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Characterization of plagioclase-hosted melt inclusions in A91-1R (Blanco Transform Fault)
Drignon, Melissa J; Nielsen, Roger L; Bodnar, Robert J; Tepley, Frank J
doi:10.1594/IEDA/111270
01/24/2019
We present a database characterizing the composition and volatile contents of plagioclase-hosted melt inclusions from a unique sample from the Blanco Transform Fault (A91-1R). The melt inclusions were homogenized on a 1-atm vertical furnace at two temperatures from 30 min to 4 days to gain a better understanding of the post entrapment processes induced by the homogenization experiments. The composition and volatile contents of the melt inclusions indicate their mantle origins.
Drignon, Melissa J; Nielsen, Roger L; Bodnar, Robert J; Tepley, Frank J (2019): Characterization of plagioclase-hosted melt inclusions in A91-1R (Blanco Transform Fault). Interdisciplinary Earth Data Alliance (IEDA). http://dx.doi.org/10.1594/IEDA/111270. Accessed 21 March 2019.
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Edited_IEDAA911Rdatabase.xls363.5 KB

Chemistry, Petrology:Experimental
Comma-separated list not exceeding 200 characters; please do not use carriage return/line breaks
plagioclase-hosted melt inclusions, spreading ridge, volatiles, chemistry
English
Collection
Drignon, Melissa J.; Nielsen, Roger L.; Tepley, Frank J. III; Bodnar, Robert J., (2018), "Upper Mantle Origin of Plagioclase Megacrysts from Plagioclase Ultraphyric MORB". Geology, 47(1): 43-46.

Drignon, Melissa J.; Nielsen, Roger L.; Tepley, Frank J. III; Bodnar, Robert J., (2019), "Reequilibration processes occurring in plagioclase-hosted melt inclusions from plagioclase ultraphyric basalts", Geochemistry, Geophysics, Geosystems, 10.1029/2018GC007795.
doi:10.1130/G45542.1
NSF (1634206), NSF (1634211)
Spatial Coverage Information
Regional (Continents, Oceans)
Pacific Ocean, Blanco Fracture Zone
Contributor Information
Melissa Drignon
Oregon State University
CEOAS
Corvallis
License Information
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]