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Origin and Evolution of Precambrian High-Grade Gneiss Terranes, with Special Emphasis on the Limpopo Complex of Southern Africa
GSA Memoirs

Origin and Evolution of Precambrian High-Grade Gneiss Terranes, with Special Emphasis on the Limpopo Complex of Southern Africa

Author(s)
Dirk D. van Reenen
Dirk D. van Reenen
Department of Geology, University of Johannesburg, Auckland Park, South Africa
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Jan D. Kramers
Jan D. Kramers
Department of Geology, University of Johannesburg, and School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa
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Stephen McCourt
Stephen McCourt
School of Geological Sciences, University of KwaZulu Natal, Durban, South Africa
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Leonid L. Perchuk
Leonid L. Perchuk
Department of Petrology, Moscow State University, and the Institute of Experimental Mineralogy, Russian Academy of Sciences, Chernogolovka, Moscow District, Russia
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Geological Society of America
Volume
207
DOI:
https://doi.org/10.1130/MEM207
Copyright:
© 2011 Geological Society of America
Attribution: You must attribute the work in the manner specified by the author or licensor (but no in any way that suggests that they endorse you or your use of the work). Noncommercial - you may not use this work for commercial purpose. No Derivative works - You may not alter, transform, or build upon this work. Sharing - Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in other subsequent works and to make unlimited photocopies of items in this journal for noncommercial use in classrooms to further education and science.
ISBN print:
9780813712079
Publication date:
February 01, 2011
Book Chapter

Petrological and experimental application of REE- and actinide-bearing accessory minerals to the study of Precambrian high-grade gneiss terranes

Author(s)
Daniel Harlov
Daniel Harlov
Deutsches GeoForschungsZentrum, Telegrafenberg, D-14473 Potsdam FR, Germany
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Doi:
https://doi.org/10.1130/2011.1207(02)
  • Published:
    February 01, 2011

The current role of rare-earth-element- (REE-) and actinide-bearing accessory minerals as both geochronological markers and recorders of geochemical processes is reviewed in this paper. The minerals covered include the most common REE- and actinide-bearing accessory minerals found in high-grade rocks—i.e., monazite, xeno-time, apatite, huttonite, thorite, zircon, allanite, and titanite. The goal of this review is to describe the most recent research developments regarding these minerals and their interaction with each other as well as their role as geochronometers. These results are then applied to two cross sections of lower crust from Rogaland–Vest Agder, SW Norway, and Tamil Nadu, S India...

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