M
Mary R. Reid
Researcher at Northern Arizona University
Publications - 61
Citations - 4530
Mary R. Reid is an academic researcher from Northern Arizona University. The author has contributed to research in topics: Basalt & Mantle (geology). The author has an hindex of 35, co-authored 58 publications receiving 4248 citations. Previous affiliations of Mary R. Reid include University of California, Los Angeles.
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Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas
Douglas W. Burbank,John Leland,Eric J. Fielding,Robert S. Anderson,Nicholas Brozovic,Mary R. Reid,Chris Duncan +6 more
TL;DR: The topography of tectonically active mountain ranges reflects a poorly understood competition between bedrock uplift and erosion as mentioned in this paper, and the Indus river incises through the bedrock at extremely high rates (2-12 mm yr-1).
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Prolonged residence times for the youngest rhyolites associated with Long Valley Caldera:230Th—238U ion microprobe dating of young zircons
TL;DR: In this paper, a new ion microprobe method for dating magmatic zircon growth was proposed based on in situ measurement of the magnitude of 238U-230Th disequilibrium.
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Geochemistry of primary and least fractionated lavas from Okmok Volcano, Central Aleutians: Implications for arc magmagenesis
Christopher J. Nye,Mary R. Reid +1 more
TL;DR: In this article, it was shown that the melting zone is localized by impingement on the subforearc mantle wedge, that is, the melting zones (and thus the location of the volcanic front) is localized for physical rather than physiochemical reasons.
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In situ U-Pb ages of zircons from the Bishop Tuff: No evidence for long crystal residence times
TL;DR: In this paper, a microprobe U-Pb isotope analysis of zircons from fallout and intercalated ash-flow deposits of the early, most chemically evolved Bishop Tuff (east-central California) yield a weighted mean age of 823 ± 11 ka (mean square of weighted deviates, MSWD = 0.8; n = 22).
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Zircon-scale insights into the history of a Supervolcano, Bishop Tuff, Long Valley, California, with implications for the Ti-in-zircon geothermometer
TL;DR: In this article, an ion microprobe approach reveals that Bishop zircon rims with diverse chemical characteristics surround intermediate domains with broadly similar compositions and therefore it is possible that there was no significant thermal gradient in the magma reservoir at some stage in its evolution.