Logo Logo
Help
Contact
Switch Language to German
Kirscher, U.; Bachtadse, Valerian ORCID: 0000-0002-1226-2986; Mikolaichuk, A. V.; Kroener, A.; Alexeiev, D. V. (2017): Palaeozoic evolution of the North Tianshan based on palaeomagnetic data - transition from Gondwana towards Pangaea. In: International Geology Review, Vol. 59, No. 16: pp. 2003-2020
Full text not available from 'Open Access LMU'.

Abstract

We present new palaeomagnetic data for Cambrian and Ordovician volcanic and sedimentary rocks from the Kyrgyz North Tianshan (NTS) and review available data from the southwestern Central Asian Orogenic Belt (CAOB) to elucidate the tectonic history and evolution of this region during the early Palaeozoic. We observed a coherent evolution of the NTS and the Kazakhstan continent (or Kazakhstania) with a constant northwards movement between the Cambrian and Devonian at approximate to 5cm/a. After the northwards movement ceased in the Devonian, the accreted terrane assemblage of Kazakhstania occupied a stable latitudinal position at approximate to 30 degrees N until the final amalgamation of Eurasia occurred in the late Carboniferous to early Permian. Amalgamation of the Tarim and Turan blocks caused a counterclockwise bending within the southwestern segment of the CAOB, which occurred in an inconsistent way by a brittle-like response of the upper crust with a large variety of rotational movement. We suggest an evolution of the Kyrgyz CAOB terranes by steady migration away from Gondwana and subsequent capture in a zone of global downwelling at similar to 30 degrees N, where accretion and subsequent amalgamation of Eurasia occurred with the CAOB terranes in its centre.