Search Results - "Anthony, Elizabeth Y."

The evolution of spinel lherzolite xenoliths and the nature of the mantle at Kilbourne Hole, New Mexico by Perkins, Dexter, Anthony, Elizabeth Y.

“…In peridotites, olivine, clinopyroxene, and orthopyroxene are complex solid solutions with wide stability fields. Depending mostly on bulk composition and…”
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Geodynamic evolution of a forearc rift in the southernmost Mariana Arc by Ribeiro, Julia M., Stern, Robert J., Martinez, Fernando, Ishizuka, Osamu, Merle, Susan G., Kelley, Katherine, Anthony, Elizabeth Y., Ren, Minghua, Ohara, Yasuhiko, Reagan, Mark, Girard, Guillaume, Bloomer, Sherman

“…The southernmost Mariana forearc stretched to accommodate opening of the Mariana Trough backarc basin in late Neogene time, erupting basalts at 3.7–2.7 Ma that…”
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Seismic anisotropy of the uppermost mantle beneath the Rio Grande rift: Evidence from Kilbourne Hole peridotite xenoliths, New Mexico by Satsukawa, Takako, Michibayashi, Katsuyoshi, Anthony, Elizabeth Y., Stern, Robert J., Gao, Stephen S., Liu, Kelly H.

“…Peridotite xenoliths from the Kilbourne Hole maar, New Mexico, consist of spinel lherzolite, harzburgite, and dunite. Because Kilbourne Hole erupted at…”
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Uppermost mantle anisotropy beneath the southern Laurentian margin: Evidence from Knippa peridotite xenoliths, Texas by Satsukawa, Takako, Michibayashi, Katsuyoshi, Raye, Urmidola, Anthony, Elizabeth Y., Pulliam, Jay, Stern, Robert

“…Peridotite xenoliths from southern Texas consist of spinel lherzolite, harzburgite and minor dunite. Based on phase relations and temperature of equilibration,…”
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Architecture of a 1.38–1.34 Ga granite–rhyolite complex as revealed by geochronology and isotopic and elemental geochemistry of subsurface samples from west Texas, USA by Barnes, Melanie A, Anthony, Elizabeth Y, Williams, Ian, Asquith, George B

“…During the evolution of Laurentia, a Mesoproterozoic felsic igneous belt extended from Fennoscandia through Canada to the southwestern United States. This…”
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Elemental fingerprinting of Kenya Rift Valley ochre deposits for provenance studies of rock art and archaeological pigments by Zipkin, Andrew M., Ambrose, Stanley H., Hanchar, John M., Piccoli, Philip M., Brooks, Alison S., Anthony, Elizabeth Y.

“…The Kenya Rift Valley contains many ochre sources that are currently used by indigenous peoples for adornment, rituals, and art. Ochre pigments occur in rock…”
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Open System evolution of peralkaline trachyte and phonolite from the Suswa volcano, Kenya rift by White, John Charles, Espejel-García, Vanessa V., Anthony, Elizabeth Y., Omenda, Peter

“…Suswa is the southernmost volcanic center in the Central Kenya Peralkaline Province (CKPP) and represents the only salic center to have erupted significant…”
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Source regions of granites and their links to tectonic environment: examples from the western United States by Anthony, Elizabeth Y.

“…This review, in honor of Ilmari Haapala's retirement, reflects on lessons learned from studies of three granitic systems in western North America: (1)…”
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Patterns of element mobility during hydrothermal alteration of the Sierrita porphyry copper deposit, Arizona by Anthony, Elizabeth Y, Titley, Spencer R

“…The geology is reviewed, and the petrography is described. Analytical methods and results are discussed. The data are tabulated, plotted and discussed…”
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Application of the QUILF thermobarometer to the peralkaline trachytes and pantellerites of the Eburru volcanic complex, East African Rift, Kenya by Ren, Minghua, Omenda, Peter A., Anthony, Elizabeth Y., White, John C., Macdonald, Ray, Bailey, D.K.

“…The Quaternary Eburru volcanic complex in the south-central Kenya Rift consists of pantelleritic trachytes and pantellerites. The phenocryst assemblage in the…”
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Geodynamic evolution of a forearc rift in the southernmost M ariana A rc by Ribeiro, Julia M., Stern, Robert J., Martinez, Fernando, Ishizuka, Osamu, Merle, Susan G., Kelley, Katherine, Anthony, Elizabeth Y., Ren, Minghua, Ohara, Yasuhiko, Reagan, Mark, Girard, Guillaume, Bloomer, Sherman

“…The southernmost M ariana forearc stretched to accommodate opening of the M ariana T rough backarc basin in late N eogene time, erupting basalts at 3.7–2.7 Ma…”
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