Relevant bibliographies by topics / Argillizit

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Academic literature on the topic 'Argillizit'

Author: Grafiati
Published: 5 June 2025
Last updated: 2 August 2025

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Journal articles on the topic "Argillizit"

1

Kochergin, Alexander Vladimirovich, and Natalia Vasilievna Granovskaya. "ARGILLIZITES IN THE WEATHERING CRUSTS OF THE WESTERN SLOPE OF THE SOUTHERN URALS." Geologicheskii vestnik, no. 3 (November 1, 2024): 48–57. http://dx.doi.org/10.31084/2619-0087/2024-3-5.

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The data on the features of the linear weathering crusts of the western slope of the Southern Urals and the presence of low-temperature hydrothermal-metasomatic clay formations similar to argillizites are presented. Mineralogical-geochemical and structural-geological features of argillizite bodies, their spatial and genetic connections with ore objects are established. Приведены данные об особенностях линейный кор выветривания западного склона Южного Урала и наличии в них низкотемпературных гидротермально-метасоматических глинистых образований, сходных с аргиллизитами. Установлены минералого-г
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Pribavkin, S. V., E. I. Soroka, O. B. Azovskova, et al. "Association of Siderite with Iron Sulfides and Silicates in Rocks of Mikheevskoe Cu(Mo,Au) Porphyry Deposit (Southern Urals)." Геология рудных месторождений 65, no. 4 (2023): 354–68. http://dx.doi.org/10.31857/s0016777023040044.

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The mineral association of siderite with Cu–Fe sulfides, cronstedtite, and goethite were first recognized when studying the Mikheevskoe Cu(Mo,Au)–porphyry deposit. This association is confined to fault zones, where it fills a network of mineralized fractures developed on porphyry- and argillizite-type ores. Minerals of this association were also identified in some argillizite samples of this deposit. The formation conditions of this mineral association and its relation to the evolution of the Late Paleozoic porphyry system or other endogenic–exogenic processes manifested during the subsequent
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Sukach, V. V., L. V. Іsakov, and Y. E. Khomych. "MINERALOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE HURIVKA COMPLEX P-U-TR ORE OCCURRENCE, INHUL MEGABLOCK, UKRAINIAN SHIELD." Geochemistry and ore formation 44 (2023): 47–62. http://dx.doi.org/10.15407/gof.2023.44.047.

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The article presents the results of the study of the Hurivka apatite-uranium-rare earth ore occurrence, which is confined to the contact of the southern part of the Hurivka granitoid massif with metasedimentary rocks of the Inhul-Inhulets series. Argillizites, which host the productive mineralization, are represented by two zones: the lower montmorillonite-chlorite zone and the upper kaolinite-chlorite zone with hydromica. The concentrator minerals of rare earths (∑TR=0.05-0.5 %) in the bedrock are xenotime and monazite, while only xenotime was detected in argillizites. At the same time, minor
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Alekseev, V. I. "ORE-BEARING METASOMATITES ASSOCIATED WITH LITHIUM-FLUORIC GRANITES OF THE SEVERNY MASSIF (CHAUN-CHUKOTKA)." Tikhookeanskaya Geologiya 44, no. 3 (2025): 18–32. https://doi.org/10.30911/0207-4028-2025-44-3-18-32.

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The facies composition and stages of formation of hydrothermal-metasomatic units spatially associated with lithium-fluoric granites of the Severny massif in Chaun-Chukotka were studied based on large-scale geological mapping, as well as petrographic, mineralogical and geochemical data. The identification of zwitters of the Severny massif - quartz-topaz-zinnwaldite greisens accompanying Li-F granites and bearing rare-metal (Nb, REE, Y, Li, Bi, Sn, W) mineralization is justified. The bulk of zwitter mineralization is distributed within the massif in the form of moderate alterations in biotite le
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Belousov, P. E., A. A. Vol’fson, A. V. Volkov, et al. "Argillizite “Hats” of Kompleksnoe Ore Occurrence in Kayenmyvaam Volcanic Uplift (Central Chukotka)." Journal of Volcanology and Seismology 14, no. 5 (2020): 283–91. http://dx.doi.org/10.1134/s0742046320050024.

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MAEDA, Hiroyuki. "An Intimate Relation between a Hydrothermally Argillized Zone and a Slide." Landslides 31, no. 1 (1994): 21–28. http://dx.doi.org/10.3313/jls1964.31.21.

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Cherepanov, A. A., N. V. Berdnikov, and I. A. Astapov. "Rare-Earth Element Mineralization in Argillized Granites of Southern Primorye: New Data." Russian Journal of Pacific Geology 16, no. 2 (2022): 153–60. http://dx.doi.org/10.1134/s1819714022020038.

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Cherepanov, A. A., N. V. Berdnikov, and I. A. Astapov. "RARE EARTH ELEMENT MINERALIZATION IN ARGILLIZED GRANITES OF SOUTHERN PRIMORYE (NEW DATA)." Tikhookeanskaya Geologiya 41, no. 2 (2022): 101–8. http://dx.doi.org/10.30911/0207-4028-2022-41-2-101-108.

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Rare earth element (REE) mineralization in the weathered granites of Primorye is localized in the basement rocks and rocks along the periphery of the coal-bearing basins, which have been recently tectonically faulted and folded and have undergone argillisite metasomatism. It was shown that the clay material from the zones of intense argillization can be a source of scarce REE and yttrium. The ion-sorption and carbonate forms of REE+Y in them in combination with the clay composition of most of the ores make it possible to use cheap and low-toxic salt and hydrochloric acid solutions during heap
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Vilor, N. V., G. V. Bogdanov, T. I. Medvedeva, et al. "PRECAMBRIAN METASOMATITES AND FLUID SYSTEMS OF THE MARGINAL SUTURE OF THE SIBERIAN PLATFORM (Southern Prebaikalia)." Russian Geology and Geophysics 35, no. 2 (1994): 29–39. https://doi.org/10.2113/rgg.1994.35.2.29.

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In the southern edge of the Siberian Platform, metamorphism and metasomatism are expressed in the lower structural stories. The Upper-Archean post-migmatic metasomatism includes a complete cycle of the inversion of acid-basic properties of a fluid at 600–500 °C and 2–7.0 kbars with corresponding metasomatic formations. The Lower-Proterozoic metasomatites (450–670 °C, 1.8–5 kbars) contain quartz, quartz-feldspar, greisen, beresite, and propylite assemblages. Chlorite metasomatites formed at 130–440 °C are found on the boundary between the Middle- to Upper-Riphean story and the crystalline basem
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Leonova, Lyubov', O. Azovskova, and E. Soroka. "The peculiarities of the framboidal pyrites of the Mikheev porphyry copper deposit (Southern Ural)." Vestnik of geosciences, no. 9 (December 6, 2023): 33–39. http://dx.doi.org/10.19110/geov.2023.9.2.

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Framboids of pyrite were found in bituminized argillic metasomatites of the Mikheev porphyry copper deposit (Southern Urals). A wide occurrence manifestation of low-temperature metasomatism — argillization — is a feature of the rock complex of this deposit. According to the results of thermoweight analysis, the values of organic matter in bituminized argillic metasomatites correspond to kerite. The organic matter support the habitation of microbial communities, including the presence of element-depositing bacteria. The use of high-resolution scanning electron microscopy allowed identifing pres
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Book chapters on the topic "Argillizit"

1

Thoreson, Ronald F. "Geology of the Post Deposit, Eureka County Nevada." In Gold Deposits of the Carlin Trend, Nevada. Society of Economic Geologists, 1993. http://dx.doi.org/10.5382/gb.18.05.

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Abstract The Post deposit is located in Eureka County, Nevada, Section 19, T36N, R50E, approximately 40 km (26 miles) northwest of the town of Carlin and 7 km (4.5 miles) northwest of the Carlin #1 mill (Figure 1). The Post deposit is located along a spur of the Tuscarora Mountains that also hosts the Blue Star/Genesis and Deep Star deposits. Host rocks for the Post orebody are the sandstones, siltstones, calcareous mudstones, and limestones of the Siluro-Devonian Roberts Mountains and Popovich Formations, and the siliceous mudstones and siltstones of the Devonian Rodeo Creek unit. The Goldstr
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Williams, Cindy L. "Blue Star Subdistrict Zoned Alteration Mineralogy and Gold Mineralization, Eureka County, Nevada." In Carlin-Type Gold Deposits Field Conference. Society of Economic Geologists, 1997. http://dx.doi.org/10.5382/gb.28.23.

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Abstract The Blue Star subdistrict in the Carlin Trend, Nevada, includes multiple gold mines with 2 million ounces in reserve and past production totaling 3. 9 million ounces. The deposits are characterized by zoned alteration mineralogy and gold grades. From orebody centers outward the zones include: 1) a silicified core with erratic gold grade; 2) adjacent mill-grade (>0.050 oz/st Au) intense quartz-sericite-pyrite alteration; 3) enveloping leach-grade (0.006 to 0.050 oz/st Au) weaker sericite-kaolinite-quartz-pyrite alteration; 4) surrounding decarbonatized and intensely argillized w
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Tosdal, Richard M., Dean A. Enderlin, Gordon C. Nelson, and Norman J. Lehrman. "Overview of the Mclaughlin Precious Metal Deposit, Napa and Yolo Counties, Northern California." In Active Geothermal Systems and Gold-Mercury Deposits in the Sonoma-Clear Lake Volcanic Fields, California. Society of Economic Geologists, 1993. http://dx.doi.org/10.5382/gb.16.18.

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Abstract A late Pliocene and Pleistocene hot-spring deposit consisting of sinter terraces underlain by veins is the site of the McLaughlin Mine in northern California. The deposit is localized along the contact between hanging wall mudstone of the Upper Jurassic Knoxville Formation (basal formation of the Upper Jurassic and Cretaceous Great Valley sequence) and serpentinized ultramafic and mafic rocks of the Middle Jurassic Coast Range ophiolite in the footwall. The Stony Creek fault separates the two units, and dips moderately northeasterly. Pliocene basaltic andesite and volcaniclastic rocks
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Štohl, Jaroslav, Eva Žáková, and Jaroslav Lexa. "High-Sulfidation Epithermal Gold Deposit at Klokoč - Podpolom." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.08.

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Abstract The paleohydrothermal systems in the central zone of the Javorie stratovolcano are represented at the surface by conspicuous outcrops of secondary quartzites (residual quartz) and much less conspicuous argillized rocks. These zones of advanced argillic alteration were assumed during the early seventies to reflect porphyry copper systems at depth. Subsequent drilling at Banisko (Konecný et al., 1997), and a systematic metallogenetic survey in the central zone of the Javorie stratovolcano (Štohl at al., 1981) confirmed this assumption and provided extensive information concerning the ge
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Lexa, J., J. Štohl, and V. Konečný. "The Banská Štiavnica ore district." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.09.

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Abstract The Banská Štiavnica ore district is in the central zone of the largest stratovolcano in the Central Slovakia Neogene Volcanic Field, which is situated at the inner side of the Carpathian arc over the Hercynian basement with the Late Paleozoic and Mesozoic sedimentary cover. Volcanic rocks of the High-K orogenic suite are of the Badenian through Pannonian age (16.5– 8.5 Ma). Their petrogenesis is closely related to subduction of flysch belt oceanic basement underneath the advancing Carpathian arc and to back-arc extension processes. The stratovolcano includes a large caldera 20 km in
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Conference papers on the topic "Argillizit"

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Ciprian, Constantina, Delia-Georgeta Dumitras, Alexandru Laslo-Faur, Nicolae Calin, and Iuliana Pasuk. "STUDY OF THE ARGILLIZED (BENTONITIZED) DEPOSITS IN GURASADA AREA � SOUTHER APUSENI MOUNTAINS, ROMANIA." In 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/1.1/s01.040.

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Yu, Haixuan, Xiangguo Liao, and Hongliang Zhai. "Development and application of conversion from highly argillized and extremely difficult separate raw coal to coking coal." In Third International Conference on Optoelectronic Science and Materials (ICOSM 2021), edited by Siting Chen and Pei Wang. SPIE, 2021. http://dx.doi.org/10.1117/12.2617333.

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