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Neoproterozoic volcanics and granitoids formed at Rodinia margins within a time span of 880Ma-700Ma, are well-documented in many terranes of the southern Central Asian Orogenic Belt (CAOB). Ages younger than 550Ma corresponding to the opening of the Terskey Ocean are also common. However, so far, there were very few published ages in the range 700Ma-550Ma from the Kyrgyz Tien Shan. In this paper we...
The Tien Shan (Tianshan) orogen formed during Late Palaeozoic collision between the Karakum–Tarim continent and the Paleo-Kazakhstan continent, a Caledonian component of the Altaid Collage. The Southern Tien Shan terrane represents an intensely deformed fold and thrust belt formed after the final closure of the Paleo-Turkestan ocean. In the Late Carboniferous–Early Permian the Tien Shan was affected...
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