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Autor:
Joris M. Gieskes, Annette Deyhle, Guram I. Buachidze, Klaus Wallmann, Anton Eisenhauer, Vasili Yu. Lavrushin, Achim J Kopf, Boris G. Polyak
Publikováno v:
International Journal of Earth Sciences. 92:407-425
The Caucasian orogenic wedge formed as a consequence of the closure of the Tethyan Ocean, and numerous fields of active mud volcanoes pepper the area adjacent to the Black and Caspian Seas. Stable isotope ratios of boron, helium, and carbon have been