Nature and significance of a Cambro-Ordovician high-K, calc-alkaline sub-volcanic suite: the late- to post-orogenic Motru Dyke Swarm (Southern Carpathians, Romania)-Reference-Cited by-同舟云学术

Nature and significance of a Cambro-Ordovician high-K, calc-alkaline sub-volcanic suite: the late- to post-orogenic Motru Dyke Swarm (Southern Carpathians, Romania)

Published:2007-03-14 Issue:3 Volume:97 Page:479-496
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Féménias Olivier,Berza Tudor,Tatu Mihai,Diot Hervé,Demaiffe Daniel

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-007-0178-y.pdf

Reference68 articles.

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4. Akay E, Erdogan B (2004) Evolution of neogene calc-alkaline to alkaline volcanism in the Aliaga-Foça region (Western Anatolia, Turkey). J Asian Earth Sci 24(3):367–387. doi: 10.1016/j.jseaes.2004.01.015

5. Berza T (1978) Studiul mineralogic şi petrografic al masivului granitoid de Tismana. An Inst Geol Geofiz LIII:5–176

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