Abstract
Observations in the S-type granites (s.l.) of the Wilson’s Promontory batholith demonstrate that one type of schlieren in granitic rocks represent accumulations of mainly mafic magmatic minerals, with internal layering formed through pulsed magma flow. Loss of interstitial magmatic liquid played, at most, a minor role in shaping the preserved compositions of the schlieren; filter pressing was not involved, and simple gravity settling of crystals was also insignificant. Through dissolution-reprecipitation and reactions with residual magmatic liquids in the Wilsons Promontory schlieren, the original accumulated crystals of mafic minerals were largely supplanted by later generations or completely new phases. In the present case, the original accumulating minerals were garnet and orthopyroxene, with minor biotite and accessory minerals. The schlieren retain some of the early, euhedral, compositionally distinct, accumulated biotite, but most biotite formed through reaction of accumulated orthopyroxene and garnet with residual liquid. Some early, accumulated garnet remains, but this is not the peritectic garnet that was originally entrained into the magmas, at source depths. Rather, these are magmatic crystals formed, at mid-crustal depths, through dissolution–reprecipitation of the original peritectic garnet. At emplacement level, another episode of garnet dissolution–reprecipitation occurred, close to the solidus, extensively reorganising the grain-scale igneous textures. Although schlieren preserve structural, chemical and some textural features that can be used to infer their origins, their present microtextures do not fully reflect their initial formation mechanisms. Also, the physical mechanisms of schlieren formation most commonly have little similarity with the processes that were responsible for the main chemical variations in the batholith. Nevertheless, the presence of schlieren indicates that the granitic magmas were flowing in sheet-like laminae, and they provide information on the high-temperature igneous minerals that were suspended in their parent magmas, prior to emplacement.
Similar content being viewed by others
References
Alasino PH, Ardill K, Stanback J, Paterson SR, Galindo G, Leopold M (2019) Magmatically folded and faulted schlieren zones formed by magma avalanching in the Sonora Pass Intrusive Suite, Sierra Nevada, California. Geosphere 15, Doi: 10.1130/GES02070.1
Barbey P (2009) Layering and schlieren in granitoids: a record of interactions between magma emplacement, crystallization and deformation in growing plutons (The André Dumont Medallist Lecture). Geol Belg 12:109–133
Barrière M (1981) On curved laminae, graded layers, convection currents and dynamic crystal sorting in the Ploumanac’h (Brittany) subalkaline granite. Contrib Min Petrol 77:214–224. https://doi.org/10.1007/BF00373537
Bhattacharji S, Smith CH (1964) Flowage differentiation. Science 145:150–153. https://doi.org/10.1126/science.145.3628.150
Burgess SD, Miller JS (2008) Construction, solidification and internal differentiation of a large felsic arc pluton: cathedral Peak granodiorite, Sierra Nevada Batholith. In: Annen C, Zellmer GF (eds) Dynamics of crustal magma transfer, storage and differentiation. Geological Society, London, Special Publications, 304. pp 203–234
Clarke DB (1981) The mineralogy of peraluminous granites: a review. Can Mineral 19:3–18
Clemens JD (1981) Origin and Evolution of Some Peraluminous Acid Magmas. PhD (unpubl.) thesis, Monash University, Australia, 577 pp
Clemens JD (2015) Forum comment: magmatic life at low reynolds number. Geology 43:E357–E357. https://doi.org/10.1130/G36512C.1
Clemens JD, Bezuidenhout A (2014) Origins of co-existing diverse magmas in a felsic intrusion: the Lysterfield Granodiorite, Australia. Contrib Min Petrol 167:197–212. https://doi.org/10.1007/s00410-014-0991-9
Clemens JD, Helps PA, Stevens G (2009) Chemical structure in granitic magmas—a signal from the source? Earth Env Sci Trans R Soc Edinburgh 100:159–172. https://doi.org/10.1017/s1755691009016053
Clemens JD, Maas R, Waight TE, Kunneke LK (2016) Genesis of felsic plutonic magmas and their igneous enclaves: the Cobaw batholith of SE Australia. J Geol 124:293–311. https://doi.org/10.1086/685509
Clemens JD, Mawer CK (1992) Granitic magma transport by fracture propagation. Tectonophysics 204:339–360. https://doi.org/10.1016/0040-1951(92)90316-X
Clemens JD, Petford N (1999) Granitic melt viscosity and silicic magma dynamics in contrasting tectonic settings. J Geol Soc London 156:1057–1060. https://doi.org/10.1144/gsjgs.156.6.1057
Clemens JD, Petford N, Mawer CK (1997) Ascent mechanisms of granitic magmas: causes and consequences. In: Holness M (ed) Deformation-enhanced fluid transport in the earth’s crust and mantle, Chapman & Hall, London, pp 144–171
Clemens JD, Stevens G (2012) What controls chemical variation in granitic magmas? Lithos 134–135:317–329. https://doi.org/10.1016/j.lithos.2012.01.001
Clemens JD, Stevens G, Elburg MA (2017) Petrogenetic processes in granitic magmas and their igneous microgranular enclaves from Central Victoria, Australia: match or mismatch? Trans R Soc S Af 72:6–32. https://doi.org/10.1080/0035919X.2016.1209702
Clemens JD, Wall VJ (1988) Controls on the mineralogy of S-type volcanic and plutonic rocks. Lithos 21:53–66. https://doi.org/10.1016/0024-4937(88)90005-9
Connolly JAD (2009) The geodynamic equation of state: what and how. Geochem Geophys Geosyst 10:Q10014. https://doi.org/10.1029/2009GC002540
Costa A, Caricchi L, Bagdassarov N (2009) A model for the rheology of particle-bearing suspensions and partially molten rocks. Geochem Geophy Geosyst 10:Q03010. https://doi.org/10.1029/2008GC002138
da Cunha FR, Hinch EJ (1996) Shear-induced dispersion in a dilute suspension of rough spheres. J Fluid Mech 309:211–223. https://doi.org/10.1017/S0022112096001619
du Plessis A, le Roux SG, Guelpa A (2016) The CT scanner facility at Stellenbosch University: an open access X-ray computed tomography laboratory. Nucl Instr Methods Phys Res Sect B 384:42–49. https://doi.org/10.1016/J.NIMB.2016.08.005
Ehlers C (1974) Layering in rapakivi granite, SW Finland. Bull Geol Soc Finland 46:145–149. https://doi.org/10.17741/bgsf/46.2.007
Emeleus CH (1963) Structural and petrographic observations on layered granites from Southern Greenland. Mineral Soc Am Special Paper 1:22–29
Fleet ME (2003) Micas. In: Fleet WE, Deer WA, Howie RA, Zussman J (eds) Rock-forming minerals, 3A, The Geological Society of London Publishing House, Bath
Gawęda A, Szopa K (2011) The origin of magmatic layering in the High Tatra granite, Central Western Carpathians—implications for the formation of granitoid plutons. Earth Env Sci Trans R Soc Edinburgh 102:1–16. https://doi.org/10.1017/S1755691012010146
Gilbert GK (1906) Gravitational assemblage in granite. Geol Soc Am Bull 17:321–328. https://doi.org/10.1130/GSAB-17-321
Glazner AF (2014) Magmatic life at low Reynolds number. Geology 42:935–938. https://doi.org/10.1130/G36078.1
Hirth G, Tullis J (1992) Dislocation creep regimes in quartz aggregates. J Struct Geol 14:145–159. https://doi.org/10.1016/0191-8141(92)90053-Y
Holland T, Powell R (1996) Thermodymanics of order–disorder in minerals: II. Symmetric formulism applied to solid solutions. Am Mineral 81:1425–1437. https://doi.org/10.2138/am-1996-11-1215
Holland TJB, Powell R (2003) Activity–composition relations for phases in petrological calculations: an asymmetric multicomponent formulation. Contrib Min Petrol 145:492–501. https://doi.org/10.1007/s00410-003-0464-z
Holland TJB, Powell R (2011) An improved and extended internally consistent thermodynamic dataset for phases of petrological interest, involving a new equation of state for solids. J Metamorphic Geol 29:333–383. https://doi.org/10.1111/j.1525-1314.2010.00923.x
Holness MB (2018) Melt segregation from silicic crystal mushes: a critical appraisal of possible mechanisms and their microstructural record. Contrib Min Petrol 173:48. https://doi.org/10.1007/s00410-018-1465-2
Jerram DA, Cheadle MJ, Philpotts AR (2003) Quantifying the building blocks of igneous rocks: Are clustered crystal frameworks the foundation? J Petrol 44:2033–2051. https://doi.org/10.1093/petrology/egg069
Leighton D, Acrivos A (1987) The shear-induced migration of particles in concentrated suspensions. J Fluid Mech 181:415–439. https://doi.org/10.1017/S0022112087002155
Marsh BD (1996) Solidification fronts and magmatic evolution. Mineralog Mag 60:5–40. https://doi.org/10.1180/minmag.1996.060.398.03
Mayne MJ, Moyen J-F, Stevens G, Kaislaniemi L (2016) Rcrust: a tool for calculating path-dependent open system processes and application to melt loss. J Metamorphic Geol 34:663–682. https://doi.org/10.1111/jmg.12199
Mayne MJ, Stevens G, Moyen J-F, Johnson T (2020) Performing process-oriented investigations involving mass transfer using Rcrust: a new phase equilibrium modelling tool. In: Janousek V, Bonin B, Collins WJ, Farina F, Bowden P (eds) Post-Archean granitic rocks: Petrogenetic processes and tectonic environments, Geological Society of London Special Publication 491. https://doi.org/10.1144/SP491-2018-85
McKenzie K, McCarthy W, Hunt E (2016) Development of modal layering in granites: a case study from the Carna Pluton, Connemara, Ireland. Geophys Res Abstr 18: EGU2016–6689–2011
Paterson SR (2009) Magmatic tubes, pipes, troughs, diapirs, and plumes: late-stage convective instabilities resulting in compositional diversity and permeable networks in crystal-rich magmas of the Tuolumne batholith, Sierra Nevada, California. Geosphere 5:496–527. https://doi.org/10.1130/GES00214.1
Paterson SR, Memeti V, Mundil R, Žák J (2016) Repeated, multiscale, magmatic erosion and recycling in an upper-crustal pluton: Implications for magma chamber dynamics and magma volume estimates. Am Min 101:2176–2198. https://doi.org/10.2138/am-2016-5576
Paterson SR, Žák J, Janoušek V (2008) Growth of complex magmatic zones during recycling of older magmatic phases: the Sawmill Canyon area in the Tuolumne Batholith, Sierra Nevada, California. J Volc Geotherm Res 177:457–484. https://doi.org/10.1016/j.jvolgeores.2008.06.024
Petford N (2003) Rheology of granitic magmas during ascent and emplacement. Annu Rev Earth Planet Sci 31:399–427. https://doi.org/10.1146/annurev.earth.31.100901.141352
Petford N (2009) Which effective viscosity? Mineralog Mag 73:167–191. https://doi.org/10.1180/minmag.2009.073.2.167
Petford N, Koenders MA, Clemens JD (2020) Igneous differentiation by deformation. Contrib Mineral Petrol 175(5):45. https://doi.org/10.1007/s00410-020-1674-3
Phillips GN, Clemens JD (2013) Strathbogie batholith: field-based subdivision of a large granitic intrusion. Appl Earth Sci 122:36–55. https://doi.org/10.1179/1743275813Y.0000000030
Pupier E, Barbey P, Toplis MJ, Bussy F (2008) Igneous layering, fractional crystallization and growth of granitic plutons: the Dolbel batholith in SW Niger. J Petrol 49:1043–1068. https://doi.org/10.1093/petrology/egn017
Ramphaka PL (2013) The origin of rhythmic magmatic layering in coarse-grained porphyritic S-type granite of the Peninsula pluton, Cape Granite Suite, South Africa. MSc thesis, Department of Earth Sciences, University of Stellenbosch, unpublished, 92 pp
Reid JB, Evans OC, Fates DG (1983) Magma mixing in granitic rocks of the central Sierra Nevada, California. Earth Planet Sci Lett 66:243–261. https://doi.org/10.1016/0012-821X(83)90139-5
Reid JB, Murray DP, Hermes OD, Steig EJ (1993) Fractional crystallization in granites of the Sierra Nevada: How important is it? Geology 21:587–590. https://doi.org/10.1130/0091-7613(1993)021%3c0587:FCIGOT %3e2.3.CO;2
Roberts MP, Pin C, Clemens JD, Pacquette JL (2000) Petrogenesis of mafic to felsic plutonic rock associations: the calc-alkaline querigut complex, French pyrenees. J Petrol 41:809–844. https://doi.org/10.1093/petrology/41.6.809
Schwindinger KR, Anderson ATJ (1989) Synneusis of Kilauea Iki olivines. Contrib Min Petrol 103:187–198. https://doi.org/10.1007/BF00378504
Solgadi F, Sawyer EW (2008) Formation of igneous layering in granodiorite by gravity flow: a field, microstructure and geochemical study of the Tuolumne Intrusive Suite at Sawmill Canyon, California. J Petrol 49:2009–2042. https://doi.org/10.1093/petrology/egn056
Vernon RH, Paterson SR (2008) Mesoscopic structures resulting from crystal accumulation and melt movement in granites. Trans R Soc Edinburgh: Earth Sci 97:369–381. https://doi.org/10.1017/S0263593300001516
Villaros A, Stevens G, Buick IS (2009) Tracking S-type granite from source to emplacement: clues from garnet in the Cape Granite Suite. Lithos 112:217–235. https://doi.org/10.1016/j.lithos.2009.02.011
Wallis GL, Clemens JD (2018) Geology and field relations of the Wilsons Promontory Batholith, Victoria: multiple, shallow-dipping, S-type, granitic sheets. Aust J Earth Sci 65:769–785. https://doi.org/10.1080/08120099.2018.1472142
Weinberg RF, Sial AN, Pessoa RR (2001) Magma flow within the Tavares pluton, northeastern Brazil: compositional and thermal convection. Geol Soc Am Bull 113:508–520. https://doi.org/10.1130/0016-7606(2001)113%3c0508:MFWTTP%3e2.0
White RW, Powell R, Clarke GL (2002) The interpretation of reaction textures in Fe-rich metapelitic granulites of the Musgrave Block, Central Australia: constraints from mineral equilibria calculations in the system. J Metamorphic Geol 20:41–55. https://doi.org/10.1046/j.0263-4929.2001.00349.x
White RW, Powell R, Holland TJB, Johnson TE, Green ECR (2014) New mineral activity-composition relations for thermodynamic calculations in metapelitic systems. J Metamorphic Geol 32:261–286. https://doi.org/10.1111/jmg.12071
White RW, Powell R, Holland TJB, Worley BA (2000) The effect of TiO2 and Fe2O3 on metapelitic assemblages at greenschist and amphibolite facies conditions: mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–Fe2O3. J Metamorphic Geol 18:497–511. https://doi.org/10.1046/j.1525-1314.2000.00269.x
Whitney DL, Evans BW (2010) Abbreviations for names of rock-forming minerals. Am Min 95:185–187. https://doi.org/10.2138/am.2010.3371
Wiebe RA, Collins WJ (1998) Depositional features and stratigraphic sections in granitic plutons: implications for the emplacement and crystallization of granitic magma. J Struct Geol 20:1273–1289. https://doi.org/10.1016/S0191-8141(98)00059-5
Žák J, Paterson SR, Janoušek V, Kabele P (2009) The Mammoth Peak sheeted complex, Tuolumne batholith, Sierra Nevada, California: a record of initial growth or late thermal contraction in a magma chamber? Contrib Min Petrol 158:447–470. https://doi.org/10.1007/s00410-009-0391-8
Acknowledgements
Scott Paterson supplied the photograph used as Fig. 1a. The CT scans used in this paper were generated at the CT Scanning laboratory of the Central Analytical Facility of Stellenbosch University, with funding supplied from the NRF SARChI Chair in Experimental Petrology, held by Gary Stevens. Points raised by two anonymous reviewers were helpful in focusing and refining various aspects of the manuscript.
Author information
Authors and Affiliations
Corresponding author
Additional information
Communicated by Timothy L. Grove.
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Electronic supplementary material
Below is the link to the electronic supplementary material.
Supplementary file3 (MP4 5059 kb)
Supplementary file4 (MP4 3988 kb)
Supplementary file5 (MP4 6313 kb)
Rights and permissions
About this article
Cite this article
Clemens, J.D., Stevens, G., le Roux, S. et al. Mafic schlieren, crystal accumulation and differentiation in granitic magmas: an integrated case study. Contrib Mineral Petrol 175, 51 (2020). https://doi.org/10.1007/s00410-020-01689-x
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00410-020-01689-x