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The Rhenohercynian Zone or Rheno-Hercynian … The Rhenohercynian Zone or Rheno-Hercynian zone in structural geology describes a fold belt of west and central Europe, formed during the Hercynian orogeny (about 350 to 280 million years ago). The zone consists of folded and thrust Devonian and early Carboniferous sedimentary rocks that were deposited in a back-arc basin along the southern margin of the then existing paleocontinent Laurussia. The Rhenohercynian Zone, named for the Rhine River and the Hercynian Forest of Antiquity, forms a narrow zone through western and central Europe, from Cornwall and Ireland in the west to the Harz mountains of central Germany in the east, including the Rhenish Massif (Ardennes, Taunus, Eifel and Hunsrück). The total length of this ancient basin (the Rhenohercynian Basin) could have been more than 2500 km. In the east the basin merges with the of southern Poland. The sedimentary rocks that were laid down in the basin are often weakly metamorphic (greenschist facies). Most geologists consider the to be a continuation of the zone to the west. Whether the Rhenohercynian Basin was a continuous feature or rather a string of temporaneously interconnected smaller basins is not well understood, because in many places the Devonian and Carboniferous rock strata are covered with younger deposits. Parts of the basin have their own names, like the in Cornwall, the Munster basin in Ireland or the Rhenisch basin in Belgium and Germany.the Rhenisch basin in Belgium and Germany.
, De Rhenohercynische Zone is in de structur … De Rhenohercynische Zone is in de structurele geologie een tektonische zone in het midden en westen van Europa, ontstaan tijdens de Hercynische of Varistische orogenese (ongeveer 350 tot 280 miljoen jaar geleden). De zone bestaat voornamelijk uit Devonische en Carbonische sedimenten die in een voormalige langs de zuidelijke rand van het paleocontinent Euramerika (Noord-Amerika samen met het tegenwoordige Noord- en Midden-Europa) werden afgezet. Dit bekken wordt het Rhenohercynisch Bekken genoemd of soms de Rhenohercynische Oceaan omdat het een smalle oceaan vormde. De zone is meer dan 2500 km lang en loopt in een band door West- en Centraal-Europa, van het zuiden van Ierland, Cornwall, de Ardennen en het Rijnleisteengebergte tot de Harz. Verder naar het oosten gaat de zone over in het van Zuid-Polen. De van Zuid-Portugal wordt door de meeste geologen als een verlengde van de Rhenohercynische Zone gezien. De precieze aard van het Rhenohercynisch Bekken is niet goed bekend omdat de Hercynische structuren op veel plaatsen overdekt worden door jongere gesteenten. Het kan zowel een continu bekken zijn geweest als aparte bekkens die een systeem van horsten en slenken verbonden waren. De verschillende delen van het bekken hebben eigen namen, zoals het Cornwall Basin in Cornwall, het Munster Basin in Ierland of het Rijns Bekken in België en Duitsland.f het Rijns Bekken in België en Duitsland.
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De Rhenohercynische Zone is in de structur … De Rhenohercynische Zone is in de structurele geologie een tektonische zone in het midden en westen van Europa, ontstaan tijdens de Hercynische of Varistische orogenese (ongeveer 350 tot 280 miljoen jaar geleden). De zone bestaat voornamelijk uit Devonische en Carbonische sedimenten die in een voormalige langs de zuidelijke rand van het paleocontinent Euramerika (Noord-Amerika samen met het tegenwoordige Noord- en Midden-Europa) werden afgezet. Dit bekken wordt het Rhenohercynisch Bekken genoemd of soms de Rhenohercynische Oceaan omdat het een smalle oceaan vormde.Oceaan omdat het een smalle oceaan vormde.
, The Rhenohercynian Zone or Rheno-Hercynian … The Rhenohercynian Zone or Rheno-Hercynian zone in structural geology describes a fold belt of west and central Europe, formed during the Hercynian orogeny (about 350 to 280 million years ago). The zone consists of folded and thrust Devonian and early Carboniferous sedimentary rocks that were deposited in a back-arc basin along the southern margin of the then existing paleocontinent Laurussia.he then existing paleocontinent Laurussia.
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Rhenohercynische Zone
, Rhenohercynian Zone
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