The Hasançelebi deposit in eastern Turkey, with proven reserves of 95 million metric tons, is a coppergold−bearing iron oxide deposit. It is chiefly hosted by rocks that underwent widespread sodic-calcic and potassic styles of alteration. In the Hasançelebi district, pervasive Na-Ca and K-Fe alteration types are overprinted by sericitization and by late alteration that occur in multiple, overprinting systems. The age of hydrothermal alteration and mineralization (ca. between 74−68 Ma) overlaps with the age of alkaline magmatism in the Hasançelebi district. Crystallization and cooling of alkaline magmatism is associated with hydrothermal features that spanned the duration of the district's igneous history. The 40 Ar/ 39 Ar and U-Pb geochronology of magmatism indicate that the hydrothermal system was synchronous with diabase and syenite and/or microsyenite porphyry intrusions and consisted of several discrete phases of Na-Ca and K-Fe alteration. The oldest alteration (phase 1) formed at ca 74.4 to 74.3 Ma; it is spatially and temporally associated with the emplacement of diabase dikes and contains scapolite and phlogopite. The next younger alteration (phase 2) formed at about 71.3 Ma and is spatially and temporally associated with syenite porphyry and microsyenite porphyry intrusions. It consists of scapolite , garnet, pyroxene, and actinolite that are superimposed on the first alteration phase. The next alteration assemblage (phase 3) formed at about 68.6 Ma and consists of phlogopite 2 and magnetite mineralization. Still later alteration (phase 4) overprints phases 1, 2, and 3 and consists of sericite-quartz, chalcopyrite, hematite, calcite, fluorite, and barite. Oxygen (δ 18 O) and hydrogen (δD) isotope analyses were carried out on phlogopite, sericite, barite, calcite, fluorite, and quartz representing the mineral assemblage formed during phases 1 and 4 of the hydrothermal alteration. The calculated δ 18 O(H 2 O) and δD(H 2 O) composition of the fluids that formed preore K-Fe alteration and postore alteration of phase 4 range between 15.1 to 8.5 and −124 to −85.6 per mil, respectively, and partially overlap the range for traditional magmatic waters. Oxygen and H isotope compositions from alteration minerals highlight two major points: Na-Ca and K-Fe alteration assemblages are likely derived from hightemperature primary magmatic fluids, and late sericitization is likely derived from fluids exsolved from cooling alkaline plutons during hydrothermal fracturing and consequent degassing at moderate temperatures. The initial εNdi values of the alteration zones range from −2.02 to −2.08, close to the calculated εNd value of associated syenite porphyry at the time of alteration (εNd (68.64Ma; −1.9). Nd-Sr isotope compositions combined with 40 Ar-39 Ar and U-Pb geochronology of the associated alteration suggest that the fluids were sourced from coeval diabase dikes and syenite porphyry and/or microsyenite porphyry intrusions. The rare earth element characteristics, 40 Ar-39 Ar and U-Pb geochronology of alteration and fr...
This study aims to investigate hydrogeological, geochemical and geotechnical properties of the Aksaray University campus area. Within this context, the hydrogeochemical results of water samples collected from 4 different water points from the campus area, geochemical analysis of 17 soil samples, and geotechnical properties of rock samples obtained from drill core and description of core-logging performed in 2008 were evaluated. Hydrogeological studies have shown that two different water facies with Na-Cl and Ca-Cl water types developed in the study area. These waters are classified as low quality, but usable, and 3 rd quality for irrigation water according to irrigation water standards and electrical conductivity values. According to geotechnical experiments, it was determined that the argillaceous limestone, which spread widely under the cover of the campus area, had bearing capacity of 36.5 kg/cm 2 and belonged to the low strength rock class. As and Pb contents of the soil samples are at higher values, compared to the average upper crust values. According to the anomaly distribution maps prepared for Cl and Na elements, it was determined that east, southwest and northwest parts of the campus area contain higher values of Na and Cl than that of other parts of campus. The results of this study will provide more planned and efficient green-area studies to be carried out in the campus area and protection of the green-areas.
In this study, an epithermal goldfields‐water quality index (EGF‐WQI) and the associated classification system have been proposed to define drinking water quality of the water resources in regions where epithermal gold mineralization exists. In this context, two hydrogeochemical data sets from 15 water resources are used. EGF‐WQI is designed using 21 different criteria under 4 main groups and 15 alternatives. To determine the importance and efficiency values of the criteria, analytical hierarchy method (AHP) is used. The water quality classification system is defined by 4 different categories, namely, “very good,” “good,” “acceptable,” and “inappropriate.” In order to ensure consistency of the findings, efficiency scores of the AHP method are compared with the results obtained from the technique for order preference by similarity to ideal solution and data envelopment analysis models. The index results obtained from AHP processes are converted into water quality distribution maps by using the Kriging interpolation method. EGF‐WQI results are observed to be compatible with the water quality standards developed by organizations such as the World Health Organization and Turkish Standards. EGF‐WQI can be used as a reliable and valid index to evaluate the water resources in regions where alteration and mineralization are present.
İnlice yüksek sülfidasyon epitermal altın yatağı, Erenlerdağ-Alacadağ Volkanik Kompleksi (EAVK) içerisinde ve Konya ilinin yaklaşık 40 km güneybatısında yer almaktadır. Çalışma alanında stratigrafik konumlarına göre alttan üste doğru andezit, blok ve kül akıntısı, bazaltik andezit lav akıntısı ve andezit lav akıntısı olmak üzere dört birime ayrılan volkanik ve volkano-sedimanter kayaçlar, yamaç molozu ve alüvyonlar tarafından uyumsuz olarak örtülürler. Andezitler içerisinde gözlenen alterasyonların merkezinden dışa doğru sırasıyla kovuklu-şeker ve kalsedonik/opalin dokulu kuvars damarlarından oluşan silisleşmeler, ileri arjilik, ortaç arjilik ve piropilitik alterasyon zonları tanımlanmıştır. Bu alterasyon topluluklarına ek olarak sadece Merkez Zonun derin kesimlerinde gözlenen manyetit, kuvars, biyotit ve anhidrit içerikli potasik bir alterasyon zonu da tanımlanmıştır. Cevherleşmeler, yaygın olarak pirit, sırasıyla daha az oranda enarjit, kalkopirit, kalkosin, kovellin, sfalerit ve markazit gibi sülfid mineralleri ile temsil edilmektedir. Petrografik olarak altın taneleri özellikle sülfid minerallerinin oksidasyona maruz kaldığı kesimlerde saçınımlı olarak 2 ile 6 µm arası boyutlarda gözlenmektedir. Alterasyon zonlarındaki jeokimyasal değişimin derecesi silisleşmelerden piropilitik alterasyona doğru azalmakta olup, bu değişim, alterasyon zonlarında gözlenen mineralojik değişimle uyumludur. Bununla birlikte taze andezitlerden ileri arjilik alterasyon ve silisleşmelere doğru özellikle As, Sb, Bi, Ag ve Au gibi elementler zenginleşme gösterirken, Zn ve Ni’deki fakirleşmeler belirginleşmektedir. Ayrıca yapılan çalışmalar kalsedonik/opalin dokulu kuvars damarlarındaki Pb ile ileri arjilik alterasyon ve silisleşmelerdeki düşük Rb/Sr değerlerinin en azından İnlice bölgesi için-jeokimyasal bir kılavuz olarak kullanılabileceğini göstermektedir.
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