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Residual rocky forms of the Flysch Carpathians are distinguished by their high scientific value. Some of the representative groups of such flysch tors are located in the Wisnicz Foothill and Ciezkowice Foothill. Those attractive assemblages of sandstone- to conglomeratic tors are the Stone Town Nature Reserve, the Witches Waterfall natural monument, and the quarry in Ostrusza. Other large objects are rocky forms: the Wieprzek Tors in Siekierczyna, the Devils Playground in Plawna, and the Devils Rocks in Bukowiec. ...

The Holocene evolution of the Black Sea remains one of the most debated topics in Quaternary geology, primarily due to the dramatic transition from a semi-isolated lake to a marine basin. The South Bulgarian coast, extending from the Balkan Mountains to the Rezovo River, represents a complex geomorphological system shaped by post-glacial sea-level rise, tectonic fluctuations, and anthropogenic pressures. This paper synthesizes current stratigraphical and archaeological data to reconstruct the Holocene evolution of...

The southern part of the Vysocina region (Bohemian-Moravian Highlands), defined by the surroundings of towns Telc and Slavonice, has been associated with the use of local crystalline limestones – marbles, since the Middle Ages. These marbles were burned to produce lime that was used not only for traditional masonry, but also for renders and plasters. Nowadays, analyses of preserved fragments of incomplete burned marble or binder-related particles in historical objects represent a valuable source for the rediscov...

High-temperature drilling in deep HPHT and geothermal wells (>180–220 °C) causes thermal degradation of drilling fluids, which compromises hydraulic performance and accelerates wear of PDC and diamond-impregnated bits. This study evaluates three fluid systems – high-temperature oil-based mud (HT-OBM), thermally stabilized water-based mud (HT-WBM), and nanoparticle-enhanced synthetic-based mud (nano-SBM) – subjected to static aging in HPHT cells at 150–240 °C for 16–40 hours, followed by measurements of...

The present study aims to develop methodological approaches for the investigation of fine-dispersed gold in ores from primary (bedrock) deposits and placers, with the objective of improving recovery efficiency. The type of gold under investigation exhibits a number of distinctive characteristics that substantially differentiate the conditions of its concentration, distribution within ore horizons and bodies, and the reliability of its analytical determination using conventional methods from those applicable to sma...

The article provides brief characteristics of the discovered deposits in the Surkhandarya oil and gas region, the results of research work by a number of scientists and a number of exploratory seismic surveys carried out. As a result of these works, the presence of a large number of areas with a high-amplitude structure was revealed, which are favorable signs for the accumulation of hydrocarbons. The analysis of new geological and geophysical materials based on modern equipment and computer programs of various com...

Rare metals such as Sn, W, Ta, Nb, Li and rare earth elements are essential for modern technologies, renewable energy systems and advanced materials. Their growing demand increases the importance of studying rare-metal provinces and identifying new perspective areas. The Kalba–Narym belt in Eastern Kazakhstan is one of the main rare-metal regions of Central Asia. However, the potential of its south-eastern part remains insufficiently evaluated. This paper considers the Cherdoyak deposit as an example of greisenâ...

The territory surrounding the Tekeli polymetallic tailing storage facility (SE Kazakhstan) represents a highly transformed technogenic landscape where natural ecosystems have been replaced by heterogeneous ecotopes with distinct abiotic constraints. This study aims to classify technogenic ecotopes and characterize their abiotic parameters to provide a scientific basis for ecological restoration. Four major ecotopes were identified based on geomorphology, substrate origin, granulometric structure, moisture regime, ...

The tectonic setting of Albania, influenced by the collision with the Adria microplate, is divided into two structural domains: an external compressional zone and an internal extensional one. Two main fault systems characterize the region-the longitudinal system (NW-SE to NNW-SSE), consisting of thrust and reverse faults, and the transversal system (NE-SW), comprising strike-slip faults. The Lushnje-Elbasan transverse fault, oriented NNE, is associated with the Dumrea diapiric dome and the Elbasan Quaternary grabe...

Crystalline limestones - marbles, are historically one of the most important raw materials exploited in the area of the Bohemian-Moravian Highlands (Vysocina region). Their use is connected with the first construction of masonry buildings since the Middle Ages. Local marbles were first used as raw material for lime burning, then as building stone, decorative stones or as individual elements in building constructions. The most famous locations where these marbles were used include the Cistercian monastery in -dar n...

The Alasehir Graben hosts a thick sedimentary sequence of terrestrial clastics deposited from the Early Miocene to the present. Oil shales occur with thin- to medium-bedded sandstones, siltstones, and shales in the upper part of Alasehir Formation. This study evaluates depositional settings and paleoenvironmental conditions via inorganic geochemistry of oil shales. X-Ray Diffractometer results show the presence of quartz, clay, mica, feldspar, calcite, chlorite, pyrite, and ilmenite. Al2O3 shows strong positive co...

The Sredogriv low-grade metamorphic rocks belongs to the Montana unit of the Western Balkan Zone in northwestern Bulgaria. The low-grade rocks mainly consist of metamorphosed greenschist facies clastic-marly-tuffaceous precursors and minor basic to acidic, presumably olistostromic magmatic rock bodies. Here, we present whole-rock geochemistry of metabasic dyke-like bodies in the Sredogriv metamorphic rocks. Field observations revealed that the dyke-like bodies are intruded into the Sredogriv sedimentary succession...

The spatial and temporal relationship between petroleum and ore deposits has attracted the attention of scientists since the 1960s, when a connection was determined between oil-gas formation processes and ore-forming processes, which led to the formation of Pb-Zn Mississippi-type deposits, Carlin-type gold deposits, and stratiform copper deposits. These studies concluded that there is a paragenetic relationship between petroleum fluids and ore mineralization. To date, studies concerning the relationship between se...

The aim of this study is to conduct an in-depth analysis of data on the genesis of pegmatite deposits of the Kalba-Narym rare metal belt, features of rare metal mineralization. The research methodology includes the analysis of existing information on the study of geology and structural-tectonic conditions of the formation of rare metal deposits within the central part of the Kalba-Narym batholith. Field studies, sampling (more than 40 samples), and study of the mineralogical composition of pegmatites and host rock...

Miocene deposits are widespread in the Carpathian Foredeep in Poland (the northernmost part of Central Paratethys). The Poreba Zegoty XXV/25 borehole is located about 25 km on the west from Krak-w in the western part of the Carpathian Foredeep. The profile of Miocene deposits in this borehole includes the Klodnica and Skawina Formations. The Skawina Formation sediments are represented by grey and ash-gray claystones slightly brecciated in places. Micropalaeontological studies were conducted on the Skawina Formatio...

Investing in ensuring the quality and safety of movement on highways is not a one-time process. Institutions charged with ensuring quality crossing surfaces must constantly monitor and repair the highway network so that it remains in the best possible condition. Because the funds available to maintain the highway network are limited, it is essential that decisions taken to maintain and rehabilitate the highway network are spent justifying each intervention. Layer management systems at the network and project level...

The article considers the systematic errors of estimation of reserves and average contents of useful component in exploration of alluvial deposits of nesting, tape, etc. structures. The article identifies and evaluates the main components of systematic errors in the assessment of mineral content, useful and harmful components in alluvial deposits based on theoretical, experimental and generalized published works: insufficient density of the exploration network; error due to unrepresentative sample size. These erro...

This study examines the geomorphological and structural factors influencing the formation of coastal dunes along the Strandzha coastline of Bulgaria. Through the integration of GIS-based analyses, morphometric data, and geological profiles, the primary morphostructural units shaping coastal dynamics have been identified. These geological, morphostructural, and geomorphological conditions have provided the necessary prerequisites for dune formation. The research identifies a total of 17 dune systems along the Stran...

Hydrothermal processes, particularly hydrothermal eruptions, play a key role in forming epithermal gold-silver deposits. Such deposits, first described by White [1] and Lloyd [2], are found in both active and ancient hydrothermal systems [3]. These processes are linked to geothermal systems, volcanic activity, and fluid circulation, but their exact mechanisms and influence on metal concentration remain debated. This study examines the role of hydrothermal eruptions and key factors (temperature, boiling, chemical c...

The Globigerina–bearing Tuffs and Marls are deposits included in the Slanic Molasse. Several formations can be separated within these deposits some of the units maintaining remarkable lithofacial consistency, so that they can be recognized in the entire out – cropping area of the Carpathian Molasse. Th e Globigerina–bearing Tuffs and Marls has been described and separated by V. Marutiu under the name of the “Slanic Tuff”[1] . The most spectacular exposures of this formation occur at Piatra Verde near Sla...

Western Anatolia is one of the world’ s most rapidly extending regions. The N-S extension commenced in Late Oligocene in this region sh ortly after the collision of Eurasian (the Pontides) and Gondwanan (the Anatolide-Tauride Platform) continental blocks. This extension lead to exhumation of deeply buried footwall rocks in core complexes (i.e. the Menderes Massif) and to development of a series of E-W, NE-SW and NW-SE-trending graben system on the hanging walls of low-angle detachment fault system. Thus, compres...

Post collisional volcanic rocks cover large areas in the east of the Biga peninsula, which is located in the NW Anatolian magmatic belt along the southern margin of Marmara Sea. These volcanic units span a compositional range from calc-akaline (i.e. andesite, dacite, and rhyodacite to rhyo lite), to alkaline (olivine basa lts) lavas. All rock units display coherent variation trends on the major and trace element Harker diagrams. Cenozoic volcanic sequences exposed in the east of Biga are divided into three volcano...

The Romanian coasts can be divided in two categories: erosion coasts (cliff shores) and accumulative coasts (barrier beaches). The activ e behavior of the cliffs is due to the action of marine abrasion and slope processes, landslides and gravitational collapses. Cliff shores between Cape Midia and Vama Veche has a complex lithological profile. Silt and clay particles are carried seaward by the rip cu rrents system, while sand and gravel particles are conveyed along the coast. Textural and mineralogical study of th...

Regularities in the distribution and forma tion mechanism of gi ant Cu-Au-porphyry deposits have been discussed by many authors. Most recent works are dedicated to the problem of their formation. The deposits of Macedonia discussed in this communication usually contain up to 150 000 t of copper with the Buchim deposits likely being the smallest in the world am ong similar recently mined deposits. The long- term economically profitable development of the latter refutes the traditional opinion that only Cu-Au-porphy...

The Dardanian zone (Serbian-Macedonian massif) represents the western part of the Rhodope crystalline basement. This zone was structured and metamorphosed during the Hercynian and post Hercynian tectonic st ages. The geological mapping at 1:25.000 [1] show that a of the studied region is built of crystalline Pale ozoic basement. The important aspects have been identified in the structure and metamorphism from this part of western Rhodopes. The study of the deformed Variscian and Hercynian tectonic phases are diffi...

Geostatistical analysis provides a powerfu l tool for enhancing the prediction and decision making capabilities of geologists and mine planners. The majority of practicing geologists are involved with mining and/or exploration ventures. As such a significant proportion of the geologist’s time is devoted to designing and impl ementing drilling and sampling progr ammes and using the resultant data to predict (and reconcile) reserve tonnages and qualities on a variety of scales, ranging from life-of-mine areas to d...

Diagenesis and geochemistry of three selected and well exposed outcrops of Qamchuqa Formation (Early Cretaceous) at Kurdistan Region northeastern Iraq were examined. Lithologically this formation is mainly composed of dolomite, and limestone beds. Petrographic study of the Qamchuqa Formation reveals that the skeletal and some non- skeletal grains within the limestone a nd dolomitic limestone beds are the main components of this formation. Micritizati on, cementation, neom orphism, compaction, dissolution and dolom...

Romanian Plain occupies from the geotecto nic point of view, the northern part of Moesian Platform, a platform forming a ri gid block between the Carpathians and the Balkans. Dacian Basin, opened after tecton ic movements, badenian , in the Sarmatian, outside the Carpathian arch, has evolved in a brackish sedimentation environment by the end of the Pliocene, after which was installed a lacustrine environment amid of water body restriction only in the southern pa rt of Romania. The lacustrine system is installed in...

The territory of our country in terms of cutting geological consists of different geological rocks of all ages from the Quaternary Neoproterozoic up. Magmata’s, and movement of plates that includes the Mediterranean region in earlie r geologic eras led to large-scale geomorphologic and geotect onic reconstruction of the whole region in general and including the region of Kosovo. The impact of these events in the wider region that exceeds the boundaries of our state led to the formation of provinces metallogeneti...

Lajaneh Fe skarn deposit is located in so uth of Shahrood City, North East of Iran. Mineralization is occurred as massive, veins and breccias in the c ontact of the dioritic intrusion with limestone. The dioritic intrusions in Lajaneh Fe skarn deposit display calc alkaline and metaluninous nature with I type characteristic. Tectonic setting discrimination diagrams show that dioritic intrusions in Lajaneh deposit belongs to volcanic arc granitoids (VAG). Negative anomalies of HFS elements like Nb, Ti, Ta and P and ...

The Upper Cretaceous Flysch series between Suhareka and Bajice is developed in the psamitic and brecciaed facies . The relation between them is tectonic, but south of the area a gradual transitio n from one to the other facies has been established. Psamitic Flysch facies is characterized by a constant composition and regular graded bedding on the whole area of its distribution. It is represented by three lithogenous types: limy, sandy and conglomeratic. The limy lithogenous types : is characterized by a fairly goo...

At Eastern Taurid , the age of Carbonate rocks, outcroping at soutgh of Yahyali (Kayseri) had been defined as Jurassic-Cret aceous age in previous studies. The unit wich had been named as Köroğlutepesi Limestones in previous studies, outcroping also Eastern Tufanbeyli (Adana) at Gümelek Hill, arround Kayap ınar and İğdebel villages. Foraminiferal biostratigraphy of The sedimantery rocks surfacing at these locationes, hase been defined. Have been get three measured stratigraph ic section in Tufanbeyli region....

Deh Salm Jurassic shales of Shemshak formation are located in south of Birjand city in East of Iran. The Jurassic shale of Shem shak formation in this area is partly metamorphosed and display finely foliation. Th e trace element data of Deh Salm shales are compared with upper continental crust, clarke value of sedimentary rocks and world's average of shales. Total sulfur concentrations vary from 0.01% to 0.55% with average of 0.18% that is lower than of sulf ur content of world's shale composition. Th, Y, Nb and Z...

This paper presents correlations of a porti on of bordering zone Kosova – Albania, in other words sheet K-34-78-A - Shishtavec. Sheet of the three neighbouring countries boarders Kosova –Macedonia – Albania and covers the are of roughly 387 km 2. Out of this area, 148 km2 or 38 % lay in Albania territory, more precisely in the surrounding of Kukës and Dibra towns. Othe r part, however, roughly 239 km 2 or 62 % lay in Kosova territory, Dragash Municipality (Sharr Mountain area). Geological map of each of the...

The presented paper describes artesian aquifer collector which is situated in the area of interest of the J. Sverma and Vrsany open pit mines. The area of interest is situated at the southern border of the central part of the Most Basin (previously North Bohemian Brown Coal Basin). The occurrence of severa l saturated collectors, which were created in this area in different geological peri ods (especially in the Upper Cretaceous and Miocene Period), is obstacle to the continuous extraction of coal from the beginni...

Considered the natural conditions for the fo rmation of gold, given the model of its deposits in the form of a schematic of industrial-genetic classification. Were shown the main types and examples of fields. We have created a model can serve as the scientific basis for prediction and exploration of new industrial facilities to enhance the mineral resource base of mining and processing enterprises of Kazakhstan.

This work presents the geological structure of the Chipupushi area which is located on the border between the Northwestern Province and Copperbelt Province in the Republic of Zambia. Geological structure of the Luswishi dom e, within which the Chipupushi area is, consists of: Igneous rocks, the complex of ultra basic, basic, intermediate and acid magmatic rocks, the Basement Complex, which was built of schist, gneiss, granite - gneiss and subordinated pegmatite as well as the Katanga super group out of which the C...

The area under study is located in east Azerbaijan and southwest of Ardabil. In this area the volcanic rocks are placed over the Oligocene and lower Miocene clastic sedimentary rocks and under lower Pliocene epiclastic sedi ments. Therefore, their age is middle and upper Miocene. These volcanic rocks have been extruded in dome shape from the fissures of an eruptive caldera. These domes are rich in silica. From the boundary to the center of caldera, these domes are categorized into three types with regard to their ...

During mining activities, as a result of removal of inert materials for unfolding layers of lignite, has resulted into covering and degradation of large areas of land. This inert material is now distributed in some areas, in the form of landfill, often referred to as wastelands or dump tuck, and occupied this area: Folding Lismir – Kuzmin 780 ha, folding Shipitullë – 136 ha, folding deep Lugu 437 ha, folding Vasilevo 157 ha, folding Palaj 49 ha. From the above data results that the degraded land from wastelan...

Forecast of international experts shows that by the end of the first quarter of this century there will be about 20-30% less copper produced from natural resources in relation to consumption (needs) in the world. Therefore, it is planned to compensate for the lack of processing of raw materials with recycling of technogene waste, which contains copper. In this respect the planned implementation of this process (technological process) has a special significance, especially as the processi ng of these raw materials,...

The Alborz range, surrounding the south Caspian basin, forms a composite orogenic belt and has suffered shortening and uplift through several tectonic events from the Late Triassic Cimmerian orogeny to the present day stage of convergence between the Arabian and Eurasian Plates. The central Alborz, comprises main ly Tertiary rock formations, is an intensively deformed portion in which deformation is accommodated on major reverse faults. These faults are transversely crosscut by several NE- and NW- trending strike-...

Significant economic mineralizations of Kosova territory are hydrothermal deposits of Pb-Zn. These deposits are located mainly in northern and eastern part of Kosovo, the so- called Trepca ore belt, which has a longitudinal stretch about 80 km and consists of a number of mineralized deposits and occurrences. In the geological context, this ore belt is part of the Vardar zone and associated with volcanic and sub volcanic rocks. Most of these deposits are located in the sequences carbonate and other rocks of differe...

The main topic of the article is mineralogical research in the North Bohemian Brown Coal Basin. This work summarises new knowledge for the 2002 – 2009 period, five new minerals were identified in the basin in the interval: anorthite, esseneite, ferrierite, melilite, and srebrodolskite. The second object of the article is the situation of important localities of the Krušné Hory Mountains. Main attention is devoted to a newly discovered amethyst locality Černý Potok.

Some 100 core samples of coal and coaly units from the Pliocene succession (Hotam Д±Еџ Formation) were collected from well KK-147, in the southern part of Central Turkey (KarapД±nar-Konya). 30 samples were screened for total organic carbon (TOC) content. Selected samples were then analyzed by Rock -Eval Pyrolysis. Visual kerogen analysis and vitrinite reflectance measurements were also undertaken. Detailed data from thick Pliocene sediments made it possible to construct an organic facies framework using different ...

This study was carried out in Golbasi (Ad Д±yaman) region (SE of TURKEY), which owns rare coal formations in the region. Chemical, petrographic analysis and organic geochemical evaluations of the Tertiary aged coals were taken into consideration. Coal quality investigation along with proximate (m oisture, volatile matter, fixed carbon, ash) and elemental analyses (C, H, O, S, N) were performed and revealed. The huminite reflectance of organically abundant matter and coal levels were found to be between 0.30 and 0....

The studied area is situated about 70 Km in west of Damghan, and from the structural point of view, the area is part of south of central Alborz zone. Granitoid bodies intruded into late Eocene volcanic and volcanoclastic, mainly composed of monzonite and granite composition. Mineralogically, these rocks contain qua rtz, plagioclase, alkali- feldspare, amphibole, clinopyr oxene, biotite, zircon, apatite, and opaque minerals. Textures of rocks are microgranular and fi eld and textural evidences show that the plutone...

Detailed petrographic studies, whole rock geochemistry and in situ U-Pb geochronology of syenite from Iwo area of the southwestern Nigeria has been performed. The results indicate that the syenite is metaaluminous belonging to the calc-alkaline magmatic series whose parental melt was derived fr om melting of the upper mantle/lower crustal source. Precise U-Pb dating of zircons is done by LA-ICP-MS and age of 625 В± 6.1 Ma is obtained. The field and petrological i nvestigations show that the syenite was emplaced sy...

Artova ophiolite complex is located along the North western and east margin in Yozgat (Turkey). The Mn-deposits in the Derbent an d Eymir areas are part of this ophiolite complex. These deposits, both banded and lenticular forms, are hosted by radiolarite and are generally overlying volcanics. Braunite, jacopsite, psilomelane and goethite are main constituents of the manganese ores in Eymir (Sorgun-Yo zgat) and manyetite, manganite, pyrolusite and goethite are main constituents of the manganese ores in Derbent (Ma...

A similar succession of Foliation Inflection/In tersection Axis trends preserved within porphyroblasts (FIAs) is present in two areas separated by 200 km along the Rocky Mountains. PreCambrian rock s in Central Colorado and Northern New Mexico were affected by deformation and metamorphism from approximately 1506 to 1370 Ma. A succession of five FIAs trending W-E, SSW-NNE, NNW-SSE, NW-SE and WSW-ENE has been distinguished in Central Colora do that have been dated at 1506В±15 Ma, 1467В±23 Ma, 1425В±18 Ma, not dated ...