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Relevant bibliographies by topics / Gold mineralized veins

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Academic literature on the topic 'Gold mineralized veins'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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Journal articles on the topic "Gold mineralized veins"

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Neumayr, P., S. G. Hagemann, and J. F. Couture. "Structural setting, textures, and timing of hydrothermal vein systems in the Val d'Or camp, Abitibi, Canada: implications for the evolution of transcrustal, second- and third-order fault zones and gold mineralization." Canadian Journal of Earth Sciences 37, no. 1 (2000): 95–114. http://dx.doi.org/10.1139/e99-105.

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In the Val d'Or camp, Archean Abitibi greenstone belt, Canada, numerous gold-mineralized second- and third-order fault zones are spatially associated with the transcrustal Cadillac Tectonic Zone (CTZ). This situation is used to test whether fluid systems in the CTZ have a similar structural timing to those in the gold-hosting structures, and hence the CTZ could represent the main fluid conduit in the camp. The transcrustal CTZ at Orenada No. 2 contains structurally complex vein systems, with mineralized quartz-tourmaline veins related to both D2 oblique-reverse faulting and F3 dextral asymmetr

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Oo, Toe, Agung Harijoko, and Lucas Setijadji. "Origin of the Kyaukmyet Low-Sulfidation Epithermal Gold Prospect, Monywa District, Central Myanmar." Iraqi Geological Journal 54, no. 1E (2021): 1–18. http://dx.doi.org/10.46717/igj.54.1e.1ms-2021-05-22.

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The Kyaukmyet prospect is one of the principal epithermal gold prospects in the Monywa District, Central Myanmar; its gold- and base metal-bearing quartz veins contain around 3 g/t gold. Ore minerals are mainly hosted by volcanic and volcaniclastic rocks of the Late Oligocene to Middle Miocene Magyigon Formation. The distribution of magmatic intrusions in the area is controlled by ENE-WSW trending faults; these faults are likely related to ore mineralization. Common ore minerals at the Kyaukmyet prospect include pyrite, sphalerite, galena, chalcopyrite, and electrum. They occur in mineralized

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Vearncombe, J. R. "Structure of veins in a gold–pyrite deposit in banded iron formation, Amalia greenstone belt, South Africa." Geological Magazine 123, no. 6 (1986): 601–9. http://dx.doi.org/10.1017/s0016756800024110.

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AbstractFibrous quartz veins in deformed banded iron formation of the Amalia greenstone belt, southwestern Transvaal, are spatially related to gold–pyrite mineralization in both wallrock and vein inclusions. Poles to quartz vein orientations show a general parallelism with mineral elongation and fold plunges of the principal deformation in the wallrock. Quartz vein fibres show a consistent anticlockwise rotation, late components being subparallel to the elongation lineation, suggesting veining was probably synchronous with the principal deformation. Antitaxial fibrous veins, which dominate the

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KAMEL, O. A., M. M. EL MAHALLAWI, and H. M. HELMY. "Geochemistry of Umm Rus gold - quartz veins, Central Eastern Desert Egypt. A new contribution." Bulletin of the Geological Society of Greece 34, no. 3 (2001): 1139. http://dx.doi.org/10.12681/bgsg.17174.

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Gold-bearing quartz veins of the Umm Rus area occur at the south-eastern contact of a Precambrian granodiorite cupola within younger gabbros of 573-615 Ma belonging to the Pan African orogenic belt. The rocks are intruded within low-grade metasediments. At such contact, a hybrid zone is developed characterized by the occurrence of quartz diorite which grades into diorite and meta-ferrogabro. A limited number of mineralized quartz veins cut the granodiorite-gabbro complex. Different alteration zones are developed in the vicinity of the quartz veins. The quartz veins have two main trends; NS and

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Piroshco, Darwin W., and C. Jay Hodgson. "Relationship of hydrothermal alteration to structure and stratigraphy at the Coniaurum gold mine, northern Ontario." Canadian Journal of Earth Sciences 25, no. 12 (1988): 2028–40. http://dx.doi.org/10.1139/e88-189.

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The gold mineralized zones of the Coniaurum mine, Porcupine camp, northeastern Ontario, are on the eastern end of the northeast-trending Hollinger–Mclntyre ore system. The ore zones are quartz–ankerite (plus accessories) veins and vein systems and associated pyritic wall rock, hosted by a sequence of mafic volcanic rocks and discordant quartz–feldspar porphyry stocks of Archean age.A least altered facies and three alteration facies can be distinguished within the mafic volcanic rocks: a chlorite facies, an ankerite facies, and a vein envelope facies. The chlorite facies is widespread, overprin

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Idrus, Arifudin, Sukamandaru Prihatmoko, Ernowo Harjanto, et al. "Metamorphic rock-hosted orogenic gold deposit style at Bombana (Southeast Sulawesi) and Buru Island (Maluku): Their key features and significances for gold exploration in Eastern Indonesia." Journal of Geoscience, Engineering, Environment, and Technology 2, no. 2 (2017): 124. http://dx.doi.org/10.24273/jgeet.2017.2.2.291.

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In Indonesia, gold is commonly mined from epithermal-, porphyry-, and skarn-type deposits that are commonly found in volcanic belts along island arcs or active continental margin settings. Numerous gold prospects, however, were recently discovered in association with metamorphic rocks. This paper focuses on metamorphic rock-hosted gold mineralization in Eastern Indonesia, in particular the Bombana (SE Sulawesi) and Buru Island (Maluku) prospects. At Bombana, gold-bearing quartz-veins are hosted by the Pompangeo metamorphic complex. Sheared, segmented veins vary in thickness from 2 cm to 2 m. G

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Wilkins, Colin, and Mike Quayle. "Structural Control of High-Grade Gold Shoots at the Reward Mine, Hill End, New South Wales, Australia." Economic Geology 116, no. 4 (2021): 909–35. http://dx.doi.org/10.5382/econgeo.4807.

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Abstract The Reward mine at Hill End hosts structurally controlled orogenic gold mineralization in moderately S plunging, high-grade gold shoots located at the intersection between a late, steeply W dipping reverse fault zone and E-dipping, bedding-parallel, laminated quartz veins (the Paxton’s vein system). The mineralized bedding-parallel veins are contained within the middle Silurian to Middle Devonian age, turbidite-dominated Hill End trough forming part of the Lachlan orogen in New South Wales. The Hill End trough was deformed in the Middle Devonian (Tabberabberan orogeny), forming tight,

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Santos Polo, Alan, Guo Weimin, Fernando Rivera, Colombo Tassinari, Luis Cerpa, and Shoji Kojima. "Early Jurassic arc related magmatism associated with porphyry copper mineralization at Zafranal, Southern Peru unraveled by zircon U-Pb ages." Andean Geology 46, no. 3 (2019): 445. http://dx.doi.org/10.5027/andgeov46n3-3041.

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Early Jurassic arc-related igneous rocks host porphyry copper prospects and gold-bearing quartz vein deposits in southern Peru. Ten new zircon U-Pb ages for wall rocks of gold-bearing quartz veins, Jurassic rocks and copper-mineralized porphyry bodies in Zafranal porphyry copper, together with published ages for Jurassic rocks, reveal a continuous magmatic evolution of the early Jurassic arc. The Jurassic rocks and gold-bearing quartz vein systems in the western flank of the Western Cordillera are hosted by Paleo- and Meso-proterozoic orthogneisses of the Arequipa Massif (1.75-1.44 Ga) that un

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HASSAN, Musab Awad Ahmed, and Aleksandr Evgen’yevich KOTEL’NIKOV. "The geological and structural controls of gold mineralization in Qala en Nahal-Um Sagata region, South Gedarif, Sudan." NEWS of the Ural State Mining University 59, no. 3 (2020): 19–26. http://dx.doi.org/10.21440/2307-2091-2020-3-19-26.

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Relevance and purpose of the work. The study area is located in Gedarif state in Sudan. The ongoing work is aimed at solving fundamental problems of the geological structure of the Qala En Nahal-Um Saqata Ophiolitic Complex and applied tasks of mineral exploration. Detailed studies are being conducted for the first time in this area. The purpose of the investigation is to study the geological and structural features of the region, as well as to obtain information about the localization of gold mineralization. Methods of research. Within the study area, a geological mapping of the ophiolitic co

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Lang, Xing Hai, Ju Xing Tang, and Fu Wei Xie. "Geological Characteristics and Exploration Potential of the NO.III Deposit in the Xiongcun District, Tibet, China." Advanced Materials Research 868 (December 2013): 217–23. http://dx.doi.org/10.4028/www.scientific.net/amr.868.217.

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The Xiongcun district is located along the south margin of the Gangdese porphyry copper belt, approximately 53 km west of the Xigaze. No.III deposit is a newly discovered porphyry copper-gold deposit in the Xiongcun district. This paper first reports geological characteristics and exploration potential of No.III deposit. No.III deposit is hosted by Early Jurassic hornblende quartz diorite porphyry. Pervasive alteration is dominated by a well-mineralized potassic alteration. Major ore-bearing vein types include quartz-sulfide and chlorite-sulfide veins. Drilling holes and geochemical anomaly in

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Dissertations / Theses on the topic "Gold mineralized veins"

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Rambo, Jonas Mangoni. "Controle estrutural e estudo das Inclusões fluídas dos garimpos da região de Terra Nova do Norte e Nova Santa Helena, província aurífera Alta Floresta, Cráton Amazônico." Universidade Federal de Mato Grosso, 2014. http://ri.ufmt.br/handle/1/545.

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Crockford, Julie-Ann. "The origin and formation temperature of mineralised hydrothermal veins at the Groundrush gold deposit, Northern Territory, Australia /." Title page, contents and introduction only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbc9389.pdf.

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Reports on the topic "Gold mineralized veins"

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Vein deposits hosted by plutonic rocks in the Croesus Stock and Hailey gold belt mineralized areas, Blaine County, Idaho. US Geological Survey, 2001. http://dx.doi.org/10.3133/b2064x.

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