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Academic literature on the topic 'Ore deposits Victoria, Northeastern'

Author: Grafiati

Published: 10 December 2022

Last updated: 29 January 2023

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Journal articles on the topic "Ore deposits Victoria, Northeastern"

1

Birch, William D. "Mineralogy of the Silver King deposit, Omeo, Victoria." Proceedings of the Royal Society of Victoria 129, no. 1 (2017): 41. http://dx.doi.org/10.1071/rs17004.

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The Silver King mine (also known as Forsyths) operated very intermittently between about 1911 and the late 1940s on Livingstone Creek, near Omeo, in northeastern Victoria. The deposit consists of six thin and discontinuous quartz lodes that are variably mineralised. Assays of up to 410 ounces of silver per ton were obtained but there are only a few recorded production figures. Examination of representative ore samples shows that the main silver-bearing minerals in the primary ore are pyrargyrite, freibergite, andorite and the rare sulphosalt zoubekite, which occur irregularly with pyrite, arsenopyrite, galena and sphalerite. Phase assemblage data indicate that crystallisation occurred over an interval from about 450°C to less than 250°C, with the silver-bearing minerals crystallising at the lowest temperatures. The lodes were formed by the emplacement of hydrothermal solutions into fractures within the Ensay Shear Zone during the Early Devonian Bindian Orogeny. There are similarities in mineralisation and timing of emplacement between the Silver King lodes and the quartz-reef-hosted Glen Wills and Sunnyside goldfields 35‒40 km north of Omeo.

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2

Mykhailov, V., and А. Tots. "A NEW GOLD ORE REGION IN TANZANIA." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 3 (82) (2018): 55–59. http://dx.doi.org/10.17721/1728-2713.82.07.

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Tanzania is one of the leading gold mining countries in the world and the discovery of new gold resources on its territory is an actual task. Known gold deposits are concentrated mainly in the northwest of the country, in the metallogenic zone of Lake Victoria, where they are associated with the Archean greenstone belts, and to a lesser extent – in the southwest, in the ore regions of Lupa and Mpanda, confined to the Ubendian Paleoproterozoic mobile belt. With regard to the eastern regions of Tanzania, where the Proterozoic structures of the Uzagaran mobile belt are developed, until recently in this region any significant manifestations of gold mineralization were not known. As a result of our research in the northern part of the Morogoro province of the Republic of Tanzania, a new previously unknown gold deposit Mananila was discovered. It is represented by a large volume, up to 400–450 m long, up to 60–80 m thick, mineralized shear zone over intensely leached and schistosed migmatites, gneisses, amphibolites, penetrated by echelon systems of quartz veins and veinlet, steeply dipping bodies of quartz breccia up to 1.0–1.5 m thick. Gold contents range from 0.61 to 8.11 g/t, the average zone content is 2.5–3.0 g/t. Parallel to the main zone, similar structures are developed on the site, although they are of lower thickness. The forecast resources of the deposit are estimated at 20 tons of gold. 2.8 km to the east from the Mananila field, the recently discovered Mazizi gold deposit is located, and a number of small occurrences of gold are also known in the region. All these objects are located within a large shear zone of the northeastern strike, up to 4–5 km width, over 20 km in length. This serves as the basis for the identification of a new gold ore region in the northern part of the Morogoro province of the United Republic of Tanzania, within the Proterozoic mobile belt of Usagaran, the possible gold content of which has never been previously discussed in geological literature.

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3

Sidorov, A. A. "Xenothermal ore deposits of Northeastern Russia." Doklady Earth Sciences 433, no. 1 (July 2010): 861–65. http://dx.doi.org/10.1134/s1028334x10070032.

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4

Ju, Nan, Sen Zhang, Lin-Lin Kou, Hai-Po Wang, Di Zhang, Yu-Chao Gu, and Tong Wu. "Source and Tectonic Setting of Porphyry Mo Deposits in Shulan, Jilin Province, China." Minerals 9, no. 11 (October 26, 2019): 657. http://dx.doi.org/10.3390/min9110657.

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The Shulan area in Jilin Province is a part of the Lesser Xing’an–Zhangguangcai Range polymetallic ore belt, which is an important Cu–Mo ore region of northeast China. The discovery of three large Mo ore deposits (Fu’anbu, Chang’anbu, and Jidetun) highlights its potential for porphyry Mo ore deposits. Here we investigated the tectonic setting and mineralization of Mo ore deposits in the Shulan area, based on comparative study of the Fu’anbu, Chang’anbu, and Jidetun deposits. The ore-controlling structures are NE–SW- and NW–SE-trending faults. The main ore mineral in all three deposits is molybdenite. The ore bodies are all hosted in granites, have a stratiform or lenticular shape, and have strongly altered wall rocks. These observations indicate the Mo deposits in the Shulan area are typical porphyry Mo deposits. All were formed during the early Yanshanian (199.6–133.9 Ma). Biotite adamellites from the Chang’anbu deposit yield a U–Pb age of 182.10 ± 1.20 Ma. Molybdenites from the Fu’anbu and Jidetun deposits have Re–Os isochron ages of 166.9 ± 6.7 and 169.1 ± 1.8 Ma, respectively. Quartz and ore minerals were analysed for H–O and S–Pb isotopes, respectively. The results suggest the ore-forming materials were predominantly of upper-mantle origin, with secondary contributions from the lower crust. The ore-hosting granites have high concentrations of SiO2 (66.67–75.43 wt.%) and Al2O3 (12.91–16.44 wt.%), low concentrations of MgO (0.09–1.54 wt.%), and Ritman index (σ = K2O + Na2O)2/(SiO2 − 43)) ratios of 2.09–2.57. The granites are enriched in large-ion lithophile elements and depleted in high-field-strength elements, and have negative Eu anomalies. The ore-hosting rocks are geochemically similar to granites in northeastern China that were generated in a collisional orogeny. We conclude that early Yanshanian (199.6–133.9 Ma) mantle–crust-derived magmatism caused by the subduction of the Palaeo-Pacific Plate was the main source of Mo deposits in the Shulan area.

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Yang, Guang Shu, Yong Feng Yan, Peng Yu Feng, and Jun Wei Zhang. "Metallogenic Geological Conditions and Prospecting Indicators of the Carbonate-Hosted Pb-Zn Deposits in Northeastern Yunnan Province, China." Advanced Materials Research 962-965 (June 2014): 296–99. http://dx.doi.org/10.4028/www.scientific.net/amr.962-965.296.

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Based on large scale geological mapping, geological-section, tectonic and geochemical studies on the carbonate-hosted Pb-Zn deposits in NE Yunnan, the metallogenic geological conditions are discussed, and the ore-prospecting indicators are summarized. The Pb-Zn deposits have many common features, which are mainly controlled by the thrust fault-fold structures and lithological conditions. The ore-forming mechanism of them is similar to the MVT Pb-Zn deposit. The combination of thrust fault-fold structures and altered carbonate rocks with geochemical anomalies are good indicators for prospecting.

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Rich, Thomas H., Li Xiao-bo, and Patricia Vickers-Rich. "A potential Gondwanan polar Jehol Biota lookalike in Victoria, Australia." Proceedings of the Royal Society of Victoria 121, no. 2 (2009): v. http://dx.doi.org/10.1071/rs09300.

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The Early Cretaceous Jehol Biota from northeastern China has produced an abundance of well preserved birds, mammals and feathered dinosaurs, amongst other fossils. The similarities in the nature of the deposits producing these fossils to the lacustrine facies of the Strzelecki Group of southwest Gippsland, Victoria, Australia suggests that a prolonged, systematic search of those rocks in Australia could yield fossils of similar quality.

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7

Ganzha, О. A., Yu V. Kroshko, and H. O. Kuzmanenko. "ORE-BEARING OF THE LIVOBEREZHNY ZIRCON-RUTILE-ILMENITE PLACER DISTRICT." Geological Journal, no. 4 (December 28, 2022): 83–100. http://dx.doi.org/10.30836/igs.1025-6814.2022.4.255682.

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The relevance of the presented publication is due to the need to highlight the current state of zirconium-titanium specialization objects, the need to modernize and unify geological information, due to the significant increase in the world community’s interest in minerals that belong to the group of critical raw materials. The article presents generalized data on the ore-bearing zircon-rutile-ilmenite deposits of the Livoberezhniy placer district of the Ukrainian placer province. This area has unique paragenetic characteristics, as it is located in the junction zone of three geostructural units: the Dnipro-Donetsk depression, the northeastern slope of the Ukrainian crystalline shield, and the Kalmius-Toretsk depression of Donbas. The Livoberezhniy placer district includes the Vovchansk, Voskresenivsk, Southern, Nova-Mykolaivka, North-Samarsk, Yuriivsk and Petropavlivsk zircon-rutile-ilmenite deposits. These deposits are located in the sediments of the Bereka and Novi Petrivtsi suites. The Petropavlivsk and Yuriivsk deposits have a two-layer structure, the rest is belongs to the deposits of the only Novi Petrivtsi suite. The genesis of deposits is buried coastal-marine placers. All deposits have a slight dip of the ore sand layers in a north-east direction, which outlines the general slope of the water basin floor. Today, the Vovchansk zircon-ilmenite-rutile deposit is being developed by DEMURINSKY GZK LLC. On the basis of the results of geological prospecting and geological exploration conducted in the 60s and 70s of the last century, maps of the strength of the ore stratum and the distribution of ore components (ilmenite, rutile, zircon) were constructed. The visualization data was built for the Voskresenivsk, Southern, Nova-Mykolaivka, North-Samarsk, Yuriivsk and Petropavlivsk deposits. An analysis of the obtained data was carried out and a number of conclusions were drawn regarding the distribution of ore components for each of the deposits.

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8

Mykhailov, V. "ORE-MAGMATIC SYSTEM SUKUMALAND (TANZANIA)." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (84) (2019): 34–41. http://dx.doi.org/10.17721/1728-2713.84.05.

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The overwhelming part of the gold ore potential of the United Republic of Tanzania is confined to the systems of the Neoarchaean greenstone belts (GSB) of the metallogenic province of Lake Victoria in the northwestern part of the country. Based on the interpretation of space imagery, in the western part of the province the Sukumaland ore-magmatic system of concentric-zonal structure has been distinguished. It is formed by a group of arched greenstone belts and associated gold deposits. They form two arcuate branches: the internal and external branch, differing in their composition and structure. The internal arc is represented by the Rwamagaza and Kahama GSB with gold deposits of Tulawaka, Buckreef, Mawe-Meru, Tembo, and Bulyanhulu. The external arc is represented by Geita and Mabale-Buhungurica GSB with gold deposits of Ridge-8, Nyankanga, Geita, Matandani, Kukuluma, Nyanzaga, Kitongo, Golden Ridge, Nyakafuru, and Miabu. Their huge gold potential (over 50 million ounces of gold) stipulates for the urgency of the study of this gigantic structure. GSB of the inner arc (Rwamagaza and Kahama) are characterized by a predominance of basic volcanic rocks, and GSB of the external arc (Geita and Mabale-Buhungurica) – by sedimentary and volcanic-sedimentary formations, in particular, banded ironstone formations (BIF). Accordingly, gold deposits of the inner arc are mainly associated with basic volcanic rocks (Tulawaka, Buckreef, Mawe-Meru, Bulyanhulu, Tembo) while gold deposits of the external arc – with BIF (Geita, Nyankanga, Kukuluma, Matandani). The nuclear part of the ore-magmatic system is of special interest, although manifestations of volcanism are absent there and gold or other mineral deposits are unknown yet, but a tectonic pattern of its structural elements indicates its significant ore potential. In particular, the presence of numerous spatially close systems of radial-circular faults attests to the presence of weakened zones in the space above the core of a hypothetical magma chamber. Gold deposits of different geological and industrial types, yet undiscovered, as well as manifestations of diatreme magmatism may be associated with these weakened zones. In particular, one cannot exclude the possible presence of diamond-bearing volcanic pipes. It is assumed that the ore-magmatic system has originated and evolved in the course of a complex multi-stage ore-magmatic process under the influence of ascending flows of depth fluids due to the long-term functioning of a zone with anomalously heated mantle in that area. During further geological exploration it is recommended to take into account the predictable availability of a single integrated ore-magmatic system of longdevelopment and its structural features.

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9

Milovsky, G. A., E. M. Shemyakina, and A. A. Belyakov. "Application of remote sensing for detection of zones of cataclastic and metasomatic rocks on the area of the Uvatsky ore cluster (Eastern Sayan)." Исследования Земли из Космоса, no. 1 (March 24, 2019): 47–54. http://dx.doi.org/10.31857/s0205-96142019147-54.

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Interpretation materials of the Russian space survey «Resource-P» (Geotone) in the visible and infrared bands made it possible to identify crush belts and faults of the northeastern, sublatitudinal and submeridional strike that determine the structural position of uranium mineralization within the Uvat ore cluster in the East Sayan. The principal possibility of using a high-resolution multi-zone space survey (3 m) for detecting metasomatically altered ore-bearing rocks of the Lower Proterozoic and Riphean-Paleozoic carbonate-terrigenous deposits was determined.

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10

Ouyang, Hegen, Jingwen Mao, and Ruizhong Hu. "Geochemistry and Crystallization Conditions of Magmas Related to Porphyry Mo Mineralization in Northeastern China." Economic Geology 115, no. 1 (January 1, 2020): 79–100. http://dx.doi.org/10.5382/econgeo.4694.

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Abstract To better understand processes leading to porphyry Mo deposit formation, the metal content, volatile content, and crystallization conditions of melt inclusions from pre- and synmineralization intrusions in six porphyry(-skarn) Mo deposits of northeastern China (Aolunhua, Hashitu, Lanjiagou, Songbei, Wanbaoyuan, and Yangjiazhangzi) were investigated by means of laser ablation-inductively coupled plasma-mass spectrometry and electron microprobe analysis. The ore-forming silicate melts were one to four times more evolved than average granite with 1 to 7 ppm Mo. The ore-related intrusions crystallized predominantly at 760° to 690°C and 3.7 to 1.0 kbar, except for the one at Hashitu, which crystallized at 770° to 740°C and lower pressures (2.0–1.0 kbar). Fertile silicate melts at Hashitu contain up to 0.4 wt % F, 0.03 to 0.09 wt % Cl, 5.0 to 7.0 wt % H2O, 10 to 24 ppm Cs, and 200 to 500 ppm Rb, whereas those at Yangjiazhangzi and Wanbaoyuan contain less Cs (3–6 ppm and 5–7 ppm, respectively), less Rb (180–220 ppm and 200–240 ppm, respectively), and negligible F (<0.15 wt %) but have similar Cl (0.03–0.05 wt %) and H2O (5.3–6.5 wt % and 4.0–5.2 wt %, respectively) contents. Calculated melt viscosities in fertile magmas (log η = 4.3–6.1 Pa s) are at the lower end of the values reported for felsic melts at the same temperature. Comparison between syn- and premineralization intrusions in individual deposits reveals that the ore-related intrusions were similarly evolved and had similar Mo contents and crystallization conditions as the nonmineralizing intrusions. The only difference is that the premineralization intrusions tend to occur as batholiths. The key to porphyry Mo mineralization lies in the focusing of fluid into and through a small rock volume on the top of the intrusion. For the studied porphyry Mo deposits, the mineralizing magmas are all Mo poor, indicating Mo enrichment is not required to form porphyry Mo deposits. Metal endowments in porphyry Mo deposits have no direct relationship with the composition and crystallization condition of mineralizing melts but are linked with the fluid flux released from the underlying magma chamber through a cupola.

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Books on the topic "Ore deposits Victoria, Northeastern"

1

Alminas, Henry V. Precious and base-metal mineralization in the west-central Vermilion district, portions of St. Louis, Lake, and Cook counties, northeastern Minnesota. [Washington]: U.S. G.P.O., 1992.

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Analytical results for 41 water samples from the South Kawishiwi River study area, northeastern Minnesota. [Denver, CO]: U.S. Dept. of the Interior, Geological Survey, 1990.

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Book chapters on the topic "Ore deposits Victoria, Northeastern"

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Jaloul, Bejaoui. "Reef Cenomanian Carbonate Hosted Fluorite Ore Deposits at Jebel Mokta, Northeastern Tunisia." In Petrogenesis and Exploration of the Earth’s Interior, 269–71. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01575-6_65.

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Janković, S. "Genetic Types of Alpine ore Deposits and Tectonic Settings in the Northeastern Mediterranean and Southwest Asia." In Geotectonic Evolution and Metallogeny of the Mediterranean Area and Western Asia, 23–35. Vienna: Springer Vienna, 1986. http://dx.doi.org/10.1007/978-3-7091-5822-7_2.

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Wang, Zizheng, Xin-Sheng Jiang, Bang-Guo Zhou, and Sheng-Lin Lu. "Sedimentary Characteristics of the Member 1 of the Middle Devonian Suotoushan Formation and Its Ore-Bearing Potential in Northeastern Yunnan." In Mineralogy. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.103826.

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Super-large quartz sandstone deposit has been discovered in Northeastern Yunnan and the major ore-bearing bed is occurred in the Member 1 of the Middle Devonian Suotoushan Formation. Systematic study on the sedimentary characteristics of the Suotoushan Formation in Yiliang region, northeastern Yunnan Province has been conducted, Profile surveying, drilling and trenching show that, microscopic identification, the thickness of the Suotoushan Formation is 62.8 m ∼ 222.7 m and principally composed of gray-white thick-bedded medium-grained quartz sandstone with well developed parallel bedding, swash bedding, oscillation cross-bedding and wave ripple, showing remarkable wave action features. Thin section observation shows that quartz sandstone in the Member 1 of the Suotoushan Formation is grain supported, siliceous cemented, concave-convex and line contact and the pressure solution and secondary overgrowth of quartz sand grains are obvious. Grain size analysis shows that the grain size is concentrated between 1.5Φ and 3.5Φ with saltation population up to 99% which is composed by tow sub populations and lacking of traction and suspension populations, showing a typical foreshore grain size distribution. Chemical analysis shows SiO2 chemical purity of the quartz sandstone is 99.05 ∼ 99.39 with weighted average 98.99 (N = 11) which has exceeded the industry standard for first-grade raw material of plate glass. Based our studies above, it can be concluded that the quartz sandstone in Member 1 of Suotoushan Formation is high energy coastal foreshore sediments with high texture and mineral maturity, and has been further purified by diagenesis, and both the grain-size characteristic and chemical purity have reached the standard of high-purity quartz sandstone, which can be expected raw material for high-purity quartz. The results in this article can provide accurate prospecting target to enlarge the resources potential of high-purity quartz deposits in northeastern Yunnan.

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Qiu, Kun-Feng, Richard J. Goldfarb, Jun Deng, Hao-Cheng Yu, Zong-Yang Gou, Zheng-Jiang Ding, Zhao-Kun Wang, and Da-Peng Li. "Chapter 35: Gold Deposits of the Jiaodong Peninsula, Eastern China." In Geology of the World’s Major Gold Deposits and Provinces, 753–74. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.35.

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Abstract The Jiaodong gold province, within the eastern margin of the North China block and the translated northeastern edge of the South China block, has a stated premining gold resource exceeding 4,500 metric tons (t). It is thus one of the world’s largest gold provinces, with a present cumulative annual production estimated at 60 t Au. More than 90% of the Jiaodong gold resource is hosted by batholiths and related bodies of the Linglong (ca. 160–145 Ma) and, to a lesser degree, Guojialing (ca. 130–122 Ma) suites. The intrusions were emplaced into high-grade metamorphic basement rocks of the Precambrian Jiaobei (North China block) and Sulu (South China block) terranes during a 70-m.y.-period of lithospheric delamination, extensional core complex formation, and exhumation. The deposits are located about 20 to 200 km to the east of the continental-scale NNE-striking Tancheng-Lujiang (Tan-Lu) strike-slip fault system. They occur along a series of more regional NNE- to NE-striking brittle and ductile-brittle faults, which appear to intersect the Tan-Lu main structure to the southwest. This system of early to middle Mesozoic regional thrust faults, reactivated during Cretaceous normal motion and ore formation, tends to occur along the margins of the main Linglong batholiths or between intrusions of the two suites of granitoids. Orebodies are mainly present as quartz-pyrite veins (Linglong-type) and as stockwork veinlets and disseminated mineralization (Jiaojia-type). The two mineralization styles are transitional and may be present within the same gold deposit. The ca. 120 Ma timing of gold mineralization correlates with major changes in plate kinematics in the Pacific Basin and the onset of seismicity along the Tan-Lu fault system, with the enormous fluid volumes and associated metal being derived from sediment devolatilization above the westerly subducting Izanagi slab.

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Conference papers on the topic "Ore deposits Victoria, Northeastern"

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Singer, Jared W., and Marian V. Lupulescu. "REE-RICH FLUORAPATITE TEXTURES FROM EASTERN ADIRONDACK IRON ORE DEPOSITS." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272533.

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Maibam, B., S. F. Foley, and D. E. Jacob. "Geochemistry of Chromian Spinels from the Indo-Myanmar Ophiolite Belt of Northeastern India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63395.

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McGrath, Monica, Brian W. Stewart, Brian W. Stewart, Matthew S. Sanchez, and Matthew S. Sanchez. "UNRAVELING THE PETROGENESIS OF ORE BODY TALC DEPOSITS: A GEOCHEMICAL AND PETROLOGICAL STUDY." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291003.

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Matt, Peter, William H. Peck, Ryan Mathur, Mary R. Hurtgen, and Linda Godfrey. "ZINC ISOTOPE CONSTRAINTS ON THE FORMATION OF SEDIMENTARY EXHALATIVE (SEDEX) ORE DEPOSITS: NEW EVIDENCE FROM THE FRANKLIN, NJ MINING DISTRICT." In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-373657.

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Moumou, Abdelhak, Khalil El Kadiri, Larbi Rddad, and Isma Amri. "THE ROLE OF THE JURASSIC RIFTING AND THE ALPINE OROGENY IN THE EMPLACEMENT OF THE PB-ZN MVT ORE DEPOSITS IN EASTERN HIGH ATLAS, MOROCCO." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328163.

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