Mid-Cretaceous extensional magmatism in the Alborz Mountains, north Iran, geochemistry and geochronology of Gasht-Masuleh gabbros

0576201 - GLÚ 2024 RIV CH eng J - Článek v odborném periodiku
Rezaei, L. - Timmerman, M. J. - Moazzen, M. - Altenberger, U. - Sláma, Jiří - Sudo, M. - Günter, C. - Wilke, F. D. H. - Schleicher, A. M.
Mid-Cretaceous extensional magmatism in the Alborz Mountains, north Iran, geochemistry and geochronology of Gasht-Masuleh gabbros.
Swiss Journal of Geosciences. Roč. 116, č. 1 (2023), č. článku 14. ISSN 1661-8726. E-ISSN 1661-8734
Institucionální podpora: RVO:67985831
Klíčová slova: Gabbro * Mid-Cretaceous * Extension * Gasht-Masuleh * Alborz Mountains * North Iran
Obor OECD: Geology
Impakt faktor: 3.1, rok: 2022
Způsob publikování: Open access
https://sjg.springeropen.com/articles/10.1186/s00015-023-00443-2

In the Gasht-Masuleh area in the Alborz Mountains, gabbroic magma intruded Palaeozoic metasediments and Mesozoic sediments and crystallised as isotropic and cumulate gabbros. LREE enrichment points to relatively low degrees of mantle melting and depletion of Ti, Nb and Ta relative to primitive mantle points to an arc related component in the magma. Clinopyroxene compositions indicate MORB to arc signatures. U–Pb zircon crystallisation ages of 99.5 ± 0.6 Ma and 99.4 ± 0.6 Ma and phlogopite ⁴⁰Ar/³⁹Ar ages of 97.1 ± 0.4 Ma, 97.5 ± 0.4 Ma, 97.1 ± 0.1 Ma, within 2σ error, indicate that gabbro intrusion occurred in the (Albian-)Cenomanian (mid-Cretaceous). As active subduction did not take place in the Cretaceous in North Iran, the small volume mafic magmatism in the Gasht-Masuleh area must be due to local, extension-related mantle melting. Melting was most likely caused by far field effects triggered by roll-back of the Neo-Tethys subducting slab. As subduction took place at a distance of ~ 400 km (present distance) from the Alborz Mountains, the observed arc geochemical signatures must be inherited from a previous subduction event and concomitant mantle metasomatism, possibly in combination with contamination of the magma by crustal material.
Trvalý link: https://hdl.handle.net/11104/0345792