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Philippot, Pascal, Selverstone, Jane (1991) Trace-element-rich brines in eclogitic veins: implications for fluid composition and transport during subduction. Contributions to Mineralogy and Petrology, 106 (4) 417-430 doi:10.1007/bf00321985

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Reference TypeJournal (article/letter/editorial)
TitleTrace-element-rich brines in eclogitic veins: implications for fluid composition and transport during subduction
JournalContributions to Mineralogy and Petrology
AuthorsPhilippot, PascalAuthor
Selverstone, JaneAuthor
Year1991 (February)Volume106
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00321985Search in ResearchGate
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Mindat Ref. ID76594Long-form Identifiermindat:1:5:76594:3
GUID0
Full ReferencePhilippot, Pascal, Selverstone, Jane (1991) Trace-element-rich brines in eclogitic veins: implications for fluid composition and transport during subduction. Contributions to Mineralogy and Petrology, 106 (4) 417-430 doi:10.1007/bf00321985
Plain TextPhilippot, Pascal, Selverstone, Jane (1991) Trace-element-rich brines in eclogitic veins: implications for fluid composition and transport during subduction. Contributions to Mineralogy and Petrology, 106 (4) 417-430 doi:10.1007/bf00321985
In(1991, February) Contributions to Mineralogy and Petrology Vol. 106 (4) Springer Science and Business Media LLC

See Also

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Philippot, Pascal, Chevallier, Pierre, Chopin, Christian, Dubessy, Jean (1995) Fluid composition and evolution in coesite-bearing rocks (Dora-Maira massif, Western Alps): implications for element recycling during subduction. Contributions to Mineralogy and Petrology, 121 (1) 29-44 doi:10.1007/s004100050088
Selverstone, Jane, Franz, Gerhard, Thomas, Sabine, Getty, Stephen (1992) Fluid variability in 2 GPa eclogites as an indicator of fluid behavior during subduction. Contributions to Mineralogy and Petrology, 112 (2) 341-357 doi:10.1007/bf00310465
Ayers, John (1998) Trace element modeling of aqueous fluid - peridotite interaction in the mantle wedge of subduction zones. Contributions to Mineralogy and Petrology, 132 (4) 390-404 doi:10.1007/s004100050431
Selverstone, Jane, Munoz, James L. (1987) Fluid heterogeneities and hornblende stability in interlayered graphitic and nongraphitic schists (Tauern Window, Eastern Alps) Contributions to Mineralogy and Petrology, 96 (4) 426-440 doi:10.1007/bf01166688
Selverstone, Jane (1982) Fluid inclusions as petrogenetic indicators in granulite xenoliths, Pali-Aike volcanic field, Chile. Contributions to Mineralogy and Petrology, 79 (1) 28-36 doi:10.1007/bf00376958
Ault, Alexis K., Selverstone, Jane (2008) Microtextural constraints on the interplay between fluid–rock reactions and deformation. Contributions to Mineralogy and Petrology, 156 (4) 501-515 doi:10.1007/s00410-008-0298-9
Liebscher, Axel (2004) Decoupling of fluid and trace element release in subducting slab? Comment on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes” by C. Spandler et al. (Contrib Mineral Petrol 146:205–222, 2003) Contributions to Mineralogy and Petrology, 148 (4) 502-505 doi:10.1007/s00410-004-0614-y
Watson, E. Bruce (1991) Diffusion in fluid-bearing and slightly-melted rocks: experimental and numerical approaches illustrated by iron transport in dunite. Contributions to Mineralogy and Petrology, 107 (4) 417-434 doi:10.1007/bf00310677
Baumgartner, L. P., Rumble, D. (1988) Transport of stable isotopes: I: Development of a kinetic continuum theory for stable isotope transport. Contributions to Mineralogy and Petrology, 98 (4) 417-430 doi:10.1007/bf00372362
Rustioni, Greta, Audetat, Andreas, Keppler, Hans (2021) The composition of subduction zone fluids and the origin of the trace element enrichment in arc magmas. Contributions to Mineralogy and Petrology, 176 (7) doi:10.1007/s00410-021-01810-8
Beitter, Thorsten, Wagner, Thomas, Markl, Gregor (2008) Formation of kyanite–quartz veins of the Alpe Sponda, Central Alps, Switzerland: implications for Al transport during regional metamorphism. Contributions to Mineralogy and Petrology, 156 (6) 689-707 doi:10.1007/s00410-008-0310-4
 
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