The Evolution of the Rheic OceanFrom Avalonian-cadomian Active Margin to Alleghenian-variscan Collision
- 592 Pages
- May 30, 2007
- 1.13 MB
- 794 Downloads
Geological Society of Amer
Earth Sciences - Geology, Science, Geology, Stratigraphic, Paleozoic, Plate tectonics, Rifts (Geology), Science/Mathem
|Contributions||Ulf Linnemann (Editor), R. Damian Nance (Editor), Petr Kraft (Editor), Gernold Zulauf (Editor)|
|The Physical Object|
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The Rheic Ocean was an ocean which separated two major palaeocontinents, Gondwana and Laurussia (Laurentia-Baltica-Avalonia).One of the principal oceans of the Palaeozoic, its sutures today stre km (6, mi) from Mexico to Turkey and its closure resulted in the assembly of the supercontinent Pangaea and the formation of the Variscan–Alleghenian–Ouachita orogenies.
The evolution of the Rheic Ocean is consequently central not only to the history of the Palaeozoic, but also to the broader issue of supercontinent assembly (e.g., Murphy et al.,Santosh et al., ).
Download: Download full-size image; Fig. Early Silurian reconstruction of the Rheic Ocean immediately prior to the closure of Iapetus Cited by: Geological evolution of middle to late Paleozoic rocks in the Avalon terrane of northern mainland Nova Scotia, Canadian Appalachians: a record of tectonothermal activity along the northern margin of the Rheic Ocean in the Appalachian-Caledonide orogen.
Christian Pin, Jarmila Waldhausrová, "Sm-Nd isotope and trace element study of Late Proterozoic metabasalts (“spilites”) from the Central Barrandian domain (Bohemian Massif, Czech Republic)", The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision, Ulf Linnemann, R.
Damian Nance, Petr Kraft, Gernold Zulauf. "Structural evolution of the Prague synform (Czech Republic) during Silurian times: An AMS, rock magnetism, and paleomagnetic study of the Svatý Jan pod Skalou dikes. Consequences for the nappes emplacement", The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision, Ulf Linnemann, R.
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Damian. Sven O. Egenhoff, "Life and death of a Cambrian–Ordovician basin: An Andean three-act play featuring Gondwana and the Arequipa-Antofalla terrane", The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision, Ulf Linnemann, R.
Damian Nance, Petr Kraft, Gernold Zulauf. The evolution of the Rheic Ocean is consequently central not only to the history of the Palaeozoic, but also to the broader issue of supercontinent assembly (e.g., Murphy et al.
The evolution of the Rheic Ocean: From Avalonian-Cadomian active margin to Alleghenian-Variscan collision: Boulder, Colorado, Geological Society of America Special Paperdoi: /(21). The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision Transition from B- to A-type subduction during closing of the Rheic remnant ocean: New geochronologic and geochemical data marking Acadian-Neoacadian orogenesis and accretion of the Carolina superterrane, southern Appalachians.
Highlights The Rheic Ocean separated Gondwana and Laurussia as the principal interior ocean of the Paleozoic. Its evolution dominates the geology of southern The Evolution of the Rheic Ocean book, eastern North America and northern Africa following the closure of the Iapetus Ocean in the Silurian.
Closure of the Rheic Ocean in the late Paleozoic created the vast Ouachita-Appalachian-Variscan orogen and assembled. The Rheic Ocean is the most significant Paleozoic ocean that detached peri-Gondwana terranes from the northern Gondwana margin throughout the closure of the Iapetus Ocean. The suture of the Rheic Ocean spreads from Mexico to the Middle East, and the timing of its final closure is well-documented by the rocks formed in the Variscan-Alleghanian.
Journals & Books; Register Sign in. These facies are associated with the evolution of the northern Gondwana epeiric sea margin of the Rheic Ocean and can tell us how ocean chemistry changed and the paleoceanographic factors involved in this particular transition of the ocean record.
We conducted an integrated study based on sedimentology. Other articles where Rheic Ocean is discussed: Silurian Period: Gondwana: Europe (Baltica) is called the Rheic Ocean and was essentially a southwestern extension of the Paleotethys Sea. The flooded margin of eastern Australia had a more-varied seafloor topography than the other shallow seas because of the extensive volcanism occurring there during Silurian time, but it shared many of the.
Granite emplacement and sediment deposition can be related to the separation of the Avalonia microterrane from the northern Gondwana margin. Amphibolite protoliths of the Randamphibolit-Serie emplaced at c. They show N-MORB to E-MORB signatures, pointing to their formation along an oceanic spreading centre within the Rheic ocean.
Palaeozoic evolution. The ocean formed when Pannotia disintegrated, Proto-Laurasia (Laurentia, Baltica, and Siberia) rifted away from a supercontinent that would become Gondwana.
Proto-Tethys formed between these two supercontinents. The ocean was bordered by Panthalassic Ocean to the north, separating it from Panthalassa by island arcs and. is a platform for academics to share research papers.
Get this from a library. The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to Alleghenian-Variscan collision. [Ulf Linnemann;] -- "This Special Paper includes 29 papers presented at several meetings of the International Geoscience Programme (IGCP) Project "The Rheic Ocean: Its origin, evolution and correlatives." The Rheic.
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The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to Alleghenian-Variscan collision in SearchWorks catalog. N2 - The Rheic Ocean, which separated Laurussia from Gondwana following the closure of Iapetus, is arguably the most important ocean of the Palaeozoic.
Its suture extends from Mexico to Turkey and its closure produced the climactic Variscan–Alleghanian–Ouachita orogeny that assembled the supercontinent, Pangaea.
Evolution of the Rheic Ocean R. Damian Nance a, ⁎, Gabriel Gutiérrez-Alonso b, J.
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Duncan Keppie c, Ulf Linnemann d, J. Brendan Murphy e, Cecilio Quesada f, Rob A. Strachan g, Nigel H. Exposures of volcanic rocks (El Castillo) in the Central Iberian Zone near Salamanca, Spain, are representative of Paleozoic volcanic activity along the northern Gondwanan passive margin.
Description The Evolution of the Rheic Ocean FB2
Alkaline basalts and mafic volcaniclastic rocks of this sequence are structurally preserved in the core of the Variscan-Tamames Syncline. On the basis of the occurrence of graptolite fossils in immediately. Ohio University geologist Damian Nance and his colleagues are trying to bring more attention to the Rheic in a new book published by the Geological Society of America called The Evolution of the Rheic Ocean.
Call it the ocean that time forgot. About million years ago, the Rheic Ocean played a big role in Earth s history.
The Rheic Ocean, which separated Laurussia from Gondwana following the closure of Iapetus, is arguably the most important ocean of the Palaeozoic. Its suture extends from Mexico to Turkey and its closure produced the climactic Variscan–Alleghanian–Ouachita orogeny that assembled the supercontinent, Pangaea.
Following protracted Cambrian rifting that represented a continuum from. PDF | On Jan 1,U. Linnemann and others published The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to Alleghanian-Variscan collision | Find, read and cite all the.
LA-MC-ICP-MS U-Pb zircon ages and whole-rock geochemical data obtained from volcanic rocks erupted in the northern margin of Gondwana provide new insights on the polyphase magmatic evolution of the NW Iberian domain during the establishment of passive margin conditions in Lower Paleozoic times.
The U-Pb data show crystallization ages of ca. Ma for two calc-alkaline rhyolites sampled in the. The book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective and discusses how Iberia played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys s.l.
and Eurasian plates over the last Ma of Earth’s history. The Rheic Ocean: Origin, evolution, and significance. Fixation and redistribution of arsenic during early and late diagenesis in the organic matter-rich members of the Lockatong Formation, Newark basin, USA: implications for the quality of groundwater.
Call it the ocean that time forgot. About million years ago, the Rheic Ocean played a big role in Earth’s history. When this massive body of water closed, the Appalachians were lifted to.
Adopting a global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the.
Buy Evidence of the Rheic Ocean in south-central Mexico: The tectonothermal history of the northwestern Acatlán Complex (La Noria) on FREE SHIPPING on qualified orders. Nance RD, Gutiérrez-Alonso G, Keppie JD et al () Evolution of the Rheic Ocean.
Gondwana Res – doi: / Article Google Scholar.The Vila de Cruces ophiolite: A remnant of the early Rheic Ocean in the Variscan suture of Galicia (northwest Iberian Massif) () Journal of Geology, (2), pp.DOI /The subject of the age of the earth and the age of the world ocean is a matter of extreme importance.
If there is evidence for an old ocean, then this could be used to support the evolutionist's supposition that life arose from primitive, inorganic marine chemicals over a billion years ago. If, however, the world ocean can be shown to be a relatively youthful feature, then the evolutionist.
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