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Petrological and experimental constraints on magma storage for large pumiceous eruptions in Dominica island (Lesser Antilles)

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Abstract

The general question of the generation of large-volume silicic eruptions is here addressed through the experimental determination of the storage conditions of the primary magmas that generated ignimbritic eruptions at Dominica Island (Lesser Antilles) during the 24–51 ka period of time. The basal plinian fallouts and pumice pyroclastic flows from the large-volume (~ 5 km3 DRE) events of Layou, Roseau and Grand Fond were investigated, together with the smaller ignimbritic eruptions of Grand Bay and Grande Savane. All samples are dacitic (63–66 wt% SiO2) and contain ~ 30 vol% phenocrysts of plagioclase (~ 21 vol%), orthopyroxene (~ 5 vol%) and Fe-Ti oxides (< 1 vol%), in a rhyolitic matrix glass. The most differentiated samples contain additional amphibole (up to 5 vol%) and quartz. Crystallization experiments were performed starting from Layou and Roseau pumice samples at 800 to 900 °C, 200 to 400 MPa, ~ ΔNNO + 1 and for H2O-saturated and H2O-undersaturated conditions. The main phase contents, assemblages and compositions of both natural samples were reproduced experimentally at ~ 850 °C, ΔNNO + 0.6, 7–8 wt% melt H2O and ~ 400 MPa (~ 16 km depth) consistent with magma ponding at the mid-crustal discontinuity. There is also evidence of more differentiated magma batches that may reflect a plumbing system with a significant vertical extension. The relationships between the chamber depth, width and volume argue for eruptions that do not form collapse calderas, in agreement with field evidence. The erupted magma volumes in Dominica are more than five times larger than those emitted in the neighbouring islands (Martinique, Guadeloupe, Montserrat; < 1 km3), which may be explained by a locally extensional tectonic context that favoured assembly of large magma bodies, but also by the rarity of frequently draining upper crustal reservoirs (as evidenced on the neighbouring volcanic systems) that favoured deep accumulation of large volumes of magma during this period and time for differentiation to dacitic compositions.

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References

  • Allen SR (2001) Reconstruction of a major caldera-forming eruption from pyroclastic deposit characteristics: Kos Plateau Tuff, eastern Aegean Sea. J Volcanol Geotherm Res 105(1):141–162

    Google Scholar 

  • Andújar J, Scaillet B, Pichavant M, Druitt TH (2016) Generation conditions of Dacite and Rhyodacite via the crystallization of an andesitic magma. Implications for the plumbing system at Santorini (Greece) and the origin of tholeiitic or Calc-alkaline differentiation trends in arc magmas. J Petrol 57(10):1887–1920

    Google Scholar 

  • Annen C (2009) From plutons to magma chambers: thermal constraints on the accumulation of eruptible silicic magma in the upper crust. Earth Planet Sci Lett 284(3):409–416

    Google Scholar 

  • Annen C, Sparks RSJ (2002) Effects of repetitive emplacement of basaltic intrusions on thermal evolution and melt generation in the crust. Earth Planet Sci Lett 203(3):937–955

    Google Scholar 

  • Bachmann O, Wallace PJ, Bourquin J (2010) The melt inclusion record from the rhyolitic Kos Plateau Tuff (Aegean arc). Contrib Mineral Petrol 159(2):187–202

    Google Scholar 

  • Bacon CR, Hirschmann MM (1988) Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides. Am Mineral 73(1–2):57–61

    Google Scholar 

  • Balcone-Boissard H, Boudon G, Blundy JD, Martel C, Brooker RA, Deloule E, Solaro C, Matjuschkin V (2018) Deep pre-eruptive storage of silicic magmas feeding Plinian and dome-forming eruptions of central and northern Dominica (Lesser Antilles) inferred from volatile contents of melt inclusions. Contrib Mineral Petrol 173:101

    Google Scholar 

  • Barclay J, Rutherford MJ, Carroll MR, Murphy MD, Devine JD, Gardner J, Sparks RSJ (1998) Experimental phase equilibria constraints on pre-eruptive storage conditions of the Soufrière Hills magma. Geophys Res Lett 25(18):3437–3440

    Google Scholar 

  • Bégué F, Gualda GA, Ghiorso MS, Pamukcu AS, Kennedy BM, Gravley DM, Chambefort I (2014) Phase-equilibrium geobarometers for silicic rocks based on rhyolite-MELTS. Part 2: application to Taupo Volcanic Zone rhyolites. Contrib Mineral Petrol 168(5):1082

    Google Scholar 

  • Boudon G, Balcone-Boissard H, Solaro C, Martel C (2017) Revised chronostratigraphy of recurrent ignimbritic eruptions in Dominica (Lesser Antilles Arc): implications on the behavior of the magma plumbing system. J Volcanol Geotherm Res 343:135–154

    Google Scholar 

  • Bouysse P, Westercamp D (1990) Subduction of Atlantic aseismic ridges and Late Cenozoic evolution of the Lesser Antilles island arc. Tectonophysics 175(4):349357–355380

    Google Scholar 

  • Boynton CH, Westbrook GK, Bott MHP, Long RE (1979) A seismic refraction investigation of crustal structure beneath the Lesser Antilles island arc. Geophys J Int 58(2):371–393

    Google Scholar 

  • Cadoux A, Scaillet B, Druitt TH, Deloule E (2014) Magma storage conditions of large Plinian eruptions of Santorini volcano (Greece). J Petrol 55:1129–1171

    Google Scholar 

  • Carazzo G, Tait S, Kaminski E, Gardner JE (2012) The recent Plinian explosive activity of Mt. Pelée volcano (Lesser Antilles): the P1 AD 1300 eruption. Bull Volcanol 74:2187–2203

    Google Scholar 

  • Carey SN, Sigurdsson H (1980) The Roseau ash: deep-sea tephra deposits from a major eruption on Dominica, Lesser Antilles arc. J Volcanol Geotherm Res 7(1–2):67–86

    Google Scholar 

  • Conrad WK, Nicholls IA, Wall VJ (1988) Water-saturated and -Undersaturated melting of Metaluminous and Peraluminous crustal compositions at 10 kb: evidence for the origin of silicic magmas in the Taupo volcanic zone, New Zealand, and other occurrences. J Petrol 29(4):765–803

    Google Scholar 

  • Costa F, Scaillet B, Pichavant M (2004) Petrological and experimental constraints on the pre-eruption conditions of Holocene Dacite from Volcan San Pedro (36 S, Chilean Andes) and the importance of Sulphur in silicic subduction-related magmas. J Petrol 45(4):855–881

    Google Scholar 

  • Dall'Agnol R, Scaillet B, Pichavant M (1999) An experimental study of a lower proterozoic A-type granite from the Eastern Amazonian Craton, Brazil. J Petrol 40:1673–1698

    Google Scholar 

  • De Silva S (2008) Arc magmatism, calderas, and supervolcanoes. Geology 36(8):671–672

    Google Scholar 

  • De Silva SL, Gosnold WD (2007) Episodic construction of batholiths: insights from the spatiotemporal development of an ignimbrite flare-up. J Volcanol Geotherm Res 167(1):320–335

    Google Scholar 

  • Degruyter W, Huber C (2014) A model for eruption frequency of upper crustal silicic magma chambers. Earth Planet Sci Lett 403:117–130

    Google Scholar 

  • Degruyter W, Huber C, Bachmann O, Cooper KM, Kent AJ (2016) Magma reservoir response to transient recharge events: the case of Santorini volcano (Greece). Geology 44(1):23–26

    Google Scholar 

  • Di Napoli R, Aiuppa A, Allard P (2014) First multi-gas based characterization of the boiling Lake volcanic gas (Dominica, Lesser Antilles). Ann Geophys 56:S0559

    Google Scholar 

  • Druitt TH, Mellors RA, Pyle DM, Sparks RSJ (1989) Explosive volcanism on Santorini, Greece. Geol Mag 126(2):95–126

    Google Scholar 

  • Erdmann S, Martel C, Pichavant M, Kushnir ARL (2014) Amphibole as an archivist of magmatic crystallization conditions: problems, potential, and implications for inferring magma storage prior to the paroxysmal 2010 eruption of Mount Merapi, Indonesia. Contrib Mineral Petrol 167:1016–1039

    Google Scholar 

  • Feuillet N, Leclerc F, Tapponnier P, Beauducel F, Boudon G, Le Friant A, Deplus C, Lebrun JF, Nercessian A, Saurel JM, Clément V (2010) Active faulting induced by slip partitioning in Montserrat and link with volcanic activity: New insights from the 2009 GWADASEIS marine cruise data. Geophys Res Lett 37. https://doi.org/10.1029/2010GL042556

    Google Scholar 

  • Fournier N, Witham F, Moreau-Fournier M, Bardou L (2009) Boiling lake of Dominica West Indies: high-temperature volcanic crater lake dynamics. J Geophys Res Solid Earth 114. https://doi.org/10.1029/2008JB005773

  • Gardner JE, Rutherford MJ, Carey S, Sigurdsson H (1995) Experimental constraints on pre-eruptive water contents and changing magma storage prior to explosive eruptions of Mount St. Helens volcano. Bull Volcanol 57:1–17

    Google Scholar 

  • Gavrilenko M, Ozerov A, Kyle P, Carr MJ, Nikulin A, Vidito C, Danyushevsky L (2016) Abrupt transition from fractional crystallization to magma mixing at Gorely volcano (Kamchatka) after caldera collapse. Bull Volcanol 78(7):1–28

    Google Scholar 

  • Geyer A, Folch A, Marti J (2006) Relationship between caldera collapse and magma chamber withdrawal: an experimental approach. J Volcanol Geotherm Res 157:375–386

    Google Scholar 

  • Ghiorso MS, Evans BW (2008) Thermodynamics of rhombohedral oxide solid solutions and a revision of the Fe-Ti two-oxide geothermometer and oxygen-barometer. Am J Sci 308(9):957–1039

    Google Scholar 

  • Hammer JE, Rutherford MJ, Hildreth W (2002) Magma storage prior to the 1912 eruption at Novarupta, Alaska. Contrib Mineral Petrol 144(2):144–162

    Google Scholar 

  • Heiken G, McCoy FJ (1984) Caldera development during the Minoan eruption, Thira, Cyclades, Greece. J Geophys Res 89(B10):8441–8462

    Google Scholar 

  • Holtz F, Sato H, Lewis J, Behrens H, Nakada S (2005) Experimental petrology of the 1991–1995 Unzen dacite, Japan. Part I: phase relations, phase composition and pre-eruptive conditions. J Petrol 46(2):319–337

    Google Scholar 

  • Houghton BF, Wilson CJN, McWilliams MO, Lanphere MA, Weaver SD, Briggs RM, Pringle MS (1995) Chronology and dynamics of a large silicic magmatic system: Central Taupo volcanic zone, New Zealand. Geology 23:13–16

    Google Scholar 

  • Howe TM, Lindsay JM, Shane P, Schmitt AK, Stockli DF (2014) Re-evaluation of the Roseau tuff eruptive sequence and other ignimbrites in Dominica, Lesser Antilles. J Quatern Sci 29(6):531–546

    Google Scholar 

  • Howe TM, Lindsay JM, Shane P (2015) Evolution of young andesitic–dacitic magmatic systems beneath Dominica, Lesser Antilles. J Volcanol Geotherm Res 297:69–88

    Google Scholar 

  • Jellinek AM, De Paolo DJ (2003) A model for the origin of large silicic magma chambers: precursors of caldera-forming eruptions. Bull Volcanol 65:363–381

    Google Scholar 

  • Kopp H, Weinzierl W, Becel A, Charvis P, Evain M, Flueh ER, Klaeschen D (2011) Deep structure of the central Lesser Antilles Island arc: relevance for the formation of continental crust. Earth Planet Sci Lett 304(1):121–134

    Google Scholar 

  • Le Guen de Kerneizon M, Carron JP, Maury R, Bellon H, Dupuy C (1982) Rhyolites with fayalite and ferroaugite in Saint-Lucia, Lesser Antilles island arc. Bull Mineral 105(2):203–211

    Google Scholar 

  • Lindsay JM, Stasiuk M, Shepherd J (2003) Geological history and potential hazards of the late-Pleistocene to recent plat pays volcanic complex, Dominica, Lesser Antilles. Bull Volcanol 65(2):201–220

    Google Scholar 

  • Lindsay JM, Robertson R, Shepherd B, Ali S (eds) (2005a) Volcanic Hazard Atlas of the Lesser Antilles. Seismic Res Center, St Augustine, Trinidad and Tobago. Univ West Indies, 279 p

  • Lindsay JM, Trumbull RB, Siebel W (2005b) Geochemistry and petrogenesis of late Pleistocene to recent volcanism in southern Dominica, Lesser Antilles. J Volcanol Geotherm Res 148:253–294

    Google Scholar 

  • Lipman PW (2007) Incremental assembly and prolonged consolidation of cordilleran magma chambers: evidence from the southern Rocky Mountain volcanic field. Geosphere 3(1):42–70

    Google Scholar 

  • Luhr J (1990) Experimental phase relations of water and sulfur saturated arc magmas and the 1982 eruptions of El Chichon volcano. J Petrol 31:1071–1114

    Google Scholar 

  • Macdonald R, Hawkesworth CJ, Heath E (2000) The Lesser Antilles volcanic chain: a study in arc magmatism. Earth Sci Rev 49(1–4):1–76

    Google Scholar 

  • Mandeville CW, Carey S, Sigurdsson H (1996) Magma mixing, fractional crystallization and volatile degassing during the 1883 eruption of Krakatau volcano, Indonesia. J Volcanol Geotherm Res 74:243–274

    Google Scholar 

  • Manea VC, Leeman WP, Gerya T, Manea M, Zhu G (2014) Subduction of fracture zones controls mantle melting and geochemical signature above slabs. Nature Commun 5

  • Martel C, Pichavant M, Bourdier JL, Traineau H, Holtz F, Scaillet B (1998) Magma storage conditions and control of eruption regime in silicic volcanoes: experimental evidence from Mt Pelée. Earth Planet Sci Lett 156:89–99

    Google Scholar 

  • Martel C, Pichavant M, Holtz F, Scaillet B, Bourdier J-L, Traineau H (1999) Effect of fO2 and H2O on andesite phase relations between 2 and 4 kbar. J Geophys Res 104(B12):29453–29470

    Google Scholar 

  • Martel C, Champallier R, Prouteau G, Pichavant M, Arbaret L, Balcone-Boissard H, Boudon G, Boivin P, Bourdier JL, Scaillet B (2013) Phase relations in trachytes and implication for magma storage conditions in the Chaîne des Puys (French Massif Central). J Petrol 54(6):1071–1107

    Google Scholar 

  • Marti J, Geyer A, Folch A, Gottsmann J (2008) A review on collapse caldera modelling. In: Gottsmann J, Marti J (eds) Caldera volcanism: analysis, modelling and response. Developments in volcanology 10, Elsevier, pp 233–283

  • Mayer K, Scheu B, Yilmaz TI, Montanaro C, Gilg HA, Rott S, Joseph EP, Dingwell DB (2017) Phreatic activity and hydrothermal alteration in the valley of desolation, Dominica, Lesser Antilles. Bull Volcanol 79:82

    Google Scholar 

  • Melekhova E, Schlaphorst D, Blundy J, Kendall JM, Connolly C, McCarthy A, Arculus R (2019) Lateral variation in crustal structure along the Lesser Antilles arc from petrology of crustal xenoliths and seismic receiver functions. Earth Planet Sci Lett 516:12–24

    Google Scholar 

  • Newman S, Lowenstern JB (2002) VolatileCalc: a silicate melt–H2O–CO2 solution model written in visual basic for excel. Comput Geosci 28(5):597–604

    Google Scholar 

  • Parat F, Holtz F, Feig S (2008) Pre-eruptive conditions of the Huerto andesite (fish canyon system, San Juan volcanic field, Colorado): influence of volatiles (C–O–H–S) on phase equilibria and mineral composition. J Petrol 49(5):911–935

    Google Scholar 

  • Pichavant M, Martel C, Bourdier JL, Scaillet B (2002) Physical conditions, structure, and dynamics of a zoned magma chamber: Mount Pelée (Martinique, Lesser Antilles arc). J Geophys Res 107(B5)

  • Pichavant M, Costa F, Burgisser A, Scaillet B, Martel C, Poussineau (2007) Equilibration scales in silicic to intermediate magmas - Implications for experimental studies. J Petrol 48:1955–1972

    Google Scholar 

  • Pichavant M, Poussineau S, Lesne P, Solaro C, Bourdier JL (2018) Experimental parametrization of magma mixing: application to the AD 1530 eruption of La Soufrière, Guadeloupe (Lesser Antilles). J Petrol 59:257–282

    Google Scholar 

  • Plail M, Barclay J, Humphreys MCS, Edmonds M, Herd RA, Christopher TE (2014) Characterization of mafic enclaves in the erupted products of Soufrière Hills volcano, Montserrat, 2009 to 2010. In: Wadge G, Robertson REA, Voight B (eds) The eruption of Soufrière Hills volcano, Montserrat from 2000 to 2010. GSL Memoirs 39, pp 343–360

  • Prouteau G, Scaillet B (2003) Experimental constraints on the origin of the 1991 Pinatubo Dacite. J Petrol 44(12):2203–2241

    Google Scholar 

  • Putirka KD (2008) Thermometers and barometers for volcanic systems. Rev Mineral Geochem 69(1):61–120

    Google Scholar 

  • Reubi O, Nicholls IA (2005) Structure and dynamics of a silicic magmatic system associated with caldera-forming eruptions at Batur volcanic field, Bali, Indonesia. J Petrol 456(7):1367–1391

    Google Scholar 

  • Ridolfi F, Renzulli A (2012) Calcic amphiboles in calc-alkaline and alkaline magmas: thermobarometric and chemometric empirical equations valid up to 1,130° C and 2.2 GPa. Contrib Mineral Petrol 163(5):877–895

    Google Scholar 

  • Roobol MJ, Smith AL (2004) Geological map of Dominica, West Indies. Geology Department, Univ Puerto Rico at Mayaquez

  • Sato H, Nakada S, Fujii T, Nakamura M, Suzuki-Kamata K (1999) Groundmass pargasite in the 1991-1995 dacite of Unzen volcano: phase stability experiments and volcanological implications. J Volcanol Geotherm Res 89:197–212

    Google Scholar 

  • Sauerzapf U, Lattard D, Burchard M, Engelmann R (2008) The titanomagnetite–ilmenite equilibrium: new experimental data and thermo-oxybarometric application to the crystallization of basic to intermediate rocks. J Petrol 49(6):1161–1185

    Google Scholar 

  • Scaillet B, Evans WE (1999) The 15 June 1991 eruption of Mount Pinatubo. I. Phase equilibria and pre-eruption P-T-fO2-f H2O conditions of the dacite magma. J Petrol 40:381–411

    Google Scholar 

  • Schlaphorst D, Kendall JM, Collier JS, Verdon JP, Blundy J, Baptie B, Latchmann JL, Massin F, Bouin MP (2016) Water, oceanic fracture zones and the lubrication of subducting plate boundaries-insights from seismicity. Geophys J Int 204(3):1405–1420

    Google Scholar 

  • Self S, Rampino M (1981) The 1883 eruption of Krakatau. Nature 294:699–704

    Google Scholar 

  • Self S, Rampino M, Newton MS, Wolff JA (1984) Volcanological study of the great Tambora eruption of 1815. Geology 12:659–663

    Google Scholar 

  • Sigurdsson H (1972) Partly-welded pyroclast flow deposits in Dominica, Lesser Antilles. Bull Volcanol 36:148–163

    Google Scholar 

  • Smith AL, Roobol MJ, Mattioli GS, Fryxell JE, Daly GE, Fernandez LA (2013) The volcanic geology of the mid-arc island of Dominica. Geol Soc Am 496

  • Solaro C (2017) Storage conditions and dynamics of magma reservoirs feeding the major pumiceous eruptions of Dominica (Lesser Antilles Arc). PhD thesis, Univ Paris Diderot, France

  • Sparks RSJ, Sigurdsson H, Carey SN (1980) The entrance of pyroclastic flows into the sea I. oceanographic and geologic evidence from Dominica, Lesser Antilles. J Volcanol Geotherm Res 7(1–2):87–96

    Google Scholar 

  • Wadge G (1984) Comparison of volcanic production rates and subduction rates in the Lesser Antilles and Central America. Geology 12:555–558

    Google Scholar 

  • Wadge G, Shepherd JB (1984) Segmentation of the Lesser Antilles subduction zone. Earth Planet Sci Lett 71:297–304

    Google Scholar 

  • Waters LE, Lange RA (2015) An updated calibration of the plagioclase-liquid hygrometer-thermometer applicable to basalts through rhyolites. Am Mineral 100:2172–2184

    Google Scholar 

  • Wilson CJN (2001) The 26.5 ka Oruanui eruption, New Zealand: an introduction and overview. J Volcanol Geotherm Res 112

    Google Scholar 

  • Wilson CJN, Blake S, Charlier BLA, Sutton AN (2006) The 26.5 ka Oruanui eruption, Taupo volcano, New Zealand: development, characteristics and evacuation of a large rhyolitic magma body. J Petrol 47(1):35–69

    Google Scholar 

  • Ziberna L, Green ECR, Blundy JD (2017) Multiple-reaction geobarometry for olivine-bearing igneous rocks. Am Mineral 102:2349–2366

    Google Scholar 

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Acknowledgements

We would like to thank Michel Fialin and Nicolas Rividi (service CAMPARIS) and Ida di Carlo (ISTO) for assistance during microprobe analyses and Omar Boudouma (SEM, Sorbonne Université) for help during SEM imaging. We thank Vincent Christmann who started the study during his master’s thesis. We are grateful to the reviewers, Jenny Riker, Maxim Gavrilenko, Elena Melekhova, the Associate Editor, Maxim Portnyagin and the Executive Editor, Andrew Harris, for their comments that significantly improved the manuscript. This work was financially supported by the French MNRT doctoral grant (to C. Solaro), the European FP7_VUELCO project (J. Gottsmann, PI; grant 282759) and the French INSU Action Incitative (G. Boudon, PI).

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Authors and Affiliations

  1. Institut de Physique du Globe de Paris (IPGP), CNRS, Université de Paris, Paris, France

    Clara Solaro & Georges Boudon

  2. Institut des Sciences de la Terre d’Orléans (ISTO), UMR 7327, Université d’Orléans – CNRS - BRGM, Orléans, France

    Caroline Martel, Rémi Champallier & Michel Pichavant

  3. UMR 7193 Université Paris 06 - CNRS – ISTeP, Sorbonne Universités (UPMC), Paris, France

    Hélène Balcone-Boissard

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  1. Clara Solaro
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Solaro, C., Martel, C., Champallier, R. et al. Petrological and experimental constraints on magma storage for large pumiceous eruptions in Dominica island (Lesser Antilles). Bull Volcanol 81, 55 (2019). https://doi.org/10.1007/s00445-019-1313-x

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