Coupled trace element mobilisation and strain softening in quartz during retrograde fluid infiltration in dry granulite protoliths

Contributions to Mineralogy and Petrology

Volumn 157, Issue 2, 2009, Pages 147-161

  Sørensen, Bjørn Eske ^a   Larsen, Rune B ^a  

^a NORWEGIAN UNIVERSITY OF SCIENCE AND TECHNOLOGY   (Norway)

Author keywords

Fluid flow; High purity quartz; Hydrolytic weakening; Mass transfer; Quartz; Quartz rheology; Shear zone; Strain hardening; Strain localisation; Strains oftening; Trace elements

Indexed keywords

DISSOLUTION; FUGACITY; GRANULITE; INDUCTIVELY COUPLED PLASMA METHOD; MOBILIZATION; P-T CONDITIONS; PHASE VELOCITY; PROTOLITH; QUARTZ; QUARTZITE; RECRYSTALLIZATION; REHYDRATION; RETROGRADE METAMORPHISM; RHEOLOGY; TRACE ELEMENT;

EID: 57849092618     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-008-0326-9     Document Type: Article

References (39)

1. Applin KR, Hicks BD (1987) Fibers of dumortierite in quartz. Am Mineral 71:786-794
2. Armington AF, Balascio JF (1984) The growth of high purity, low dislocation quartz. In: Proceedings of the 38th annual frequency control symposium, vol., USA, pp 3-7
3. den Brok B, Spiers CJ (1991) Experimental evidence for water weakening of quartzite by microcracking plus solution-precipitation creep. J Geol Soc London 148:541-548. doi: 10.1144/gsjgs.148.3.0541
4. Flem B, Larsen RB, Grimstvedt A, Mansfeld J (2002) In situ analysis of trace elements in quartz by using laser ablation inductively coupled plasma mass spectrometry. Chem Geol 182(2-4):237-247. doi: 10.1016/ S0009-2541(01)00292-3
5. Goetze J, Plotze M, Habermann D (2001) Origin, spectral characteristics and practical applications of the cathodolumimescence (CL) of quartz - a review. Mineral Petrol 71(3-4):225-250. doi: 10.1007/s007100170040
6. Goetze J, Ploetze M, Graupner T, Hallbauer DK, Bray CJ (2004) Trace element incorporation into quartz; a combined study by ICP-MS, electron spin resonance, cathodoluminescence, capillary ion analysis, and gas chromatography. Geochim Cosmochim Acta 68(18):3741-3759. doi: 10.1016/ j.gca.2004.01.003
7. Goetze J, Ploetze M, Trautmann T (2005) Structure and luminescence characteristics of quartz from pegmatites. Am Mineral 90(1):13-21. doi: 10.2138/am.2005.1582
8. Goreva JS, Ma C, Rossman GR (2001) Fibrous nanoinclusions in massive rose quartz: The origin of rose coloration. Am Mineral 86:466-472
9. Griggs DT, Blacic JD (1965) Quartz: Anomalous weakness of synthetic crystals. Science 147(3655):292-295. doi: 10.1126/science.147.3655.292
10. 2-rich fluids during granulite genesis. Contrib Mineral Petrol 139:180-197. doi: 10.1007/PL00007670
11. Jacamon F (2006) The significance of textures and trace element chemistry of quartz with regard to the petrogenesis of granitic rocks. Dissertation, Faculty of Engineering Science and Technology, Department of Geology and Mineral Resources Engineering, Norwegian University of Science and Technology, Trondheim
12. Jessell MW (1987) Grain-boundary migration microstructures in a naturally deformed quartzite. J Struct Geol 9(8):1007-1014. doi: 10.1016/ 0191-8141(87)90008-3
13. Knudsen TL (1996) Petrology and geothermobarometry of granulite facies metapelites from the Hisøy-Torungen area, South Norway: New data on the Sveconorvegian P-T-t path of the Bamble sector. J Metamorph Geol 14(3):267-287. doi: 10.1111/j.1525-1314.1996.00267.x
14. Kronenberg AK (1994) Hydrogen speciation and chemical weakening of quartz. In: Heaney PJ, Prewitt CT, GibbsPGV (eds) Silica: physical behavior, geochemistry and materials applications, vol 29. Mineralogical Society of America, Washington, DC, pp 123-176
15. Kronenberg AK, Tullis J (1984) Flow strengths of quartz aggregates: grain size and pressure effects due to hydrolytic weakening. In: Kirby Stephen H, Scholz CH (eds) Chemical effects of water on the strength and deformation of crustal rocks., vol 89: 6. American Geophysical Union, Washington, DC, United States, pp 4281-4297
16. Kronenberg AK, Kirkby SH, Aines RD, Rossman GR (1986) Solubility and diffusional uptake of hydrogen in quartz at high water pressures: implication for hydrolytic weakening. J Geophys Res B Solid Earth Planets 91:12723-12744. doi: 10.1029/JB091iB12p12723
17. Kronenberg AK, Segall P, Wolf GH (1990) Hydrolytic weakening and penetrative deformation within a natural shear zone. In: Duba AG, Durham WB, Handin JW, Wang Herbert F (eds) The brittle-ductile transition in rocks, vol 56. American Geophysical Union, Washington, DC, pp 21-36
18. Landtwing MR, Pettke T (2005) Relationships between SEM-cathodoluminescence response and trace-element composition of hydrothermal vein quartz. Am Mineral 90(1):122-131. doi: 10.2138/ am.2005.1548
19. Larsen RB (2004) Distribution and petrogenetic behaviour of trace elements in granitic pegmatite quartz. Geochim Cosmochim Acta 68(11):A667-A667
20. Müller A, Lennox P, Trzebski R (2002) Cathodoluminescence and microstructural evidence for crystallisation and deformation processes of granites in the eastern lachlan fold belt (se austia). Contrib Mineral Petrol 143:510-524
21. Müller A, Wiedenbeck M, Van den Kerkhof AM, Kronz A, Simon K (2003) Trace elements in quartz: A combined electron microprobe, secondary ion mass spectrometry, laser-ablation ICP-MS, and cathodoluminescence study. Eur J Mineral 15(4):747-763. doi: 10.1127/0935-1221/2003/0015-0747
22. Nakashima S, Matayoshi H, Yuko T, Michibayashi K, Masuda T, Kuroki N et al (1995) Infrared microspectroscopy analysis of water distribution in deformed and metamorphosed rocks. In: Spiers CJ, Takeshita T (eds) Influence of fluids on deformation processes in rocks, vol 245. Elsevier, Amsterdam, pp 263-276
23. Nijland TG, Maijer C (1993) The regional amphibolite to granulite facies transition at Arendal, Norway: Evidence for a thermal dome. Neues Jahrb Miner Abh 165:191-221
24. Nijland TG, Touret JLR (2001) Replacement of graphic pegmatite by graphic albite-actinolite-clinopyroxene intergrowths (Mjavatn, southern Norway). Eur J Mineral 13(1):41-50. doi: 10.1127/0935-1221/01/0013-0041
25. Nijland TG, Liauw F, Visser D, Maijer C, Senior A (1993a) Metamorphic petrology of the Froland corundum-bearing rocks: The cooling and uplift history of the Bamble sector, South Norway. Bull Nor Geol Unders 424:51-63
26. Nijland TG, Maijer C, Senior A, Verschure RH (1993b) Primary sedimentary structures and composition of the high-grade metamorphic Nivelda quartzite complex (Bamble, Norway), and the origin of nodular gneisses. Proceedings of the Koninklijke Nederlandse Akademie van Wetenschappen (1990) 96(2):217-232
27. Nijland TG, Touret JLR, Visser D (1998) Anomalously low temperature orthopyroxene, spinel, and sapphirine occurrences in metasediments from the Bamble amphibolite-to-granulite facies transition zone (South Norway); possible evidence for localized action of saline fluids. J Geol 106(5):575-590
28. Passchier CW, Trouw RAJ (2005) Microtectonics. 2 ed, vol. Springer, Berlin, Federal Republic of Germany, pp 366
29. Post A, Tullis J (1998) The rate of water penetration in experimentally deformed quartzite: Implications for hydrolytic weakening. In: Chester Fred M, Engelder T, Shimamoto T (eds) Rock deformation; the Logan volume., vol 295; 1-2. Elsevier, Amsterdam, Netherlands, pp 117-137
30. Post AD, Tullis J, Yund RA (1996) Effects of chemical environment on dislocation creep of quartzite. J Geophys Res B Solid Earth and Planets 101(10):22,143-122,155
31. Sørensen BE (2007) Metamorphic refinement of quartz under influence of fluids during exhumation with reference to the metamorphic/ metasomatic evolution observed in amphibolites: A detailed field, microtectonic and geochemical study from the Bamble sector, South Norway. In: Department of Geology and Mineral Ressources Engineering. Dissertation, at Norges teknisk-naturvitenskapelige universitet, Fakultet for ingeniørvitenskap og teknologi, Trondheim, pp 215. http://www.diva-portal.org/diva/ getDocument?urn_nbn_no_ntnu_diva-1563-1_fulltext.pdf
32. Touret J (1968) The Precambrian metamorphic rocks around the Lake Vegår (Aust-Agder, southern Norway), vol 257, pp 45
33. Touret J (1971) Le faciès granulite en Norvège méridionale II Les inclusions fluides. Lithos 4:423-436. doi: 10.1016/0024-4937(71)90125-3
34. Touret J (1985) Fluid regime in southern Norway: The record of fluid inclusions. In: Tobi AC, Touret J (eds) The deep Proterozoic crust in the North Atlantic Provinces vol 158, pp 517-549
35. Touret J, Olsen SN (1985) Fluid inclusions in migmatites. In: Ashworth JR (ed) Migmatites, vol. Shiva, Glasgow, pp 265-288
36. Tullis J (2002) Deformation of Granitic Rocks: Experimental Studies and Natural Examples In: S.-i. Karato and H.-R. Wenk (Editors), Plastic Deformation in Minerals and Rocks. Reviews in Mineralogy. MSA
37. Van den Kerkhof AM, Kronz A, Simon K, Scherer T (2004) Fluid-controlled quartz recovery in granulite as revealed by cathodoluminescence and trace element analysis; Bamble sector, Norway. Contrib Mineral Petrol 146(5):637-652. doi: 10.1007/s00410-003-0523-5
38. Wark D, Watson EB (2006) TitaniQ: A titanium-in-quartz geothermometer. Contrib Mineral Petrol 152(6):743-754. doi: 10.1007/s00410-006-0132-1
39. Watson EB, Brenan JM (1987) Fluids in the Lithosphere, 1. Experimentally determined wetting characteristics of CO2-H2O fluids and their implications for fluid transport, host-rock physical properties, and fluid inclusion formation. Earth Planet Sci Lett 85:496-515