Paleoaltimetry and paleotectonic reconstruction using triple oxygen and hydrogen isotopes: Depleted δ18O and δD values in ignimbrites of Verkhneavachinskaya caldera record collisional uplift during Miocene arc accretion to Kamchatka

Author:

Vialichka Kseniya,Bindeman Ilya N.,Bergal-Kuvikas Olga,Rogozin Alexei

Funder

National Science Foundation

Publisher

Elsevier BV

Reference71 articles.

1. Collision of the Kronotskiy arc at the NE Eurasia margin and structural evolution of the Kamchatka–Aleutian junction;Alexeiev;Int. J. Earth Sci.,2006

2. The geodynamic conditions for the generation of adakites and Nb-rich basalts (NEAB) in Kamchatka;Avdeiko;Volcanol. Seismol.,2015

3. Evolution of the Kurile-Kamchatkan volcanic arcs and dynamics of the Kamchatka-Aleutian Junction;Avdeiko;Volcanism and Subduction: The Kamchatka Region,2007

4. Stratigraphy, structure, and geology of late Miocene Verkhneavachinskaya Caldera with basaltic-andesitic ignimbrites at Eastern Kamchatka;Bergal-Kuvikas;J. Geosci.,2019

5. The analysis of spatial distributions, origins of caldera-forming eruptions with basaltic-andesitic magma compositions, and genesis of Miocene ignimbrites of the Eastern volcanic belt, Kamchatka;Bergal-Kuvikas;Geodynamics & Tectonophysics,2019

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