Initiation of large-volume silicic centers in the Yellowstone hotspot track: insights from H2O- and F-rich quartz-hosted rhyolitic melt inclusions in the Arbon Valley Tuff of the Snake River Plain-Reference-Cited by-同舟云学术

Initiation of large-volume silicic centers in the Yellowstone hotspot track: insights from H2O- and F-rich quartz-hosted rhyolitic melt inclusions in the Arbon Valley Tuff of the Snake River Plain

Published:2016-01 Issue:1 Volume:171 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Drew Dana L.,Bindeman Ilya N.,Loewen Matthew W.,Wallace Paul J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-015-1210-z.pdf

Reference87 articles.

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2. Almeev R, Bolte T, Nash B, Holtz F, Erdmann M, Cathey H (2012) High-temperature, low-H2O Silicic Magmas of the Yellowstone Hotspot: an Experimental Study of Rhyolite from the Bruneau–Jarbidge Eruptive Center, Central Snake River Plain, USA. J Petrol 53(9):1837–1866

3. Anders M, Saltzman J, Hemming S (2009) Neogene tephra correlations in eastern Idaho and Wyoming; Implications for Yellowstone hotspot-related volcanism and tectonic activity. Geol Soc Am Bull 121(5–6):837–856

4. Anders MH, Rodgers DW, Hemming SR, Saltzman J, DiVenere VJ, Hagstrum JT, Embree GF, Walter RC (2014) A fixed sublithospheric source for the late Neogene track of the Yellowstone hotspot: implications of the Heise and Picabo volcanic fields. J Geophys Res Solid Earth 119:2871–2906

5. Anderson AT, Davis AM, Fangqiong L (2000) Evolution of Bishop Tuff rhyolitic magma based on melt and magnetite inclusions and zoned phenocrysts. J Petrol 41(3):449–473

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