Geochemical constraints from zoned hydrothermal tourmalines on fluid evolution and Sn mineralization; an example from fault breccias at Roche, SW England

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doi: 10.1093/petrology/41.9.1439
Authors:Williamson, B. J.; Spratt, J.; Adams, J. T.; Tindle, A. G.; Stanley, C. J.
Author Affiliations:Primary:
University of Bristol, Department of Earth Sciences, Bristol, United Kingdom
Other:
Natural Museum, United Kingdom
Open University, United Kingdom
Volume Title:Journal of Petrology
Source:Journal of Petrology, 41(9), p.1439-1453. Publisher: Oxford University Press, Oxford, United Kingdom. ISSN: 0022-3530
Publication Date:2000
Note:In English. 66 refs.; illus., incl. 1 table, sketch map
Summary:Hydrothermal fluid evolution north of the Permian St Austell granite was studied by EPMA for zoned tourmalines from a < 2 cm fault breccia within massive quartz-tourmaline rocks. Four chemically distinct overgrowth zones were caused by episodic mixing between Mg-, Al-rich magmatic hydrothermal fluids, dominant in the inner zone, with increasingly more oxidizing, Fe-rich formation waters, giving high Sn contents (< 0.35 wt.%) with Sn present as Sn4+, not the more usual Sn2+. Overgrowths and tourmaline nucleation is also studied. Major element analyses of 18 points of tourmaline are listed. [B.E.L.]
Sections:Mineral data
Subsections:Silicates
Subjects:Breccia; Chemical composition; Clastic rocks; Fluid inclusions; Geochemistry; Hydrothermal alteration; Inclusions; Metal ores; Metallogeny; Metasomatism; Mineral deposits, genesis; Mineralization; Ore-forming fluids; Ring silicates; Sedimentary rocks; Silicates; Tectonic breccia; Tin ores; Tourmaline group; Cornwall England; England; Europe; Great Britain; United Kingdom; Western Europe; Roche England; Saint Austell Granite
Coordinates:N500000 N505000 W0041500 W0063000
Abstract Numbers:01M/1995
Record ID:2000069668
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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