The Petrogenesis of Saricimen (caldiran-Van) Quartz Monzodiorite: Implication for Initiation of Magmatism (Late Medial Miocene) in the East Anatolian Collision Zone, Turkey
| dc.authorscopusid | 6603134081 | |
| dc.authorscopusid | 6701725950 | |
| dc.contributor.author | Colakoglu, Ali Riza | |
| dc.contributor.author | Arehart, Greg B. | |
| dc.date.accessioned | 2025-05-10T16:48:58Z | |
| dc.date.available | 2025-05-10T16:48:58Z | |
| dc.date.issued | 2010 | |
| dc.department | T.C. Van Yüzüncü Yıl Üniversitesi | en_US |
| dc.department-temp | [Colakoglu, Ali Riza] Yuzuncu Yil Univ, Dept Geol Engn, TR-65080 Van, Turkey; [Arehart, Greg B.] Univ Nevada, Dept Geol Sci, Reno, NV 89557 USA | en_US |
| dc.description.abstract | The Saricimen porphyry is exposed as a sub-volcanic pluton within the Upper Cretaceous ophiolitic rocks in East Anatolian Accretionary Complex. The pluton is quartz monzodioritic in composition consisting of feldspar, hornblende, and biotite phenocrysts set in a fine-grained matrix. Major element geochemistry indicates the pluton is of high-K, calc-alkaline, metaluminous character, with a low (0.81-0.90) Aluminum Saturation Index (ASI). Trace element and sulfur isotope geochemistry suggests that the Sancimen porphyry was mantle-derived and contaminated by crustal materials during ascent. Tectonically, this and related volcanic and plutonic rocks in eastern Turkey and Iran are subduction-related and comprise the earliest documented neotectonic igneous activity associated with the final closure of the neo-Tethys between the Arabian and Eurasia plates at similar to 14-13 Ma. (C) 2010 Elsevier B.V. All rights reserved. | en_US |
| dc.description.sponsorship | TUBITAK [107Y339] | en_US |
| dc.description.sponsorship | K-Ar dating analyses of this paper was supported by TUBITAK project no.: 107Y339. Prof. Dr. Simon Poulson (Reno University, Nevada-USA) is thanked for his efforts during S isotopic analyses. Finally, the authors appreciate the useful comments and suggestions made by Editor Nelson Eby and the referees. | en_US |
| dc.description.woscitationindex | Science Citation Index Expanded | |
| dc.identifier.doi | 10.1016/j.lithos.2010.08.014 | |
| dc.identifier.endpage | 620 | en_US |
| dc.identifier.issn | 0024-4937 | |
| dc.identifier.issn | 1872-6143 | |
| dc.identifier.issue | 3-4 | en_US |
| dc.identifier.scopus | 2-s2.0-77956936472 | |
| dc.identifier.scopusquality | Q1 | |
| dc.identifier.startpage | 607 | en_US |
| dc.identifier.uri | https://doi.org/10.1016/j.lithos.2010.08.014 | |
| dc.identifier.uri | https://hdl.handle.net/20.500.14720/1702 | |
| dc.identifier.volume | 119 | en_US |
| dc.identifier.wos | WOS:000283462000028 | |
| dc.identifier.wosquality | Q1 | |
| dc.language.iso | en | en_US |
| dc.publisher | Elsevier | en_US |
| dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
| dc.rights | info:eu-repo/semantics/closedAccess | en_US |
| dc.subject | Geochemistry | en_US |
| dc.subject | Geodynamics | en_US |
| dc.subject | Quartz Monzodiorite | en_US |
| dc.subject | Late Medial Miocene | en_US |
| dc.subject | Eastern Anatolian Accretionary Complex | en_US |
| dc.title | The Petrogenesis of Saricimen (caldiran-Van) Quartz Monzodiorite: Implication for Initiation of Magmatism (Late Medial Miocene) in the East Anatolian Collision Zone, Turkey | en_US |
| dc.type | Article | en_US |