Bubbles; CSD; Dacite; Enclaves; Santorini; Texture; Geophysics; Geochemistry and Petrology
Abstract :
[en] Dacite lavas erupted from Kameni Islands volcanic centre (Greece) during the last 2000 years have a limited range in chemical composition (SiO2 = 64.0–68.5%) which contrasts with their wide range in plagioclase abundance (3–22%) and crystal size distributions. Most plagioclase crystals have simple zoning and occur independently or in loose clusters with finer-grained cores. We propose that magmatic diversity was produced by the interaction between crystals that formed at the base of a magma reservoir and bubbles produced by injection and vesiculation of more mafic magma. Two end-member situations can be identified: in juvenile systems, the basal crystal mass is loosely connected and readily disrupted by bubble formation. The crystal–bubble couples accumulate at the top of the reservoir, from where they can enter the sub-volcanic plumbing system to produce high-crystal content, chemically unevolved magmas. In the mature system, the crystal mass is well connected so bubbles displace the evolved, interstitial magma and liberate only a smaller number of crystals from the crystal mass. This process produces chemically evolved magmas, with lower crystal contents. The oldest lavas seem to have been produced from mature systems, whereas the youngest eruptions were of lavas produced from juvenile systems. This progression may reflect an overall reduction in repose times during the last 2000 years.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Higgins, Michael D. ; Sciences Appliquées, Université du Québec à Chicoutimi, Québec, Canada
Debecq, Anouk; Université Libre de Bruxelles, Bruxelles, Belgium
Vander Auwera, Jacqueline ; Université de Liège - ULiège > Département de géologie > Pétrologie, géochimie endogènes et pétrophysique
Nomikou, Paraskevi; National and Kapodistrian University of Athens, Athens, Greece
Language :
English
Title :
Chemical and textural diversity of Kameni (Greece) dacites: role of vesiculation in juvenile and mature basal crystal masses
Publication date :
February 2021
Journal title :
Contributions to Mineralogy and Petrology
ISSN :
0010-7999
eISSN :
1432-0967
Publisher :
Springer Science and Business Media Deutschland GmbH
Barton M, Huijsmans JPP (1986) Post-caldera dacites from the Santorini volcanic complex, Aegean sea, Greece: an example of the eruption of lavas of near-constant composition over a 2,200 year period. Contrib Miner Petrol 94:472–495. 10.1007/BF00376340 DOI: 10.1007/BF00376340
Boudreau A (2016) Bubble migration in a compacting crystal-liquid mush. Contrib Miner Petrol 171(4):32. 10.1007/s00410-016-1237-9 DOI: 10.1007/s00410-016-1237-9
Cashman KV (1993) Relationship between plagioclase crystallisation and cooling rate in basaltic melts. Contrib Miner Petrol 113:126–142. 10.1007/BF00320836 DOI: 10.1007/BF00320836
Cashman KV, Marsh BD (1988) Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallisation II. Makaopuhi lava lake. Contrib Miner Petrol 99:292–305. 10.1007/BF00375363 DOI: 10.1007/BF00375363
Druitt TH, Edwards L, Mellors RM, Pyle D, Sparks RSJ, Lanphere M, Davies M, Barreirio B (1999a) Santorini volcano. In: Memoir vol. 19. Geological Society, London, p 176
Druitt TH, McCoy FW, Vougioukalakis GE (2019a) The Late Bronze Age eruption of Santorini volcano and Its impact on the ancient Mediterranean world. Elements 15(3):185–190. 10.2138/gselements.15.3.185 DOI: 10.2138/gselements.15.3.185
Druitt TH, Pyle DM, Mather TA (2019b) Santorini volcano and its plumbing system. Elements 15(3):177–184. 10.2138/gselements.15.3.177 DOI: 10.2138/gselements.15.3.177
Fornaciai A, Perinelli C, Armienti P, Favalli M (2015) Crystal size distributions of plagioclase in lavas from the July–August 2001 Mount Etna eruption. Bull Volcanol 77(8):1–15. 10.1007/s00445-015-0953-8 DOI: 10.1007/s00445-015-0953-8
Francalanci L, Vougioukalakis G, Eleftheriadis G, Pinarelli L, Petrone C, Manetti P, Christofides G (1998) Petrographic, chemical and isotope variations in the intracaldera post-Minoan rocks of the Santorini volcanic field, Greece. In: Casale R (ed) Proceedings of the second workshop, Santorini, Greece, pp 175–186
Götze J, Schertl H-P, Neuser RD, Kempe U, Hanchar JM (2012) Optical microscope-cathodoluminescence (OM–CL) imaging as a powerful tool to reveal internal textures of minerals. Mineral Petrol 107(3):373–392. 10.1007/s00710-012-0256-0 DOI: 10.1007/s00710-012-0256-0
Helz RT (1987) Differentiation behavior of Kilauea Iki lava lake, Kilauea Volcano, Hawaii; an overview of past and current work. Magmatic processes; physicochemical principles; a volume in honor of Hatten S Yoder, Jr, vol 1. Geochemical Society, Dayton, Ohio, pp 241–258
Higgins MD (1996a) Crystal size distributions and other quantitative textural measurements in lavas and tuff from Mt Taranaki (Egmont volcano), New Zealand. Bull Volcanol 58:194–204 DOI: 10.1007/s004450050135
Higgins MD (1996b) Magma dynamics beneath Kameni volcano, Thera, Greece, as revealed by crystal size and shape measurements. J Volcanol Geoth Res 70(1–2):37–48. 10.1016/0377-0273(95)00045-3 DOI: 10.1016/0377-0273(95)00045-3
Higgins MD (2000) Measurement of crystal size distributions. Am Mineral 85(9):1105–1116. 10.2138/am-2000-8-901 DOI: 10.2138/am-2000-8-901
Higgins MD (2006) Quantitative textural measurements in igneous and metamorphic petrology. Cambridge University Press, Cambridge, UK DOI: 10.1017/CBO9780511535574
Higgins MD (2010a) Imaging birefringent minerals without extinction using circularly polarized light. Can Mineral 48(1):231–235. 10.3749/canmin.48.1.231 DOI: 10.3749/canmin.48.1.231
Higgins MD, Voos S, Vander Auwera J (2015) Magmatic processes under Quizapu volcano, Chile, identified from geochemical and textural studies. Contrib Miner Petrol 170(5–6):1–16. 10.1007/s00410-015-1209-5 DOI: 10.1007/s00410-015-1209-5
Hooft EEE, Heath BA, Toomey DR, Paulatto M, Papazachos CB, Nomikou P, Morgan JV, Warner MR (2019) Seismic imaging of Santorini: subsurface constraints on caldera collapse and present-day magma recharge. Earth Planet Sci Lett 514:48–61. 10.1016/j.epsl.2019.02.033 DOI: 10.1016/j.epsl.2019.02.033
Huijsmans JPP (1985) Calc-alkaline lavas from the volcanic complex of Santorini, Aegean Sea, Greece: a petrological, geochemical and stratigraphic study. Geologica Ultraiectina 41:1–316
Le Maitre RW, Streckeisen A, Zanettin B, Le Bas MJ, Bonin B, Bateman P, Bellieni G, Dudek A, Efremova S, Keller J, Lameyre J, Sabine PA, Schmid R, Sorensen H, Woolley AR (2002) Igneous rocks: a classification and glossary of terms: recommendations of the International Union of Geological Sciences subcommission on the systematics of igneous rocks. Cambridge University Press, Cambridge DOI: 10.1017/CBO9780511535581
Marsh BD (1988) Crystal size distribution (CSD) in rocks and the kinetics and dynamics of crystallization I. Theory. Contrib Miner Pet 99:277–291. 10.1007/BF00375362 DOI: 10.1007/BF00375362
Martin VM (2005) Geochemical and textural analysis of mafic enclaves from Nea Kameni, Santorini, Greece. PhD Thesis, University of Cambridge
Martin VM, Holness MB, Pyle DM (2006) Textural analysis of magmatic enclaves from the Kameni Islands, Santorini, Greece. J Volcanol Geoth Res 154(1–2):89–102. 10.1016/j.jvolgeores.2005.09.021 DOI: 10.1016/j.jvolgeores.2005.09.021
Martin VM, Morgan DJ, Jerram DA, Caddick MJ, Prior DJ, Davidson JP (2008) Bang! month-scale eruption triggering at Santorini volcano. Science 321(5893):1178. 10.1126/science.1159584 DOI: 10.1126/science.1159584
McVey BG, Hooft EEE, Heath BA, Toomey DR, Paulatto M, Morgan JV, Nomikou P, Papazachos CB (2019) Magma accumulation beneath Santorini volcano, Greece, from P-wave tomography. Geology 48(3):231–235. 10.1130/g47127.1 DOI: 10.1130/g47127.1
Mills RD, Glazner AF (2013) Experimental study on the effects of temperature cycling on coarsening of plagioclase and olivine in an alkali basalt. Contrib Miner Petrol 166(1):97–111. 10.1007/s00410-013-0867-4 DOI: 10.1007/s00410-013-0867-4
Mora CI, Ramseyer K (1992) Cathodoluminescence of coexisting plagioclases, boehls butte anorthosite-Cl activators and fluid-flow paths. Am Mineral 77(11–12):1258–1265
Mungall JE (2015) Physical Controls of Nucleation, Growth and Migration of Vapor Bubbles in Partially Molten Cumulates. In: Charlier B, Namur O, Latypov R, Tegner C (eds) Layered Intrusions. Springer, Dordrecht, pp 331–377 DOI: 10.1007/978-94-017-9652-1_8
Newman AV, Stiros S, Feng L, Psimoulis S, Moschas S, Saltogianni V, Jiang Y, Papazachos C, Karaginni E, Vamvakaris D (2012) Recent geodetic unrest at Santorini Caldera, Greece. Geophys Res Lett. 10.1029/2012gl051286 DOI: 10.1029/2012gl051286
Nicholls IA (1971) Petrology of Santorini Volcano, Cyclades. Greece J Petrol 12(1):67–119. 10.1093/petrology/12.1.67 DOI: 10.1093/petrology/12.1.67
Nomikou P, Parks MM, Papanikolaou D, Pyle DM, Mather TA, Carey S, Watts AB, Paulatto M, Kalnins ML, Livanos I, Bejelou K, Simou E, Perros I (2014) The emergence and growth of a submarine volcano: The Kameni islands, Santorini (Greece). GeoResJ 1-2(Supplement C):8-18 doi:10.1016/j.grj.2014.02.002
Pagel M, Barbin V, Blanc P, Ohnenstetter D (2000) Cathodoluminescence in geosciences. Springer, Berlin DOI: 10.1007/978-3-662-04086-7
Parks MM, Biggs J, England P, Mather TA, Nomikou P, Palamartchouk K, Papanikolaou X, Paradissis D, Parsons B, Pyle DM, Raptakis C, Zacharis V (2012) Evolution of Santorini volcano dominated by episodic and rapid fluxes of melt from depth. Nat Geosci 5(10):749–754. 10.1038/ngeo1562 DOI: 10.1038/ngeo1562
Parks MM, Moore JDP, Papanikolaou X, Biggs J, Mather TA, Pyle DM, Raptakis C, Paradissis D, Hooper A, Parsons B, Nomikou P (2015) From quiescence to unrest: 20 years of satellite geodetic measurements at Santorini volcano, Greece. J Geophys Res Solid Earth 120(2):1309–1328. 10.1002/2014JB011540 DOI: 10.1002/2014JB011540
Petrone C, Francalanci L, Vougioukalakis G (2013) Mixing, mingling and enclave crumbling in the post-Minoan dacitic magmas of Santorini volcano, Greece. In: Goldschmidt 2013 conference proceedings
Pleše P, Higgins MD, Baker DR, Kudrna Prašek M (2019) Nucleation and growth of bubbles on plagioclase crystals during experimental decompression degassing of andesitic melts. J Volcanol Geoth Res 388:106679. 10.1016/j.jvolgeores.2019.106679 DOI: 10.1016/j.jvolgeores.2019.106679
Pleše P, Higgins MD, Mancini L, Lanzafame G, Brun F, Fife JL, Casselman J, Baker DR (2018) Dynamic observations of vesiculation reveal the role of silicate crystals in bubble nucleation and growth in andesitic magmas. Lithos 296–299:532–546. 10.1016/j.lithos.2017.11.024 DOI: 10.1016/j.lithos.2017.11.024
Pyle DM (2017) What Can We Learn from Records of Past Eruptions to Better Prepare for the Future? In: Fearnley CJ, Bird DK, Haynes K, McGuire WJ, Jolly G (eds) Observing the volcano world. Springer, Heidelberg, pp 1–18
Rasband WS (2010) ImageJ. U. S. National Institutes of Health, Bethesda, Maryland, USA http://rsb.info.nih.gov/ij/
Rizzo AL, Barberi F, Carapezza ML, Di Piazza A, Francalanci L, Sortino F, D’Alessandro W (2015) New mafic magma refilling a quiescent volcano: evidence from He-Ne-Ar isotopes during the 2011–2012 unrest at Santorini, Greece. Geochem Geophys Geosyst 16(3):798–814. 10.1002/2014gc005653 DOI: 10.1002/2014gc005653
Ruprecht P, Simon AC, Fiege A (2020) The Survival of Mafic Magmatic Enclaves and the Timing of Magma Recharge. Geophysical Research Letters 47(14):e2020GL087186 doi:https://doi.org/10.1029/2020GL087186
Sigurdsson H, Carey S, Alexandri M, Vougioukalakis G, Croff K, Roman C, Sakellariou D, Anagnostou C, Rousakis G, Ioakim C, Goguo A, Ballas D, Misaridis T, Nomikou P (2006) Marine investigations of Greece’s Santorini volcanic field. Eos, Transactions American Geophysical Union 87(34):337–342. 10.1029/2006eo340001 DOI: 10.1029/2006eo340001
Stamatelopoulou-Seymour K, Vlassopoulos D, Pearce TH, Rice C (1990) The record of magma chamber processes in plagioclase phenocrysts at Thera volcano, Aegean volcanic arc, Greece. Contrib Miner Petrol 104:73–84. 10.1007/BF00310647 DOI: 10.1007/BF00310647
Theodorakopoulou K, Kyriakopoulos K, Athanassas CD, Galanopoulos E, Economou G, Maniatis Y, Godelitsas A, Dotsika E, Mavridis F, Darlas A (2020) First Speleothem Evidence of the Hiera Eruption (197 BC), Santorini, Greece. Environmental Archaeology:1-13 doi:10.1080/14614103.2020.1755196 DOI: 10.1080/14614103.2020.1755196
Vougioukalakis GE, Fytikas M (2005) Volcanic hazards in the Aegean area, relative risk evaluation, monitoring and present state of the active volcanic centers. In: Fytikas M, Vougioukalakis GE (eds) The South Aegean active volcanic arc-present knowledge and future perspectives, milos conferences, vol 7. Elsevier, Greece, pp 161–183 DOI: 10.1016/S1871-644X(05)80037-3
Watts AB, Nomikou P, Moore JDP, Parks MM, Alexandri M (2015) Historical bathymetric charts and the evolution of Santorini submarine volcano. Greece Geochem Geophys Geosyst 16(3):847–869. 10.1002/2014gc005679 DOI: 10.1002/2014gc005679
Zellmer G, Turner S, Hawkesworth C (2000) Timescales of destructive plate margin magmatism; new insights from Santorini, Aegean volcanic arc. Earth Planet Sci Lett 174(3–4):265–281. 10.1016/S0012-821X(99)00266-6 DOI: 10.1016/S0012-821X(99)00266-6
Zellmer GF, Blake S, Vance D, Hawkesworth C, Turner S (1999) Plagioclase residence times at two island arc volcanoes (Kameni Islands, Santorini, and Soufriere, St. Vincent) determined by Sr diffusion systematics. Contributions to Mineralogy and Petrology 136(4):345-357 doi:10.1007/s004100050543 DOI: 10.1007/s004100050543