Open Access. Powered by Scholars. Published by Universities.®

Physical Sciences and Mathematics Commons

Open Access. Powered by Scholars. Published by Universities.®

Earth Sciences

Bulletin of the Mineral Research and Exploration

Eastern Anatolia

Publication Year

Articles 1 - 4 of 4

Full-Text Articles in Physical Sciences and Mathematics

Geochemical And Petrologic Evolution Of Otlakbaşı Basaltic Volcanism To The East Of Lake Van, Vural Oyan Dec 2018

Geochemical And Petrologic Evolution Of Otlakbaşı Basaltic Volcanism To The East Of Lake Van, Vural Oyan

Bulletin of the Mineral Research and Exploration

Collision-related Otlakbaşı volcanism to the east of Lake Van occurred by eruptions from extensional fissures. In this study, it is investigated new Ar-Ar age data and major, trace and rare earth elements characteristics of the Otlakbaşı basaltic volcanism. The Ar-Ar age data indicate that this basaltic volcanism erupted in Early Pliocene time in contrast to its previously known as Quaternary age. The volcanic products are basaltic composition and close to alkaline-subalkaline division line. Results of fractional crystallization accompanied by assimilation (AFC) modeling imply that fractional crystallization can be negligible compared to crustal contamination in the evolution processes of the magma …


Tectonic Geomorphology Of Başkale Fault Zone, Azad Sağlam Selçuk, Meryem Düzgün Dec 2017

Tectonic Geomorphology Of Başkale Fault Zone, Azad Sağlam Selçuk, Meryem Düzgün

Bulletin of the Mineral Research and Exploration

Başkale Fault Zone is located between Şemdinli-Yüksekova fault zone in southeast Turkey and Guilato–Siahcheshmeh–Khoy fault system in southeast Iran. The fault zone starts from Yavuzlar town extending to Işıklar village in southwest. The BFZ is composed of three different segments which have orientations varying N75°E to N 80°E. Offset streams, fault-controlled drainage system such as Çığılsuyu stream, alluvial fans which line up parallel to the fault and contain deformation structures, fault flats, Plio-Quaternary volcanic rocks and volcanic structures, and fissure ridge travertines with formation continuing today are among morphotectonic characteristics that indicate the BFZ is active.

The objective of the …


Tectonic Deformations In The Quaternary Deposits Of The Lake Van (Edremi̇t Bay), Eastern Anatolia, Turkey, Selim Özalp, B. Serkan Aydemi̇r, Şeyda Olgun, Barbaros Şi̇mşek, Hasan Elmaci, Murat Evren, Ömer Emre, M. Burak Aydin, Oktar Kurtuluş, Füsun Öcal, Aslı Z. Can, Mehmet N. Yanmaz, Ramazan Apa, Tamer Y. Duman Oct 2016

Tectonic Deformations In The Quaternary Deposits Of The Lake Van (Edremi̇t Bay), Eastern Anatolia, Turkey, Selim Özalp, B. Serkan Aydemi̇r, Şeyda Olgun, Barbaros Şi̇mşek, Hasan Elmaci, Murat Evren, Ömer Emre, M. Burak Aydin, Oktar Kurtuluş, Füsun Öcal, Aslı Z. Can, Mehmet N. Yanmaz, Ramazan Apa, Tamer Y. Duman

Bulletin of the Mineral Research and Exploration

The 23 October 2011 Van Earthquake (Mw: 7.2) was generated by the Van Fault Zone (VFZ) with reverse fault characteristics. The earthquake on the fault caused surface deformation with 10 cm displacement observed in engineering structures. On land the VFZ has general E-W strike and 28 km length. The western end of the fault is within Lake Van. This study aimed to determine the tectonic structures and evolution in the Quaternary of Edremit Bay using detailed mapping of the VFZ with land and underwater research methods, investigation of its continuation into Lake Van and common assessment of land and underwater …


Vertical And Horizantal Analysis Of Crustal Structure In Eastern Anatolia Region, Oya Pamukçu, Tolga Gönenç, Ayça Yurdakul Çirmik, Şevket Demi̇rbaş, Seyit Tosun Dec 2015

Vertical And Horizantal Analysis Of Crustal Structure In Eastern Anatolia Region, Oya Pamukçu, Tolga Gönenç, Ayça Yurdakul Çirmik, Şevket Demi̇rbaş, Seyit Tosun

Bulletin of the Mineral Research and Exploration

The tectonic regime of Eastern Anatolia is determined by Arabian-Eurasian continentcontinent convergence and the mechanism occurred with the convergence. North Anatolian Fault Zone (NAFZ), Eastern Anatolian Fault Zone (EAFZ), North Eastern Anatolian Faults and Bitlis Zagros Suture Zone are formed by this convergence, represent the characteristic of lithospheric structure of the region. In the scope of this study, the gravity anomalies of Eastern Anatolia were used for investigating the lithospheric structure. Firstly, second order trend analyses were applied to gravity data for examining the characteristic of the anomaly. Later, the vertical and horizontal derivatives methods were applied to the same …