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Titlebook: Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia; Geology and Metallog Thomas Dittrich,Thomas Seifert,J?rg Pf?nder Book 2019

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發(fā)表于 2025-3-21 19:00:48 | 只看該作者 |倒序瀏覽 |閱讀模式
期刊全稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia
期刊簡稱Geology and Metallog
影響因子2023Thomas Dittrich,Thomas Seifert,J?rg Pf?nder
視頻videohttp://file.papertrans.cn/162/161216/161216.mp4
發(fā)行地址Presents the first comparative study on LCT pegmatites within the Yilgarn Craton.Offers radiogenic isotope data on LCT pegmatites within the Yilgarn Craton.Integrates evolution of LCT pegmatites into
學(xué)科分類SpringerBriefs in World Mineral Deposits
圖書封面Titlebook: Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia; Geology and Metallog Thomas Dittrich,Thomas Seifert,J?rg Pf?nder Book 2019
影響因子.Lithium-cesium-tantalum (LCT) pegmatites are important resources for rare metals. For Cs, only the LCT pegmatites with the zeolite group mineral pollucite at Bikita (Zimbabwe Craton) and Tanco (Superior Province Craton) are of commercial importance. Common characteristics of world-class LCT pegmatite deposits include their Meso- to Neoarchean age and geological setting within greenstone belt lithologies on Archean Cratons..This study presents the first coherent and comparative scientific investigation of five major LCT pegmatite systems from the Yilgarn, Pilbara and Zimbabwe Craton. For the evaluation of their Cs potential and of the genetic concepts of pollucite formation, the pegmatites from Wodgina, Londonderry, Mount Deans and Cattlin Creek were compared to the Bikita pollucite mineralization.?.The integration of the new data (e.g., geochronological and radiogenic isotope data) into the complex geological framework: 1) enhances our knowledge of the formation ofLCT pegmatite systems, and 2) will contribute to the further exploration of additional world-class LCT pegmatite deposits, which 3) may host massive pollucite mineralisations.?.
Pindex Book 2019
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Geochemistry of LCT Pegmatites,the massive pollucite mineralisation. The geochemical study was also designed for potential prediction if a pegmatite potentially might host a yet not recognised massive pollucite mineralisation. Following these goals, the data from the pollucite-bearing Bikita pegmatite field are used for character
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Geochronology of Archean LCT Pegmatites,anco, Greenbushes, Bikita, Wodgina) were formed in relative narrow time intervals within the earth history. In addition, the temporal and spatial relation-ships of the pegmatites to potential source granites, their crystallisation history and geotectonic settings are still under debate. For the eval
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