Werner E. Halter
McGill University
6 Papers
21 Citations
Werner E. Halter is an academic researcher from McGill University. The author has contributed to research in topics: Muscovite & Cassiterite. The author has an hindex of 6, co-authored 6 publications.
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Papers
The role of greisenization in cassiterite precipitation at the East Kemptville tin deposit, Nova Scotia
TL;DR: The role of fluid-rock (leucogranite) interaction in forming the greisen-hosted tin (Cu-Zn-Ag) deposit at East-Kemptville, Nova Scotia was investigated by evaluating compositional and mineralogical changes in a representative zoned greisen, and by using this information to estimate physicochemical changes in the fluidrock system at each step of the alteration.
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Modeling fluid–rock interaction during greisenization at the East Kemptville tin deposit: implications for mineralization
TL;DR: In this article, an interaction between a tin-bearing greisenizing fluid and a leucogranitic rock was modeled in order to evaluate the possible role of alteration induced changes in fluid chemistry in cassiterite deposition.
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Origin and evolution of the greisenizing fluid at the East Kemptville tin deposit, Nova Scotia, Canada
TL;DR: The process responsible for greisen-hosted tin mineralization at East Kemptville was investigated using petrographic, chemical, and fluid inclusion analyses of samples from a single deep drill hole (90-1) in the western part of the deposit as discussed by the authors.
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The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada
Daniel J. Kontak,Kevin M. Ansdell,Jaroslav Dostal,Werner E. Halter,Robert F. Martin,Anthony E. Williams-Jones +5 more
TL;DR: Pegmatites at the East Kemptville Sn-Zn-Cu-Ag deposit occur within a F and P-rich, 370 Ma topaz-muscovite leucogranite, the most evolved phase of the chemically zoned Davis Lake Pluton as mentioned in this paper.
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Application of topaz-muscovite F-OH exchange as a geothermometer
TL;DR: In this paper, the F-OH exchange between muscovite and topaz has been used as a geothermometer for estimating the temperature of greisen-forming systems.
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