levels in subduction zones (<40 kilometers depth), expulsion of large volumes of pore waters and CH 4 -H 2 O fluids produced by diagenetic and low-grade metamorphic reactions affect the thermal and rheological evolution of the accretionary prism and provide nutrients for deep-sea biological communities. At greater depths, H 2 O and CO 2 released by metamorphic reactions in the subducting oceanic crust may alter the bulk composition in the overlying mantle wedge and trigger partial melting reactions. The location and conse-quences of fluid production in subduction zones can be constrained by consideration of phase diagrams for relevant bulk compositions in conjunction with fluid and rock pressure-temperature-time paths predicted by numerical heat-transfer models. Partial melting of subducting, amphibole-bearing oceanic crust is predicted only within several tens of million years of the initiation of subduction in young oceanic lithosphere. In cooler subduction zones, partial melting appears to occur primarily in the overlying mantle wedge as a result of fluid infiltration.
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Cites
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Cited by
Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation
Schmidt, M. W., & Poli, S. (1998) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(98)00142-3 · Cited by 1,935
Adakitic magmas: Modern analogues of Archaean granitoids
Martin, H. (1999) · Lithos · doi:10.1016/s0024-4937(98)00076-0 · Cited by 1,642
von Huene, R., & Scholl, D. W. (1991) · Reviews of Geophysics · doi:10.1029/91rg00969 · Cited by 1,283
Bending-related faulting and mantle serpentinization at the Middle America trench
Ranero, C. R., Phipps Morgan, J., McIntosh, K., & Reichert, C. (2003) · Nature · doi:10.1038/nature01961 · Cited by 1,014
Subduction factory: 4. Depth-dependent flux of H 2 O from subducting slabs worldwide
van Keken, P. E., Hacker, B. R., Syracuse, E. M., & Abers, G. A. (2011) · Journal of Geophysical Research · doi:10.1029/2010jb007922 · Cited by 949
Metadata
- Authors
- Peacock, S. M.
- Venue
- Science
- Published
- 1990-04-20
- Volume
- 248
- Issue
- 4953
- Pages
- 329-337
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2026889131
- Cited by
- 989
- References
- 93
- FWCI
- 21.60
- Type
- journal article
- Language
- en
- Open access
- closed
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
