Abstract
Examples of structurally controlled regional metasomatism span most metamorphic temperatures, pressures, and tectonic settings. Permeability is crucial, and may be intrinsic or the result of deformation processes such as micro-fracturing (e.g. grain boundary sliding), fracturing, faulting, foliation and shear zone development, and hydro-fracturing. Chromatographic theory has been developed to explain metasomatic zonation, and applies not only where mineral reaction and isotopic fronts formed normal to the fluid flow in a porous medium, but also where flow was parallel to fractures or lithological contacts. Metasomatic fronts may be sharp or broadened by diffusion and dispersion effects during fluid advection. In the upper crust, fluid advection involved in regional metasomatism, such as silicification, albitization, potassic alteration and dolomitization, is controlled mainly by intrinsic permeability, faults, fractures and microfractures in sedimentary basins, volcanic sequences and some granites. For skarn formation, fluid advection is controlled by interface-coupled dissolution-precipitation (“reaction-controlled permeability”) in addition to fractures and microfractures. Cross-layer diffusion in addition to layer-parallel advection is probably important in the formation of skarns along lithological contacts. Although subject to some debate, many workers have provided mineralogical and isotopic evidence for the existence of high time-integrated fluid fluxes and fluid flow directions in many thermal aureoles and regional metamorphic belts. Studies of quartz veins and vein selvages in metamorphic rocks have provided examples both of local derivation of veins and derivation of silica and metasomatic changes in the selvages during advection of external fluids. Also subject to debate is whether metamorphic fluids in the middle crust are solely derived from devolatilization reactions at depth or whether such processes as dilatancy pumping or syn-metamorphic intrusion can lead to lateral or downward fluid advection. Regional metasomatism occurs in many Proterozoic metamorphic belts, but the Mount Isa Inlier is probably the best natural laboratory regarding structural controls. It exhibits enormous strain heterogeneity at all scales that led to fluid channeling, diverse reactive rocks, episodic metamorphic and intrusive events spanning at least 250 Ma, and abundant sources of reactive saline and hypersaline fluids. Examples of widespread metasomatism in the Mount Isa Inlier include Na-Ca alteration associated with extensive breccia development in calcsilicate rocks, albitization of schists and metapsammitic rocks, and the formation in high-strain zones of tremolite pods, quartz-chlorite rocks, and unusual cordierite-rich rocks.
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Ague JJ (1994a) Mass transfer during Barrovian metamorphism of pelites. south-central Connecticut. I: evidence for changes in composition and volume. Am J Sci 297:679–706
Ague JJ (1994b) Mass transfer during Barrovian metamorphism of pelites. south-central Connecticut. II: channelized fluid flow and the growth of staurolite and kyanite. Am J Sci 297:1061–1134
Ague JJ (2003) Fluid infiltration and transport of major, minor, and trace elements during regional metamorphism of carbonate rocks, Wepawaug Schist, Connecticut, USA. Am J Sci 303:753–816
Ague JJ (2004) Fluid flow in the deep crust. In: Holland HD, Tuekian KK, Rudnick RL (eds) Treatise on geochemistry, vol 3, The Crust. Elsevier, Amsterdam, pp 195–228
Ague JJ (2011) Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism. Amer Mineral 96:333–352
Angus NS, Kanaris-Sotiriou R (1995) Adinoles revisited: hydrothermal Na (Ca)-metasomatism of pelitic screens adjacent to tholeiitic dykes in the Dublin terrane. Ireland Mineral Mag 59:367382
Aslund T, Oliver NHS, Cartwright I (1995) Metasomatism of the revenue granite and aureole rocks, Mt Isa Inlier, Queensland: syndeformational fluid flow and fluid-rock interaction. Aust J Earth Sci 42:291–299
Austin JR, Blenkinsop TG (2010) Cloncurry fault zone: strain partitioning and reactivation in a crustal-scale deformation zone, Mt Isa Inlier. Aust J Earth Sci 57:1–21
Barton MD, Johnson DA (1996) Evaporitic-source model for igneous-related Fe oxide-(REE-Cu-Au-U) mineralization. Geology 24:259–262
Battles DA, Barton MD (1995) Arc-related sodic hydrothermal alteration in the western United States. Geology 24:913–916
Baumgartner LP, Ferry JM (1991) A model for coupled fluid-flow and mixed-volatile mineral reactions with applications to regional metamorphism. Contrib Miner Petrol 106:273–286
Beach A (1976) The interrelation of fluid transport, deformation, geochemistry, and heat flow in early proterozoic shear zones in the Lewisian complex. Phil Trans Roy Soc Lond A280:596–604
Beach A (1977) Vein arrays, hydraulic fractures and pressure-solution structures in a deformed flysch sequence. S.W. England. Tectonophysics 40:201–226
Beach A (1980) Retrograde metamorphic process in shear zones with special reference to the Lewisian complex. J Struct Geol 2:257–263
Bear J (1972) Dynamics of fluids in porous media. Dover, New York
Beinlich A, Austrheim H, Glodny J, Erambert M, Anderson TB (2010) CO2 sequestration and extreme Mg depletion in serpentinized peridotite clasts from the Devonian Soland basin, SW-Norway. Geochim Cosmo Acta 74:6935–6994
Bell TH (1981) Foliation development – the contribution, geochemistry and significance of progressive bulk inhomogeneous shortening. Tectonophysics 75:273–296
Bell TH (1986) Foliation development and refraction in metamorphic rocks: reactivation of earlier foliations and decrenulation due to shifting patterns of deformation partitioning. J Metam Geol 4:421–444
Bertelli M, Baker T (2010) A fluid inclusion study of the suicide ridge breccia pipe, Cloncurry District, Australia: implications for breccia genesis and IOCG mineralization. Precamb Res 179:69–87
Bibby HM, Caldwell TG, Davey FJ, Webb TH (1995) Geophysical evidence on the structure of the Taupo volcanic zone and its hydrothermal circulation. J Volcan Geotherm Res 68:29–58
Bickle MJ (1992) Transport mechanisms by fluid-flow in metamorphic rocks: oxygen and strontium decoupling in the Trois Seigneurs massif – a consequence of kinetic dispersion? Am J Sci 292:289–316
Bickle MJ, Baker J (1990) Advective-diffusive transport of isotopic fronts: an example from Naxos, Greece. Earth Planet Sci Lett 97:78–93
Bickle MJ, McKenzie D (1987) The transport of heat and matter by fluids during metamorphism. Contrib Miner Petrol 95:384–392
Bjorlykke K (1997) Lithological control on fluid flow in sedimentary basins. In: Jamveit B, Yardley BWD (eds) Fluid flow and transport in rocks, mechanisms and effects. Chapman & Hall, London, pp 15–34
Bjorlykke K (1994) Fluid flow processes and diagenesis in sedimentary basins. In: Parnell J (ed) Geofluids: origin, migration and evolution of fluids in sedimentary Basins, vol 78, Geological Society Special Publication. Geological Society, London, pp 127–140
Boles JR (1982) Active albitization of plagioclase, Gulf Coast tertiary. Am J Sci 282:165–180
Brace WF (1980) Permeability of crystalline and argillaceous rocks. Int J Rock Mech Miner Sci 17:241–251
Breeding CM, Ague JJ (2002) Slab-derived fluids and quartz-vein formation in an accretionary prism, Otago Schist, New Zealand. Geology 30:499–502
Brimhall GH (1979) Lithologic determination of mass transfer mechanisms of multiple-stage porphyry copper mineralization at Butte, Montana: vein formation by hypergene leaching and enrichment of the potassium silicate protolith. Econ Geol 74:556–589
Cartwright I (1994) The two dimensional pattern of metamorphic fluid flow at Mary Kathleen, Australia: fluid focusing, transverse dispersion, and implications for modeling fluid flow. Am Miner 79:526–535
Cartwright I (1997) Permeability generation and resetting of traces during metamorphic fluid flow: implications for advection-dispersion models. Contrib Miner Petrol 129:198–208
Cartwright I, Buick IS (1995) Formation of wollastonite-bearing marbles during late regional metamorphic channeled fluid flow in the upper calcsilicate unit of the Reynolds range group, central Australia. J Metam Geol 13:397–417
Cartwright I, Oliver NHS (1994) Fluid flow during contact metamorphism at Mary Kathleen, Queensland, Australia. J Petrol 35:1493–1519
Cartwright I, Weaver TR (1993) Fluid-rock interaction between syenites and marbles at Stephen cross quarry, Quebec, Canada: petrological and stable isotope data. Contrib Miner Petrol 113:533–544
Cathles LM (1990) Scales and effects of fluid flow in the upper crust. Science 248:323–328
Chapin CE, Lindley JI (1986) Potassium metasomatism of igneous and sedimentary rocks in detachment terranes and other sedimentary basins: economic implications. Arizona Geol Soc Dig 16:118–126
Clark C, Hand M, Faure K, Schmid Mumm A (2006) Up-temperature flow of surface derived fluids in the mid crust: the role of pre-orogenic burial of hydrated fault rocks. J Metam Geol 24:367–387
Connolly JAD (2010) The mechanics of metamorphic fluid expulsion. Elements 6:165–172
Cook SJ, Bowman JR (2000) Mineralogical evidence for fluid-rock interaction accompanying prograde contact metamorphism of siliceous dolomites: Alta Stock, Utah, USA. J Petrol 41:739–757
Cook SJ, Bowman JR, Foster CB (1997) Contact metamorphism surrounding the Alta Stock: finite element model simulation of heat- and 18O16O mass-transport during prograde metamorphism. Amer J Sci 297:1–55
Cox SC (1993) Veins, fluids, fractals, scale and schist- an investigation of fluid-rock interaction during deformation of the Torlesse Terrane, New Zealand. Ph.D. thesis, University of Otago, Dunedin
Cox SF, Etheridge MA (1989) Coupled grain-scale dilatancy and mass transfer during deformation at high fluid pressure: examples from Mount Lyell, Tasmania. J Struct Geol 11:147–162
Cox SF, Wall VJ, Etheridge MA, Potter TF (1991) Deformation and metamorphic processes in the formation of mesothermal vein-hosted gold deposits – examples from the Lachlan Fold Belt in central Victoria, Australia. Ore Geol Rev 6:391–423
Davidson GJ (1999) Feldspar metasomatism along a Proterozoic rift-basin margin- “Smoke” around a base-metal “fire” (HYC deposit, Australia) or a product of background diagenesis? Geol Soc Am Bull 111:663–673
de Jong G, Williams PJ (1995) Giant metasomatic system formed during exhumation of mid-crustal Proterozoic rocks in the vicinity of the Cloncurry Fault, northwest Queensland. Aust J Earth Sci 42:281–290
Dipple GM, Ferry JM (1990) Identification of the scales of differential element mobility in a ductile fault zone. J Metam Geol 8:645–651
Dipple GM, Ferry JM (1992) Fluid flow and stable isotope alteration in rocks at elevated temperatures with applications to metamorphism. Geochim Cosmo Acta 56:3539–3550
Einaudi M, Meinert LD, Newberry RJ (1981) Skarn deposits. In: Economic geology 75th anniversary, El Paso, pp 317–391 (referred to also top of page 11, so should remain)
Engvik AK, Putnis A, Fitzgerald JD, Austrheim H (2008) Albitization of granitic rocks: the mechanism of replacement of oligoclase by albite. Can Miner 46:1401–1415
Engvik AK, Mezger K, Wortelkamp S, Bast R, Corfu F, Korneliussen A, Ihlen P, Bingen B, Austrheim H (2011) Metasomatism of gabbro – mineral replacement and element mobilization during the Sveconorwegian metamorphic event. J Metam Geol 29:399–423
Ennis DJ, Dunbar NW, Campbell AR, Chapin CE (2000) The effects of K-metasomatism on the mineralogy and geochemistry of silicic ignimbrites near Socorro, New Mexico. Chem Geol 167:285–312
Etheridge MA, Wall VJ, Vernon RH (1983) The role of the fluid phase during regional metamorphism and deformation. J Metam Geol 1:205–226
Etheridge MA, Wall VJ, Cox SF, Vernon RH (1984) High fluid pressures during regional metamorphism and deformation. J Geophys Res 89:4344–4358
Fedo CM, Young GM, Nesbitt HW, Hanchar JM (1997) Potassic and sodic metasomatism in the southern province of the Canadian shield: evidence from the paleoproterozoic serpent formation, Huronian Supergroup, Canada. Precamb Res 84:17–36
Ferry JM (1983) On the control of temperature, fluid composition, and reaction progress during metamorphism. Am J Sci 283A:201–232
Ferry JM (1986) Reaction progress: a monitor of fluid-rock interaction during metamorphic and hydrothermal events. In: Walther JV, Woods BJ (eds) Fluid-Rock interactions during metamorphism. Springer, New York, pp 60–88
Ferry JM (1984) A biotite isograd in south-central Maine, U.S.A.: mineral reactions, fluid transfer, and heat transfer. J Petrol 25:871–893
Ferry JM (1987) Metamorphic hydrology at 13 km depth and 400–500°C. Am Miner 72:39–58
Ferry JM (1992) Regional metamorphism of the waits river formation, eastern Vermont. Delineation of a new type of giant metamorphic hydrothermal system. J Petrol 33:45–94
Ferry JM (1994a) A historical review of metamorphic fluid flow. J Geophys Res 99:15487–15498
Ferry JM (1994b) Overview of the petrologic record of fluid flow during regional metamorphism in northern New England. Am J Sci 294:905–988
Ferry JM (1996) Prograde-retrograde fluid flow during contact metamorphism of siliceous carbonate rocks from the Ballachulish aureole, Scotland. Contrib Miner petrol 24:235–254
Ferry JM (2007) The role of volatile transport by diffusion and dispersion in driving biotite-forming reactions during regional metamorphism of the Gile Formation, Vermont. Am Miner 92:1288–1302
Ferry JM, Dipple GM (1991) Fluid flow, mineral reactions and metasomatism. Geology 19:211–214
Ferry JM, Dipple GM (1992) Models for coupled fluid flow, mineral reaction, and isotopic alteration during contact metamorphism: the Notch Peak aureole, Utah. Am Miner 77:577–591
Ferry JM, Gerdes M (1998) Chemically reactive fluid flow during metamorphism. Ann Rev Earth Planet Sci 26:255–287
Ferry JM, Gottschalk M (2009) The effect of fluid salinity on infiltration-driven contact metamorphism of carbonate rocks. Contrib Miner Petrol 158:619–636
Ferry JM, Rumble D III (1997) Formation and destruction of periclase by fluid flow in two contact aureoles. Contrib Miner Petrol 130:313–334
Ferry JM, Rumble DIII, Wing BA, Penniston-Dorland SC (2005) A new interpretation of centimeter-scale variations in the progress of infiltration-driven metamorphic reactions: case study of carbonated metaperidotite, Val d’Efra, Central Alps Switzerland. J Petrol 46:1725–1746
Ferry JM, Wing BA, Penniston-Dorland SC, Rumble D III (2002) The direction of fluid flow during the contact metamorphism of siliceous carbonate rocks: new data for the Monzoni and Predazzo aureoles, northern Italy, and a global review. Contrib Miner Petrol 142:679–699
Fletcher RC, Hoffman AW (1974) Simple models of diffusion and combined diffusion-infiltration metasomatism. In: Hoffman AW, Giletti B, Yoder HS Jr, Yund RA (eds) Geochemical transport and kinetics. Carnegie Institute of Washington, Washington, pp 242–262
Fyfe WS, Kerrich R (1985) Fluids and thrusting. Chem Geol 49:353–362
Fyfe WS, Price NJ, Thompson AB (1978) Fluids in the Earth’s crust. Elsevier, Amsterdam
Garven G (1985) The role of regional fluid flow in the genesis of the pine point deposit, Western Canada sedimentary basin. Econ Geol 80:307–324
Garven G (1995) Continental-scale groundwater flow and geologic processes. Ann Rev Earth Planet Sci 23:89–117
Gerdes ML, Valley JW (1994) Fluid flow and mass transport at the Valentine wollastonite mine, Adirondack Mountains, New York. J Metam Geol 12:589–608
Graham CM, Valley JW, Eiler JM, Wada H (1998) Timescales and mechanisms of fluid infiltration in a marble: an ion microprobe study. Contrib Miner Petrol 132:371–389
Gray DR (1997) Volume loss and slaty cleavage development. In: Sengupta S (ed) Evolution of geological structures in micro- to macro-scales. Chapman Hall, London, pp 273–291
Hanson RB (1992) Effects of fluid production on fluid flow during regional and contact metamorphism. J Metam Geol 10:87–97
Hitzman NW, Oreskes N, Carlson WD (1992) Geological characteristics and tectonic setting of proterozoic iron oxide (Cu-Au-U-REE) deposits. Precamb Res 58:241–287
Holness MB (2003) Growth and albitization of K-feldspar in crystalline rocks in the shallow crust: a tracer for fluid circulation during exhumation. Geofluids 3:89–102
Holness MB, Graham CM (1991) Equilibrium dihedral angles in the system H2O-CO2-NaCl-calcite, and implications for fluid flow during metamorphism. Contrib Miner Petrol 119:301–313
Huang W, Rubenach MJ (1995) Structural controls on syn-tectonic metasomatic tremolite and tremolite-plagioclase pods in the Molanite Valley, Mt. Isa, Australia. J Struct Geol 17:83–94
Jamtveit B, Bucher-Nurminen K, Stijfhoon DE (1992a) Contact metamorphism of layered shale-carbonate sequences in the Oslo rift: I. Buffering, infiltration and the mechanism of mass transport. J Petrol 33:377–422
Jamtveit B, Grorud HF, Bucher-Nurminen K (1992b) Contact metamorphism of layered shale-carbonate sequences in the Oslo rift: II. Migration of isotopic and reaction fronts around cooling plutons. Earth Planet Sci Let 114:131–148
Jamtveit B, Yardley BWD (1997) Fluid flow and transport in rocks, mechanisms and effects. Chapman & Hall, London
Kendrick MA, Baker T, Fu B, Phillips D, Williams PJ (2008) Noble gas and halogen constraints on regionally extensive mid-crustal Na-Ca metasomatism, the Proterozoic Eastern Mount Isa Block, Australia. Precamb Res 163:131–150
Kent AJR, Ashley PM, Fanning CM (2000) Metasomatic alteration associated with regional metamorphism: an example from the Willyama Supergroup, South Australia. Lithos 54:33–62
Korzhinskii DS (1950) Phase rule and geochemical mobility of elements. In: Eighteenth international geological congress, Part 2 Sect. A, London, pp 50–57
Korzhinskii DS (1959) Physicochemical basis of the analysis of the paragenesis of minerals. Consultants Bureau, New York
Korzhinskii DS (1970) The theory of metasomatic zoning. Clarendon, Oxford
Kwak TAP (1978) Mass balance relationships and skarn forming processes at the King Island scheelite deposit, Tasmania, Australia. Am J Sci 278:943–968
Kwak TAP, Askins PW (1981a) The nomenclature of carbonate replacement deposits, with emphasis on Sn-F (Be-Zn) ‘wrigglite’ skarns. Geol Soc Aust J 28:123–136
Kwak TAP, Askins PW (1981b) The geology and genesis of laminar F-Sn-W (-Be-Zn) skarns at Moina, Tasmania, Australia. Econ Geol 76:439–467
Labotka TC, Nabelek PI, Papike JJ (1988) Fluid infiltration through the big horse limestone member in the Notch Peak contact-metamorphic aureole, Utah. Amer Miner 73:1302–1324
Lee JI, Lee YI (1998) Feldspar albitization in Cretaceous non-marine mudrocks, Gyeongsang Basin, Korea. Sedimentology 45:1959–1981
Lentz DR (1998) Mineralized intrusion-related skarn systems, vol 26, Min Soc Canada Short Course Series. Mineralogical Association of Canada, Ottawa, p 66
Lonker SW, Fitzgerald JD, Hedenquist JW, Walshe JL (1990) Mineral-fluid interactions in the Broadlands-Ohaaki geothermal system, New Zealand. Am J Sci 290:995–1068
Lyubetskaya T, Ague JJ (2010) Modeling metamorphism in collisional orogens intruded by magmas: II. Fluid flow and implications for Barrovian and Buchan metamorphism, Scotland. Am J Sci 310:459–491
Mark G, Oliver NHS, Williams PJ (2006) Mineralogical and chemical evolution of the Ernest Henry Fe oxide-Cu-Au ore system, Cloncurry district, northwest Queensland. Miner Deposita 40:769–801
Marshall LJ, Oliver NHS (2008) Constraints on the hydrothermal pathways within Mary Kathleen Group stratigraphy of the Cloncurry iron-oxide-copper-gold District, Australia. Precamb Res 163:151–158
Masters RL, Ague JJ (2005) Regional-scale fluid flow and element mobility in Barrow’s metamorphic zones, Stonehaven, Scotland. Contrib Miner Petrol 97:1–18
McCaig AM (1997) The geochemistry of volatile fluid flow in shear zones. In: Holness MB (ed) Deformation-enhanced fluid transport in the earth’s crust and mantle. Chapman and Hall, London, pp 227–266
McLellan JG, Oliver NHS (2008) Application of numerical modeling to extension, heat and fluid flow in the genesis of giant banded iron formation-hosted hematite ore deposits. Soc Econ Geol Rev 15:185–196
Meinert LD, Dipple GM, Nicolescu S (2005) World skarn deposits. In: Hedenquist JW, Thompson JFH, Goldfarb RJ, Richards JPC (eds) Economic geology 100th anniversary volume. Soc Econ Geol, Littleton, pp 299–336
Mottl MJ (1983) Metabasalts, axial hot springs, and the structure of hydrothermal systems at mid-ocean ridges. Bull Geol Soc Am 94:161–180
Nabelek PI (1991) Stable isotope monitors. In: Kerrick DM (ed) Contact metamorphism, vol 26, Reviews in Mineralogy. Mineralogical Society of America, Washington, DC, pp 395–435
Nabelek PI, Labotka TC (1993) Implications of geochemical fronts in the Notch Peak contact aureole, Utah, USA. Earth Planet Sci Lett 119:539–559
Nabelek PI, Labotka TC, O’Neil JR, Papike JJ (1984) Contrasting fluid/rock interaction between the Notch Peak granitic intrusion and argillites and limestones in western Utah: evidence from stable isotopes and phase assemblages. Contrib Miner Petrol 86:25–34
Norton DL (1988) Metasomatism and permeability. Am J Sci 288:604–618
Oliver NHS (1995) Hydrothermal history of the Mary Kathleen Fold Belt, Mt Isa Block, Queensland. Aust J Earth Sci 42:267–280
Oliver NHS (1996) Review and classification of structural controls on fluid flow during regional metamorphism. J Metam Geol 14:477–492
Oliver NHS, Bons PD (2001) Mechanisms of fluid flow and fluid-rock interaction in fossil metamorphic hydrothermal systems inferred from vein-wall rock patterns, geometry and microstructure. Geofluids 1:137–162
Oliver NHS, Butera K, Rubenach MJ, Marshall LJ, Cleverley JS, Mark G, Fu B, Tullemans F, Esser D (2008) The protracted hydrothermal evolution of the Mount Isa eastern succession: a review and tectonic implications. Precamb Res 163:108–130
Oliver NHS, Cleverley JS, Mark G, Pollard PJ, Fu B, Marshall LJ, Rubenach MJ, Williams PJ, Baker T (2004) Modeling the roll of sodic alteration in the genesis of iron oxide-copper-gold deposits, eastern Mount Isa Block, Australia. Econ Geol 99:1145–1176
Oliver NHS, Pearson PJ, Holcombe RJ, Ord A (1999) Mary Kathleen metamorphic-hydrothermal uranium-rare earth deposit: ore genesis and a numerical model of coupled deformation and fluid flow. Aust J Earth Sci 46:467–484
Oliver NHS, Rubenach MJ, Fu B, Baker T, Blenkinsop TG, Cleverley JS, Marshall LJ, Ridd PJ (2006) Granite-related overpressure and volatile release in the mid crust: fluidized breccias from the Cloncurry district, Australia. Geofluids 6:346–358
Oliver NHS, Valenta RK, Wall VJ (1990) The effect of heterogeneous stress and strain on metamorphic fluid flow, Mary Kathleen, Australia, and a model for large-scale fluid circulation. J Metam Geol 8:311–331
Parnell J (1994) Geofluids: origin, migration and evolution of fluids in sedimentary Basins, vol 78, Geological Society Special Publication. Geological Society, London
Penniston-Dorland SC, Ferry JM (2006) Development of spatial variations in reaction progress during regional metamorphism of micaceous carbonate rocks, northern New England. Am J Sci 306:475–524
Penniston-Dorland SC, Ferry JM (2008) Element mobility and scale of mass transport in the formation of quartz veins during regional metamorphism of the waits river formation, east-central Vermont. Am Miner 93:7–21
Person M, Garven G (1994) A sensitivity study of the driving forces on fluid flow during continental-rift basin evolution. Geol Soc Am Bull 106:461–475
Pettijohn FJ, Baston H (1959) Chemical composition of argillites of the Cobalt Series (Precambrian) and the problem of soda-rich sediments. Geol Soc Am Bull 70:593–599
Polito PA, Kyser TK, Southgate PN, Jackson MJ (2006) Sandstone diagenesis in the Mount Isa Basin: an isotopic and fluid inclusion perspective in relationship to district-wide Zn, Pb and Cu mineralization. Econ Geol 101:1159–1185
Putnis A, Austrheim H (2010) Fluid-induced processes: metasomatism and metamorphism. Geofluids 10:254–269
Qiu L, Rudnick RL, Ague JJ, McDonough WF (2011) A lithium isotope study of sub-greenschist-facies metamorphism in an accretionary prism, New Zealand. Earth Planet Sci Let 301:213–221
Roselle GT, Baumgartner LP, Valley JW (1999) Stable isotope evidence of heterogeneous fluid infiltration at the Ubhebe Peak contact aureole, Death Valley national park, California. Am J Sci 299:93–138
Rowland JV, Sibson RH (2004) Structural controls on hydrothermal flow in a segmented rift system, Taupo Volcanic Zone, New Zealand. Geofluids 4:259–283
Rubenach MJ (1992) Proterozoic low pressure/high temperature metamorphism and an anticlockwise P-T-t path for the Hazeldene area, Mount Isa Inlier, Queensland. Aust J Metam Geol 10:333–346
Rubenach MJ (2005) Relative timing of albitization and chlorine enrichment in biotite in Proterozoic schists, Snake Creek Anticline, Mount Isa Inlier, northeastern Australia. Canad Miner 43:349–72
Rubenach MJ, Barker AJ (1998) Metamorphic and metasomatic evolution of the Snake Creek Anticline, eastern succession, Mount Isa Inlier. Aust J Earth Sci 45:363–372
Rubenach MJ, Foster DRW, Evins PM, Blake KL, Fanning CM (2008) Age constraints on the tectonothermal evolution of the Selwyn Zone, Eastern Fold Belt, Mount Isa Inlier. Precamb Res 163:81–107
Rubenach MJ, Lewthwaite KA (2002) Metasomatic albitites and related biotite-rich schists from a low-pressure metamorphic terrane, Snake Creek Anticline, Mount Isa Inlier, north-eastern Australia: microstructures and P-T-d paths. J Metam Geol 20:191–202
Rumble DIII (1994) Water circulation in metamorphism. J Geophys Res 99:15499–15502
Scholle PA, Ulmer-Scholle DS (2003) A color guide to the petrography of carbonate rocks: grains, textures, porosity, diagenesis, vol 77, American Association of Petroleum Geologists Memoir. American Association of Petroleum Geologists, Tulsa
Sibson RH (1987) Earthquake rupturing as a mineralizing agent in hydrothermal systems. Geology 15:701–704
Sibson RH (1989) Earthquake faulting as a structural process. J Struct Geol 11:1–14
Skelton ADL, Graham CM, Bickle MJ (1995) Lithological and structural controls on regional 3-D fluid flow patterns during greenschist-facies metamorphism of the Dalradian of the SW Scottish Highlands. J Petrol 36:563–586
Skelton ADL, Valley JW, Graham CM (2000) The correlation of reaction and isotopic fronts and the mechanism of metamorphic fluid flow. Contrib Miner Petrol 138:364–375
Steiner A (1977) The Waiakei geothermal area, North Island, New Zealand. New Zeal Geol Surv Bull 90:136
Streit JE, Cox SF (1998) Fluid infiltration and volume change during mid-crustal mylonitization of Proterozoic granite, King Island, Tasmania. J Metam Geol 16:197–212
Upton P, Craw D (2009) Mechanisms of strain-rate-and reaction-dependent permeability in the mid-crust of the Southern Alps: insight from three-dimensional mechanical models. Geofluids 9:287–302
Vernon RH (1998) Chemical and volume changes during deformation and prograde metamorphism of sediments. In: Treloar PJ, O’Brien P (eds) What drives metamorphism and metamorphic reactions? vol 138, Geological society London special publication. Geological Society, London, pp 215–246
Vernon RH, Clarke GL (2008) Principles of metamorphic geology. Cambridge University Press, New York
Vidale R (1969) Metasomatism in a chemical gradient and the formation of calc-silicate bands. Am J Sci 267:857–874
Vidale R, Hewitt DA (1973) “Mobile” components in the formation of calc-silicate bands. Am Miner 58:91–97
Williams PJ (1998) Metalliferous economic geology of the Mount Isa eastern succession, Queensland. Aust J Earth Sci 45:329–342
Wing BA, Ferry JM (2002) Three-dimensional geometry of metamorphic fluid flow during Barrovian regional metamorphism from an inversion of combined petrologic and stable isotope data. Geology 30:639–642
Wing BA, Ferry JM (2007) Magnitude and geometry of reactive fluid flow from direct inversion of spatial patterns of geochemical alteration. Am J Sci 307:793–832
Wood BW, Walther JV (1986) Fluid flow during metamorphism and its implications for fluid-rock ratios. In: Walther JV, Wood BJ (eds) Fluid-Rock interactions during metamorphism. Springer, New York, pp 89–108
Yardley BWD (1986) Fluid migration and veining in the Connemara Schists, Ireland. In: Walther JV, Wood BJ (eds) Fluid-rock interaction during metamorphism. Springer, New York, pp 109–131
Yardley BWD (2009) The role of water in the evolution of the continental crust. J Geol Soc Lond 166:585–600
Yardley BWD, Bottrell SH (1992) Silica mobility and fluid movement during metamorphism of the Connemara schists, Ireland. J Metam Geol 10:453–464
Yardley BWD, Lloyd GE (1995) Why metasomatic fronts are metasomatic sides. Geology 23:53–56
Acknowledgments
The author has spent over 38 years at James Cook University researching metamorphic and metasomatic rocks of north Queensland, and colleagues T. Bell, T. Blenkinsop, D. Foster, W. Laing, N. Oliver, and P. Williams are particularly thanked for numerous discussions, especially on field trips. J. Ague, J. Ferry and B. Yardley provided very helpful reviews and suggestions. The editors, D. Harlov and H. Austrheim are thanked for their help and patience.
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Rubenach, M. (2013). Structural Controls of Metasomatism on a Regional Scale. In: Metasomatism and the Chemical Transformation of Rock. Lecture Notes in Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-28394-9_4
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DOI: https://doi.org/10.1007/978-3-642-28394-9_4
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