The Year Leading to a Supereruption.
Supereruptions catastrophically eject 100s-1000s of km3 of magma to the surface in a matter of days to a few months. In this study, we use zoning in quartz crystals from the Bishop Tuff (California) to assess the timescales over which a giant magma body transitions from relatively quiescent, pre-eru...
Main Authors: | Guilherme A R Gualda, Stephen R Sutton |
---|---|
Format: | Article |
Language: | English |
Published: |
Public Library of Science (PLoS)
2016-01-01
|
Series: | PLoS ONE |
Online Access: | http://europepmc.org/articles/PMC4954661?pdf=render |
Similar Items
-
Post-supereruption recovery at Toba Caldera
by: Adonara E. Mucek, et al.
Published: (2017-05-01) -
Understanding the What, When, Where, and Why of Supereruptions
by: Pamukcu, Ayla Susan
Published: (2014) -
The potential impacts of a sulfur- and halogen-rich supereruption such as Los Chocoyos on the atmosphere and climate
by: H. Brenna, et al.
Published: (2020-06-01) -
Petrochemical Constraints on Generation of the Peach Spring Tuff Supereruption Magma, Arizona, Nevada, and California
by: Frazier, William Oliver
Published: (2013) -
Textural and Geochemical Investigation of the Peach Spring Tuff CA-NV-AZ: Evidence for Dynamic Pre-Supereruption Processes
by: Foley, Michelle Lee
Published: (2017)