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Archean rare-metal pegmatites in Zim...

Dittrich, Thomas.

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Archean rare-metal pegmatites in Zimbabwe and Western Australia = geology and metallogeny of pollucite mineralisations /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Archean rare-metal pegmatites in Zimbabwe and Western Australia/ by Thomas Dittrich ... [et al.].
Reminder of title:	geology and metallogeny of pollucite mineralisations /
other author:	Dittrich, Thomas.
Published:	Cham :Springer International Publishing : : 2019.,
Description:	xi, 125 p. :ill., digital ;24 cm.
[NT 15003449]:	Introduction -- Geological Settings of Archean Cratons -- Fieldwork and Sampling of Selected Pegmatites and Pegmatite Fields -- Petrography and Mineralogy -- Geochemistry -- Geochronology -- Stable and Radiogenic Isotopes.
Contained By:	Springer eBooks
Subject:	Pegmatites. -
Online resource:	https://doi.org/10.1007/978-3-030-10943-1
ISBN:	9783030109431

Archean rare-metal pegmatites in Zimbabwe and Western Australia = geology and metallogeny of pollucite mineralisations /
Archean rare-metal pegmatites in Zimbabwe and Western Australiageology and metallogeny of pollucite mineralisations /[electronic resource] :by Thomas Dittrich ... [et al.]. - Cham :Springer International Publishing :2019. - xi, 125 p. :ill., digital ;24 cm. - SpringerBriefs in world mineral deposits,2509-7857. - SpringerBriefs in world mineral deposits..

Introduction -- Geological Settings of Archean Cratons -- Fieldwork and Sampling of Selected Pegmatites and Pegmatite Fields -- Petrography and Mineralogy -- Geochemistry -- Geochronology -- Stable and Radiogenic Isotopes.

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 of LCT pegmatite systems, and 2) will contribute to the further exploration of additional world-class LCT pegmatite deposits, which 3) may host massive pollucite mineralisations.

ISBN: 9783030109431

Standard No.: 10.1007/978-3-030-10943-1doiSubjects--Topical Terms:

971679
Pegmatites.

LC Class. No.: QE462.P4

Dewey Class. No.: 552.3

Archean rare-metal pegmatites in Zimbabwe and Western Australia = geology and metallogeny of pollucite mineralisations /
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245 0 0 $a Archean rare-metal pegmatites in Zimbabwe and Western Australia $h [electronic resource] : $b geology and metallogeny of pollucite mineralisations / $c by Thomas Dittrich ... [et al.].
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520 $a 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 of LCT pegmatite systems, and 2) will contribute to the further exploration of additional world-class LCT pegmatite deposits, which 3) may host massive pollucite mineralisations.
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