WebNorthern Corsica exposes a nonmetamorphosed Palaeozoic succession lying on Panafrican mica schist related to a microcontinent (most likely Armorica or from a microcontinent from the Hun superterrane) that had drifted away directly from Gondwana.

Geological Society, London, Special Publications

WebOct 1, 2001 · The cause could have been regional stress reorganization after the collision of the Hun superterrane and Laurussia (Figure 16, frame 3a). However, many previous models (e.g. Robertson and Dixon, 1984) envisage no such Carboniferous rifting along northern Gondwana. Hence, while poor seismic data beneath the Palmyrides prevent … WebApr 15, 2024 · The Proto-Tethys closed in the Silurian at ca. 440–420 Ma when this “Asian Hun superterrane” collided with the northern Gondwana margin. Subsequently, the Lancang Block is interpreted to have separated from the Baoshan Block during the Early Devonian when the Paleo-Tethys opened as a back-arc basin. helsinki vantaa pysäköinti p4

(PDF) Review of Middle East Paleozoic Plate tectonics

Webbined in the so-called Hun (or Hunic or Hunia) superterrane,aspostulatedbyvonRaumer,Stampfli and their co-authors (e.g. von Raumer et al. 2002; Stampfli & Borel 2002, 2004). There is clear consensus on the existence of rifting between core Gondwana and some of its marginal terranes over much of the area to … WebThe Vertiskos Terrane may have been part of the Hun Superterrane, which evolved at the northern active continental margin of Gondwana in the early Palaeozoic and rifted away from it during the opening of the Rheic Ocean in the Cambrian to Silurian. Parts of this superterrane such as the Vertiskos Terrane are present throughout the Variscan and ... WebSep 1, 2010 · The Uchur-Batomga terrane in the east of the Aldan domain again reveals a 2.6 Ga granite-greenstone basement, superimposed by 2.3–1.7 Ga magmatic arc and sedimentary rocks ( Rosen et al., 2006 ), which can be correlated with events in the Mojave orogen of Laurentia. helsinki-vantaa pysäköinti p3