Unraveling the early–middle Paleozoic paleogeography of Kazakhstan on the basis of Ordovician and Devonian paleomagnetic results

• Published in: Gondwana research Vol. 22; no. 3-4; pp. 974 - 991
• Main Authors: Bazhenov, Mikhail L., Levashova, Natalia M., Degtyarev, Kirill E., Van der Voo, Rob, Abrajevitch, Alexandra V., McCausland, Phil J.A.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-11-2012
• Subjects: Accretionary tectonics; Central Asian Orogenic Belt; Kazakhstania; Oroclinal bending; Paleomagnetism; Central Asian Orogenic Belt; Kazakhstania; Oroclinal bending; Paleomagnetism; Accretionary tectonics
• ISSN: 1342-937X; 1878-0571
• DOI: 10.1016/j.gr.2012.02.023

It is a common concept that different tectonic units in the western part of the Central Asian Orogenic Belt were united into the landmass of the Kazakhstania continent in the Paleozoic but many important details of its history remain enigmatic and controversial. Recently published paleomagnetic data from this region demonstrate that the ~2000km long horseshoe-shaped Devonian Volcanic Belt was created by oroclinal bending of an originally rectilinear active margin of Kazakhstania. Still, the Silurian and Devonian paleomagnetic results which this interpretation is based upon are limited and unevenly spread along the belt, and additional middle Paleozoic data are highly desirable. Accordingly, we studied three mid-Paleozoic objects from different segments of this volcanic belt. Two of the three new objects yielded paleomagnetic directions that fit perfectly into the oroclinal scenario, whereas the third one provided no interpretable data. The earlier history of Kazakhstania, however, remains misty. We obtained three new Ordovician results in north–central Kazakhstan and found similar inclinations but widely dissimilar declinations. Previously published data show a large scatter of Ordovician declinations in South Kazakhstan and Kyrgyzstan as well. We analyzed all seven Middle–Late Ordovician paleolatitudes and came to the conclusion that a nearly E–W trending active margin of the Kazakhstania landmass had existed at low (~10°S) latitudes at that time. We hypothesize that this margin of the Kazakhstania landmass collided with another island arc, called Baydaulet–Akbastau, and with the Aktau–Junggar microcontinent by the Ordovician–Silurian boundary. As a result of this collision, subduction ceased, and regional deformation, magmatism, and rotations of crustal fragments took place in most of Kazakhstania. In Silurian time, Kazakhstania moved northward crossing the equator and rotating clockwise by ~45°. This changed the orientation of the Kazakhstania to NW–SE, and thereby established the (rectilinear) predecessor of the modern curved Devonian Volcanic Belt.
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► Five new Middle-Late Devonian and Ordovician paleomagnetic results from the western Central Asian orogenic belt are reported. ► Devonian results fit perfectly into the oroclinal scenario of the Kazakhstan tectonic evolution. ► Paleolatitudes and orientation of the Middle-Late Ordovician active margin of the Kazakhstania landmass are determined. ► A new tectonic scenario of the western Central Asian orogenic belt since mid-Ordovician until mid-Devonian time is proposed.