Synchronism in compression of the lithosphere in the central Atlantic and Western Tethys at the Tortonian-Messinian transition

Author:

Knipper A. L.,Raznitsin Yu. N.

Publisher

Pleiades Publishing Ltd

Subject

Geology

Reference45 articles.

1. G. V. Agapova, “Morphology of the Interrift S o Paulo Fracture Zone (Equatorial Atlantic),” Okeanologiya 334(1), 107–112 (1994).

2. E. A. Denisova, “Ultramafic Mylonites of St. Paul Island (Equatorial Atlantic),” Dokl. Akad. Nauk 319(5), 1167–1172 (1991).

3. A. O. Mazarovich, Geological Structure of the Central Atlantic: Faults, Volcanic Structure, and Deformations of the Oceanic Floor (Nauchnyi Mir, Moscow, 2000) [in Russian].

4. A. O. Mazarovich, S. Yu. Sokolov, G. V. Agapova, et al., “Computer Technologies As an Instrument for Obtaining New Data on the Structure of Oceanic Fracture Zones (with Reference to Active Part of the S o Paulo Fracture Zone, Central Atlantic),” Ros. Zh. Nauk Zemle 3(1) (2001) (Electronic Version on the Centre of Geophysical Survey Site).

5. E. E. Milanovsky, “Neotectonic Stage of the Earth’s Evolution: Its Time Span and the Main Tectonic Deformations, Morphogenesis, Magmatism, and Geodynamics,” in Proceedings of XXIX Tectonic Conference (GEOS, Moscow, 1996) [in Russian], p. 169.

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