Pliocene tourmaline rhyolite dykes from Ikaria Island in the Aegean back-arc region: geodynamic implications-Reference-Cited by-同舟云学术

Pliocene tourmaline rhyolite dykes from Ikaria Island in the Aegean back-arc region: geodynamic implications

Published:2009-08 Issue:4 Volume:22 Page:189-199
ISSN:0985-3111
Container-title:Geodinamica Acta
language:en
Short-container-title:Geodinamica Acta

Author:

Baltatzis Emmanuel¹,Kostopoulos Dimitrios¹,Godelitsas Athanassios¹,Zachariadis Panagiotis²,Papanikolaou Dimitrios¹

Affiliation:

1. a National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Mineralogy and Petrology , Panepistimioupoli Zographou, 15784 , Athens , Greece

2. b Institut für Geowissenschsften , Johannes Gutenberg-Universität , Becherweg 21, 55099 , Mainz , Germany

Publisher

Informa UK Limited

Subject

Earth-Surface Processes,Geophysics

Link

https://www.tandfonline.com/doi/pdf/10.3166/ga.22.189-199

Reference66 articles.

1. The Aegean Sea

2. Timing, kinematics and cause of Aegean extension: a scenario based on a comparison with simple analogue experiments

3. Subduction, convergence and the mode of backarc extension in the Mediterranean region

4. Active tectonics of the Alpine--Himalayan belt: the Aegean Sea and surrounding regions

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