Late Miocene transcurrent tectonics in NW Turkey: evidence from palaeomagnetism and 40Ar–39Ar dating of alkaline volcanic rocks

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Date

2007-2-9

Author

KAYMAKCI, N.
Kaymakcı, Nuretdin
LANGEREIS, C.
SPELL, T. L.
GURER, O. F.
ZANETTI, K. A.

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A number of intra-continental alkaline volcanic sequences in NW Turkey were emplaced along localized extensional gaps within dextral strike-slip fault zones prior to the initiation of the North Anatolian Fault Zone. This study presents new palaeomagnetic and 40Ar–39Ar geochronological results from the lava flows of NW Turkey as a contribution towards understanding the Neogene–Quaternary tectonic evolution of the region and possible roles of block rotations in the kinematic history of the region. 40Ar–39Ar analyses of basalt groundmass indicate that the major volume of alkaline lavas of NW Turkey spans about 4 million years of episodic volcanic activity. Palaeomagnetic results reveal clockwise rotations as high as 73° in Thrace and 33° anticlockwise rotations in the Biga Peninsula. Movement of some of the faults delimiting the areas of lava flows and the timing of volcanic eruptions are both older than the initiation age of the North Anatolian Fault Zone, implying that the region experienced transcurrent tectonics during Late Miocene to Pliocene times and that some of the presently active faults in the region are reactivated pre-existing structures.

Subject Keywords

Palaeomagnetism, Block rotation, 40Ar–39Ar ages, Alkaline volcanism, NW Turkey, Strikeslip faulting, North Anatolian Fault Zone

URI

https://hdl.handle.net/11511/28480

Journal

Geological Magazine

DOI

https://doi.org/10.1017/s0016756806003074

Collections

Department of Geological Engineering, Article

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Citation Formats

N. KAYMAKCI, N. Kaymakcı, C. LANGEREIS, T. L. SPELL, O. F. GURER, and K. A. ZANETTI, “Late Miocene transcurrent tectonics in NW Turkey: evidence from palaeomagnetism and 40Ar–39Ar dating of alkaline volcanic rocks,” Geological Magazine, pp. 379–392, 2007, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/28480.