The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Phlogopite and K‐amphibole in the upper mantle: Implication for magma genesis in subduction zones
Abstract
High‐pressure phase relations have been examined for phlogopite + diopside with and without enstatite under vapor absent conditions in the pressure range of 5 to 13 GPa and in the temperature range of 1000 to 1300°C. Phlogopite in these systems can be stable up to 6–7 GPa and decomposes through pressure‐dependent reactions to crystallize phases including potassic amphibole. The experimental results suggest that phlogopite, which is one of main hydrous phases in the downdragged hydrated peridotite at the base of mantle wedge, plays an important role in the formation of magmas at the backarc side of a volcanic arc. The existence of potassic amphibole at higher pressure regions may imply the involvement of subduction component in magma generation in the region far away from the trench axis.
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Citations
Cites
Generation of arc basalt magmas and thermal structure of the mantle wedge in subduction zones
Tatsumi, Y., Sakuyama, M., Fukuyama, H., & Kushiro, I. (1983) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb088ib07p05815 · Cited by 529
Self-citation
Cited by
The role of water in the petrogenesis of Mariana trough magmas
Stolper, E., & Newman, S. (1994) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(94)90074-4 · Cited by 768
Physical model of source region of subduction zone volcanics
Davies, J. H., & Stevenson, D. J. (1992) · Journal of Geophysical Research: Solid Earth · doi:10.1029/91jb02571 · Cited by 593
Carminati, E., Lustrino, M., & Doglioni, C. (2012) · Tectonophysics · doi:10.1016/j.tecto.2012.01.026 · Cited by 489
Poli, S., & Schmidt, M. W. (1995) · Journal of Geophysical Research: Solid Earth · doi:10.1029/95jb01570 · Cited by 391
TAPPE, S., FOLEY, S. F., JENNER, G. A., HEAMAN, L. M., KJARSGAARD, B. A., ROMER, R. L., STRACKE, A., JOYCE, N., & HOEFS, J. (2006) · Journal of Petrology · doi:10.1093/petrology/egl008 · Cited by 373
Metadata
- Authors
- Sudo, A., & Tatsumi, Y.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 1990-01
- Volume
- 17
- Issue
- 1
- Pages
- 29-32
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W1965658370
- Cited by
- 178
- References
- 1
- FWCI
- 7.64
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: Phlogopite and K‐amphibole in the upper mantle: Implication for magma genesis in subduction zones. https://app.cochat.ai/papers/10.1029/gl017i001p00029
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- Sudo, A., & Tatsumi, Y. (1990). Phlogopite and K‐amphibole in the upper mantle: Implication for magma genesis in subduction zones. Geophysical Research Letters. https://doi.org/10.1029/gl017i001p00029
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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.
