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Relevant bibliographies by topics / Tectono-metallogenic model

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Academic literature on the topic 'Tectono-metallogenic model'

Author: Grafiati

Published: 24 March 2023

Last updated: 31 July 2025

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Journal articles on the topic "Tectono-metallogenic model"

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Jiang, Hongjun, Chunsi Yang, Dequan Wang, Hui Zheng, Jie Li, and Huayong Chen. "Multiple-Stage Mineralization in the Huayangchuan U−REE−Mo−Cu−Fe Ore Belt of the Qinling Orogen, Central China: Geological and Re−Os Geochronological Constraints." Journal of Earth Science 33, no. 1 (2022): 193–204. http://dx.doi.org/10.1007/s12583-021-1557-1.

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AbstractThe Huayangchuan ore belt is located in the western segment of Xiaoqinling Orogen in the southern margin of the North China Craton (NCC), and hosts voluminous magmatism and significant U−REE−Mo−Cu−Fe polymetallic mineralization. However, geochronological framework of the various mineralization phases in this region is poorly understood. Here, we present new Re−Os isochron ages on magnetite from the Caotan Fe deposit (2 675 ± 410 Ma, MSWD = 0.55), and on pyrite from the Jialu REE deposit (2 127 ± 280 Ma, MSWD = 1.9) and Yuejiawa Cu deposit (418 ± 23 Ma, MSWD = 11.5), and Re−Os weighted

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2

Li, Bo, Wen Bo Wei, and Le Tian Zhang. "Electrical Structure Revealed by Magnetotelluric Data at the East Part of Central Asian Orogenic Belt, Central Inner Mongolia." Applied Mechanics and Materials 448-453 (October 2013): 3788–91. http://dx.doi.org/10.4028/www.scientific.net/amm.448-453.3788.

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The cental Asian orogenic belt (CAOB) which between the North China Craton and the Siberian Craton is one of the tectono-metallogenic belts in the world. The central Inner Mongolia belongs to the eastern part of the CAOB, recently a series of research and exploration work has been done in this region. However, no breakthrough has been made in the exploration of metal ore. In order to research current mineralization issues in the eastern part of the CAOB, a long magnetotelluric (MT) profile was acquired across the central part of Inner Mongolia. The profile starts within the DongUjimqinqi in th

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3

An, Weicai, Chunji Xue, Yun Zhao, Chao Li, Dengfeng Xu, and Bo Chen. "Petrogenesis and Tectonic Implications of Late Carboniferous Intrusions in the Tuwu-Yandong Porphyry Cu Belt (NW China): Constraints from Geochronology, Geochemistry and Sr–Nd–Hf Isotopes." Minerals 12, no. 12 (2022): 1573. http://dx.doi.org/10.3390/min12121573.

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The Tuwu-Yandong porphyry Cu belt is located on the southern margin of the Dananhu island arc in eastern Tianshan, constituting the largest Cu metallogenic belt in Northwest China. Two episodes (~334 Ma and ~317 Ma) of porphyry Cu-Mo mineralization in the belt have been recognized, associated with Early and Late Carboniferous felsic intrusions, respectively. The Carboniferous intrusions, therefore, provide a unique opportunity to investigate tectono-magmatic-metallogenic evolution of the belt. New LA–ICP–MS zircon U–Pb dating indicates that the mineralization-related and post-mineralization in

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Ilienko, V., Т. Burakhovich, and А. Kushnir. "INTERPRETATION OF THE 3D GEOELECTRICAL MODEL OF THE INTERSECTION AREA OF THE ZVIZDAL-ZALISKA AND NEMYRIVSK FAULT ZONES." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 2 (101) (2023): 31–37. http://dx.doi.org/10.17721/1728-2713.101.04.

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The interpretation of the deep three-dimensional geoelectricalal model of the central part of the Zvizdal-Zaliska and Brusyliv fault zones of the Ukrainian shield, which was built with the involvement of data from experimental observations of the Earth's low-frequency electromagnetic field conducted in 2019 by the Institute of Geophysics named after S.I. Subotin of the National Academy of Sciences of Ukraine, within the Ordyntsi-Lobachiv and Zoziv-Stryzhavka profiles was done. Experimental materials were processed with the PRC_MTMV software package, tipper estimates were obtained for periods o

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5

Darabi-Golestan, F. "Gold metallogeny in Iran, implications for gold exploration and conceptual modeling." Geochemistry: Exploration, Environment, Analysis, June 16, 2023. http://dx.doi.org/10.1144/geochem2023-010.

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Significant progress in the classification, definition, and understanding of the main Au deposit types could significantly aid improvements in Au exploration. Because of the wide occurrence of Au in the central part of the Tethyan Eurasian Metallogenic Belt, Iranian structures composed of more than seventeen zones (arcs and blocks) are considered as having one of the largest Au reserves in the Middle East. Without attempts at understanding the tectono-magmatic evolution of Iran and the geodynamic settings of Au deposition, the establishment of a reliable predictive exploration model for Au-typ

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Liu, Ruiqin, Chao Chen, Xinbiao Lv, et al. "Petrogenesis and geological implications of the qiyishan triassic granitoids in east Beishan orogen, inner Mongolia, NW China: evidence from geochronology, geochemistry and Nd-Hf isotopes." Frontiers in Earth Science 11 (October 11, 2023). http://dx.doi.org/10.3389/feart.2023.1260852.

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The Qiyishan deposit is a large-scale Rb polymetallic deposit in the Beishan orogen. However, there remain debates regarding its metallogenic age and tectonic setting. In addition, studies of Triassic tectono-magmatic events in the Beishan orogen are still insufficient, and conducting genesis studies on the Qiyishan Triassic granitoids will help to enhance the understanding of Triassic magmatism and tectonic evolution in the Beishan orogen. In this contribution, we report new data for the ore-forming granitoids of Qiyishan deposit, including zircon U-Pb ages, major and trace element concentrat

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Sillitoe, Richard H. "Metallogeny and Mineral Exploration – Some Personal Reminiscences." Geochemical Perspectives, April 2024, 1–196. http://dx.doi.org/10.7185/geochempersp.13.1.

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The following personalised narrative aims to document the highlights of my involvement in some of the ground breaking developments in Economic Geology and their direct application to mineral exploration and discovery over the past half century. The story begins with my introduction to geology at secondary school and university, followed by doctoral research based on fieldwork in the Andes of South America. Then, as an employee of the Chilean Geological Survey, I got my introduction to porphyry copper deposits before returning to the UK to take up a post-doctoral research fellowship. This forma

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Dissertations / Theses on the topic "Tectono-metallogenic model"

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Grare, Alexis. "Tectono-metallogenic model of the Kiggavik uranium deposits, Nunavut, Canada." Electronic Thesis or Diss., Sorbonne université, 2018. http://www.theses.fr/2018SORUS628.

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Les bassins Paléo- à Mésoproterozoiques (1750-1500 Ma) de l’Athabasca (Saskatchewan) et du Thelon (Nunavut), ainsi que le socle sous-jacent, présentent des gisements d’uranium de classe mondiale. Néanmoins, malgré son fort potentiel exploratoire, le bassin du Thelon, moins accessible, a été bien moins étudié à ce jour. La zone de Kiggavik, sur la bordure Est de ce bassin, a été intensément explorée par AREVA Resources Canada (ARC) jusqu’en 2016 ; elle abrite des minéralisations à uranium économiquement importantes, présentant un contrôle clair par la fracturation. Préciser la genèse, le contrô

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