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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Matthew R. Sanders,John A. Pickeringineralisation as at Bikita. The pegmatites of Bikita are hosted by metabasalts and metadiorites of the Upper Bulawayan Group in the Masvingo greenstone belt in the SE part of the Zimbabwe Craton. At about 2670 Ma the southern part of this craton was affected by deformation and up to granulite-facies

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Trauma-Focused Cognitive-Behavioral Therapythe 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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Book 2019ucite 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 th

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