Geological and Geophysical Studies of the Charlie Gibbs Fracture Zone (North Atlantic)
Autor: | Enrico Bonatti, K. N. Sholukhov, Filippo Muccini, A. N. Ivanenko, I. A. Veklich, V. N. Dobrolybov, S. G. Skolotnev, A. A. Razumovskii, Camilla Palmiotto, Valentin Basch, Alessio Sanfilippo, Lorenzo Petracchini, Marco Cuffaro, Camilla Sani, K. O. Dobrolybova, S. Yu. Sokolov, Yago Nestola, Y. V. Brusilovsky, Carlotta Ferrando, Alexander A Peyve, Marco Ligi, A. N. Pertsev, A. S. Bich |
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Rok vydání: | 2021 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences North Atlantic Transform fault Fracture zone Charlie Gibbs transform fault megatransform system Detailed data Geophysics 010502 geochemistry & geophysics 01 natural sciences Mantle (geology) Ridge Earth and Planetary Sciences (miscellaneous) General Earth and Planetary Sciences System structure Geology 0105 earth and related environmental sciences |
Zdroj: | Doklady earth sciences (Online) 497 (2021): 191–194. doi:10.1134/S1028334X21030107 info:cnr-pdr/source/autori:Skolotnev S.G.; Sanfilippo A.; Peyve A.A.; Nestola Y.; Sokolov S.Y.; Petracchini L.; Dobrolybova K.O.; Basch V.; Pertsev A.N.; Ferrando C.; Ivanenko A.N.; Sani C.; Razumovskii A.A.; Muccini F.; Bich A.S.; Palmiotto C.; Brusilovsky Y.V.; Bonatti E.; Sholukhov K.N.; Cuffaro M.; Veklich I.A.; Ligi M.; Dobrolybov V.N./titolo:Geological and Geophysical Studies of the Charlie Gibbs Fracture Zone (North Atlantic)/doi:10.1134%2FS1028334X21030107/rivista:Doklady earth sciences (Online)/anno:2021/pagina_da:191/pagina_a:194/intervallo_pagine:191–194/volume:497 |
ISSN: | 1531-8354 1028-334X |
Popis: | The geological and geophysical data obtained during the 50th cruise of R/V Akademik Nikolaj Strakhov on the Charlie Gibbs megatransform system structure in the North Atlantic are presented. The structure of the Charlie Gibbs Fracture Zone was examined in detail, considering previously published data. It has been shown that the northern and southern segments of the Mid-Atlantic Ridge, separated by the Charlie Gibbs transform fault, are entirely different in morphology, and hence in terms of formation. The dredged rocks are represented by an entire spectrum from the mantle to upper crustal varieties and allow us to determine the origin of the main structures of the Charlie Gibbs megatransform system considering detailed data on the morphology. |
Databáze: | OpenAIRE |
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