1977
DOI: 10.1130/0016-7606(1977)88<1305:lpsfis>2.0.co;2
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Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Result of a right-lateral shear zone between the Appalachians and the Urals

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Cited by 724 publications
(299 citation statements)
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“…The general interpretation of the western Tethys in this figure is based on Ziegler and Stampfli (2001), Ziegler (1988), Stampfli and Borel (2002) and Ford and Golonka (2003). Some of the basins of Iberia were the result of reactivation of ancient Hercynian faults (Arthaud and Matte, 1977;Alvaro et aI., 1979;Ziegler, 1988;Arche and L6pez-G6mez, 1996), representing the initial phase of post-Variscan plate reorganization. This initial break-up of Pangea was related to a series of strike-slip fuults that dissected the Variscan foldbelt and its associated foreland areas.…”
Section: During Latest Pennian-earliest Triassic Times Thementioning
confidence: 94%
“…The general interpretation of the western Tethys in this figure is based on Ziegler and Stampfli (2001), Ziegler (1988), Stampfli and Borel (2002) and Ford and Golonka (2003). Some of the basins of Iberia were the result of reactivation of ancient Hercynian faults (Arthaud and Matte, 1977;Alvaro et aI., 1979;Ziegler, 1988;Arche and L6pez-G6mez, 1996), representing the initial phase of post-Variscan plate reorganization. This initial break-up of Pangea was related to a series of strike-slip fuults that dissected the Variscan foldbelt and its associated foreland areas.…”
Section: During Latest Pennian-earliest Triassic Times Thementioning
confidence: 94%
“…This megastructure wa s origi nated during a continent-{;ontinent collision between the North Ame rica (Laurentia) Plate, Fennoscandia Plate, se veral South Europe Mic roplates and Africa Plate. Deformation took place in several phases (Late Devonian-Late Carboniferous) (Arthaud and Matte, 1977;Dewey and Burke, 19 73;Nicholls, 1974, 1984) and led to crustal shortening and thick ening, regional metamorphism and widespread gran itization (Matte, 1986).…”
Section: The Hercynian Basementmentioning
confidence: 99%
“…Since the works of Arthaud and Matte (1977), it is generally accepted that the Iberian Microplate was part of a dextral megashear zone between the South ern Appalachians and the Urals, just after the Her cynian Orogenesis (Stephanian-Autunian). Using a simple Riedel di agram (Fig.…”
Section: The Orientation Of the Iberian Basin And Its Relations With mentioning
confidence: 99%
“…However, we agree with the suggestion of Gaetani et al (2005), who suggested strike-slip movements in this region. They might have been related to the activity of the major shear zone located just to the north of the Western Caucasus (Arthaud and Matte, 1977;Ruban and Yoshioka, 2005;Tawadros et al, 2006).…”
Section: Western Caucasusmentioning
confidence: 99%