İlgi alanları

Sürdürülebilir Kalkınma Amaçları

• 4
• 2
• 1
• 1
• 1

• MakaleYalnız künye2025/r/gumushane/12548
  Mantle genesis and crustal contamination in Carboniferous granitoids using U-Th-K concentrations at the Akşar Pluton in the Eastern Pontides, NE Türkiye

  Maden, Nafız; Gücer, Mehmet Ali; Akaryalı, Enver

  New radiogenic heat production (RHP) data are presented for Carboniferous granites outcropping in the Akşar region (Bayburt, NE Turkey) to contribute to ongoing debates on the genetic and lithologic relationship between the Akşar and Gümüşhane plutons, which is the most widely distributed granitic rocks in the region. The scope of this study consists of rocks composed of enriched mantle material metasomatized by fluids from the previously subducted plate. We observed average K value for the Akşar Pluton was found to be 3.09 ± 1.58 %. Additionally, average Th/U and U/Th values of 3.95 ± 1.37 and 0.29 ± 0.10, respectively. The calculated RHP value for the Akşar Pluton was 2.20 ± 0.56 μWm−3. Numerical results suggest that the Carboniferous Akşar pluton's primary magma was the product of mixing lithospheric mantle and mid-to-lower crustal melts because of partial melting, differentiation, and emplacement in the shallow continental magma chamber. The geochemical and petrogenetic characteristics of the Akşar region magmas suggest that crustal contamination occurred at multiple levels, particularly within the lower to middle crust of the plutonic core complex. This complex likely retains geochemical signatures indicative of subducted Paleotethys oceanic lithosphere. These findings provide critical insights into the magmatic evolution of the Eastern Pontides, contributing to a more comprehensive understanding of crust–mantle interactions and the broader geodynamic framework of northeastern Türkiye.

  İncele
• MakaleAçık Erişim2023/r/gumushane/20387
  Köprüyanı (Maçka-Trabzon) Fe-Cu skarn cevherleşmesinin jeolojisi ve mineral kimyası özellikleri

  Akaryali, Enver; Gücer, Mehmet Ali; Sivrikaya, Adem

  Bu çalışmada, Doğu Pontidler’ in Kuzey Zonunda Trabzon ili sınırlarında Köprüyanı mevkiindeki Fe-Cu skarn cevherleşmesinin; jeolojisi, petrografisi, cevher mikroskobisi özellikleri ve mineral kimyası içeriklerinin belirlenmesi amaçlanmıştır. Köprüyanı cevherleşme sahasında, aktinolit, tremolit, pirit, kalkopirit, manyetit ve malakit mineralleri ile kırık çatlak zonları boyunca gelişmiş limonitleşme, hematitleşme kloritleşme ve epidotlaşma türü alterasyonlar gözlenmektedir. Manyetit minerallerinin genellikle kalkopirit, pirit ve granat ile birlikte bulunduğu, TiO2 içeriklerinin çok düşük (%0.02-1.02) olduğu buna karşılık FeOt içeriklerinin ise %83.13-92.00 arasında değiştiği belirlenmiştir. Manyetit ile beraber bulunan ve ekzoskarn zonunda yer alan kalkopirit minerallerinin Cu içeriğinin %33.50-43.27 ve Fe içeriği %29.84-39.11 arasında değiştiği belirlenmiştir. Epidot minerallerinin Al içeriklerinin yüksek (2.06-2.46), Mn içeriklerinin düşük (0.01-0.03) ve Fe+3 içeriklerinin ise nispeten yüksek (0.59-0.96) olduğu belirlenmiştir. Al bakımından zengin olan epidotların türünün ise klinozoisit olduğu tespit edilmiştir. Granat türleri ağırlıklı olarak andradit ve grossular-andradittir. Cevher mikroskobisi ve mineral kimyası çalışmaları kapsamında derlenen verilere bağlı olarak, Köprüyanı cevherleşmesinin Fe-Cu skarn tipinde olduğu ve bölgede var olan skarn cevherleşmelerinin parajenez, süksesyon ve mineral kimyası verileri ile benzerlik gösterdiği sonucuna ulaşılmıştır.

  İncele
• MakaleAçık Erişim2023/r/gumushane/11995
  Investigation of the structural damage caused by blasting activities in tunnels to surrounding buildings: The case of Gümüşhane belt highway; [Tünellerde patlatma faaliyetlerinin çevre binalara verdiği yapısal hasarın incelenmesi: Gümüşhane çevre yolu örneği]

  Seferoğlu, Mehmet Tevfik; Seferoğlu, Ayşegül Güneş; Akaryali, Enver

  Tunnels are road transport structures that reduce traffic and expropriation problems, noise, and possible damage to animals and plants, and provide safer, more comfortable, and faster transportation for vehicles compared to highways. However, some environmental problems occur during tunnel construction. These problems such as vibration, noise, rock throwing, etc. caused by the blasting process used during tunnel excavation on buildings and people should be well investigated. In this study, two buildings located close to the exit and entrance of two tunnels (T2 and T3 tunnels) on the Gümüşhane belt road were chosen to investigate. Firstly, the existing damages in the first building, which is 7 m away from the T2 tunnel exit, and the second building, which is 60 m away from the T3 tunnel entrance, were analyzed by considering criteria such as the geological and ground condition of the land and the building materials used during the construction of those building. In addition, the negative effects on the buildings were evaluated by calculating the vibrations after the blasting process in the tunnel with the help of various empirical formulas. Investigation on site showed that building 1 was built of masonry and building 2 was built of reinforced concrete, and that deep cracks had formed in the bearing systems of both buildings, spills occurred in the walls, and fractures in the windows. Also, calculations with empirical formulas showed that the vibration rates caused by blasting process in the 1st and 2nd buildings were as 385.68 mm/sec and 6.91 mm/sec, respectively, and these vibration values were above the standard values. The data obtained through examination on-site and empirical approaches show that it would be dangerous for people to be resident in both buildings.

  • 
  • 
  İncele
• MakaleAçık Erişim2022/r/gumushane/17264
  Gold Mining, History and Today: The Case of Gümüşhane

  Zeybek, Halil İbrahim; Akaryali, Enver; Çavuşoğlu, İbrahim; Gücer, Mehmet Ali; Sipahi, Ferkan

  As in the history of humanity, the need for mines, causing important developments in human life, is gradually increasing. The mines, whose names are given to historical ages, have been a necessary source of raw materials for human beings to survive. Mines are one of the factors that directly affect the country's economy. Gold is a mine whose history is based on ancient history, its production has gained importance especially in recent years as a result of increasing demand and the research for new gold sources. Türkiye is a rich country with a 2% share in the world, with gold deposits of different geological characteristics and 431 ton reserves. Depending on the gold mining in recent years, gold explorations in Türkiye continue intensively and the annual gold production has increased to 39 tons in 2021. It has been determined that gold mining is concentrated in the Aegean and Marmara Regions with the Eastern Black Sea part in Türkiye. Gümüşhane is one of the provinces where gold mining is intense. In this study, the gold mining and importance in Gümüşhane are discussed by giving information about the history of gold mining.

  İncele
• MakaleAçık Erişim2022/r/gumushane/14533
  Petrogenesis of post-collisional Middle Eocene volcanism in the Eastern Pontides (NE, Turkey): Insights from geochemistry, whole-rock Sr-Nd-Pb isotopes, zircon U-Pb and 40Ar-39Ar geochronology

  Aydınçakır, Emre; Yücel, Cem; Ruffet, Gilles; Gücer, Mehmet Ali; Akaryalı, Enver; Kaygusuz, Abdullah

  The debate about whether Eocene magmatism is considered to be post-collisional or subduction-related or not still continues. Here we offer new 40Ar-39Ar ad U-Pb zircon geochronology, mineral chemistry, bulk rock and Sr-Nd-Pb isotope geochemistry data obtained from the southern dike (SD) suite, in comparison with the northern dike (ND) suite, from the Eastern Pontides. The geochronological data indicate that the SD suite erupted between 45.89 and 45.10 Ma corresponding to the Lutetian (Middle Eocene). The magmas of the ND suite are characterised by slightly more alkaline affinity compared to the SD suite. The trace and rare earth element (REEs) content of the SD suite is characterised by large ion lithophile element (LILEs; Sr, K2O, Ba, Rb) enrichment and depletion of Nb, Ta, and TiO2 elements to different degree with high Th/Yb ratios, which indicate that the magmas forming the SD and ND suites were derived from lithospheric mantle sources enriched by mostly slab-derived fluids in the spinel stability field. The Sr, Nd and Pb radiogenic isotope ratios of the dikes support the view that the magma for the hydrous group (H-SD) was derived from a relatively more enriched mantle source than the other SD and ND suites. The ND suite and the anhydrous group (A-SD) display similar geochemical features characterised by moderate light earth element (LREE)/heavy rare earth element (HREE) ratios, while the H-SD group has respectively lower LREE/HREE ratios indicating higher melting degree. Detailed considerations of the alkalinity, enrichment and partial melting degree for the source of the studied volcanic rocks indicate that the magmas of the northern dike suite are characterised by slightly more alkaline affinity, whereas the magmas throughout the southern dike suite show increments in the enrichment rate and melting degree. In light of the obtained data and comparative interpretations, the geodynamic evolution and differences in petrogenetic character of the Lutetian magmas from both the northern and southern parts of the Eastern Pontides may be explained by different degrees of melting of a net veined mantle source initially metasomatized by mostly subduction fluids during asthenospheric upwelling due to fragmented asymmetric delamination in a post-collisional extensional tectonic environment.

  İncele
• MakaleYalnız künye2021/r/gumushane/17403
  Gümüşdamla (aydıntepe-bayburt) skarn cevherleşmesinin \rmineral kimyası özellikleri

  Akaryali, Enver; Kurt, Ali Hakim

  İnceleme alanı, Bayburt ilinin kuzeyinde yer alan Aydıntepe İlçesi Gümüşdamla Köyü yakın çevresini \rkapsamaktadır. Çalışma alanında Kabaköy formasyonunun tortul birimleri ve Kaçkar Granitoyidine ait kayaçlar \ryüzeyleme vermektedir. Detaylı inceleme yapılan cevherleşme alanı ve yakın çevresi Eosen yaşlı Kaçkar \rGranitoyidi ile Kabaköy formasyonu kontağında bulunmaktadır. Cevherleşmenin parajenezini ağırlıklı olarak \rmanyetit ve hematit az oranda ise pirit ve kalkopirit oluşturmaktadır. Arazide yapılan gözlemler sonucunda \rhematitleşme, limonitleşme, epidotlaşma ve killeşme türü alterasyonlar tespit edilmiştir. Cevherli örneklerden \ryapılan mineral kimyası analiz sonuçlarına göre piroksenlerin diyopsit, plajiyoklasların andezin ve anortit, \rgranatların grossular ve andradit bileşiminde olduğu belirlenmiştir. Piroksen ve granatların mineral kimyası \rdeğerlerine göre çalışma alnında bulunan skarn cevherleşmesinin Fe-Skarn tipinde olduğu sonucuna varılmıştır.

  İncele
• DüzeltmeAçık Erişim2021/r/gumushane/14934
  Correction to: Crustal Contamination of Tertiary Volcanic Rocks: Evidence from K, U, Th and Radiogenic Heat Production Data in Eastern Pontides (NE Turkey) (Pure and Applied Geophysics, (2021), 178, 5, (1871-1888), 10.1007/s00024-021-02739-6)

  Maden, Nafiz; Akaryalı, Enver; Aydınçakır, Emre

  In the original version of this paper the captions of figures 5, 6 and 7 were inadvertently interchanged.

  İncele
• MakaleYalnız künye2021/r/gumushane/14575
  Crustal Contamination of Tertiary Volcanic Rocks: Evidence from K, U, Th and Radiogenic Heat Production Data in Eastern Pontides (NE Turkey)

  Maden, Nafiz; Akaryalı, Enver; Aydınçakır, Emre

  Herein, we present new 238U, 232Th, and 40K radionuclide concentrations, density and radiogenic heat production (RHP) data on the Tertiary volcanic rocks outcropping in Borçka, Gumushane and Trabzon regions within the Eastern Pontide Orogenic Belt (EPOB). The mean K values for Trabzon, Borçka and Gümüşhane regions were 2.19 ± 0.87%, 0.90 ± 0.70% and 0.59 ± 0.25%, respectively, the mean U values for Trabzon, Borçka and Gümüşhane regions were 2.12 ± 0.76 ppm and 1.29 ± 0.68 ppm and 0.90 ± 0.32 ppm, and the average Th values were calculated as 6.54 ± 2.32 ppm, 2.49 ± 1.93 ppm and 1.33 ± 0.60 ppm for Trabzon, Borçka and Gümüşhane regions, respectively. The average Th/U values are 3.38 ± 1.48 for the Trabzon region, 2.01 ± 1.22 for the Borçka region, and 1.69 ± 1.09 for the Gümüşhane region. Average U/Th values were calculated as 0.35 ± 0.14, 0.71 ± 0.52 and 0.89 ± 0.72 for the Trabzon, Borçka and Gümüşhane regions, respectively. The RHP values were determined as 1.16 ± 0.35 μW m - 3, 0.58 ± 0.33 μW m - 3 and 0.37 ± 0.10 μW m - 3 for Trabzon, Borçka and Gümüşhane regions, respectively. The Tertiary aged rocks in the EPOB that we have examined within this study scope have been derived from an enriched mantle, previously metasomatized by fluids derived from subducted slab. The parental magma of Eocene basaltic rocks was contaminated with crustal material during the ascension of the magma through the crust or in the shallow-level crustal magma chambers.

  İncele
• MakaleAçık Erişim2020/r/gumushane/17860
  Geological and Mineralogical Investigation of Kılıçören (Gümüşhane) Pb-Zn-Cu±Au±Ag Mineralization

  Akaryali, Enver; Şal, Fatih

  The study area is located in Madenin Sırtı region of Kılıçören village of Gümüşhane. The mineralization found in the study area is developed within andesitic rocks of Early-Mid Jurassic Şenköy Formation. The ratios of Nb/Y and Zr/TiO2 of volcanic rocks in the area indicated these rocks are andesite and andesite/basalt according to the chemical analyzes. It is determined that the volcanics have calc-alkaline character based on the AFM, SiO2 versus K2O and SiO2 versus ThCo diagram. The mineralization is observed as a vein situated in the NW-SE trending fractures developed in andesites belonging to Early-Middle Jurassic Şenköy Formation. The veins observed in the field have the thicknesses ranging from a few centimeters to several meters and length continues for several meters. The silicified ridge pointing to an epithermal system is about 5 meters in thickness and 50 meters long, having a bearing of N25°W. In the field, besides to silicification, the alteration types such as hematitization, limonitization, chloritization and sulfurization have been identified in the rocks around the mine. The pyrite, chalcopyrite, galena, sphalerite, fahlerz and quartz form the paragenesis of mineralization. In the mineralization, which is developed in two different phases, the replacement, separation, inclusion and cataclastic textures are the most important texture types observed. Especially, the observation of space filling and comb textures in quartz-containing samples, suggests that the mineralization in the field may have developed in the epithermal system.

  İncele
• MakaleAçık Erişim2020/r/gumushane/17771
  Flotasyon Tesis Atıklarının Asit Üretme Potansiyeli ve Kirliliğin Önlenmesi, Gümüşhane, KD Türkiye

  Alemdag, Selcuk; Akaryali, Enver; Gücer, Mehmet Ali

  Madencilik faaliyetlerindeki çevre kirliliğinin birincil kaynağını, çoğunlukla metalik, kömür ve asfaltit madenlerinde meydana gelen asit drenajı oluşturmaktadır. Bu çalışmada, Pb-Zn cevherleşmesinin flotasyon tesisi atıklarının asit üretme potansiyelleri jeokimyasalanalizler, kısa-dönem temas sızıntı testleri ve Asit-Baz Muhasebesi (ABM) işlemlerini kapsayan statik testlerle incelenmiştir. İşlenen cevherin mineral parajenezini başlıca pirit, kalkopirit, sfalerit ve galen mineralleri oluşturmaktadır. Cevherli atık örneklerinin iz element konsantrasyonlarında, özellikle S, Zn, Cu, As, Sb, Cd, Hg, Ag ve Bi gibi potansiyel toksik metallerdeki yüksek zenginleşme cevherin türü ile doğrudan ilişkili olup, yeraltı suyunu kirletme potansiyeline sahiptir. Kısa-dönem temas sızıntı testlerine göre, örneklerin pH değerleri (9.55-10.60, n= 10), kıta içi su kaynaklarının kalite sınıflandırmasına göre, dördüncü-sınıf (IV) kalite sularını işaret etmektedir. Bununla birlikte, sülfit-sülfür (%S2: 2.92-3.98, n= 10), Net Nötralizasyon Potansiyeli (NNP; 32 kg CaCO3/t 149 kg CaCO3/t, n= 10) ve Nötralizasyon Potansiyel Oranı (NPO; 0.20-0.80, n= 10) değerleri cevherli atık malzemenin potansiyel asit üreticisi olduğunu göstermektedir. Baraj eksen yeri ve rezervuar alanında açılan sondaj kuyularında kaya kütle geçirimliliğini değerlendirmek için lugeon deneyleri yapılmış ve geçirgen özellikte (K= 2x10-6 m/s) olduğu belirlenmiştir.

  • 
  • 
  İncele