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rheic ocean (249) 249
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Tectonophysics, ISSN 0040-1951, 2008, Volume 461, Issue 1-4, pp. 9 - 20
.... Consequently, the Gondwana margin has to be subdivided into a more western domain, where the future Avalonian blocks will be separated from Gondwana by the opening Rheic Ocean, whereas in its eastern... 
Palaeotethys | Rheic Ocean | Extensional crust | Subsidence | Early Palaeozoic | Gondwana margin | PRE-ALPINE BASEMENT | METAMORPHIC EVOLUTION | CENTRAL IBERIAN ZONE | BOHEMIAN MASSIF | WESTERN ALPS | GEOCHEMISTRY & GEOPHYSICS | ORDOVICIAN MAGMATISM | OSSA-MORENA ZONE | U-PB ZIRCON | TEPLA-BARRANDIAN UNIT | GEODYNAMIC EVOLUTION | Earth | Crust | Analysis | Rockslides | Detritus | Tectonics (Geology) | Quartzite | Sandstone | Erosion
Journal Article
地学前缘:英文版, ISSN 1674-9871, 2012, Volume 3, Issue 2, pp. 125 - 135
The Rheic Ocean was one of the most important oceans of the Paleozoic Era. It lay between Laurentia and Gondwana from the Early Ordovician and closed to produce the vast Ouachita- Alleghanian-Variscan orogen during the assembly of Pangea... 
古生代 | 冈瓦纳大陆 | 大陆边缘 | 大黄 | 历史 | 新元古代 | 海洋 | 早奥陶世 | Pangea | Rheic Ocean | North America | Europe | Variscan-Alleghanian-Ouachita orogen | BOHEMIAN MASSIF | SAXO-THURINGIAN ZONE | SOUTHERN MEXICO | ROCKS | NORTHERN | GEOSCIENCES, MULTIDISCIPLINARY | PERI-GONDWANAN TERRANES | ACATLAN COMPLEX | CONSTRAINTS | NOVA-SCOTIA | TECTONIC EVOLUTION
Journal Article
Journal Article
Geology, ISSN 0091-7613, 01/2007, Volume 35, Issue 1, pp. 53 - 56
.... As with other Devonian ophiolites in the European Variscan belt, it was generated within a contracting Rheic Ocean... 
NW Spain | Devonian ophiolite | Rheic Ocean | Suprasubduction | Galicia | ZIRCON | BOHEMIAN MASSIF | CENTRAL-EUROPE | VARISCAN BELT | GEOPHYSICAL INVESTIGATIONS | EXHUMATION | MARGIN | BOUNDARIES | GEOLOGY | suprasubduction | PALEOZOIC AMALGAMATION | TECTONIC EVOLUTION | Ophiolites | Ocean bottom | Research
Journal Article
Journal Article
International journal of earth sciences : Geologische Rundschau, ISSN 1437-3254, 2012, Volume 102, Issue 2, pp. 415 - 433
Journal Article
Journal Article