Growth of intra-caldera lava domes controlled by various modes of caldera collapse, the Štiavnica volcano–plutonic complex, Western Carpathians-Reference-Cited by-同舟云学术

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Growth of intra-caldera lava domes controlled by various modes of caldera collapse, the Štiavnica volcano–plutonic complex, Western Carpathians

Published:2016-02 Issue: Volume:311 Page:183-197
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Tomek Filip,Žák Jiří,Holub František V.,Chlupáčová Marta,Verner Kryštof

Funder

Czech Science Foundation

Charles University

Czech Academy of Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference110 articles.

1. Caldera types: how end-members relate to evolutionary stages of collapse;Acocella;Geophys. Res. Lett.,2006

2. Understanding caldera structure and development: an overview of analogue models compared to natural calderas;Acocella;Earth Sci. Rev.,2007

3. Geologic evolution of the Donguinyó–Huichapan caldera complex, central Mexican Volcanic Belt, Mexico;Aguirre-Díaz;J. Volcanol. Geotherm. Res.,2009

4. Crease structures: indicators of emplacement rates and surface stress regimes of lava flows;Anderson;Geol. Soc. Am. Bull.,1992

5. Analogue and numerical modelling of shape fabrics: application to strain and flow determination in magmas;Arbaret;Trans. Roy. Soc. Edinb. Earth Sci.,2000

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