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'Bretonian' contraction-dominated deformation in Central Armorica caused by the docking of the Léon microcontinental Block at the southern margin of the Rheic Ocean

机译：莱昂微型大陆块在莱茵河南缘的对接导致中阿莫里卡的“布雷顿尼亚式”收缩为主变形

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status: published

机译：状态：已发布

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Sintubin Manuel; Berwouts Isaac; Muchez Philippe; Van Noorden Michiel;
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年度 2009
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1. Late Devonian-early Carboniferous contraction-dominated deformation in Central Armorica (Monts d'Arree, Brittany, France) and its relationship with the closure of the Rheic Ocean [J] . Sintubin M, van Noorden M, Berwouts I Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth . 2008,第1a4期

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2. Ordovician-Silurian rift-passive margin on the Mexican margin of the Rheic Ocean overlain by Carboniferous-Permian periarc rocks: Evidence from the eastern Acatlan Complex, southern Mexico [J] . Morales-Gamez M, Keppie JD, Norman M Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth . 2008,第1a4期

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3. Geochemistry and Sm-Nd isotopic systematics of Ediacaran-Ordovician, sedimentary and bimodal igneous rocks in the western Acatlan Complex, southern Mexico: Evidence for rifting on the southern margin of the Rheic Ocean [J] . Carlos Ortega-Obregon, J. Brendan Murphy, J. Duncan Keppie Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry . 2010,第1a2期

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'Bretonian' contraction-dominated deformation in Central Armorica caused by the docking of the Léon microcontinental Block at the southern margin of the Rheic Ocean

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