‘Snake River (SR)-type’ volcanism at the Yellowstone hotspot track: distinctive products from unusual, high-temperature silicic super-eruptions

Author:

Branney M. J.,Bonnichsen B.,Andrews G. D. M.,Ellis B.,Barry T. L.,McCurry M.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference115 articles.

1. Andrews GDM (2006) The emplacement and deformation of high-temperature tuffs: a structural analysis of the Grey’s Landing ignimbrite, Snake River Plain, Idaho. PhD thesis, University of Leicester, UK

2. Andrews GDM, Branney MJ (2005) Folds, fabrics, and kinematic criteria in rheomorphic ignimbrites of the Snake River Plain, Idaho: insights into emplacement and flow. Geol Soc Am Field Guide 6:311–328

3. Andrews GDM, Branney MJ, Bonnichsen B (2007) Volcanic stratigraphy and eruption history of the voluminous high-grade ignimbrites and tephra deposits of the Rogerson Graben, Snake River Plain, Idaho. Bull Volcanol (this issue)

4. Bennett VC, DePaolo DJ (1987) Proterozoic crustal history of the western United States as determined by neodymium isotopic mapping. Geol Soc Amer Bull 99:674–685

5. Bonnichsen B (1982) Rhyolite lava flows in the Bruneau-Jarbidge Eruptive Centre, southwestern Idaho. In: Bonnichsen B, Breckenridge RM (eds) Cenozoic Geology of Idaho. Idaho Bur Mines Geol Bull 26:283–320

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