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A Jurassic volcanic passive margin in Iran and Turkey

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Date

2022

Author

Azizi, Hossein
Stern, Robert J.
Kandemir, Raif
Karslı, Orhan

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Citation

Azizi, H., Stern, R.J., Kandemir, R. & KArsli, O. (2022). A Jurassic volcanic passive margin in Iran and Turkey. Terra Nova. https://doi.org/10.1111/ter.12638

Abstract

Broadly similar Early to Middle Jurassic stratigraphic sequences including bimodal igneous rocks of the Sanandaj–Sirjan Zone of Iran and the Sakarya Zone of Turkey suggest that these formed in a common tectonic setting in an extensional basin that evolved from a terrestrial magmatic rift to a marine shelf and passive continental margin. Whole-rock chemistry and Sr–Nd isotope signatures indicate derivation of mafic melts from partial melting of the subcontinental lithosphere. Decompression associated with extension led to 5%–30% partial melting of spinel–garnet lherzolite with minor involvement of continental crust, producing tholeiitic to transitional basaltic magma. Extensional basins inverted during the Mid-Late Jurassic. These relationships suggest the Early to Middle Jurassic formation of a volcanic rifted margin on the SW Eurasian margin, similar to that of offshore Norway.

Source

Terra Nova

Volume

35

Issue

3

URI

https://doi.org/10.1111/ter.12638
https://hdl.handle.net/11436/7373

Collections

  • Jeoloji Mühendisliği Bölümü Koleksiyonu [78]
  • Scopus İndeksli Yayınlar Koleksiyonu [5931]



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