The DOI matches its Crossref record; 35 of the 35 references it cites were found in a registry or an index.
Generic model of subduction erosion
Abstract
Erosion by high stress abrasion of convergent margins from bursts and grabens on the subducting plate is not shown in seismic images. In a proposed model, the frontal sediment prism is a dynamic mass that elevates pore-fluid pressure. Overpressured fluid invades fractures in the upper plate and separates fragments that are dragged into a subduction channel along the plate interface., Removed fragments are smaller than surface ship seismic techniques have resolved and beyond the reach of past scientific ocean drilling; however, current drill capability and downhole geophysics can test the model.
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Citations
Cites
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
Eos, Transactions American Geophysical Union
(2018) · Eos · doi:10.1002/(issn)2324-9250 · Cited by 1,659
Back‐arc opening and the mode of subduction
Uyeda, S., & Kanamori, H. (1979) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb084ib03p01049 · Cited by 1,286
von Huene, R., & Scholl, D. W. (1991) · Reviews of Geophysics · doi:10.1029/91rg00969 · Cited by 1,283
Relations among subduction parameters
Jarrard, R. D. (1986) · Reviews of Geophysics · doi:10.1029/rg024i002p00217 · Cited by 1,044
Clift, P., & Vannucchi, P. (2004) · Reviews of Geophysics · doi:10.1029/2003rg000127 · Cited by 906 · cited 1×
“Convergent margins dominated by subduction erosion are the most prevalent type (von Huene and Scholl, 1991; Clift and Vannucchi, 2004), but the processes shaping them are scarcely understood.”
BackgroundSelf-citationSubduction erosion along the Middle America convergent margin
Ranero, C. R., & von Huene, R. (2000) · Nature · doi:10.1038/35008046 · Cited by 561
Self-citationCloos, M., & Shreve, R. L. (1988) · pure and applied geophysics · doi:10.1007/bf00874549 · Cited by 514
Moore, J. C., & Saffer, D. (2001) · Geology · doi:10.1130/0091-7613(2001)029<0183:ulotsz>2.0.co;2 · Cited by 481
Yáñez, G. A., Ranero, C. R., von Huene, R., & Díaz, J. (2001) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2000jb900337 · Cited by 382
Self-citation
Cited by
Formation of enriched mantle components by recycling of upper and lower continental crust
Willbold, M., & Stracke, A. (2010) · Chemical Geology · doi:10.1016/j.chemgeo.2010.06.005 · Cited by 310
Wakabayashi, J. (2015) · International Geology Review · doi:10.1080/00206814.2014.998728 · Cited by 260
Yin and yang of continental crust creation and destruction by plate tectonic processes
Stern, R. J., & Scholl, D. W. (2010) · International Geology Review · doi:10.1080/00206810903332322 · Cited by 254
Coseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquake.
Kodaira, S., No, T., Nakamura, Y., Fujiwara, T., Kaiho, Y., Miura, S., Takahashi, N., Kaneda, Y., & Taira, A. (2012) · Nature Geoscience · doi:10.1038/ngeo1547 · Cited by 222
Santosh, M., & Kusky, T. (2010) · Terra Nova · doi:10.1111/j.1365-3121.2009.00914.x · Cited by 224
Metadata
- Authors
- von Huene, R., Ranero, C. R., & Vannucchi, P.
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2004
- Volume
- 32
- Issue
- 10
- Pages
- 913
- ISSN
- 0091-7613 (ISSN-L)
- OpenAlex
- W2162447099
- Cited by
- 396
- References
- 35
- FWCI
- 7.38
- 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.
