Browsing Araştırma Çıktıları | WoS by Publisher "TMMOB JEOLOJI MUHENDISLERI ODASI"
Now showing items 1-17 of 17
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02.03.2017 and 24.04.2018 Samsat (Adiyaman) Earthquakes and Their Importance in Regional Seismotectonics
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2019)In this study, Synthetic Aperture Radar Interferometry (InSAR) method is used together with field observations to determine whether surface deformations occur in the region after the 5,5 Mw (AFAD) Samsat Earthquake occurred ... -
Alteration Mineralogy and Geochemistry of the rocks from Tekirova (Antalya) Ophiolite Nappe
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2015)The Tekirova Ophiolite Nappe, part of the Antalya Unit in the southwest Anatolia, consists of a dismembered oceanic crust sequence with tectonic slices in different sizes. Three types of subsequent mineralizations are ... -
Applications of Unmanned Aerial Vehicle (UAV) in open-pit mines
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2019)In recent years, mapping operations in open-pit mines are made by using Unmanned Aerial Vehicles (UAV) having the advantages of cost, time and occupational safety. Using UAV.s, easy, fast, high sensitive and economic ... -
Approaches to the Low-Grade Metamorphic History of the Karakaya Complex by Chlorite Mineralogy and Geochemistry
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2015)Chlorite minerals are commonly found in the units of Karakaya Complex that reflect different tectonic settings and evolution. In this study, the availability of chlorites has been investigated as a parameter on the ... -
Cultural Geology and Geological Heritage; new initiatives for earthsciences
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2017)Rapid urbanization, increase in population and unemployment has a great effect on society and as a consequence seems to have caused unawareness to earth sciences. However, increasing demand on water and energy, natural ... -
Diagenesis/Metamorphism History of Lower Triassic Cigli Group Rocks in Uludere-Uzungecit (Sirnak) area (Eastern Part of the Southeast Anatolian Autochthone)
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)This study aims to reveal the mineralogical characteristics of the carbonate and pelitic rocks in the Lower Triassic Cigli Group in the Uludere-Uzungecit (Sirnak) region from Southeast Anatolian Autochthone (SEAA). Cigli ... -
Geology-Mineralogy and Isotope (O-D, S, Cu And Ar/Ar) Geochemistry of Sisorta High Sulfidation Epithermal Gold Deposit (Koyulhisar-Sivas)
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)This study presents geological and geochemical features of gold deposit located in Sisorta area near Evliya Tepe, Guzelyurt village. The investigation area covers 42 km(2) land and located in 200 km NW of Sivas province ... -
Hasankeyf (Batman) Site From Cultural Geological Perspective
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2017)Hasankeyf, a district of Batman, is positioned near Tigris river, assigned as protected area and consists hundreds of residents which are located in carved rocks. Although, Hasankeyf has lost its importance today, it was ... -
Humic Acid Properties of Bituminous Shales in the Region of Duzagac (Kozan-Adana)
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2015)Bituminous shale in our country takes second place in terms of reserve, when compared the fossil energy resources such as coal, petroleum and natural gas and for this reason, it appears that they have an important value ... -
Kinematics of the faults around the Koyulhisar (Sivas) region on the North Anatolian Fault Zone
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)The study area is located on the eastern part of the North Anatolian Fault Zone (NAFZ) around the Koyulhisar (Sivas) region. The region is represented by a 6-8 km wide and 32 km long deformation belt. This belt is divided ... -
Mineral Chemistry of Chlorite and Illite/Mica in the Clastic Rocks of Karakaya Complex: Origin and Diagenesis/Metamorphism
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2018)The Karakaya Complex units representing the relicts of environments related with the closure of PreJurassic Paleotethys Ocean outcrop within the Sakarya Composite Terrane. The compositions of illite/white micas change among ... -
Petrology of the Plio-Quaternary Gobekoren Volcanics (Kangal-Sivas)
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2019)The study area is located at 15 km W-SW of Kangal district of Sivas province. Lithological units are observed in the study area ranging from Late Miocene to Plio-Quaternary in age. The rock units start with Late Miocene-Pliocene ... -
Phlogopite Occurrences within Limestone-Ophiolite-Granitoid Triple Contact from Sivas-Divrigi Iron Deposit
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)Alteration minerals determined in the ultramafic rocks of Gunes Ophiolite were divided into three main groups as pre-, syn-and post-serpentinization. Of these, phlogopite from pre-serpentinization minerals is one of the ... -
Phyllosilicate/Clay Geochemistry of Mineralogy and Upper Cretaceous-Paleocene Germav Formation in Mardin-Dargecit Area
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2018)In this study, it is aimed to determine the mineralogical and geochemical features of the rocks from the Germav Formation of Upper Cretaceous-Paleocene age belonging to Sirnak Group. The clastic and chemical originated ... -
Shale Gas; Geological Properties, Environmental Effects and Global Economic Meaning
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)Global energy prospecting has significantly shown change with the development of technology that can be used in the production of energy sources which are unconventional such as tight reservoir and shale gas especially ... -
Shallow Marine Benthic Foraminifera Assemblage of the Early Eocene Succession in the Northern Arac (Kastamonu) and Paleoecological Interpretation
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)Soganli Formation of Early Eocene age in the northeastern of Arac (Kastamonu) has been investigated in order to determine their paleontology and palaeoecology. The sequence consists of gray, yellowish, clayey limestone, ... -
Tectonic setting and structural evolution of post-Late Cretaceous the Oltu-Balkaya basin (NE Turkey)
(TMMOB JEOLOJI MUHENDISLERI ODASI, 2016)The Oltu-Balkaya basin has started to open by the collision (soft-collision) between Pontide Arc and Anatolide-Tauride Platform since late Maastrihtian and was evolved as collisional foreland basins during Upper Maastrihtian ...