Palaeomagnetic study of the Karacadag Volcanic Complex, SE Turkey: Monitoring Neogene anticlockwise rotation of the Arabian Plate

Abstract

The Karacadak Volcanic Centre in south east Turkey is a major basaltic complex sited at the northern margin of the Arabian Plate and emplaced in several pulses between similar to 11 Ma and Late Quaternary times. We have sampled 71 sites in lavas of this complex to constrain the palaeomagnetic record and hence the chronology of magmatic activity and regional rotation. Palaeomagnetic study at sixty two sites yields significant component definition with mixed normal and reversed polarities. From age dating and morphologic criteria we identify three major episodes of lava emplacement and site mean directions of magnetisation for these divisions resolve migration of the palaeofield direction for the northern sector of the Arabian Plate since mid-Miocene times. Successive (reversed polarity) group mean directions are: D/I = 175 degrees/-50.5 degrees (N = 37, R = 33.13, alpha(95) = 4.1 degrees) for the oldest (Siverek) division (mean age estimate 11.1-6.7 Ma), D/I = 173.4 degrees/-46.0 degrees (N = 16, R = 15.67, alpha(95) = 5.5 degrees) for the middle (Karacadak) division (mean age 33 Ma) and D/I = 167.7 degrees/-47.6 degrees (N = 6, R = 5.93, alpha(95) = 7.9 degrees) for the youngest (Ovabag) division (similar to 1.9 Ma present). The first two results merit a tectonic interpretation and consistent anticlockwise rotation of similar to 9 degrees is recognised in the Karacadag Volcanic Centre between similar to 11 and 3.3 Ma. The mean directions conform to palaeomagnetic results from other undeformed Neogene igneous complexes of comparable age range further to the west along the northern perimeter of the Arabian Plate. The amount of tectonic rotation observed in late Pliocene and older volcanic units from this plate is found to be statistically-constant Tectonism responsible for rotation therefore appears to have been temporally-confined to the last similar to 2 Myr which is long after collision with the Anatolides and closure of the Bitlis suture. This conclusion conforms to the young distributed block rotations recognised in the Anatolides and Aegean and correlates with the regime of tectonic escape of terranes to the west. (C) 2013 Elsevier B.V. All rights reserved.