The DOI matches its Crossref record; 91 of the 91 references it cites were found in a registry or an index.
Fluids in accretionary prisms
Abstract
Subduction zones are the most dynamic tectonic environments on the face of Earth. Most subduction zones are submarine and at many, large accretionary prisms are formed of sediments scraped from the subducting oceanic lithosphere. These prisms grow in a water‐saturated environment; consequently, their tectonic, thermal and chemical evolution is strongly influenced by fluids, and the role of the aqueous phase must be considered in any study in this realm. In view of widespread and growing interest, the North Atlantic Treaty Organization and National Science Foundation sponsored the workshop “The Role of Fluids in Sediment Accretion, Deformation, Diagenesis and Metamorphism at Subduction Zones,” which convened September 19–23, 1988, at Il Ciocco, Tuscany, Italy. This meeting assembled 60 geologists, geochemists and geophysicists representing eight countries whose interests spanned both marine and continental environments.
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Cites
Byerlee, J. (1978) · pure and applied geophysics · doi:10.1007/bf00876528 · Cited by 4,029
DeMets, C., Gordon, R. G., Argus, D. F., & Stein, S. (1990) · Geophysical Journal International · doi:10.1111/j.1365-246x.1990.tb06579.x · Cited by 3,760
Mechanics of fold‐and‐thrust belts and accretionary wedges
Davis, D., Suppe, J., & Dahlen, F. A. (1983) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb088ib02p01153 · Cited by 2,304
ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING
KING HUBBERT, M., & RUBEY, W. W. (1959) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1959)70[115:rofpim]2.0.co;2 · Cited by 2,081
Geologic Analysis of Naturally Fractured Reservoirs
(2001) · Elsevier eBooks · doi:10.1016/b978-0-88415-317-7.x5000-3 · Cited by 1,367
Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks
PLATT, J. P. (1986) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1986)97<1037:doowat>2.0.co;2 · Cited by 1,292
von Huene, R., & Scholl, D. W. (1991) · Reviews of Geophysics · doi:10.1029/91rg00969 · Cited by 1,283
Fluid Processes in Subduction Zones
Peacock, S. M. (1990) · Science · doi:10.1126/science.248.4953.329 · Cited by 989
CRITICAL TAPER MODEL OF FOLD-AND-THRUST BELTS AND ACCRETIONARY WEDGES
Dahlen, F. A. (1990) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.ea.18.050190.000415 · Cited by 848
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Cited by
Fault zone architecture and permeability structure
Caine, J. S., Evans, J. P., & Forster, C. B. (1996) · Geology · doi:10.1130/0091-7613(1996)024<1025:fzaaps>2.3.co;2 · Cited by 2,603
Stern, R. J. (2002) · Reviews of Geophysics · doi:10.1029/2001rg000108 · Cited by 1,517
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
Serpentinization of the forearc mantle
Hyndman, R. D., & Peacock, S. M. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(03)00263-2 · Cited by 907
Kopf, A. J. (2002) · Reviews of Geophysics · doi:10.1029/2000rg000093 · Cited by 869
Metadata
- Authors
- Langseth, M. G., & Casey Moore, J.
- Venue
- Eos, Transactions American Geophysical Union
- Publisher
- American Geophysical Union (AGU)
- Published
- 1990-01-30
- Volume
- 71
- Issue
- 5
- Pages
- 245-246
- ISSN
- 0096-3941 (ISSN-L)
- 2324-9250
- OpenAlex
- W1971534802
- Cited by
- 465
- References
- 91
- FWCI
- 5.98
- 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.
