Relevant bibliographies by topics / Babin Porphyry Cu District

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  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers
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Academic literature on the topic 'Babin Porphyry Cu District'

Author: Grafiati
Published: 4 June 2021
Last updated: 28 July 2025

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Journal articles on the topic "Babin Porphyry Cu District"

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Real, Irene del, Farhad Bouzari, Amelia Rainbow, et al. "Spatially and Temporally Associated Porphyry Deposits with Distinct Cu/Au/Mo Ratios, Woodjam District, Central British Columbia." Economic Geology 112, no. 7 (2017): 1673–717. http://dx.doi.org/10.5382/econgeo.2017.4526.

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Abstract The Woodjam district is a cluster of porphyry Cu-Au deposits of Early Jurassic age (~196 Ma) and is located in the Quesnel terrane in central British Columbia. Porphyry centers include the Southeast zone Cu-Mo porphyry, the Deerhorn and Megabuck Au-Cu porphyries, and the Takom and Three Firs Cu-Au porphyries. The Takomkane batholith, which intruded strata of the Nicola Group and is host to the Southeast zone, has characteristics of a calc-alkalic Cu-Mo porphyry. The Deerhorn, Megabuck, and Takom deposits are centered on narrow monzonite bodies with pencil-like geometries that intruded
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Díaz Castro, Carlos, David R. Cooke, Ivan Belousov, et al. "The Cascabel Porphyry Cu-Au-Ag District, Northern Ecuador." Economic Geology 120, no. 2 (2025): 335–62. https://doi.org/10.5382/econgeo.5147.

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Abstract The Cascabel Cu-Au-Ag porphyry cluster is part of the Eocene metallogenic belt of the northern Western Cordillera of Ecuador, and formed during east-directed, low-angle subduction and eastward migration of the Macuchi arc. Cascabel is part of the Imbaoeste mining district, a NE-trending mineralized belt located between the regional-scale Chimbo-Toachi shear zone to the west and the Calacalí-Pujilí-Pallatanga fault to the east. The basement rocks of the Cascabel district are gabbros and mafic volcanic breccias. They are overlain by late Eocene volcanic and volcanosedimentary rocks inte
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Du, Jingguo, and Andreas Audétat. "Early sulfide saturation is not detrimental to porphyry Cu-Au formation." Geology 48, no. 5 (2020): 519–24. http://dx.doi.org/10.1130/g47169.1.

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Abstract Ore-forming magmas are commonly considered to have been unusually metal rich. Because Cu and Au are strongly chalcophile, early sulfide saturation has been regarded as detrimental to porphyry Cu-Au mineralization. Here we demonstrate, based on amphibole-rich cumulate xenoliths and amphibole megacrysts from the Tongling porphyry(-skarn) Cu-Au mining district in southeastern China, that this view is not necessarily correct. Age data combined with petrological and geochemical evidence suggest that the mineralizing magmas at Tongling underwent significant fractional crystallization of amp
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Bensaman, Benny, Mega Fatimah Rosana, and Euis Tintin Yuningsih. "High Sulphidation Mineralization and Advanced Argillic Alteration within Concealed Gajah Tidur Porphyry, Grasberg District, Papua." Indonesian Journal on Geoscience 11, no. 1 (2024): 15–33. http://dx.doi.org/10.17014/ijog.11.1.15-33.

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High sulphidation (HS) mineralization and associated advanced argillic alteration have been intersected by three drill holes below the Grasberg porphyry Cu-Au deposit, known as the Gajah Tidur prospect. The prospect is located between 1,500 ̶ 2,750 m level, in Grasberg District, Papua, Indonesia. The holes are of KL98-10-21, KL98-10-22, and GRD39-08 which intersected 3.4 Ma Gajah Tidur monzonite, Grasberg Igneous Complex, the wall rocks of Kembelangan, and New Guinea Limestone Group. This research aims to determine the characteristics of high sulphidation mineralization associated with advance
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Ouyang, Yongpeng, Qi Chen, Runling Zeng, and Tongfei Li. "Chronological and Geochemical Characteristics of a Newly Discovered Biotite Granite Porphyry in the Zhuxi W-Cu Polymetallic Deposit, Jiangxi Province, South China: Implications for Cu Mineralization." Minerals 15, no. 6 (2025): 624. https://doi.org/10.3390/min15060624.

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Multiple occurrences of adakitic rocks, with crystallization ages clustering around ~160 Ma, have been documented in the Zhuxi district, northeast Jiangxi Province, South China. This research identifies a new adakitic biotite granite porphyry within the Zhuxi W-Cu polymetallic deposit. Zircon U-Pb geochronology of this porphyry yields a crystallization age of 161.6 ± 2.1 Ma. Integrated with previously published data, the adakitic rocks in the study area—comprising diorite porphyrite, biotite quartz monzonite porphyry, and the newly identified biotite granite porphyry—are predominantly calc-alk
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Murad, Fida, Abdul Ghaffar, Innayat Ullah, Abdul Shakoor Mastoi, and Muhammad Tariq Zaman. "The Alteration and Mineralization Characteristics of Miocene Porphyry Cu-Au Deposits of Chagai Magmatic Belt, District Chagai, Balochistan, Pakistan." International Journal of Economic and Environmental Geology 12, no. 1 (2021): 1–8. http://dx.doi.org/10.46660/ijeeg.vol12.iss1.2021.550.

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Subduction related Miocene porphyry type deposits are found in the east-west trending Chagai magmatic belt (CMB) in Pakistan's western margin, Balochistan. This arc exists on the west segment of the Tethyan metallogenic belt in the south-west of Pakistan. Tethyan metallogenic belt is widely spread over 12,000 km from east to west direction from Indochina, Tibet, Pakistan, Iran, Turkey and Alpine mountain range in Europe. During the last thirty to forty years several porphyry deposits have been reported in the Chagai magmatic arc, including the very large Reko Diq H14-H15, large Saindak, Tanjee
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Pan, Jun-Yi, Pei Ni, Zhei Chi, Wen-Bin Wang, Wen-Can Zeng, and Kai Xue. "Alunite 40Ar/39Ar and Zircon U-Pb Constraints on the Magmatic-Hydrothermal History of the Zijinshan High-Sulfidation Epithermal Cu-Au Deposit and the Adjacent Luoboling Porphyry Cu-Mo Deposit, South China: Implications for Their Genetic Association." Economic Geology 114, no. 4 (2019): 667–95. http://dx.doi.org/10.5382/econgeo.4658.

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AbstractThe large Zijinshan high-sulfidation epithermal Cu-Au deposit, together with the adjacent Luoboling porphyry Cu-Mo deposit, constitutes a major porphyry-epithermal ore district in South China. Current debate centers on whether the Zijinshan and the adjacent Luoboling deposits are cogenetic or represent separate ore-forming events, which is a question of importance for exploration in the district. In this contribution, the magmatichydrothermal history of the relationship between Zijinshan and Luoboling is reconstructed based on new alunite 40Ar/39Ar ages from Zijinshan and zircon U-Pb a
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Lunge, Moira, and Joseph O. Espi. "Trace Element Geochemistry of Chalcopyrites and Pyrites from Golpu and Nambonga North Porphyry Cu-Au Deposits, Wafi-Golpu Mineral District, Papua New Guinea." Geosciences 11, no. 8 (2021): 335. http://dx.doi.org/10.3390/geosciences11080335.

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Studying elemental geochemistry of hypogene sulphides can discriminate the hydrothermal fluids responsible for ore formation. To determine whether Golpu porphyry Cu-Au deposits are related to the Nambonga North porphyry system which is located 2.5 km apart in the Wafi-Golpu Mineral District, Papua New Guinea, we compare the trace element compositions of drill core chalcopyrites and pyrites analysed using Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS). The results for the Golpu chalcopyrites revealed high concentrations of Au, As, Se, Mo, Sb, Te and Bi and lower concentr
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Murad, Fida, Abdul Ghaffar, Inayat Ullah, Abdul Shakoor Mastoi, and Muhammad Tariq Zaman. "The Alteration and Mineralization Characteristics of Miocene Porphyry Cu-Au Deposits of Chagai Magmatic Belt, District Chagai, Balochistan, Pakistan." International Journal of Economic and Environmental Geology 12, no. 1 (2024): 1–8. http://dx.doi.org/10.46660/ijeeg.v12i1.139.

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Subduction related Miocene porphyry type deposits are found in the east-west trending Chagai magmaticbelt (CMB) in Pakistan's western margin, Balochistan. This arc exists on the west segment of the Tethyan metallogenicbelt in the south-west of Pakistan. Tethyan metallogenic belt is widely spread over 12,000 km from east to westdirection from Indochina, Tibet, Pakistan, Iran, Turkey and Alpine mountain range in Europe. During the last thirty toforty years several porphyry deposits have been reported in the Chagai magmatic arc, including the very large RekoDiq H14-H15, large Saindak, Tanjeel, H3
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Byrne, Kevin, Guillaume Lesage, Sarah A. Gleeson, Stephen J. Piercey, Philip Lypaczewski, and Kurt Kyser. "Linking Mineralogy to Lithogeochemistry in the Highland Valley Copper District: Implications for Porphyry Copper Footprints." Economic Geology 115, no. 4 (2020): 871–901. http://dx.doi.org/10.5382/econgeo.4733.

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Abstract The Highland Valley Copper porphyry deposits, hosted in the Late Triassic Guichon Creek batholith in the Canadian Cordillera, are unusual in that some of them formed at depths of at least 4 to 5 km in cogenetic host rocks. Enrichments in ore and pathfinder elements are generally limited to a few hundred meters beyond the pit areas, and the peripheral alteration is restricted to narrow (1–3 cm) halos around a low density of prehnite and/or epidote veinlets. It is, therefore, challenging to recognize the alteration footprint peripheral to the porphyry Cu systems. Here, we document a wor
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Dissertations / Theses on the topic "Babin Porphyry Cu District"

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Washburn, Malissa. "Architecture of the Silurian sedimentary cover sequence in the Cadia porphyry Au-Cu district, NSW, Australia : implications for post-mineral deformation." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/1064.

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Alkalic porphyry style Au-Cu deposits of the Cadia district are associated with Late-Ordovician monzonite intrusions, which were emplaced during the final phase of Macquarie Arc magmatism at the end of the Benambran Orogeny. N-striking faults, including the curviplanar, northerly striking, moderately west-dipping basement thrust faults of the Cadiangullong system, developed early in the district history. NE-striking faults formed during rifting in the late Silurian. Subsequent E-W directed Siluro- Devonian extension followed by regional E-W shortening during the Devonian Tabberabberan Orogeny
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Dickinson, Jenni Michelle. "Jura-triassic magmatism and porphyry Au-Cu mineralization at the Pine Deposit, Toodoggone District, North-central British Columbia." Thesis, University of British Columbia, 2006. http://hdl.handle.net/2429/3959.

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The Pine, Fin, and Mex porphyry Au-Cu ± Mo systems are all located within a 10 km² area in the Toodoggone district, along the eastern margin of the Stikine terrane in British Columbia. Multiple episodes of porphyry-style mineralization are associated with these three magmatic centres. The Fin monzogranite is the oldest dated pluton in the district, with a U-Pb zircon emplacement age of 217.8 ± 0.6 Ma. A cross-cutting main-stage quartz-pyrite-chalcopyrite ± molybdenite ± sphalerite vein gives an older Re-Os molybdenite mineralization age of 221.0 ± 1.4 Ma. Hence the vein probably cross-cuts a s
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Wainwright, Alan John. "Volcanostratigraphic framework and magmatic evolution of the Oyu Tolgoi porphyry Cu-Au district, South Mongolia." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/2760.

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The super-giant Oyu Tolgoi porphyry copper-gold deposits in the South Gobi desert, Mongolia, consist of multiple discrete porphyry centers aligned within a north-northeast trending, >6.5 km long, arc-transverse mineralized corridor. The porphyries are linked to a tectono-magmatic event at ~372 Ma within a Devonian to Carboniferous volcanic arc, and U-Pb (zircon) geochronology records magmatic activity from ~390 Ma to ~320 Ma. The Oyu Tolgoi district underwent at least three discrete periods of syn- to post-mineral shortening and there is evidence for at least three unconformities within the Pa
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Alva, Jimenez Tatiana Romy. "Variation in hydrothermal muscovite and chlorite composition in the Highland Valley porphyry Cu-Mo district, British Columbia, Canada." Thesis, University of British Columbia, 2011. http://hdl.handle.net/2429/38209.

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Muscovitic mica and chlorite are common alteration components in porphyry Cu-Mo deposits. Their mineral chemistry varies depending on the degree of fluid rock interaction, pressure and temperature and can therefore be used as alteration vector. At the Valley porphyry Cu-Mo deposit of the Highland Valley porphyry district, southern British Columbia, muscovitic mica forms part of the high-temperature K-silicate assemblage. It also forms in the adjacent Bethsaida Zone and the abandoned Alwin mine some 4 km to the west, where it is associated with quartz-sulfide veins. The host rock of these areas
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Pudack, Claudia. "Evolution of ore-forming fluids at the porphyry to epithermal transition: the Famatina Cu-Mo-Au district (NW Argentina) /." Zürich : ETH/ Department of earth sciences fluids and mineral deposits group, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17378.

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McKinley, Bradley Scott Mason. "Geological characteristics and genesis of the Kemess North porphyry Au-Cu-Mo deposit , Toodoggone district, north-central British Columbia, Canada." Thesis, University of British Columbia, 2006. http://hdl.handle.net/2429/2293.

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The Kemess North porphyry Au-Cu-Mo deposit (300 Mt resource @ 0.30 g/t Au and 0.16% Cu)i s situated in the Toodoggone district, along the eastern margin of the Stikinia terrane in British Columbia. Mineralization is genetically related to the ca. 202 Ma, moderately SE-plunging, Kemess North diorite and is also hosted by proximal Takla Group basalt country rock. The nearby 202.7 ± 1.9 Ma Sovereign diorite has a comparable emplacement age, mineralogy, and chemistry to the Kemess North diorite, but is unmineralized. Toodoggone Formation volcaniclastic rocks (199.1 ± 0.3 Ma) crop out as prominent
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Sapiie, Benyamin. "Strike-slip faulting, breccia formation and porphyry Cu-Au mineralization in the Gunung Bijih (Ertsberg) mining district, Irian Jaya, Indonesia /." Digital version accessible at:, 1998. http://wwwlib.umi.com/cr/utexas/main.

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Thesis (Ph. D.)--University of Texas at Austin, 1998.<br>Vita. Four folded plates in pocket. Includes bibliographical references (leaves 285-303). Available also in a digital version from Dissertation Abstracts.
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Lickfold, V. "Intrusive history and volatile evolution of the Endeavour porphyry Cu-Au deposits, Goonumbla district, NSW, Australia." Thesis, 2002. https://eprints.utas.edu.au/11364/2/Lickfold-Whole-Thesis_2002.pdf.

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The Goonumbla Volcanic Complex (GVC) of central-west New South Wales, Australia, is part of the Ordovician Macquarie Island Arc. The upper unit of the GVC, the Wombin Volcanics, comprises submarine shoshonitic lavas and associated volcaniclastic rocks, and hosts four economic porphyry Cu-Au deposits, Endeavour 22 (E22), E26, E27 and E48. Together these deposits have a combined ore reserve of 63.6Mt @ 1.1 % Cu and 0.5g/t Au. Mineralisation is centred on thin, pipe-like quartz monzonite porphyry (QMP) complexes that intruded the Wombin Volcanics in an extensional regime towards the end of the La
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Fox, N. "Controls on alteration and mineralisation at the Cadia East alkalic porphyry Au-Cu deposit, NSW." Thesis, 2012. https://eprints.utas.edu.au/15914/1/Nathan_Fox_PhD_2012_UTAS.pdf.

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Chen, J. "Hydrothermal and structural evolution of the Zijinshan high sulfidation Au-Cu deposit, Fujian Province, China." Thesis, 2019. https://eprints.utas.edu.au/32634/1/Chen_whole_thesis.pdf.

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The Zijinshan ore field is a world class mineral district located in southwest Fujian Province, southeast China. It contains a diverse array of ore deposits hosted by the Zijinshan granite complex and surrounding volcano-sedimentary rocks. Associated deposits include high sulfidation epithermal gold-copper, intermediate sulfidation epithermal polymetallic silver-base metal, and porphyry molybdenum-copper deposits. The Zijinshan high-sulfidation Au-Cu deposit is in the middle of the Zijinshan ore field. Its ore zones are hosted in the Zijinshan lithocap. The granitic host rocks are part of a Ju
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Book chapters on the topic "Babin Porphyry Cu District"

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Kouzmanov, K., R. Moritz, M. Chiaradia, D. Fontignie, and C. Ramboz. "Sr and Pb isotope study of Au-Cu epithermal and porphyry-Cu deposits from the southern part of the Panagyurishte district, Sredna Gora zone, Bulgaria." In Mineral Deposits at the Beginning of the 21st Century. CRC Press, 2022. http://dx.doi.org/10.1201/9781003077503-137.

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John, David A. "Geologic Setting and Characteristics of Mineral Deposits in the Central Wasatch Mountains, Utah." In Geology and Ore Deposits of the Oquirrh and Wasatch Mountains, Utah. Society of Economic Geologists, 1998. http://dx.doi.org/10.5382/gb.29.02.

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Abstract Base- and precious-metal deposits in the central Wasatch Mountains southeast of Salt Lake City were mined for more than 100 years beginning in 1868. Deposits present in the Park City, Little Cottonwood, and Big Cottonwood mining districts include Ag-Pb-Zn ± Cu ± Au replacements and veins, a low-grade porphyry Cu-Au deposit, Cu-bearing skarns, a quartz monzonite-type (low F) porphyry Mo deposit, and high sulfidation (quartz-alunite) Au deposits. Most production came from polymetallic replacement and vein deposits in the Park City mining district, which has a recorded production of more
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Harris, Anthony C., David R. Cooke, Ana Liza Garcia Cuison, et al. "Chapter 30: Geologic Evolution of Late Ordovician to Early Silurian Alkalic Porphyry Au-Cu Deposits at Cadia, New South Wales, Australia." In Geology of the World’s Major Gold Deposits and Provinces. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.30.

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Abstract The Cadia district of New South Wales contains four alkalic porphyry Au-Cu deposits (Cadia East, Ridgeway, Cadia Hill, and Cadia Quarry) and two Cu-Au-Fe skarn prospects (Big Cadia and Little Cadia), with a total of ~50 Moz Au and ~9.5 Mt Cu (reserves, resources, and past production). The ore deposits are hosted by volcaniclastic rocks of the Weemalla Formation and Forest Reefs Volcanics, which were deposited in a submarine basin on the flanks of the Macquarie Arc during the Middle to Late Ordovician. Alkalic magmatism occurred during the Benambran orogeny in the Late Ordovician to ea
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Yang, Zhiming, and David R. Cooke. "Chapter 5 Porphyry Copper Deposits in China." In Mineral Deposits of China. Society of Economic Geologists, 2019. http://dx.doi.org/10.5382/sp.22.05.

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Abstract Porphyry Cu deposits in China contain a total resource of ~47 million tonnes (Mt) Cu at average grades ranging mostly from 0.2 to 0.7% Cu (most &amp;lt;0.5% Cu), accounting for 42% of China’s Cu reserves. In terms of contained Cu, 14 Cu-rich porphyry deposits are classified as giant (≥2.0 Mt Cu), and 38 are classified as intermediate (≥0.06 Mt Cu). These giant and intermediate deposits are mainly concentrated in seven belts or districts: Gangdese belt, southern Tibet; Yulong and Zhongdian belts, eastern Tibet; Duolong district, central Tibet; Dexing district and Middle-Lower Yangtze R
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Rabayrol, Fabien, Craig J. R. Hart, Richard M. Friedman, and Richard A. Spikings. "Diachronous Magmatic and Cu-Au-Mo Metallogenic Responses to Slab Roll-Back Initiation from Northwest Anatolia to the Balkans, Western Tethyan Eocene Magmatic Belt." In Tectonomagmatic Influences on Metallogeny and Hydrothermal Ore Deposits: A Tribute to Jeremy P. Richards (Volume I). Society of Economic Geologists, 2021. http://dx.doi.org/10.5382/sp.24.02.

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ABSTRACT The Bursa mineral district in northwest Anatolia (Turkey) is an emerging prospective area for porphyry Cu-Mo (Au-Re) mineralization along the Western Tethyan Eocene magmatic belt that links the Balkan to Lesser Caucasus regions along the southern Black Sea coast. Field observations as well as time constraints on mineralized magmas of the Bursa district are limited. Additionally, the tectonic setting of Eocene magmatism in northwest Turkey is controversial and includes either Neotethyan slab roll-back or break-off scenario. We show that the Bursa mineral district consists of porphyry C
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Viala, M., and K. Hattori. "Magmatism and Related Au-Cu Mineralization in the Hualgayoc Mining District, Northern Peru." In Tectonomagmatic Influences on Metallogeny and Hydrothermal Ore Deposits: A Tribute to Jeremy P. Richards (Volume I). Society of Economic Geologists, 2021. http://dx.doi.org/10.5382/sp.24.09.

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Abstract The Hualgayoc district in the Cajamarca region of northern Peru experienced middle Miocene andesitic to rhyolitic magmatism and magmatic hydrothermal activity that produced Au and Cu mineralization, including the Cerro Corona porphyry Au-Cu, Tantahuatay high-sulfidation epithermal Au, and the AntaKori skarn Cu-Au-Ag deposits. We examined 32 samples from 22 units that encompass the entire igneous rock record in the district. Our new U-Pb dating of 454 zircon grains from these 22 igneous units yielded Concordia ages showing continuous magmatic activity in the district, from 14.8 to 9.7
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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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Deino, Alan, and Jeffrey D. Keith. "Ages of Volcanic and Intrusive Rocks in the Bingham Mining District, Utah." In Geology and Ore Deposits of the Oquirrh and Wasatch Mountains, Utah. Society of Economic Geologists, 1998. http://dx.doi.org/10.5382/gb.29.07.

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Abstract Latitic volcanic rocks about 39 to 38 Ma and 33 to 31 Ma occur along the eastern flank of the Oquirrh Mountains in the vicinity of the Bingham Canyon porphyry Cu-Au-Mo deposit. Extrapolation of the basal contact of the 39 Ma volcanic rocks shows that they likely covered parts of the Bingham intrusions less than 500 m above the pre-mining surface. Some Bingham intrusions may have vented to the surface to help form the volcanic sequence. Minette and shoshonite lavas occur in subordinate amounts within the volcanic sequence. Minette dikes (37.74 ±0.11 Ma) in the Bingham Canyon ore body a
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Lee, Well-Shen, Daniel J. Kontak, Jeremy P. Richards, Tony Barresi, and Robert A. Creaser. "Superimposed Porphyry Systems in the Dawson Range, Yukon." In Tectonomagmatic Influences on Metallogeny and Hydrothermal Ore Deposits: A Tribute to Jeremy P. Richards (Volume I). Society of Economic Geologists, 2021. http://dx.doi.org/10.5382/sp.24.03.

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ABSTRACT Superimposed porphyry systems are a subset of telescoped porphyry deposits, whereby significantly younger ore zones overprint older, nongenetically related systems. Recognition of superimposed features in porphyry systems is important for determining and assessing their prospectivity. The Mount Nansen gold corridor in the southern Dawson Range gold belt of Yukon, Canada, contains porphyry prospects and epithermal deposits with enigmatic genetic models. Geologic, petrologic, temporal (U-Pb zircon, Re-Os molybdenite), and geochemical (whole-rock) studies are used to demonstrate the pres
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Tarantola, Alexandre, Christophe Scheffer, Olivier Vanderhaeghe, Adonis Photiades, and Denis Morin. "Geologic and metallogenic overview of the Lavrion mining district: A guide for archaeological exploration." In Der Anschnitt, Beihefte. Deutsches Bergbau-Museum Bochum, 2023. https://doi.org/10.46586/dbm.264.388.

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The Lavrion mining district (SE Attica, Greece) comprises ore deposits of (1) low-grade Mo-Cu porphyry style, (2) Cu-Fe skarn, (3) high-temperature carbonate replacement Pb-Zn-Ag-(Au), and (4) vein and breccia Pb-Zn-Ag mineralizations. These are the result of the transport and deposition of economic elements from fluids that circulated from the construction to the gravitational collapse of the Hellenides-Aegean Domain along the Africa-Eurasia convergent plate boundary active for the last 80 Ma. Oceanic and continental rocks of the African plate were buried to high pressure conditions in the su
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Conference papers on the topic "Babin Porphyry Cu District"

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Garces, Daniel, Yolanda Sanchez-Palencia, Samantha Jimenez, and Juan Llamas. "ENVIRONMENTAL STATISTICAL ANALYSIS OF THE BASINS OF THE MINING DISTRICT OF PONCE ENRIQUEZ (ECUADOR)." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.09.

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Camilo Ponce Enriquez is in the southwest coastal zone of Ecuador, and it is surrounded by 4 river basins (Gala, Tenguel, Siete and Pagua) with an area of 1,780 km2. Mining has been the main economic activity since 1980 and is classified as Artisanal and Small-Scale Mining Activity. However, since 2000s there is evidence of contamination by heavy metals in water and sediments due to irregular mining practices and inefficiency environmental�s regulations. Despite the evidence, there are not enough scientific studies, and few reports are published about chemistry and contamination. The study goa
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Munkhtsengel, B., O. Gerel, N. Tsuchiya, and M. Ohara. "Petrochemistry of Igneous Rocks in Area of the Erdenetiin Ovoo Porphyry Cu-Mo Mineralized District, Northern Mongolia." In WATER DYANMICS: 4th International Workshop on Water Dynamics. AIP, 2007. http://dx.doi.org/10.1063/1.2721250.

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Swaim, Nathan T., Simone E. Runyon, and Ralph J. Stegen. "DISTRIBUTION AND STYLES OF HYPOGENE ALTERATION IN THE MIAMI-INSPIRATION PORPHYRY CU(-MO) DEPOSIT, GLOBE-MIAMI DISTRICT, ARIZONA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334825.

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Campbell, Michelle, and John Dilles. "EVOLVING METAL RATIOS IN THE LONG-LIVED SULPHURETS PORPHYRY AU-CU-MO DISTRICT: A LINK BETWEEN METAL ENDOWMENT IN PORPHYRY COPPER DEPOSITS AND DEEP CRUSTAL PROCESSES." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-378090.

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Aluç, Ali, Ilkay Kuşcu, Alexey Ulianov, Mehtap Karcı, David Selby, and Robert Moritz. "Magmatic evolution and timing of ore formation at the high-sulfidation epithermal Au-Ag deposit and porphyry Cu-Mo mineralization, Kirazlı district, Biga Peninsula, Turkey." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6020.

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Reports on the topic "Babin Porphyry Cu District"

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Mercier-Langevin, P., R. A. Creaser, J. Goutier, and I. Kjarsgaard. Rhenium-rich molybdenite and Re-Os age of the Archean porphyry-style Don Rouyn deposit, Abitibi greenstone belt, Rouyn-Noranda, Québec. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332556.

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This report presents Re-Os dating of molybdenite from the Don Rouyn deposit and St. Jude breccia prospect in the Rouyn-Noranda mining district in the southern Abitibi greenstone belt, Quebec. Both have been described as porphyry-style, magmatic-hydrothermal Cu-(Au-Mo) deposits associated with the Flavrian and Powell subvolcanic plutons based on the nature of the mineralized zones, their setting and available U-Pb age constraints. To further constrain the timing of mineralization, molybdenite was sampled at both sites for Re-Os geochronology. Although the analyzed sample from the St. Jude prosp
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Neyedley, K., J. J. Hanley, Z. Zajacz, and M. Fayek. Accessory mineral thermobarometry, trace element chemistry, and stable O isotope systematics, Mooshla Intrusive Complex (MIC), Doyon-Bousquet-LaRonde mining camp, Abitibi greenstone belt, Québec. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328986.

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The Mooshla Intrusive Complex (MIC) is an Archean polyphase magmatic body located in the Doyon-Bousquet-LaRonde (DBL) mining camp of the Abitibi greenstone belt, Québec, that is spatially associated with numerous gold (Au)-rich VMS, epizonal 'intrusion-related' Au-Cu vein systems, and shear zone-hosted (orogenic?) Au deposits. To elucidate the P-T conditions of crystallization, and oxidation state of the MIC magmas, accessory minerals (zircon, rutile, titanite) have been characterized using a variety of analytical techniques (e.g., trace element thermobarometry). The resulting trace element an
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