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The Sarmatian Craton or Sarmatia is the so … The Sarmatian Craton or Sarmatia is the southern segment/region of the East European Craton or Baltica, also known as Scythian Plateau. The craton contains Archaean rocks 2.8 to 3.7 billion years old (Ga). During the Carboniferous the craton was rifted apart by the Dnieper-Donets rift. As a result, geomorphologically the cratonic area is split by the Donbass Fold Belt, also known as a part of the large Pripyat-Dniepr-Donets aulacogen, which transects Sarmatia, dividing it into the Ukrainian Massif or shield on the southwest and the Voronezh Massif to the northeast. Sarmatia is made up of several once-independent Archaean land masses that formed respectively at 3.7–2.9, 3.6–2.8, 3.2–3.0, and 2.7–2.6 Ga. These are separated by a series of 2.2–2.1 Ga orogenic belts. Sarmatia's northwestern margin has an extensive continental magmatic arc dating back to 2.0–1.95 Ga. The Ukrainian Shield and Voronezh Massif are the exposed areas of the Sarmatian Craton. The craton can be divided into Archaean (c. 3.7–2.7 Ga) terranes separated by Palaeoproterozoic (c. 2.2–2.1 Ga and 2.0–1.9 Ga) belts. The Osnitsk-Mikashevichi Belt in the northwest is 150–200 km (93–124 mi)-wide and extends for more than 1,000 km (620 mi) from the Trans-European Suture Zone to Moscow. It is exposed only in the northwest corner of the Ukrainian Shield and in the Pripyat Trough (west of the Devonian Dniepr–Donets Aulacogen). Although mostly hidden beneath Phanerozoic sedimentary rocks the belt can be traced magnetically. The presence of granitic batholiths intruded by diorites and gabbros at c. 1.98–1.95 Ga and hypabbysal and metavolcanic rocks dated to 2.02 Ga indicate the Osnitsk-Mikashevichi Belt formed at an Andes-type active margin along which 2.0–1.95 Ga-old oceanic crust subducted. This subduction was followed by a calm period after which Sarmantia and Fennoscandia collided c. 1.84–1.82 Ga. The Palaeoproterozoic Volyn Domain is made of 2.06–2.02 Ga-old granitoids emplaced within the 2.2 Ga-old, strongly deformed rocks of the Teterev–Belaya Tserkov belt. The area was strongly deformed at 1.98–1.95 Ga but it can be interpreted as a setting of intense volcanism and sedimentation in a coastal-marine environment in which island arcs reused detritus from Archaean sources.The 1.80–1.74 Ga-old Korosten pluton in northern Ukraine formed from a succession of volcanism. It was originally believed to be an anorogenic process fueled by mantle underplating. More recently, however, it has been demonstrated that the Korosten pluton is not made of mantle-derived igneous material but from the lower crust of the Osnitsk-Mikashevichi Belt extruded in the Central Belarus Suture Zone. The Podolian Domain in southern Sarmantia is made mostly of Archaean-Palaeoproterozoic granulites (up to 3.7 Ga) and divided by major faults into the Vinnitsa and Gayvoron regions.Archaean charnockite intrusions are common in the southeast. Exposed rocks in western Sarmantia are 10–15 km (6.2–9.3 mi)-thick Archaean to Palaeoproterozoic crust. Granulites in southern Sarmantia were exhumed from a depth of at least 35 km (22 mi). The Golovanevsk Suture Zone in the east contains almost 3.0 Ga-old igneous rocks. The oldest rocks are probably derived from early Archaean oceanic crust.derived from early Archaean oceanic crust.
, Il cratone sarmatico o Sarmatia, è il segm … Il cratone sarmatico o Sarmatia, è il segmento meridionale del cratone dell'Europa Orientale o Baltica. È citato a volte anche come piattaforma scitica. Il cratone contiene rocce risalenti all'Archeano che hanno un'età compresa tra 3,7 e 2,8 miliardi di anni. Nel corso del Carbonifero, il cratone fu staccato dal rift Dnieper-Donets. Ne risulta che da un punto di vista geomorfologico l'area del cratone è suddivisa dalla cintura del Donbass, che fa parte del più esteso aulacogeno del Pripyat-Dniepr-Donets che attraversa la Sarmatia, suddividendola nello scudo ucraino a sudovest e nel a nordest. scudo ucraino a sudovest e nel a nordest.
, Le craton sarmatique est un terme employé … Le craton sarmatique est un terme employé en géologie et en tectonique pour désigner la moitié méridionale du ou plateau de Scythie. Ce craton est constitué de roches archéennes formées entre 3,7 et 2,8 milliards d'années. Durant la période du Carbonifère, le craton s'est scindé sous l'action du . C'est pourquoi le relief est divisé par la chaîne du Donbass, qui est une composante de l’aulacogène Pripyat-Dniepr-Donets : on trouve ainsi le bouclier ukrainien au sud-ouest et le au nord-est. Le craton Sarmatia est formé de plusieurs masses continentales autrefois séparées, apparues aux premiers âges de la Terre. Elles sont séparées par une série de couronnes orogéniques apparues entre 2,2 et 2,1 milliards d'années. La périphérie nord-ouest de Sarmatia comporte un arc magmatique continental étendu apparu entre 2 et 1,95 milliard d'années. Il y a environ 200 millions d'années, Sarmatia est entrée en collision avec la plaque fennoscandienne. collision avec la plaque fennoscandienne.
, Kraton sarmacki, Sarmacja – kraton stanowi … Kraton sarmacki, Sarmacja – kraton stanowiący obecnie południową część większego kratonu wschodnioeuropejskiego. Kraton sarmacki jest zbudowany z kilku masywów archaicznych, powstałych w okresach 3,7-2,9 mld lat temu, 3,2-3,0 mld lat temu i około 2,7 mld lat temu. Masywy te zostały połączone w toku ruchów górotwórczych w okresie 2,3-2,1 mld lat temu. Cokół kratonu zawiera skały o wieku 3,7-2,8 mld lat. Północno-zachodni skraj kratonu zawiera szeroki kontynentalny łuk wulkaniczny sprzed 2,0 mld lat. Powstały w karbonie aulakogen dnieprowsko-doniecki podzielił kraton sarmacki na część południowo-zachodnią – tarczę ukraińską i północno-wschodnią – , rozdzielone doniecką strukturą fałdową. Około 2 mld lat temu Sarmacja zderzyła się z płytą bałtycką (Fennoskandią). W wyniku kolizji doszło do zespolenia tych jednostek i powstania kratonu wschodnioeuropejskiego. powstania kratonu wschodnioeuropejskiego.
, Sarmatia ist eines der drei Kratonfragmente Balticas. Es enthält im Ukrainischen Schild die ältesten Gesteine Europas aus dem Eoarchaikum.
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Le craton sarmatique est un terme employé … Le craton sarmatique est un terme employé en géologie et en tectonique pour désigner la moitié méridionale du ou plateau de Scythie. Ce craton est constitué de roches archéennes formées entre 3,7 et 2,8 milliards d'années. Durant la période du Carbonifère, le craton s'est scindé sous l'action du . C'est pourquoi le relief est divisé par la chaîne du Donbass, qui est une composante de l’aulacogène Pripyat-Dniepr-Donets : on trouve ainsi le bouclier ukrainien au sud-ouest et le au nord-est. ukrainien au sud-ouest et le au nord-est.
, Kraton sarmacki, Sarmacja – kraton stanowi … Kraton sarmacki, Sarmacja – kraton stanowiący obecnie południową część większego kratonu wschodnioeuropejskiego. Kraton sarmacki jest zbudowany z kilku masywów archaicznych, powstałych w okresach 3,7-2,9 mld lat temu, 3,2-3,0 mld lat temu i około 2,7 mld lat temu. Masywy te zostały połączone w toku ruchów górotwórczych w okresie 2,3-2,1 mld lat temu. Cokół kratonu zawiera skały o wieku 3,7-2,8 mld lat. Północno-zachodni skraj kratonu zawiera szeroki kontynentalny łuk wulkaniczny sprzed 2,0 mld lat.ntalny łuk wulkaniczny sprzed 2,0 mld lat.
, The Sarmatian Craton or Sarmatia is the so … The Sarmatian Craton or Sarmatia is the southern segment/region of the East European Craton or Baltica, also known as Scythian Plateau. The craton contains Archaean rocks 2.8 to 3.7 billion years old (Ga). During the Carboniferous the craton was rifted apart by the Dnieper-Donets rift. As a result, geomorphologically the cratonic area is split by the Donbass Fold Belt, also known as a part of the large Pripyat-Dniepr-Donets aulacogen, which transects Sarmatia, dividing it into the Ukrainian Massif or shield on the southwest and the Voronezh Massif to the northeast. and the Voronezh Massif to the northeast.
, Sarmatia ist eines der drei Kratonfragmente Balticas. Es enthält im Ukrainischen Schild die ältesten Gesteine Europas aus dem Eoarchaikum.
, Il cratone sarmatico o Sarmatia, è il segm … Il cratone sarmatico o Sarmatia, è il segmento meridionale del cratone dell'Europa Orientale o Baltica. È citato a volte anche come piattaforma scitica. Il cratone contiene rocce risalenti all'Archeano che hanno un'età compresa tra 3,7 e 2,8 miliardi di anni. Nel corso del Carbonifero, il cratone fu staccato dal rift Dnieper-Donets. Ne risulta che da un punto di vista geomorfologico l'area del cratone è suddivisa dalla cintura del Donbass, che fa parte del più esteso aulacogeno del Pripyat-Dniepr-Donets che attraversa la Sarmatia, suddividendola nello scudo ucraino a sudovest e nel a nordest. scudo ucraino a sudovest e nel a nordest.
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Cratone sarmatico
, Craton sarmatique
, Sarmatia (Kraton)
, Kraton sarmacki
, Sarmatian Craton
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