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Journal articles on the topic 'Minerogenic'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

GURYANOV, VALENTIN, and VADIM KIRILLOV. "The nickel-bearing potential of the Kun-Manie minerogenic zone in the southeastern framing of the Siberian Platform." Domestic geology, no. 2 (June 5, 2023): 43–55. http://dx.doi.org/10.47765/0869-7175-2023-10008.

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The article summarizes results of researches of the nickel-bearing potential of the Kun-Manie minerogenic zone in the southeastern frame of the Siberian platform. The data of recent medium-scale gravimetric and geochemical surveys were analyzed. A brief characteristics are presented of PGE-containing Cu-Ni ores of the Kun-Manie deposit in the ore cluster of the same name, as well as of the Tuksani-Kukur ore region promising for the PGE-containing Cu-Ni mineralization. The main types of the ores and their mineral composition were determined. The perspectives of the minerogenic zone are consider

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2

Derbyshire, Edward. "Natural Minerogenic Dust and Human Health." AMBIO: A Journal of the Human Environment 36, no. 1 (2007): 73–77. http://dx.doi.org/10.1579/0044-7447(2007)36[73:nmdahh]2.0.co;2.

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3

Syrykh, Liudmila S. "SEDIMENTATION AS A CLASSIFICATION CRITERION FOR LAKES ON THE EAST EUROPEAN PLAIN." Географический вестник = Geographical bulletin, no. 3 (2023): 19–26. http://dx.doi.org/10.17072/2079-7877-2023-3-19-26.

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The article studies lake sedimentation on the East European Plain and adjacent areas. Lake sediment formation is researched in detail in paleolimnology. The main aim of the present study is to describe the features of lake sedimentogenesis on the East European Plain and to identify classes of lakes in accordance with the types of sedimentogenesis. PaleoLake Database, created for the analysis, contains paleolimnological information about the bottom sediments of lakes of the East European Plain and nearby territories. We analyzed 216 lakes located in different climatic and geological zones, for

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4

Pu, Wan. "Minerogenic Model of Chrysotile Deposits in Ultramafic Rocks." Acta Geologica Sinica - English Edition 3, no. 1 (2009): 31–39. http://dx.doi.org/10.1111/j.1755-6724.1990.mp3001004.x.

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5

Brain, Matthew J., Antony J. Long, David N. Petley, Benjamin P. Horton, and Robert J. Allison. "Compression behaviour of minerogenic low energy intertidal sediments." Sedimentary Geology 233, no. 1-4 (2011): 28–41. http://dx.doi.org/10.1016/j.sedgeo.2010.10.005.

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6

Yang, Bingjie, Anne Birgitte Nielsen, Karl Ljung, Elise Fahlgren, Anne Hormes, and Dan Hammarlund. "Quantitative landscape reconstruction and erosion history during the past 1,100 years in the Skogaryd Research Catchment, southern Sweden." Vegetation History and Archaeobotany 29, no. 6 (2020): 657–70. http://dx.doi.org/10.1007/s00334-020-00770-6.

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Abstract A sediment sequence from a small forest lake in southwestern Sweden was investigated to explore the effects of forestry and land-use on catchment erosion and delivery of organic and minerogenic matter to the lake. Catchment-scale vegetation changes during the last 1,100 years were reconstructed quantitatively at 50-year resolution using pollen analysis and the Landscape reconstruction algorithm (LRA). Variations in terrestrial organic matter input to lake sediments were assessed by total organic carbon (TOC) content and carbon to nitrogen (C/N) ratios. Changes in minerogenic matter we

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7

Kylander, Malin E., Anna Plikk, Johan Rydberg, et al. "New insights from XRF core scanning data into boreal lake ontogeny during the Eemian (Marine Isotope Stage 5e) at Sokli, northeast Finland." Quaternary Research 89, no. 1 (2017): 352–64. http://dx.doi.org/10.1017/qua.2017.84.

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AbstractBiological proxies from the Sokli Eemian (Marine Isotope Stage 5e) paleolake sequence from northeast Finland have previously shown that, unlike many postglacial records from boreal sites, the lake becomes increasingly eutrophic over time. Here, principal components (PC) were extracted from a high resolution multi-element XRF core scanning dataset to describe minerogenic input from the wider catchment (PC1), the input of S, Fe, Mn, and Ca-rich detrital material from the surrounding Sokli Carbonatite Massif (PC2), and chemical weathering (PC3). Minerogenic inputs to the lake were elevate

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8

Kortelainen, P., and S. Saukkonen. "Organic vs. minerogenic acidity in headwater streams in Finland." Water, Air, & Soil Pollution 85, no. 2 (1995): 559–64. http://dx.doi.org/10.1007/bf00476888.

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9

Grinenko, Vitalii, Valerii Baranov та Vladimir Deviatov. "North-Asian black shale ore-bearing megaprovince in the Northеastern Eurasia and its prospective minerogeny". Ores and metals, № 2 (6 серпня 2022): 36–55. http://dx.doi.org/10.47765/0869-5997-2022-10009.

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The North-Asian ore-bearing black shale megaprovince has first been distinguished in the northеastern Eurasia. Its distinguishing within the two contiguous platforms, the Siberian and East Siberian (buried under the Verkhoyansk-Kolyma folded area) ones, is based on a cyclic formation of rock sequences enriched in clayey and organic matter in the boreal sea basin. Within these contiguous platforms, clayey and black shale rocks was identified, assigned to geological formations of the “class of black shale troughs, depressions, and basins”. Their appearance was synchronous in the evolution of the

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10

SAVICHEV, Aleksandr Nikolaevich, and Vitaliy Nikolaevich OGORODNIKOV. "Ufa mantle ridge fault – main tectonic, geological and minerogenic consequences." NEWS of the Ural State Mining University, no. 4 (December 20, 2020): 73–85. http://dx.doi.org/10.21440/2307-2091-2020-4-73-85.

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Relevance of the work. The data on the structure and properties of the subsoil, obtained on the basis of geophysical studies, make it possible to significantly revise the ideas about the structure and patterns of formation of mineral deposits within the Ufimsky ridge fault and its zone of influence (55º–56º north latitude in the Urals). Purpose of the work: constructing a model of the formation of the Ufa mantle ridge fault and identifying its mineragenic features using the example of deposits of ferruginous quartzite, kyanites and rare earth mineralization. The methodology of the research. Th

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11

Ambrosiani, Karin Garcia. "Interstadial minerogenic sediments at the Leveäniemi mine, Svappavaara, Swedish Lapland." Geologiska Föreningen i Stockholm Förhandlingar 113, no. 4 (1991): 273–87. http://dx.doi.org/10.1080/11035899109453201.

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12

Francus, Pierre, Raymond S. Bradley, Mark B. Abbott, Whit Patridge, and Frank Keimig. "Paleoclimate studies of minerogenic sediments using annually resolved textural parameters." Geophysical Research Letters 29, no. 20 (2002): 59–1. http://dx.doi.org/10.1029/2002gl015082.

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13

Zolitschka, Bernd, Irene Sophie Polgar, and Hermann Behling. "Created by the Monte Peron rock avalanche: Lago di Vedana (Dolomites, Italy) and its sediment record of landscape evolution after a mass wasting event." Landslides 19, no. 2 (2021): 297–311. http://dx.doi.org/10.1007/s10346-021-01787-2.

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AbstractThe timing of the Monte Peron Landslide is revised to 2890 cal. BP based on a radiocarbon-dated sediment stratigraphy of Lago di Vedana. This age fosters the importance of hydroclimatic triggers in the light of accelerating global warming with a predicted increase of precipitation enhancing the regional predisposition to large landslides. Moreover, a layer enriched in allochthonous organic and minerogenic detritus dating to the same wet period is interpreted as response to a younger and yet unidentified mass wasting event in the catchment of Lago di Vedana. Rock debris of the Monte Per

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14

Xianxiao, XIONG. "Classification, Minerogenic Models and Prospecting of Realgar/Orpiment Deposits in China." Acta Geologica Sinica - English Edition 74, no. 3 (2010): 618–22. http://dx.doi.org/10.1111/j.1755-6724.2000.tb00033.x.

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15

Mili, WANG, LIU Chenglin, JIAO Pengcheng, and YANG Zhichen. "Minerogenic Theory of the Superlarge Lop Nur Potash Deposit, Xinjiang, China." Acta Geologica Sinica - English Edition 79, no. 1 (2005): 53–65. http://dx.doi.org/10.1111/j.1755-6724.2005.tb00867.x.

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16

Peichl, Matthias, Jörgen Sagerfors, Anders Lindroth, et al. "Energy exchange and water budget partitioning in a boreal minerogenic mire." Journal of Geophysical Research: Biogeosciences 118, no. 1 (2013): 1–13. http://dx.doi.org/10.1029/2012jg002073.

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17

Wang, Ping'An, and Shunso Ishihara. "Metallogeny, Minerogenic Series, and Gold Mineralization of the Qinling Orogen, China." International Geology Review 43, no. 6 (2001): 523–38. http://dx.doi.org/10.1080/00206810109465030.

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18

Cherepanov, A. A., та N. V. Berdnikov. "Флюоритоносность Северо-Востока России". Bulletin of the North-East Science Center, № 1 (28 березня 2022): 3–13. http://dx.doi.org/10.34078/1814-0998-2022-1-3-13.

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One deposit and 217 occurrences of fluorite, grouped in the fluorite, the rare-metal-fluorite, and the polymetal-fluorite mineral formations, are known in RussiaТs North-East. Occurrences of fluorite formations are most widespread, while the stratiform occurrences in the Urultun-Taskan zone at the Omulevskoye uplift are especially rich in resources. Fluorite occurrences themselves are widespread within the Okhotsk-Chukotka volcanogenic belt. Fluorite-bearing belts, areas, and zones are distinguished. Fluorite minerogenic resources of RussiaТs North-East are estimated.

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19

Sadokov, D. O., T. V. Sapelko, and G. B. Fedorov. "Late-Glacial and Early Holocene history of Lake Khotavets (Mologa-Sheksna Lowland, NW Russia): a geodiversity conservation case study." Limnology and Freshwater Biology, no. 4 (2022): 1562–64. http://dx.doi.org/10.31951/2658-3518-2022-a-4-1562.

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Abstract. Evolution and regional climate changes during the Late Glacial/Holocene transition were studied using organic and inorganic geochemical proxies and pollen data from Lake Khotavets (NW Russia). Palaeoclimatic and palaeosedimentation sequence was described for the time slices 13.5 12.9, 12.9 11.8 and 11.8 11.1 cal. ka BP, attributed to the Aller d, Younger Dryas and Preboreal, respectively. Rapid organic accumulation, decrease of minerogenic input and woods expansion ~11.8 cal. ka BP were associated with the Holocene warming. The presented reconstruction determines scientific justifica

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20

Reimann, Clemens, and Karl Fabian. "Quantifying diffuse contamination: Comparing silver and mercury in organogenic and minerogenic soil." Science of The Total Environment 832 (August 2022): 155065. http://dx.doi.org/10.1016/j.scitotenv.2022.155065.

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21

Franzen, C., R. Kilian, and H. Biester. "Natural mercury enrichment in a minerogenic fen—evaluation of sources and processes." J. Environ. Monit. 6, no. 5 (2004): 466–72. http://dx.doi.org/10.1039/b315767a.

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22

Effler, Adam Joseph Peter, Feng Peng, Steven W. Effler, Christopher M. Strait, MaryGail Perkins, and Kimberly L. Schulz. "Light absorption by phytoplankton and minerogenic particles in Cayuga Lake, New York." Inland Waters 5, no. 4 (2015): 433–50. http://dx.doi.org/10.5268/iw-5.4.807.

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23

Effler, Steven W., and Feng Peng. "Long-term study of minerogenic particle optics in Cayuga Lake, New York." Limnology and Oceanography 59, no. 2 (2014): 325–39. http://dx.doi.org/10.4319/lo.2014.59.2.0325.

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24

Li, Qiang. "The Mineralization Theories and Techniques of Exploration for the Crisis Mines, a Case Study at the Shiyingtan Gold Deposit in Xinjiang." Advanced Materials Research 524-527 (May 2012): 231–35. http://dx.doi.org/10.4028/www.scientific.net/amr.524-527.231.

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How to resolve the resources exploration in deep and surrounding of the crisis mines is a very urgent problem which confronts with mining industry. Choosing the suitable prediction theory and technology is the key to success in evaluating. According to the particularity of resource exploration in deep and surrounding of crisis mines and application at domestic and international, author analyzes the regional minerogenic geological setting, structure and lithogeochemistry characteristic, predicates surrounding favorable region –Huangni po by using the geochemical appraisal criteria of primary ha

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25

Robinson, Marie. "Microfossil analyses and radiocarbon dating of depositional sequences related to Holocene sea-level change in the Forth valley, Scotland." Transactions of the Royal Society of Edinburgh: Earth Sciences 84, no. 1 (1993): 1–60. http://dx.doi.org/10.1017/s0263593300005915.

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ABSTRACTMicrofossil (pollen and diatom) evidence is presented from sites in the Forth valley, south-central Scotland, where alternating organic and estuarine minerogenic deposits record the influence of the changing Holocene sea level. Radiocarbon dating confirms the age of the Main and Low Buried Beaches, and of the Main Postglacial Transgression, in different parts of the Forth valley. Radiocarbon dates on shells from beds in the carse sediment and a Mesolithic shell midden near Grangemouth relate to the falling sea level in the 4th and 5th millennia BP. Sea-level curves are constructed for

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26

Spooner, Ian S., Ian MacDonald, Brandon Beierle, and AJ Timothy Jull. "A multi-proxy lithostratigraphic record of Late Glacial and Holocene climate variability from Piper Lake, Nova Scotia." Canadian Journal of Earth Sciences 42, no. 11 (2005): 2039–49. http://dx.doi.org/10.1139/e05-063.

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A multi-proxy lithostratigraphic record from Piper Lake, Nova Scotia reveals environmental variability during the Late Glacial and Holocene. Piper Lake is a small, shallow (3 m), closed dystrophic basin located in the eastern Nova Scotia Highlands. The site was deglaciated about 14.5 cal (calibrated) ka BP and elevated loss on ignition values and relatively low carbon/nitrogen (C/N) isotope ratios indicate the establishment of a productive aquatic environment consistent with Allerød warming. The Late Glacial Lake record is punctuated by two thin, very fine-grained clay layers that are correlat

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27

Effler, Steven, Anthony Prestigiacomo, Feng Peng, Rakesh Gelda, and David Matthews. "Partitioning the contributions of minerogenic particles and bioseston to particulate phosphorus and turbidity." Inland Waters 4, no. 2 (2014): 179–92. http://dx.doi.org/10.5268/iw-4.2.681.

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28

Peng, Feng, and Steven W. Effler. "Suspended minerogenic particles in a reservoir: Light-scattering features from individual particle analysis." Limnology and Oceanography 52, no. 1 (2007): 204–16. http://dx.doi.org/10.4319/lo.2007.52.1.0204.

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29

Mattsson, Tuija, Pirkko Kortelainen, Ahti Lepistö, and Antti Räike. "Organic and minerogenic acidity in Finnish rivers in relation to land use and deposition." Science of The Total Environment 383, no. 1-3 (2007): 183–92. http://dx.doi.org/10.1016/j.scitotenv.2007.05.013.

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30

Wigand, Cathleen, Earl Davey, Roxanne Johnson, et al. "Nutrient Effects on Belowground Organic Matter in a Minerogenic Salt Marsh, North Inlet, SC." Estuaries and Coasts 38, no. 6 (2015): 1838–53. http://dx.doi.org/10.1007/s12237-014-9937-8.

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31

Effler, Steven W., Michael E. Spada, Rakesh K. Gelda, et al. "Daphnia grazing, the clear water phase, and implications of minerogenic particles in Onondaga Lake." Inland Waters 5, no. 4 (2015): 317–30. http://dx.doi.org/10.5268/iw-5.4.765.

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32

Wójcicki, Krzysztof. "The Valley-Fill Deposits of the Kłodnica River (Southern Poland): Environmental Drivers of Facies Changes from the Late Vistulian Through the Holocene." Geochronometria 35, no. -1 (2010): 49–66. http://dx.doi.org/10.2478/v10003-010-0005-5.

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The Valley-Fill Deposits of the Kłodnica River (Southern Poland): Environmental Drivers of Facies Changes from the Late Vistulian Through the HoloceneLithological analyses and radiocarbon dating were used to elucidate the patterns and controls of Late Quaternary valley floor development of the Kłodnica River, the Upper Odra Basin. The research results were discussed with data obtained from valleys of rivers draining piedmont basins and highlands of southern Poland. In consequence, five stages of morpho-sedimentary evolution of the Kłodnica valley were distinguished. In the Late Vistulian a lar

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33

Iblaminov, R. G. "GEOLOGICAL AND INDUSTRIAL TYPES OF DEPOSITS. TITANMAGNETITE-ILMENITE TYPE." Вестник Пермского университета. Геология 21, no. 1 (2022): 51–71. http://dx.doi.org/10.17072/psu.geol.21.1.51.

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The identification of geological and industrial types of mineral deposits has an important theoretical and applied significance for their prospecting, resource evaluation and development. This problem has transformed into an independent branch of mineral science. It is shown by the example of the titanmagnetite-ilmenite type of deposits in stratified intrusions, where the main useful elements are the triad Fe, Ti and V. The geochemical, mineralogical, minerogenic, structural, and material aspects of this type are considered. The Kusinskoye field, studied in detail during 30 years of mining, is

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34

SERAVINA, Tatyana, Svetlana KUZNETSOVA, and Ludmila FILATOVA. "Compositional peculiarities of the host rocks and ores of the Lazursky ore field, Zmeinogorsk ore region of the Rudny Altai minerogenic zone." Domestic geology, no. 3-4 (September 14, 2021): 36–47. http://dx.doi.org/10.47765/0869-7175-2021-10020.

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The article describes composition of the host rocks and ores of the Lazursky and Maslyansky polymetallic volcanogenic massive sulfide deposits of the Lazursky ore field located within the Zmeinogorsk ore region of the Rudny Altai minerogenic zone. The ore field is composed of various facies of the Devonian (Late Givetian – Frasnian) ore-bearing siliceous-terrigenous basalt-rhyolite formation containing horizons of synvolcanic metasomatites. All rocks of the ore field were subjected to folding and schistosity with zones of tectonic brecciation. Hydrothermal alterations are represented by carbon

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35

Margielewski, Włodzimierz. "Landslide Fens as a Sensitive Indicator of Paleoenvironmental Changes Since the Late Glacial: A Case Study of the Polish Western Carpathians." Radiocarbon 60, no. 4 (2018): 1199–213. http://dx.doi.org/10.1017/rdc.2018.68.

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AbstractIn the sequences of landslide fen (mire) deposits of the Polish Western Carpathians, Late Glacial-Holocene paleoenvironmental changes were recorded. Downpours and/or continuous rains cyclically repeated during phases of climate humidity growth, causing supplies of mineral material to the minerogenic mires. In effect, illuvial or mineral horizons were formed in landslide fen deposits, as well as mineral covers overly fens in some sites. Sedimentological records reflect various, overlapping factors, as climatic changes, human activity (e.g. accelerating erosion), as well the specificity

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Pérez-Rodríguez, Marta, Ingrid Horák-Terra, Luis Rodríguez-Lado, and Antonio Martínez Cortizas. "Modelling mercury accumulation in minerogenic peat combining FTIR-ATR spectroscopy and partial least squares (PLS)." Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 168 (November 2016): 65–72. http://dx.doi.org/10.1016/j.saa.2016.05.052.

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37

Effler, Steven W., Feng Peng, and Rakesh K. Gelda. "Size Distributions and Light Scattering Features of Minerogenic Particles in a Stream during Runoff Events." Journal of Environmental Engineering 133, no. 9 (2007): 931–40. http://dx.doi.org/10.1061/(asce)0733-9372(2007)133:9(931).

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38

Frederiksen, Rasmus R., Søren E. Larsen, Gitte Blicher-Mathiesen, and Brian Kronvang. "Development and application of a parsimonious statistical model to predict tile flow in minerogenic soils." Agricultural Water Management 281 (May 2023): 108244. http://dx.doi.org/10.1016/j.agwat.2023.108244.

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39

Molchanov, Anatoly, Artem Terekhov, Gleb Kozlov, Ivan Lebedev, Elena Horochorina, and Vladislav Gusev. "Aldan-Vilyui ore-placer gold-bearing province, Russia." Ores and metals, no. 2 (August 16, 2021): 25–39. http://dx.doi.org/10.47765/0869-5997-2021-10009.

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Analysis of materials of the State Geological Map 1 : 1 000 000 (3rd generation) for the southern Sakha–Yakutiya territory in the course of compilation of the Minerogenic forecast map of the Russian Federation and its continental shelf, 1 : 2 500 000, and of the Map of the distribution regularities and forecast for porphyry goldcopper, large-tonnage black-shale gold, and epithermal gold deposits of the Russian Federation, 1 : 2 500 000, has allowed the authors to substantiate distinguishing the new Aldan-Vilyui ore-placer gold-bearing province with a total area of 450 000 km2 in the basins of

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40

Suchkov, Aleksandr, and Denis Vydrich. "Alteration-mineralization zonality of the Teploe 2 and Intruzivnoe molybdenum prospects in the Djetsky ore cluster, Eastern Sayan." Ores and metals, no. 2 (July 11, 2023): 78–89. http://dx.doi.org/10.47765//0869-5997-2023-10010.

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Molybdenum mineralization in the Eastern Sayan is represented by the stockwork, vein, and skarn types. The article is devoted to molybdenum ore occurrences of the Dzhetsky ore cluster of the Sisim-Divnogorsk minerogenic zone, that are characterized by the stockwork type mineralization. The Dzhetsky ore cluster is located 160 km northeast of Abakan and 150 km south of Krasnoyarsk. The study included investigations of the host rocks, ores, and ore-accompanying metasomatic alterations; their mineral assemblages; and the morphological types, relationships, and spatial distribution of the ore segre

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KUZNETSOV, VLADIMIR, TATYANA SERAVINA, ALEKSANDR DONETS, NELLY KUDRYAVTSEVA, TATYANA KUZNETSOVA, and SVETLANA FILIPPOVA. "History of the study and the principal features of the MVT-type lead-zinc massive sulfide deposits of the Priargunsk minerogenic zone." Domestic geology, no. 5 (November 22, 2023): 3–25. http://dx.doi.org/10.47765/0869-7175-2023-10021.

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Two types of ore deposits are distinguished within the Priargunsk minerogenic zone: the lead-zinc massive sulfide ore deposits in the Vendian-Cambrian carbonate sedimentary rocks (MVT type) and the polymetallic massive sulfide ones in the Mesozoic volcanogenic rocks (VMS type). The MVT-type deposits are confined to the volcanogenic-carbonate–terrigenous formation and comprise two genetic types of the ore bodies, the stratiform (stratified) beds and the stockwork-shaped hydrothermal-metasomatic zones in the feeding channels. The stratiform ore bodies occur concordantly with stratification of th

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42

Eskola, Tiina, Riitta Kontio, and Juha Pekka Lunkka. "Comparison between modified LST Fastfloat and conventional HF methods for pollen preparation in highly minerogenic sediments." Bulletin of the Geological Society of Finland 93, no. 1 (2021): 5–18. http://dx.doi.org/10.17741/bgsf/93.1.001.

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Pollen analysis is a commonly used method to interpret vegetation and environmental change. The standard pollen preparation technique in minerogenic sediments involves the use of hydrofluoric acid (HF) which is highly toxic. Currently the European legislation requires that hazardous chemicals should be substituted with less hazardous or non-toxic chemicals if possible. In the present paper the authors introduce a safer pollen preparation method, based on the use of low-toxic heavy liquid lithium heteropoly-tungstate (LST Fastfloat) and provide instructions for pollen preparation with the LSTFa

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43

Peng, Feng, Steven W. Effler, David O'Donnell, Mary Gail Perkins, and Alan Weidemann. "Role of minerogenic particles in light scattering in lakes and a river in central New York." Applied Optics 46, no. 26 (2007): 6577. http://dx.doi.org/10.1364/ao.46.006577.

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44

Monna, F., D. Galop, L. Carozza, et al. "Environmental impact of early Basque mining and smelting recorded in a high ash minerogenic peat deposit." Science of The Total Environment 327, no. 1-3 (2004): 197–214. http://dx.doi.org/10.1016/j.scitotenv.2004.01.010.

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45

Peng, Feng, and Steven W. Effler. "Quantifications and water quality implications of minerogenic particles in Cayuga Lake, New York, and its tributaries." Inland Waters 5, no. 4 (2015): 403–20. http://dx.doi.org/10.5268/iw-5.4.867.

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46

Peng, Feng, and Steve W. Effler. "Mass-specific scattering coefficient for natural minerogenic particle populations: particle size distribution effect and closure analyses." Applied Optics 51, no. 13 (2012): 2236. http://dx.doi.org/10.1364/ao.51.002236.

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Jumagulov, Aydos, Mekhroj Juraev, Ulugkhuja Raxmatov, et al. "Localization conditions of apometaterrigenous non-carbon the Sarykul deposit of the Karatyubinsky ore district in Uzbekistan." E3S Web of Conferences 497 (2024): 03048. http://dx.doi.org/10.1051/e3sconf/202449703048.

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This article explores the occurrence of apometaterrigenous non-carbon tungsten mineralization at the Sarykul deposit in the Karatyubinsk Mountains. Initially considered unpromising, this newly discovered tungsten mineralization was found during gold mining operations. The prospecting activities targeting calcification zones in metaterrigenous rocks revealed their tungsten-bearing nature. This discovery has reshaped the understanding of tungsten mineralization genesis, lithological and structural conditions, and the overall minerogenic potential of the Karatyubinsky ore field.Apometaterrigenous

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Daxian, Zhao, and Tang Guangting. "The Geochemical Characteristics and Minerogenic Model for the Amo Hypothermal Tin Deposit in Ximeng County, Yunnan Province." Acta Geologica Sinica - English Edition 4, no. 3 (2009): 271–87. http://dx.doi.org/10.1111/j.1755-6724.1991.mp4003005.x.

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Congxi, CHEN, and CAI Keqin. "Minerogenic System of Magnesian Nonmetallic Deposits in Early Proterozoic Mg-rich Carbonate Formations in Eastern Liaoning Province." Acta Geologica Sinica - English Edition 74, no. 3 (2010): 623–31. http://dx.doi.org/10.1111/j.1755-6724.2000.tb00034.x.

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NILSSON, MATS, JÖRGEN SAGERFORS, ISHI BUFFAM, et al. "Contemporary carbon accumulation in a boreal oligotrophic minerogenic mire - a significant sink after accounting for all C-fluxes." Global Change Biology 14, no. 10 (2008): 2317–32. http://dx.doi.org/10.1111/j.1365-2486.2008.01654.x.

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