Please use this identifier to cite or link to this item: https://hdl.handle.net/11147/11918
Title: Structural controls and hydrogeochemical properties of geothermal fields in the varto region, East Anatolia
Authors: Uzelli, Taygun
Şener, Mehmet Furkan
Dölek, İskender
Baba, Alper
Sözbilir, Hasan
Dirik, Ramazan Kadir
Izmir Institute of Technology
İzmir Bakırçay Üniversitesi
Muş Alparslan Üniversitesi
Izmir Institute of Technology
Dokuz Eylül Üniversitesi
Hacettepe Üniversitesi
Keywords: Eastern Anatolia
Structural geology
Triple junction
Geothermal energy
Issue Date: 2021
Publisher: TÜBİTAK
Abstract: Abstract Varto and the surrounding region have important geothermal fields, developing in strike-slip tectonic setting in East Anatolia, which resulted from the collision of the Arabian and Eurasian plates. The main structural elements in the area are the NE-trending sinistral and NW-trending dextral strike-slip fault segments and N-S trending extension zones. In order to determine fault-controlled geothermal circulation, it is very important to fully characterize the structural elements in these complex environments. The widely distributed volcanic rocks have fracture and crack systems that play an important role in surface infiltration, geothermal fluid, and groundwater circulation. Especially in areas where the fault segments intersect, hot springs outlets and natural resources easily come to the surface. In order to understand the flow paths of geothermal fluid along the faults in these geothermal systems, it is necessary to determine the stress state of the faults and to map the distribution of the structural elements. For this reason, we conducted a detailed study on the Varto Fault Zone, which has important geothermal fields in Eastern Anatolia. We present conceptual models of the geothermal fields in the Varto region that show favorable geothermal activity on the intersecting fault segments, fault bends, step-overs, and accompanying fracture-crack sets. As a result, we emphasize that the planes of strike-slip faults in transtensional areas are more favorable for secondary permeability and enhances the geothermal fluid circulation, and this can be supported by hydrogeochemical data.
Description: This research was partly supported by the Muş Alparslan University Scientific Research Projects (BAP-17.EMF- 4914-01), Eastern Anatolia Development Agency (EADA), and Muş Governorship.
URI: https://doi.org/10.3906/yer-2106-13
https://hdl.handle.net/11147/11918
Appears in Collections:IZTECH Research Centers Collection / İYTE Araştırma Merkezleri Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection

Files in This Item:
File Description SizeFormat 
yer-30-si-2-6-2106-13.pdfArticle (Makale)30.24 MBAdobe PDFView/Open
Show full item record

CORE Recommender

Page view(s)

56
checked on Jan 17, 2022

Download(s)

4
checked on Jan 17, 2022

Google ScholarTM

Check

Altmetric


Items in GCRIS Repository are protected by copyright, with all rights reserved, unless otherwise indicated.