
Fetullah Arik- Prof. Dr.
- Head of Ore Deposit - Geochemistry Sub Divisison at Konya Technical University Faculty of Engineering and Natural Sciences
Fetullah Arik
- Prof. Dr.
- Head of Ore Deposit - Geochemistry Sub Divisison at Konya Technical University Faculty of Engineering and Natural Sciences
Konya Technical University
Sinkhole Applicatin and Research Center
About
76
Publications
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Introduction
Fetullah Arik currently works at the Geological Engineering Department, Konya Technical University, Geological Engineering Department Chamber of Geological Engineers. Fetullah does research in Mineral deposits and geochemistry , Environmental Geochemistry, Medical Geology, Geological heritages, Geosites, geoparks, Fossil fuels, Geological Hazards and Engineering Education. His current project is Konya Technical University Sinkhole Application and Research Center"'.
Current institution
Konya Technical University Faculty of Engineering and Natural Sciences
Current position
- Head of Ore Deposit - Geochemistry Sub Divisison
Additional affiliations
October 2018 - January 2022
Konya Technical University Faculty of Engineering and Natural Sciences
Position
- Head of Department
November 2018 - present
Konya Technical University Faculty of Engineering and Natural Sciences
Position
- Head of Department
Description
- This Geological Engineering Department is old Geological Engineering Department of Selcuk University
November 2016 - December 2019
Selcuk University, Geological Engineering Department Chamber of Geological Engineers
Position
- Head of Department
Education
September 1996 - June 2002
September 1993 - May 1995
Selcuk University Institution Natural and Applied Science
Field of study
- Ore Deposits - Geochemisrty
September 1987 - June 1991
Publications
Publications (76)
The Mediterranean-type karst-bauxite deposit of Mortaş, south Turkey, placed unconformably between Cenomanian and Senonian shallow marine limestones is built of massive (MB), oolithic (OB), breccia-bearing (BB) and earthy (EB) bauxite horizons, from top to bottom. The MB layer is enriched in Al and REE (except Ce) due to loss of Si, Na, K, Mg and P...
The Attepe district consists of Precambrian, Lower–Middle Cambrian, Upper Cambrian–Lower Ordovician and Mesozoic formations. It contains several iron deposits and occurrences. Three types of iron-mineralizations can be distinguished in the area; (i) Sedimentary Fe-sulfide in Precambrian bituminous metapelitic rocks, and Fe-oxides in Precambrian met...
The Inkaya Cu-Pb-Zn-(Ag) mineralization, located about 20 km west of the Simav (Kütahya-Turkey), is situated in the northern part of the Menderes Massif Metamorphics. The mineralization is located along an E-W trending fault in the Cambrian Simav metamorphics consisting of quartz-muscovite schist, quartz-biotite schist, muscovite schist, biotite sc...
The İnkaya Cu-Pb-Zn-(Ag) prospect is a typical example of the hydrothermal mineralization occurring in the Menderes Massif, which crop out in Western Anatolia. The prospect located approximately 20 km west of Simav (Kütahya- Turkey) in northern part of the Menderes Massif have been characterized through the detailed examinations involving geologica...
Basic information about karstification and especially sinkholes. Definition, types, classification, formation conditions, factors triggering collapse. Examples from the world. Sinkhole formations in Konya Closed Basin and Turkey. Sinkhole indicators. Structural and non-structural precautions and solutions.
Karstlaşma ve özel olarak Obruklarla ilgi...
Obruk (sinkhole) oluşumları, Obruk Araştırma Yöntemleri: Uzaktan Algılama (Harita, Uydu, İHA), Saha ve Laboratuvar Araştırmaları(Obruk Envanter Çalışmaları, Jeolojik, Mineralojik-Petrografik, Jeokimyasal, Yapısal, Sedimantolojik Çalışmalar), Hidrojeolojik: (Hidrolojik, Hidrojeolojik, Hidrokimyasal Çalışmalar), Jeofiziksel (Elektrik, Özdirenç, Gravi...
Obruklar (Sinkholes) tanım, sınıflandırma, oluşum koşulları, Dünya'da ve Türkiye'de obruk oluşumları, obruk oluşum belirtileri, obruk tehlikesi için mühendislik çözümleri
The Goshgarchay Cu‐Au deposit is located in the central part of the northwest flank of the Murovdagh region in the Lesser Caucasus. The Goshgarchay Cu‐Au deposit is associated with Middle Jurassic volcanic and Late Jurassic–Early Cretaceous high‐K calc‐alkaline intrusive rocks. The Cu‐Au mineralization is commonly related to quartz‐sericite‐chlorit...
Her yıl dünyada ve ülkemizde doğal ve jeolojik nedenlerle deprem, heyelan, su baskınları, kaya düşmeleri vb. mal ve can kaybına neden olabilecek tehlikeli ve büyük çaplı bir çok olay gerçekleşmektedir. Genellikle insanların kontrolü dışında gerçekleşen bu olayların oluşum zamanının önceden kestirilmesi ve önlenmesi çoğu zaman mümkün olmamaktadır. B...
Günlük hayatta doğal çevreden ve temel besinlerden temin edilen mineraller ve eser elementleri hiç sorgulamadan her an yiyor, içiyor ve soluyoruz. Bünyemize aldığımız bu doğal malzemelerle etkileşim, çoğu zaman zararsız, hatta belki faydalı olmasına karşın bazı mineraller ve eser elementlerle etkileşim yıkıcı, hatta ölümcül etkilere sahip olabilmek...
The Karapınar region (Sultaniye basin) located within the Konya Closed Basin, which consists of
approximately 42.000 km2, is bounded by the Seyithacı fault zone in the west and the Nasuhpınarı fault
zone in the east. Arid climate regime started 12.000 years ago in Konya region and wetlands have almost
completely dried up in the last 6.000 years. Th...
Kurşunlu ve Dağdere (Selçuklu-Konya) civarında yaklaşık 132 km2 lik bir alanın cevher potansiyelinin araştırılması amaçlanmıştır. İnceleme alanında Ladik Metamorfikleri’ne ait Silüriyen (?)-Permiyen yaşlı Sızma grubunda yer alan rekristalize kireçtaşı, dolomitik kireçtaşı ve dolomitlerden oluşan Bozdağ formasyonu, fillit, metakumtaşı, rekristalize...
The study area is located within the borders of Tokat province, which is one of the richest provinces in Turkey in terms of gemstone diversity. The region has very high quality and various gemstone formations such as jasper, opal, chalcedony, agate, chrysoprase, which have both geological and commercial value. Metamorphic, magmatic, and sedimentary...
The Upper Cretaceous Artova ophiolite complex, represented by metabasic and ultrabasic rocks, overlies the Paleozoic aged Tokat metamorphites, which form the basis of the study area, by the tectonic boundary. Haydaroğlu formation, which includes Middle Eocene aged volcanogenic units, cuts and covers the older units. Agates (agates) in the Almus reg...
The Daghkesemen Au-bearing polymetallic vein-type deposit, which is the most important ore deposit of the Kazakh graben located in the northwestern part of the Lesser Caucasus, is hosted by calc-alkaline volcanic rocks (andesite, dacite, basaltic trachyandesite, trachyandesite, rhyodacite and their pyroclastics), subvolcanic rocks (andesite porphyr...
In this study, it is aimed to give the geological and morphometric features of the sinkholes around Kızören Settlement, 65 km northeast of Konya region The number of sinkholes identified in the region which is located on the Konya- Aksaray Road, is 50. There are many fracture systems in the region. These fracture systems have NS, DB and NW-SE trend...
Uncontrolled extraction of water from groundwater aquifers causes groundwater depletion, which in turn triggers the formation of sinkholes in many parts of the world. Monitoring and detection of these geomorphologic features are of utmost importance and priority for the decision-makers to minimize significant environmental as well as socioeconomic...
The Gadir Au-Ag-Cu-Pb-Zn deposit, located in the western part of Azerbaijan, was extensively occurred in quartz porphyry, and rarely in the contact of the hornfelsed andesite and quartz porphyry. The hydrothermal alterations associated with mineralization are quartz-adularia±sericite and propylitic alterations. The Gadir deposit is mainly composed...
The Gadir Au-Ag-Cu-Pb-Zn deposit is located at the east of the Yoğundağ Mountain, about 400 m northwest of the Gedabek Au-Cu deposit in the Lesser Caucasus region of the Republic of Azerbaijan. The Gadir Au-Ag-Cu-Pb-Zn mineralization is observed in the contact of the andesitic tuff and quartz porphyry, and in the quartz porphyry. The main ore miner...
Gedabey (Western Azerbaijan) mine province is located in the Lesser Caucasus region of Tethys metallogenic belt, which is one of the most important metallogenic provinces of the
world. Mineralization occurred in the subduction zone within the Lok-Karabakh structuralformation zone of the Lesser Caucasus. The Gedabey ore province is one of the main p...
Abstract
The Gedabek Au-Ag-Cu deposit located in the western part of Azerbaijan is hosted by quartz porphyry which is situated at contact between Middle Jurassic andesitic tuff and Late Jurassic-Early Cretaceous Gedabek intrusive rocks consisting of granodiorite, diorite and gabbro. Geochemical investigations for the Gedabek intrusive rocks indicat...
The Gedabek district is one of the major porphyry-epithermal mineralization fields of Azerbaijan. The Gadir Au-Ag-Cu-Pb-Zn deposit is located in the east of Yogundag within the Shamkir uplift of the Lok-Karabakh suture zone in the Gedabek district of the Lesser Caucasus. The study area is composed mainly of the sequentially differentiated Lower-Upp...
The Pınarbaşı porphyry Cu-Mo mineralization is located at northwest of Gediz (Kütahya-Turkey) and east of Simav (Kütahya-Turkey) in western Anatolia. The Pınarbaşı CueMo mineralization is hosted by Pınarbaşı granitoidic intrusion consisting of granite, granodiorite and quartz monzonite. Geochemical and geochronological evidences for Pınarbaşı grani...
In this study, we aimed to determine the geological, mineralogical and petrographical characteristics of the agate nodule formations and wall rocks in the northern part of the Almus Dam Lake and the gemological characteristics of the agates. In the study area, metamorphic, magmatic and sedimentary units formed from Paleozoic to the present day are...
In this study, it was aimed to investigate the relations of chalcedony formations with the rocks located in around of the Gümenek and Döllük villages of Tokat City center and their petrographical and gemological features. In the region, consisting of Paleozoic to today, it is observed magmatic and sedimentary units. The Tokat Massif, which forms th...
It is aimed that to investigate of the geological, mineralogical, petrographic and gemological characteristics of the chrysoprase that exposed in a large area in the west of the Gümüşyurt village, approximately 20 km from Artova (Tokat), in this study. The oldest unit in the area is the Late Triassic age Devecidağ Complex, which is represented by v...
The Pınarbaşı porphyry Cu-Mo mineralization is located at the western part of Anatolia and in southern part of the İzmir-Ankara suture zone. The Pınarbaşı porphyry Cu-Mo mineralization hosted in the Early Miocene Pınarbaşı granitoidic intrusion consisting of granite, granodiorite, quartz monzonite and granite porphyry, composes of molybdenite, chal...
İnsanoğlu varoluşundan bu yana doğal taşları değişik amaçlar için kullanmıştır. İnsanlık tarihinin ilk devirleri kullandıkları taşlara göre adlandırılmıştır; yontma taş devri, cilalı taş devri, bakır devri, tunç devri, demir devri vs. Ayrıca doğal taşların kullanımı, toplulukların refah düzeyi ve kültürünün gelişiminin de bir ölçüsü olmuştur. Doğal...
In this study, it is investigated whether the soil classes in the region between Hatıp and Kaşınhanı (Konya-Turkey) are related to geological units. The Upper Triassic-Lower Cretaceous Lorasdağı formation which is composed of limestone, dolomitic limestone and dolomites and the Upper Cretaceous aged Midostepe formation consisting of clayey limeston...
The study area covers around the Gümeli Village, located in the Zonguldak Basin which is the Turkey's most important coal basin, approximately 70 km west of the Zonguldak city centre and 20 km southeast of Alaplı District. In this study, it is aimed to investigate of the geological features of the region, stratigraphic sequence of rock units outcro...
The Gedabek Au-Cu deposit is located at the northwest slope of the Shahdag Mountain Range, 50 km west of the Ganja Province, north of the Nagorno-Karabakh Region of the Republic of Azerbaijan, and on the northwestern of Gedabek. The Gedabek Au-Cu mineralization is located in the quartz porphyry occurring in the contact of andesitic rocks (Middle Ju...
Konya is the largest city of Turkey and has been the capital of many civilizations. The current study intends to determine the geochemical characteristics and the distribution of trace elements of soils in an area of approximately 600 km 2 around Konya. Many different types of rocks and younger detricious units are exposed in Konya, formed from the...
In this study, it was aimed to investigate the geological and mineralogical properties of Gedabek (West Azerbaijan) gold-copper deposit, which is one of the most important gold copper deposits of Azerbaijan, in the northwest of Gedabek and 50 km west of Ganja (West Azerbaijan). Gedabek gold-copper deposit, extending from Pakistan, Iran, Azerbaijan,...
Bilindiği gibi Jeoloji Bilimi; Fizik, Kimya, Matematik ve Biyoloji ile birlikte beş temel bilimden biri olup Jeoloji Mühendisliği Jeoloji biliminin temel uygulama alanıdır. Jeoloji Mühendisliği başta ülke çapında mekânsal strateji planlarından başlayarak her ölçekte planlama için yerleşime uygunluk değerlendirmelerinde, yerleşime uygun olan inşa ed...
Çağırankaya Obsidians 46 km away from Rize Province Center 24 km away from İkizdere District, it is exposed on an area approximately 12 km2 among the Madentepe, Büyük Yayla, Sırıklıtepe and Karatepe in the vicinity of the Güvenköy. In this study, it is aimed to investigate the geological characteristics of Çağırankaya region, the relations of obsid...
Presidency of Konya Plain Project Regional Development Administration (KOP-RDA) was established to support regional development in eight provinces, namely Konya, Aksaray, Karaman, Niğde, Kırıkkale, Kırşehir, Nevşehir and Yozgat in Central Anatolia. Almost half of the 4 million population in the KOP region live in the mountainous / rural areas and t...
Her yıl dünyada ve ülkemizde doğal ve jeolojik nedenlerle deprem, heyelan, su baskınları, kaya düşmeleri vb. mal ve can kaybına neden olabilecek tehlikeli ve büyük çaplı bir çok olay gerçekleşmektedir. Genellikle insanların kontrolü dışında gerçekleşen bu olayların oluşum zamanının önceden kestirilmesi ve önlenmesi çoğu zaman mümkün olmamaktadır. B...
Önemli petrol ve doğal gaz yataklarına sahip olan Azerbaycan’da aynı zamanda ekonomik altın, demir, bakır ve civa gibi pek çok metalik maden yatağı da yer almaktadır. Bu çalışmada Gence’nin (Batı Azerbaycan) 50 km batısındaki Şahdağ Sıradağları’nın kuzeybatı yamacında ve Gedebey’in kuzeybatısında bulunana en önemli altın bakır yataklarından biri ol...
Kiziltepe Skarn Mineralization located 35 km south of the Canakkale and 8 km southwest of Ezine County near the Kestanbol Pluton. Cambrian to Holocene aged magmatic, metamorphic and sedimentary rocks crop out in the study area. The basement of the study area is formed by Pre(?)-Lower Cambrian metasandstone, metaconglomerate, phyllite and chalcschis...
The Pınarbaşı Cu-Mo mineralization is located at the west part of Anatolia, in south part of the-Ankara suture zone and in northeast border of Menderes Massif. The mineralization located-core samples were-Mo mineralization area. According to chemical analyses and petrographical investigations, the magmatic rocks are classified as granite, granodior...
The Değirmenciler mineralization is located approximately 500 m southwest of the Değirmenciler district in the Simav (Kütahya- Turkey) in northern part of the Menderes Massif. The mineralization occurred in the intense silicification and brecciation zone along the E-W trending faults developed in the final step of the Simav Graben. The Değirmencile...
The study area covers an area of approximately 360 km2, including Karadiğin, Yenibahçe, Kaşınhananı, Hatunsaray, Çatören Çarıklar, Boruktolu, Kavak and Seçme neighbourhoods among the Meram, Akören and Çumra Counties (Konya). In this study, it is aimed to determine the heavy element distributions in the soil and the factors controlling them by revea...
Medical geology investigates the positive and negative effects of natural geological materials (elements, rocks and minerals, water, geothermal, petroleum etc), geological processes (volcanism, earthquake, tsunami, dusts) and anthropological factors (water, energy, mine, food and agricultural activities, domestic, industrial and medical wastes) on...
Meram is one of the central districts of Konya, Turkey’s geographically largest city and rapidly urbanized. Metamorphic, magmatic and sedimentary rocks formed from Paleozoic
to the present are crop out in the study area. These rocks were discussed in two main groups such as basic and cover units. In the investigation area, soils belonging to a zona...
The Gürkuyu Sb mineralization is located in the western part of Anatolian tectonic belt, in southern part of İzmirAnkara zone and in northern part of Menderes Massif. The mineralization located at west of the Koca hill in east of Gürkuyu village of Gediz (Kütahya-Turkey) has been characterized through the detailed examinations involving sulfur and...
This book including abstracts of the contributions of the 2nd Medical Geology Symposium hold in Konya 12-15 November 2015 by UCTEA Chamber of of Geological Engineers Konya Subdivision
"Mineral bilimi anlamına gelen mineraloji minerallerin fiziksel, kimyasal, geometrik, optik ve kristalografik özelliklerini inceleyen ve mineralleri bu özelliklerine göre sınıflayan bir bilim dalıdır.
Mineralleri, temel fiziksel, geometrik, kristalografik özelliklerine göre inceleyen Genel Mineraloji ile mineralleri farklı özelliklerine göre sınıf...
Geochemical and Isotopic (S and O) investigation of the Değirmenciler (Simav-Kütahya) Sb Mineralization, NW Turkey
Fetullah ARIK1, Yeşim ÖZEN2
1 Department of Geological Engineering, Selçuk University, 42250 Konya, Turkey, farik@selcuk.edu.tr
2 Department of Geological Engineering, Selçuk University, 42250 Konya, Turkey, ybozkir@selcuk.edu.tr
The...
Heavy metal distributions and pollutions of soils in the Konya Residential Area, Central Turkey.
Fetullah ARIK1, Bilgehan Yabgu Horasan2
1Selçuk University, Geological Engineering Department, 42250 Selçuklu / Konya, Turkey, farik@selcuk.edu.tr
2 Selçuk University Graduate School of Natural Sciences Selçuklu / Konya, Turkey, bilgehanyabgu@gmail.com...
Doç. Dr. Fetullah Arık:
Sayın Arık, enerjide önemli olanın birincil ve ikincil enerji kaynakları olduğunun altını çizdi. Birincil enerji kaynaklarının, doğrudan tüketilebilen kaynaklar; kömür, doğalgaz petrol vb. olarak sayılabileceğini, dünyada enerji kullanımına bakıldığı zaman fosil yakıtların ciddi bir orana sahip olduğunu ifade etti. Enerji ür...
THE IMPORTANCE OF DRILLING EDUCATION IN THE GEOLOGICAL ENGINEERING TEACHING PROCESSES
Fetullah ARIKa and Alican ÖZTÜRKa
aSelçuk University, Engineering Faculty, Geolog Department, 42080 SELÇUKLU/KONYA
(farik@selcuk.edu.tr, fetullaharik@gmail.com, acan@selcuk.edu.tr)
ABSTRACT
Drilling have been used more and more widely, depending on the country...
THE IMPORTANCE OF DRILLING EDUCATION IN THE GEOLOGICAL ENGINEERING TEACHING PROCESSES
Fetullah ARIKa and Alican ÖZTÜRKa
aSelçuk University, Engineering Faculty, Geolog Department, 42080 SELÇUKLU/KONYA
(farik@selcuk.edu.tr, fetullaharik@gmail.com, acan@selcuk.edu.tr)
ABSTRACT
Drilling have been used more and more widely, depending on the country...
ABSTRACT
Konya is the largest city of Turkey and the settlement area of the city has been home and capital of the many historical civilizations. This study was intended to determine geochemical characteristics and trace element distributions of soils which were exposed in an area of approximately 600 km2 around the Konya.
In Konya, which is a plain...
Gözeçukuru As-Sb-Pb-Zn mine is located 1.2 km NW of Sahin village and 22 km west of Kütahya in NW Turkey. The aim of this study is to explain the genetic characteristics of the As-Sb deposits by using multivariate statistical analysis methods. Low-grade metamorphic rocks of the upper Paleozoic Sahin Formation occur as the basement of the study area...
Geological and Geochemical Features Of The Sarıçayır (Yenice/Çanakkale) Skarn Deposits
FETULLAH ARIK AND İLKNUR AKIŞ1
1Selcuk University, Geological Engineering Department, Konya, Turkey (correspondence: fetullah42@hotmail.com)
The Sariçayir Skarn Deposit is located around the Sarıçayır village and 70 km southwest of Çanakkale. Oligo-Miocene magma...
Mineralogical and petrographical characteristics of the
Aladag skarn deposit (Ezine/Canakkale-West Turkey)
Fetullah Arik1* and Umit Aydin2
1Selcuk University, Department of Geological Engineering, Konya, Turkey.
2General Directorate of Mineral Research and Exploration, Ankara, Turkey.
Accepted 15 November, 2010
The study area located 35 km south of...
The investigation area is located to the east of Kütahya–Tavşanlı and, covers an area about 150 km2. The units cropping out in the study area comprise of metamorphic, volcanic, and sedimentary rocks ranging from Upper Paleozoic to Quaternary. There are some polymetallic ore deposits represented by silver, zinc, lead, and antimony deposits and some...
!CASTOR Journal of Engineering
Vol. 2, No. 3(3) (2009) 363- 382
ENVIRONMENTAL POLLUTION EFFECT OF As-Pb-Zn DEPOSITS
IN SE TAV~ANLI (KUTAHY A-TURKEY)
ABSTRACT
Fetullah Arik, Tahsin Yaldiz
Geological Engineering Department
Selr,:uk University
Selr,:uklu, Turkey
The rock units in the study area which host some important polymetallic ore deposits (e.g....
GEOLOGY, MINERALOGY AND GEOCHEMICAL CHARACTERISTICS OF
THE GOZECUKURU (KUTAHYA) As-Sb DEPOSITS, NW TURKEY
Fetullah Arik
University of SelCuk, Faculty of Engineering- Architecture,
Department of Geological Engineering, Konya, Turkey
ABSTRACT
The Gozeçukuru As-Sb mineralization was occured in an area of 2,1 km2, which is
located near the small town o...
GEOLOGICAL INVESTIGATION OF THE CARIKSARAYLAR - KOZLUCAY
AREA (ISPARTA-TURKEY)
Yesim Bozkir, Ahmet Ayhan, Fetullah Arik
Selcuk University, Geological Engineering Department, Turkey
ABSTRACT
The study area is located in southeastern part of Sultandaglari, 50 km to the northeast of
Isparta. The geological units exposed in the area are: The Lower-Midd...
This study investigated the effects of chronic arsenic exposure on QT- and QTc-interval prolongation, QTc dispersion (QTcd) and transmural dispersion of repolarization (TDR). We compared cardiac parameters from 40 male subjects chronically exposed to arsenic (group A) with those of 40 male subjects not exposed to arsenic (group B). Although subject...
The Çatmakaya bauxite deposit occurs in a karstic depression at the top of the Cenomanian limestone, namely the Katrangedii formation, and is overlain by the Senonian limestones of the Doankuzu formation. These forma- tions are tectonically overlain by the ophiolitic slices of the Bozk›r unit mainly comprising diabase-dolerite, serpen- tinite, radi...
The Çatmakaya bauxite deposit occurs in a karstic depression at the top of the Cenomanian limestone, namely the Katrangediǧi formation, and is overlain by the Senonian limestones of the Doǧankuzu formation. These formations are tectonically overlain by the ophiolitic slices of the Bozkir unit mainly comprising diabase-dolerite, serpentinite, radiol...
The upper Cretaceous Katrangediǧi formation comprising carbonaceous rock occurs at the base of the bauxite in the study area, which is located 30 km to the south of Seydişehir and 500 m to the west of the Çatmakaya village. The Upper Cretaceous (Senonian - Maestrichtian) Doǧankuzu formation lies on the bauxite deposited in the karstic openings at t...
Questions
Question (1)
How can we prevent sinkhole formations?
How can we prevent sinkhole formations? If a sinkhole has formed, how can we produce a solution?