Oscillatory epitactic-growth zoning in biotite and muscovite from the Lake Lewis leucogranite, South Mountain Batholith, Nova Scotia, Canada

Canadian Mineralogist

Volumn 41, Issue 4, 2003, Pages 1027-1047

  Clarke, D Barrie ^a   Bogutyn, Patrick A ^a  

^a DALHOUSIE UNIVERSITY   (Canada)

Author keywords

Biotite; Epitactic growth; Eruption; Exsolution; Fluid phase; Fluorine; Lake Lewis pluton; Muscovite; Nova Scotia; Overpressure

Indexed keywords

LAKES; MINERAL RESOURCES; QUARTZ; TRACE ELEMENTS;

BIOTITE;

ALKALI METALS;

BIOTITE; CHEMICAL COMPOSITION; CRYSTALLIZATION; EXSOLUTION; LEUCOGRANITE; MUSCOVITE; PETROGRAPHY; ZONING;

CANADA; NOVA SCOTIA; SOUTH MOUNTAIN BATHOLITH;

EID: 0242583148     PISSN: 00084476     EISSN: None     Source Type: Journal    
DOI: 10.2113/gscanmin.41.4.1027     Document Type: Article

References (52)

1. BAU, M. (1996): Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect. Contrib. Mineral. Petrol. 123, 323-333.
2. BLAKE, S. (1984): Volatile oversaturation during the evolution of silicic magma chambers as an eruption trigger. J. Geophys. Res. 89, 8237-8244.
3. BOGUTYN, P.A. (2001): White Micas in the Lake Lewis Leucogranite, Nova Scotia. B.Sc. Honours thesis, Dalhousie Univ., Halifax, Nova Scotia.
4. BREITER, K. (2002): From explosive breccia to unidirectional solidification textures: magmatic evolution of a phosphorus- and fluorine-rich granite system (Podlesí, Krušné hory Mts., Czech Republic). Bull. Czech Geol. Surv. 77, 67-92.
5. BROSKA, I., KUBIŚ, M., WILLIAMS, C. T. & KONENČNÝ, P. (2002): The compositions of rock-forming and accessory minerals from the Gemeric granites (Hnilec area, Gemeric Superunit, western Carpathians). Bull. Czech Geol. Surv. 77, 147-155.
6. BURNHAM, C.W. (1979): The importance of volatile constituents. In The Evolution of the Igneous Rocks Fiftieth Anniversary Perspectives (H.S. Yoder Jr., ed.). Princeton University Press, Princeton, N.J. (439-482).
7. CABARCOS, E.L., KUO, CHEIN-SHIU, SCALA, A., & BANSIL, R. (1996): Crossover between spatially confined precipitation and periodic pattern formation in reaction diffusion systems. Phys. Rev. Lett. 77, 2834-2837.
8. CARRUZZO, S., KONTAK, D.J. & CLARKE, D.B. (2000): Granite-hosted mineral deposits of the New Ross area, South Mountain Batholith, Nova Scotia, Canada: P, T, and X constraints of fluids using fluid inclusion thermometry and decrepitate analysis. Trans. R. Soc. Edinburgh: Earth Sci. 91, 303-319.
9. 2}. Contrib. Mineral. Petrol. 48, 89-114.
10. CLARKE, D.B., MACDONALD, M.A., REYNOLDS, P.H. & LONGSTAFFE, F.J. (1993): Leucogranites from the eastern part of the South Mountain Batholith, Nova Scotia. J. Petrol. 34, 653-679.
11. CLARKE, D.B., MUECKE, G.K. (1985): Review of the petrochemistry and origin of the South Mountain Butholith and associated plutons, Nova Scotia, Canada. In High Heat Production (HHP) Granites, Hydrothermal Circulation and Ore Genesis (C. Halls, ed.). Institute of Mineralogy and Metallurgy, London, U.K. (41-54).
12. DING, Y. (1995): AFM Minerals in the Halifax Pluton. M.Sc. thesis, Dalhousie Univ., Halifax, N.S.
13. DOMANIK, K.J. & HOLLOWAY, J.R. (2000): Experimental synthesis and phase relations of phengitic muscovite from 6.5 to 11 GPa in a calcareous metapelite from the Dabie mountains, China. Lithos 52, 51-77.
14. FERRARIS, C., GROBETY, B. & WESSICKEN, R. (2001): Phlogopite exsolutions within muscovite a first evidence for a higher temperature re-equilibration, studied by HRTEM and AEM techniques. Eur. J. Mineral. 13, 15-26.
15. FERROW, E.A., LONDON, D., GOODMAN, K.S. & VEBLEN, D.R. (1990): Sheet silicates of the Lawler Peak granite, Arizona: chemistry, structural variations, and exsolution. Contrib. Mineral. Petrol. 105, 491-501.
16. FOURNIER, R.O. (1999): Hydrothermal processes related to movement of fluid from plastic into brittle rock in the magmatic-epithermal environment. Econ. Geol. 94, 1193-1211.
17. GOMES, M.E.P. & NEIVA, A.M.R. (2000): Chemical zoning of muscovite from the Ervedosa granite, northern Portugal. Mineral. Mag. 64, 347-358.
18. GREEN, T.H. (1981): Synthetic high-pressure micas compositionally intermediate between the dioctahedral and trioctahedral mica series. Contrib. Mineral. Petrol. 78, 452-458.
19. HALTER, W.E. & WILLIAMS-JONES, A.E. (1999): Application of topaz-muscovite F-OH exchange as a geothermometer. Econ. Geol. 94, 1249-1258.
20. HALTER, W.E., WILLIAMS-JONES, A.E. & KONTAK, D.J. (1998a): Modeling of fluid-rock interaction during greisenization at the East Kemptville tin deposit: implications for mineralization. Chem. Geol. 150, 1-17.
21. HALTER, W.E., WILLIAMS-JONES, A.E. & KONTAK, D.J. (1998b): Origin and evolution of the greisenizing fluid at the East Kemptville tin deposit, Nova Scotia, Canada. Econ. Geol. 93, 1026-1051.
22. HAM, L.J. (1991): Geological map of Windsor, Nova Scotia, NTS 21A/16 west half and part of 21H/01. Nova Scotia Department of Mines and Fnergy, Map 90-10 (1:50 000).
23. HAM, L.J. & KONTAK, D.J. (1988): A textural and chemical study of white mica in the South Mountain Batholith, Nova Scotia: primary versus secondary origin. Marit. Sediments Atlantic Geol. 24, 111-121.
24. HOGAN, J.P. (1996): Insights from igneous reaction space: a holistic approach to granite crystallization. Trans. R. Soc. Edinburgh: Earth Sci. 87, 147-157.
25. +5) and anhydrous haplogranite melts. Geochim. Cosmochim. Acta 63, 2419-2428.
26. 2O). Am. Mineral. 80, 1229-1251.
27. LONGERICH, H.P., JACKSON, S.E. & GUNTHER, D. (1996): Laser ablation inductively coupled plasma mass spectrometric transient signal data acquisition and analyte concentration calculation. J. Anal. At. Spectrom. 9, 899-904.
28. LOWENSTERN, J.B. & SINCLAIR, W.D. (1996): Exsolved magmatic fluid and its role in the formation ot comb-layered quartz at the Cretaceous Lotung W-Mo deposit, Yukon Territory, Canada. Trans. R. Soc. Edinburgh: Earth Sci. 87, 291-304.
29. MACDONALD, M.A. (2001): Geology of the South Mountain Batholith, southwestern Nova Scotia. N.S. Dep. Natural Resources, Open File Rep. ME 2001-2.
30. MASSONNE, H.-J. & SCHREYER, W. (1989): Stability field of the high-pressure assemblage, talc + phengite and two new phengite barometers. Eur. J. Mineral. 1, 391-410.
31. 2O. Lithos 41, 229-250.
32. MCKENZIE, C.B. (1974): Petrology of the South Mountain Batholith, Western Nova Scotia. M.Sc. thesis, Dalhousie Univ., Halifax, N.S.
33. MILLER, C.F., STODDARD, E.F., BRADFISH, L.J. & DOLLASE, W.A. (1981): Composition of plutonic muscovite: genetic implications. Can. Mineral. 19, 25-34.
34. 2O and comparison with natural Li-free white micas. Mineral. Mag. 50, 257-266.
35. H20: comparison with natural lithium micas. Mineral. Mag. 50, 641-651.
36. MUNOZ, J.L. (1984): Fluorine index: a simple guide to high fluorine environments. In Micas (S.W. Bailey. ed.). Rev. Mineral. 13, 469-493.
37. ORTOLEVA, P.J. (1994): Geochemical Self-Organization. Oxford University Press, Oxford. U.K.
38. PELRINE, K.M. (2003): Ilmenite-Pyrophanite and Niobian Rutile in the South Mountain Batholith, Nova Scotia. B.Sc. Honours thesis, Dalhousie Univ., Halifax, Nova Scotia.
39. RAIMBAULT, L. & BURNOL, L. (1998): The Richemont rhyolite dyke, Massif Central, France: a subvolcanic equivalent of rare-metal granites. Can. Mineral. 36, 265-282.
40. RICHARDSON J.M., BELL, K., WATKINSON, D.H. & BLENKINSOP, J. (1990): Genesis and fluid evolution of the East Kemptville greisen-hosted tin mine, southwestern Nova Scotia, Canada. In Ore-Bearing Granite Systems: Petrogenesis and Mineralizing Processes (H.J. Stein & J.L. Hannah, eds.). Geol. Soc. Am., Spec. Pap. 246, 181-203.
41. RIEDER, M., CAVAZZINA, G., D'YAKONOV, Y.S., FRANK-KAMENTSKII, V.A., GOTTARDI, G., GUGGENHEIM, S., KOVAL.', P.V., MÜLLER, G., NEIVA, A.M.R., RADOSLOVICH, E.W., ROBERT, J.-L., SASSI, F.P., TAKEDA, H., WEISS, Z. & WONES, D.R. (1998): Nomenclature of the micas. Can. Mineral. 36, 905-912.
42. ROYCROFT, P.D. (1989): Zoned muscovite from the Leinster Granite, S.E. Ireland. Mineral. Mag. 53, 663-665.
43. ROYCROFT, P.D. (1991): Magmatically zoned muscovite from the peraluminous two-mica granites of the Leinster batholith, southeast Ireland. Geology 19, 437-440.
44. SCHMITT, A.K. (2001): Gas-saturated crystallization and degassing in large-volume, crysial-rich dacitic magmas from the Altiplano-Puna, northern Chile. J. Geophys. Res. 106, 30561-30578.
45. SPEER, L.A. (1994): Micas in igneous rocks. In Micas (S.W. Bailey, ed.). Rev. Mineral. 13, 229-356.
46. TATE, M.C. & CLARKE, D.B. (1997): Compositional diversity among Late Devonian peraluminous granitoid intrusions in the Meguma Zone of Nova Scotia, Canada. Lithos 39, 179-194.
47. TISCHENDORF, G., GOTTESMANN, B., FÖRSTER. H.-J. & TRUMBULL, R.B. (1997): On Li-bearing micas: estimating Li from electron microprobe analyses and an improved diagram for graphical representation. Mineral Mag. 61, 809-834.
48. VELDE, B. (1965): Phengite micas: synthesis, stability, and natural occurrence. Am. J. Sci. 263, 886-913.
49. VELDE, B. (1980): Cell dimensions, polymorph type, and infrared spectra of synthetic while micas: the importance of ordering. Am. Mineral 65, 1277-1282.
50. 2 fluids and topaz rhyolite melt: implications for mineralizing magmatic-hydrothermal fluids in F-rich granitic systems. Contrib. Mineral. Petrol. 104, 424-438.
51. WEIDNER, J.R. & MARTIN, R.F. (1987): Phase equilibria of a fluorine-rich leucogranite from the St. Austell pluton, Cornwall. Geochim. Cosmohim. Acta 51, 1591-1597.
52. ZEN, E-AN (1988): Phase relations of peraluminous granitic rocks and their petrogenetic implications. Annu. Rev. Earth Planet. Sci. 16, 21-51.