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Titlebook: Isotope Geology of the Norilsk Deposits; Oleg Petrov Book 2019 Springer Nature Switzerland AG 2019 isotope data.ore deposits.metallogeny.z

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发表于 2025-3-21 17:17:05 | 显示全部楼层 |阅读模式
书目名称Isotope Geology of the Norilsk Deposits
编辑Oleg Petrov
视频video
概述Addresses open problems in the analysis of crude ore and hosting silicate rocks, the relationship of the ore process with magmatic, sedimentary, and hydrothermal-metasomatic processes.Presents the iso
丛书名称Springer Geology
图书封面Titlebook: Isotope Geology of the Norilsk Deposits;  Oleg Petrov Book 2019 Springer Nature Switzerland AG 2019 isotope data.ore deposits.metallogeny.z
描述The book presents isotope-geochemical investigations of the world’s largest reserves of copper, nickel, and platinum-group elements in the Norilsk ore region. Ever since its discovery, generations of geologists have been fascinated by the geology of these deposits, described as a 250 Ma magmatic formation with mafic and ultramafic layered intrusions, disseminated ore and continuous copper-nickel ore bed. The book includes the results of more than 5,000 analyses of eleven isotopic systems, performed at the Russian Research Geological Institute’s Center of Isotopic Research between 2005 and 2014.. .The book is intended for specialists in isotope geology, metallogeny, ore geology and students of geology..
出版日期Book 2019
关键词isotope data; ore deposits; metallogeny; zircon ages; Taimyr Peninsula; Norilsk ore
版次1
doihttps://doi.org/10.1007/978-3-030-05216-4
isbn_ebook978-3-030-05216-4Series ISSN 2197-9545 Series E-ISSN 2197-9553
issn_series 2197-9545
copyrightSpringer Nature Switzerland AG 2019
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Isotope Geology of the Norilsk Deposits978-3-030-05216-4Series ISSN 2197-9545 Series E-ISSN 2197-9553
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Oleg PetrovAddresses open problems in the analysis of crude ore and hosting silicate rocks, the relationship of the ore process with magmatic, sedimentary, and hydrothermal-metasomatic processes.Presents the iso
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Springer Geologyhttp://image.papertrans.cn/i/image/475782.jpg
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Strontium and Neodymium Isotopes,of igneous rocks from the studied massifs, the primary ratio of strontium varies from 0.7049 to 0.7128, and ε. varies from −7.7 to +7.0. These data indicate a significant effect of the crustal component in the formation of igneous rocks during the injection of mantle material with the parameters .Sr
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