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Perkins, George B., Sharp, Zachary D., Selverstone, Jane (2006) Oxygen isotope evidence for subduction and rift-related mantle metasomatism beneath the Colorado Plateau–Rio Grande rift transition. Contributions to Mineralogy and Petrology, 151 (6) 633-650 doi:10.1007/s00410-006-0075-6

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Reference TypeJournal (article/letter/editorial)
TitleOxygen isotope evidence for subduction and rift-related mantle metasomatism beneath the Colorado Plateau–Rio Grande rift transition
JournalContributions to Mineralogy and Petrology
AuthorsPerkins, George B.Author
Sharp, Zachary D.Author
Selverstone, JaneAuthor
Year2006 (June)Volume151
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-006-0075-6Search in ResearchGate
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Mindat Ref. ID78610Long-form Identifiermindat:1:5:78610:4
GUID0
Full ReferencePerkins, George B., Sharp, Zachary D., Selverstone, Jane (2006) Oxygen isotope evidence for subduction and rift-related mantle metasomatism beneath the Colorado Plateau–Rio Grande rift transition. Contributions to Mineralogy and Petrology, 151 (6) 633-650 doi:10.1007/s00410-006-0075-6
Plain TextPerkins, George B., Sharp, Zachary D., Selverstone, Jane (2006) Oxygen isotope evidence for subduction and rift-related mantle metasomatism beneath the Colorado Plateau–Rio Grande rift transition. Contributions to Mineralogy and Petrology, 151 (6) 633-650 doi:10.1007/s00410-006-0075-6
In(2006, June) Contributions to Mineralogy and Petrology Vol. 151 (6) Springer Science and Business Media LLC

See Also

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Roy, Mousumi, MacCarthy, Jonathan K., Selverstone, Jane (2005) Upper mantle structure beneath the eastern Colorado Plateau and Rio Grande rift revealed by Bouguer gravity, seismic velocities, and xenolith data. Geochemistry, Geophysics, Geosystems, 6 (10) doi:10.1029/2005gc001008
Kil, Y., Wendlandt, R. F. (2007) Depleted and enriched mantle processes under the Rio Grande rift: spinel peridotite xenoliths. Contributions to Mineralogy and Petrology, 154 (2) 135-151 doi:10.1007/s00410-007-0183-y
Perinelli, Cristina, Armienti, Pietro, Dallai, Luigi (2006) Geochemical and O-isotope constraints on the evolution of lithospheric mantle in the Ross Sea rift area (Antarctica) Contributions to Mineralogy and Petrology, 151 (3) 245-266 doi:10.1007/s00410-006-0065-8
Kil, Y., Wendlandt, R. F. (2004) Pressure and temperature evolution of upper mantle under the Rio Grande Rift. Contributions to Mineralogy and Petrology, 148 (3) 265-280 doi:10.1007/s00410-004-0608-9
Selverstone, Jane, Sharp, Zachary D. (2011) Chlorine isotope evidence for multicomponent mantle metasomatism in the Ivrea Zone. Earth and Planetary Science Letters, 310 (3) 429-440 doi:10.1016/j.epsl.2011.08.034
Shaw, C. S., Heidelbach, F., & Dingwell, D. B. (2006). The origin of reaction textures in mantle peridotite xenoliths from Sal Island, Cape Verde: the case for “metasomatism” by the host lava. Contributions to Mineralogy and Petrology, 151(6), 681-697. doi.org/10.1007/s00410-006-0087-2
Porreca, Courtney, Selverstone, Jane, Samuels, Kimberly (2006) Pyroxenite xenoliths from the Rio Puerco volcanic field, New Mexico: Melt metasomatism at the margin of the Rio Grande rift. Geosphere, 2. 333pp. doi:10.1130/ges00058.1
Gurenko, Andrey A., Sobolev, Alexander V. (2006) Crust–primitive magma interaction beneath neovolcanic rift zone of Iceland recorded in gabbro xenoliths from Midfell, SW Iceland. Contributions to Mineralogy and Petrology, 151 (5) 495-520 doi:10.1007/s00410-006-0079-2
Shaw, Cliff S. J., Heidelbach, Florian, Dingwell, Donald B. (2006) The origin of reaction textures in mantle peridotite xenoliths from Sal Island, Cape Verde: the case for “metasomatism” by the host lava. Contributions to Mineralogy and Petrology, 151 (6) 681-697 doi:10.1007/s00410-006-0087-2
Steffen, Kurt J., Selverstone, Jane (2006) Retrieval of P–T information from shear zones: thermobarometric consequences of changes in plagioclase deformation mechanisms. Contributions to Mineralogy and Petrology, 151 (5) 600-614 doi:10.1007/s00410-006-0073-8
Manning, Christina J., Thirlwall, Matthew F. (2014) Isotopic evidence for interaction between Öræfajökull mantle and the Eastern Rift Zone, Iceland. Contributions to Mineralogy and Petrology, 167 (1) doi:10.1007/s00410-013-0959-1
 
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