Tectonotype of nonvolcanic passive margins in the Iberia-Newfoundland region

Author:

Melankholina E. N.

Publisher

Pleiades Publishing Ltd

Subject

Geology

Reference73 articles.

1. A. L. Knipper and A. Ya. Sharas’kin, “Exhumation of Upper-Mantle and Lower Crustal Rocks through Rifting,” Geotektonika 32(5), 19–31 (1998) [Geotectonics 32 (5), 354–365 (1998)].

2. E. N. Melankholina, “Tectonotype of Volcanic Passive Margins in the Norwegian-Greenland Region,” Geotektonika 42(3), 73–96 (2008) [Geotectonics 42 (3), 225–244 (2008)].

3. Yu. M. Pushcharovsky, “Tectonic Phenomena of Oceans,” in Basic Problems of General Tectonics (Nauchnyi Mir, Moscow, 2001), pp. 174–230 [in Russian].

4. A. Afilhado, L. Matias, H. Shiobara, et al., “From Unthinned Continent to Ocean: The Deep Structure of the West Iberia Passive Continental Margin at 38° N,” Tectonophysics 458(1/4), 9–50 (2008).

5. T. M. Alves, C. Moita, F. Sandnes, et al., “Mesozoic-Cenozoic Evolution of North Atlantic Continental-Slope Basins: The Peniche Basin, Western Iberian Margin,” Amer. Assoc. Petrol. Geol. Bull. 90(1), 31–60 (2006).

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