Post-Miocene Deformation in the South of the Galatean Volcanic Province, NW of Central Anatolia (Turkey)

2008-01-01
Central Anatolia, located on the immense Alpine-Himalayan orogenic belt, has a complicated neotectonic evolution, and NE-SW-trending Neogene horsts-graben systems that rejuvenate pre-existing palaeostructures are among the most important structures which help us understand the tectonic evolution of Central Anatolia.
TURKISH JOURNAL OF EARTH SCIENCES

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Citation Formats
F. B. Rojay, “Post-Miocene Deformation in the South of the Galatean Volcanic Province, NW of Central Anatolia (Turkey),” TURKISH JOURNAL OF EARTH SCIENCES, pp. 653–672, 2008, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/53650.