Abstract
The magmatic processes responsible for triggering nature’s most destructive eruptions and their associated timescales remain poorly understood. Yellowstone Caldera is a large silicic volcanic system that has had three supereruptions in its 2.1-Ma history, the most recent of which produced the Lava Creek Tuff (LCT) ca. 631 ka. Here we present a petrologic study of the phenocrysts, specifically feldspar and quartz, in LCT ash in order to investigate the timing and potential trigger leading to the LCT eruption. The LCT phenocrysts have resorbed cores, with crystal rims that record slightly elevated temperatures and enrichments in magmaphile elements, such as Ba and Sr in sanidine and Ti in quartz, compared to their crystal cores. Chemical data in conjunction with mineral thermometry, geobarometry, and rhyolite-MELTS modeling suggest the chemical signatures observed in crystal rims were most likely created by the injection of more juvenile silicic magma into the LCT sub-volcanic reservoir, followed by decompression-driven crystal growth. Geothermometry and barometry suggest post-rejuvenation, pre-eruptive temperatures and pressures of 790–815 °C and 80–150 MPa for the LCT magma source. Diffusion modeling utilizing Ba and Sr in sanidine and Ti in quartz in conjunction with crystal growth rates yield conservative estimates of decades to years between rejuvenation and eruption. Thus, we propose rejuvenation as the most likely mechanism to produce the overpressure required to trigger the LCT supereruption in less than a decade.
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References
Allan ASR, Wilson CJN, Millet MA, Wysoczanski RJ (2012) The invisible hand: tectonic triggering and modulation of a rhyolitic supereruption. Geology 40:563–566. https://doi.org/10.1130/G32969.1
Allan ASR, Morgan DJ, Wilson CJN, Millet MA (2013) From mush to eruption in centuries: assembly of the super-sized Oruanui magma body. Contrib Mineral Petrol 166(1):143–164
Bachmann O, Bergantz GW (2003) Rejuvenation of the Fish Canyon magma body: a window into the evolution of large-volume silicic magma systems. Geology 31(9):789
Bachmann O, Huber C (2016) Silicic magma reservoirs in the Earth’s crust. Am Mineral 101:2377–2404. https://doi.org/10.2138/am-2016-5675
Bachmann O, Deering CD, Lipman PW, Plummer C (2014) Building zoned ignimbrites by recycling silicic cumulates: insight from the 1,000 km3 Carpenter Ridge Tuff, CO. Contrib Mineral Petrol 167:1–13. https://doi.org/10.1007/s00410-014-1025-3
Befus KS, Bruyere RH, Manga M (2018) Lava Creek Tuff Love. Goldschmidt Abstracts 162
Bergantz GW, Schleicher JM, Burgisser A (2017) On the kinematics and dynamics of crystal-rich systems. J Geophys Res Solid Earth 122(8):6131–6159
Bindeman IN, Valley JW (2001) Low-d18O rhyolites from Yellowstone: magmatic evolution based on analyses of zircon and individual phenocrysts. J Petrol 42:1491–1517
Blundy JD, Wood BJ (1991) Crystal-chemical controls on the partitioning of Sr and Ba between plagioclase feldspar, silicate melts, and hydrothermal solutions. Geochem Cosmochim Acta 55:193–209
Blundy J, Cashman K, Humphreys M (2006) Magma heating by decompression-driven crystallization beneath andesite volcanoes. Nat Lett 443:76–80. https://doi.org/10.1038/nature05100
Blundy J, Cashman KV, Rust A, Witham F (2010) A case for CO2-rich arc magmas. Earth Planet Sci Lett 290:289–301. https://doi.org/10.1016/j.epsl.2009.12.013
Cabaniss HE, Gregg PM, Grosfils EB (2018) The role of tectonic stress in triggering large silicic caldera eruptions. Geophys Res Lett 45:3889–3895. https://doi.org/10.1029/2018GL077393
Calzolaio M, Arzilli F, Carroll MR (2010) Growth rate of alkali feldspars in decompression-induced crystallization experiments in a trachytic melt of the Phlegraean Fields (Napoli, Italy). Eur J Mineral 22:485–493. https://doi.org/10.1127/0935-1221/2010/0022-2012
Cashman KV, Sparks RSJ (2013) How volcanoes work: a 25 year perspective. GSA Bull 125:664–690. https://doi.org/10.1130/b30720.1
Cassidy M, Castro JM, Helo C, Troll VR, Deegan FM, Muir D, Mueller SP (2016) Volatile dilution during magma injections and implications for volcano explosivity. Geology 44(12):1027–1030
Cassidy M, Castro J, Helo C, Ebmeier S, Watt S (2017) Combining experimental petrology with InSAR deformation constraints on the magmatic system prior to recent eruptions at Kelud volcano, Indonesia. EGU Gen Assembly Conf Abstr 19:9156
Chamberlain KJ, Morgan DJ, Wilson CJN (2014) Timescales of mixing and mobilisation in the Bishop Tuff magma body: perspectives from diffusion chronometry. Contrib Mineral Petrol 168:1–24. https://doi.org/10.1007/s00410-014-1034-2
Cherniak DJ (1996) Strontium diffusion in sanidine and albite, and general comments on strontium diffusion in alkali feldspars. Geochim Cosmochim Acta 60:5037–5043. https://doi.org/10.1016/S0016-7037(96)00293-1
Cherniak DJ (2002) Ba diffusion in feldspar. Geochim Cosmochim Acta 66:1641–1650. https://doi.org/10.1016/S0016-7037(01)00866-3
Cherniak DJ, Watson EB, Wark DA (2007) Ti diffusion in quartz. Chem Geol 236:65–74. https://doi.org/10.1016/j.chemgeo.2006.09.001
Christiansen RL (2001) The quaternary and pliocene Yellowstone Plateau Volcanic Field of Wyoming, Idaho, and Montana. USGS Professional Papers. No. 729-G
Costa F, Morgan D, Dosseto A, Turner S, Van Orman J (2011) Time constraints from chemical equilibration in magmatic crystals. Timescales of magmatic processes: from core to atmosphere. Wiley, Chichester, pp 125–159
Couch S, Harford CL, Sparks RSJ, Carroll MR (2003) Experimental constraints on the conditions of formation of highly calcic plagioclase microlites at the Soufriere Hills Volcano, Montserrat. J Petrol 44:1455–1475. https://doi.org/10.1093/petrology/44.8.1455
Degruyter W, Huber C, Bachmann O et al (2016) Magma reservoir response to transient recharge events: the case of Santorini volcano (Greece). Geology 44:23–26. https://doi.org/10.1130/G37333.1
Druitt TH, Costa F, Deloule E, Dungan M, Scaillet B (2012) Decadal to monthly timescales of magma transfer and reservoir growth at a caldera volcano. Nature 482:77–80. https://doi.org/10.1038/nature10706
Eaton GP, Christiansen RL, Iyer HM, Pitt AM, Mabey DR, Blank HR, Zietz I, Gettings ME (1975) Magma Beneath Yellowstone. Science 188:787–796
Farrell J, Smith R, Husen S, Diehl T (2014) Tomography from 26 years of seismicicty revealing that the spatial extent of the Yellowstone crustal reservoir extends well beyond the Yellowstone caldera. Geophys Res Lett 41:3068–3073. https://doi.org/10.1002/2014GL059588
Fenn PM (1977) The nucleation and growth of alkali feldspars from hydrous melts. Can Mineral 15:135–161
Flaherty T, Druitt TH, Tuffen MD et al (2018) Multiple timescale constraints for high-flux magma chamber assembly prior to the Late Bronze Age eruption of Santorini (Greece). Contrib Mineral Petrol 173:75. https://doi.org/10.1007/s00410-018-1490-1
Gansecki CA (1998) 40Ar/39Ar geochronology and pre-eruptive geochemistry of the Yellowstone Plateau volcanic field rhyolites. Unpublished doctoral dissertation, Stanford University, p 212
Gansecki CA, Mahood GA, McWilliams M (1998) New ages for the climactic eruptions at Yellowstone: single-crystal 40Ar/39Ar dating identifies contamination. Geology 26(343):346. https://doi.org/10.1130/0091-7613
Gardner JE, Befus KS, Gualda GAR, Ghiorso MS (2014) Experimental constraints on rhyolite-MELTS and the Late Bishop Tuff magma body. Contrib Mineral Petrol 168:1–14. https://doi.org/10.1007/s00410-014-1051-1
Ghiorso MS, Gualda GAR (2015) An H2O–CO2 mixed fluid saturation model compatible with rhyolite-MELTS. Contrib Mineral Petrol 169:1–30. https://doi.org/10.1007/s00410-015-1141-8
Ginibre C, Wörner G, Kronz A (2004) Structure and dynamics of the Laacher See magma chamber (Eifel, Germany) from major and trace element zoning in sanidine: a cathodoluminescence and electron microprobe study. J Petrol 45:2197–2223. https://doi.org/10.1093/petrology/egh053
Gregg PM, Gros EB, De Silva SL (2015) Catastrophic caldera-forming eruptions II: the subordinate role of magma buoyancy as an eruption trigger. J Volcanol 305:100–113. https://doi.org/10.1016/j.jvolgeores.2015.09.022
Gualda GA, Ghiorso MS (2014) Phase-equilibrium geobarometers for silicic rocks based on rhyolite-MELTS. Part 1: Principles, procedures, and evaluation of the method. Contrib Mineral Petrol 168(1):1033
Gualda GAR, Sutton SR (2016) The year leading to a supereruption. PLoS One 11:1–18. https://doi.org/10.1371/journal.pone.0159200
Gualda GAR, Ghiorso MS, Lemons RV, Carley TL (2012) Rhyolite-MELTS: a modified calibration of MELTS optimized for silica-rich, fluid-bearing magmatic systems. J Petrol 53:875–890. https://doi.org/10.1093/petrology/egr080
Guo J, Green TH (1989) Barium partitioning between alkali feldspar and silicate liquid at high temperature and pressure. Contrib Mineral Petrol 102(3):328–335
Hawkesworth C, George R, Turner S, Zellmer G (2004) Time scales of magmatic processes. Earth Planet Sci Lett 218:1–16. https://doi.org/10.1016/S0012-821X(03)00634-4
Hayden LA, Watson EB (2007) Rutile saturation in hydrous siliceous melts and its bearing on Ti-thermometry of quartz and zircon. Earth Planet Sci Lett 258:561–568. https://doi.org/10.1016/j.epsl.2007.04.020
Hildreth W (1981) Gradients in silicic magma chambers: implications for lithospheric magmatism. J Geophys Res Solid Earth 86(B11):10153–10192
Hildreth W, Christiansen RL, O’Neil JR (1984) Catastrophic isotopic modification of rhyolitic magma at times of caldera subsidence, Yellowstone Plateau volcanic field. J Geophys Res Solid Earth 89(B10):8339–8369
Hildreth W, Halliday AN, Robert L (1991) Isotopic and chemical evidence concerning the genesis and contamination of basaltic and rhyolitic magma beneath the Yellowstone Plateau Volcanic Field. J Petrol 32:63–138
Huang R, Audétat A (2012) The titanium-in-quartz (TitaniQ) thermobarometer: a critical examination and re-calibration. Geochim Cosmochim Acta 84:75–89. https://doi.org/10.1016/j.gca.2012.01.009
Huber C, Bachmann O, Dufek J (2012) Crystal-poor versus crystal-rich ignimbrites: a competition between stirring and reactivation. Geology 40:115–118. https://doi.org/10.1130/G32425.1
Humphreys MCS, Edmonds M, Klöcking MS (2016) The validity of plagioclase-melt geothermometry for degassing-driven magma crystallisation. Am Mineral 101:769–779
Iacovino K (2015) Linking subsurface to surface degassing at active volcanoes: a thermodynamic model with applications to Erebus volcano. Earth Planet Sci Lett 431(59):74. https://doi.org/10.1016/j.epsl.2015.09.016
Icenhower J, London D (1996) Experimental partitioning of Rb, Cs, Sr, and Ba between alkali feldspar and peraluminous melt. Am Mineral 81:719–734. https://doi.org/10.2138/am-1996-5-619
Jellinek AM, DePaolo DJ (2003) A model for the origin of large silicic magma chambers: precursors of caldera-forming eruptions. Bull Volcanol 65:363–381. https://doi.org/10.1007/s00445-003-0277-y
Jicha BR, Singer BS, Sobol P (2016) Re-evaluation of the ages of 40 Ar/39 Ar sanidine standards and supereruptions in the western US using a Noblesse multi-collector mass spectrometer. Chem Geol 431:54–66
Kelley SP, Wartho JA (2000) Rapid kimberlite ascent and the significance of Ar–Ar ages in xenolith phlogopites. Science 289(5479):609–611
Leeman W, Vicenzi E, Macrae C et al (2008) Systematics of cathodoluminescence and trace element compositional zoning in natural quartz from volcanic rocks: Ti mapping in quartz. Microsc Microanal 18:1322–1341. https://doi.org/10.1017/S1431927608088995
Leeman WP, MacRae CM, Wilson NC, Torpy A, Lee CT, Student JJ, Thomas JB, Vicenzi EP (2012) A study of cathodoluminescence and trace element compositional zoning in natural quartz from volcanic rocks: mapping titanium content in quartz. Microsc Microanal 18(6):1322–1341
Lejeune AM, Richet P (1995) Rheology of crystal-bearing silicate melts: an experimental study at high viscosities. J Geophys Res Solid Earth 100(B3):4215–4229
Long PE (1978) Experimental determination of partition coefficients for Rb, Sr, and Ba between alkali feldspar and silicate liquid. Geochim Cosmochim Acta 42:833–846
Mark DF, Renne PR, Dymock RC, Smith VC, Simon JI, Morgan LE, Pearce NJ (2017) High-precision 40Ar/39Ar dating of Pleistocene tuffs and temporal anchoring of the Matuyama-Brunhes boundary. Quat Geochron 39:1–23
Matthews NE, Huber C, Pyle DM, Smith VC (2012) Timescales of magma recharge and reactivation of large silicic systems from Ti diffusion in quartz. J Petrol 53:1385–1416. https://doi.org/10.1093/petrology/egs020
Matthews N, Vazquez J, Calvert A (2015) Age of the Lava Creek supereruption and magma chamber assembly at Yellowstone based on 40Ar/39Ar and U–Pb dating of sanidine and zircon crystals. Geochem Geophys Geosyst 16:1–21. https://doi.org/10.1002/2015GC005881
Morgan DJ, Blake S, Rogers NM et al (2006) Magma chamber recharge at Vesuvius in the century prior to the eruption of A.D. 79. Geology 34:845–848. https://doi.org/10.1130/G22604.1
Müller A, Wiedenbeck M, van den Kerkhof AM et al (2003) Trace elements in quartz—a combined electron microprobe, secondary ion mass spectrometry, laser-ablation ICP-MS, and cathodoluminescence study. Eur J Mineral 15:747–763. https://doi.org/10.1127/09351221/2003/0015-0747
Nichols ML, Malone SD, Moran SC, Thelen WA, Vidale JE (2011) Deep long-period earthquakes beneath Washington and Oregon volcanoes. J Volcanol Geotherm Res 200(3–4):116–128
Oppenheimer C, Moretti R, Kyle PR et al (2011) Mantle to surface degassing of alkalic magmas at Erebus volcano, Antarctica. Earth Planet Sci Lett 306:261–271. https://doi.org/10.1016/j.epsl.2011.04.005
Pamukcu AS, Ghiorso MS, Gualda GAR (2016) High-Ti, bright-CL rims in volcanic quartz: a result of very rapid growth. Contrib Mineral Petrol 171:1–9. https://doi.org/10.1007/s00410-016-1317-x
Putirka KD (2008) Thermometers and barometers for volcanic systems. Rev Mineral Geochem 69:61–120. https://doi.org/10.2138/rmg.2008.69.3
Ren M (2004) Partitioning of Sr, Ba, Rb, Y and LREE between alkali feldspar and peraluminous silicic magma. Am Mineral 89(8–9):1290–1303
Rubin KH, van der Zander I, Smith MC, Bergmanis EC (2005) Minimum speed limit for ocean ridge magmatism from 210Pb–226Ra–230Th disequilibria. Nature 437:534–538
Rubin AE, Cooper KM, Till CB et al (2017) Rapid cooling and cold storage in a silicic magma reservoir recorded in individual crystals. Science 356:1154–1156. https://doi.org/10.1126/science.aam8720
Saunders K, Blundy J, Dohmen R, Cashman K (2012) Linking petrology and seismology at an active volcano. Science 336(6084):1023–1027
Schleicher JM, Bergantz GW (2017) The mechanics and temporal evolution of an open-system magmatic intrusion into a crystal-rich magma. J Petrol 58(6):1059–1072
Schneider CA, Rasband WS, Eliceiri KW (2012) NIH Image to ImageJ: 25 years of image analysis. Nat Methods 9(7):671–675
Sigurdsson H, Carey S, Cornell W, Pescatore T (1985) The eruption of Vesuvius in A.D. 79. Natl Geogr Res 1(3):332–387
Sisson TW, Bacon CR (1999) Gas-driven filter pressing in magmas. Geology 27:613–616. https://doi.org/10.1130/0091-7613(1999)027%3c0613:GDFPIM%3e2.3.CO
Sisson T, Power J, Haney M (2017) The deep-crustal roots of arc stratovolcanoes illuminated by long-period seismicity caused by degassing and fluid-enhanced wallrock embrittlement. IAVCEI General Assembly Submission 920
Smith RB, Braile LW (1994) The Yellowstone hotspot. J Volcanol Geotherm Res 61:121–187. https://doi.org/10.1016/0377-0273(94)90002-7
Smith J, Brown WL (1988) Feldspar minerals: crystal structures, physical, chemical and microtextural properties. Springer, Berlin, p 828
Smith RB, Jordan M, Steinberger B et al (2009) Geodynamics of the Yellowstone hotspot and mantle plume: seismic and GPS imaging, kinematics, and mantle flow. J Volcanol Geotherm Res 188:26–56. https://doi.org/10.1016/j.jvolgeores.2009.08.020
Sparks S (2005) Super-eruptions: global effects and future threats, report of a Geological Society of London Working Group. Geological Society, London
Stelten ME, Cooper KM, Vazquez JA et al (2013) Magma mixing and the generation of isotopically juvenile silicic magma at Yellowstone caldera inferred from coupling 238 U–230 Th ages with trace elements and Hf and O isotopes in zircon and Pb isotopes in sanidine. Contrib Mineral Petrol 166(2):587–613. https://doi.org/10.1007/s00410-013-0893-2
Stelten ME, Cooper KM, Vazquez JA et al (2015) Mechanisms and timescales of generating eruptible rhyolitic magmas at Yellowstone Caldera from Zircon and sanidine geochronology and geochemistry. J Petrol 56:1607–1642. https://doi.org/10.1093/petrology/egv047
Stelten ME, Cooper KM, Wimpenny JB et al (2017) The role of mantle-derived magmas in the isotopic evolution of Yellowstone’s magmatic system. Geochem Geophys Geosyst 18:1350–1365. https://doi.org/10.1002/2016GC006664
Stracke A, Bourdon B, McKenzie D (2006) Melt extraction in the Earth’s mantle: constraints from U-Th–Pa–Ra studies in oceanic basalts. Earth Planet Sci Lett 244:97–112
Streck MJ (2008) Mineral textures and zoning as evidence for open system processes. Rev Mineral Geochem 69:595–622. https://doi.org/10.2138/rmg.2008.69.15
Swanson SE (1974) Phase equilibria and crystal growth in granodioritic and related systems with H2O + CO2. Ph.D. thesis, Stanford University
Swanson SE (1977) Relation of nucleation and crystal-growth rate to the development of granitic textures. Am Mineral 62:966–978
Thomas JB, Watson EB, Spear FS et al (2010) TitaniQ under pressure: the effect of pressure and temperature on the solubility of Ti in quartz. Contrib Mineral Petrol 160:743–759. https://doi.org/10.1007/s00410-010-0505-3
Till CB, Vazquez JA, Boyce JW (2015) Months between rejuvenation and volcanic eruption at Yellowstone caldera, Wyoming. Geology. https://doi.org/10.1130/g36862
Turner S, Costa F (2007) Measuring timescales of magmatic evolution. Elements 3:267–272
Vazquez JA, Kyriazis SF, Reid MR et al (2009) Thermochemical evolution of young rhyolites at Yellowstone: evidence for a cooling but periodically replenished postcaldera magma reservoir. J Volcanol Geotherm Res 188:186–196. https://doi.org/10.1016/j.jvolgeores.2008.11.030
Wallace G, Bergantz GW (2002) Wavelet-based correlation (WBC) of zoned crystal populations and magma mixing. Earth Planet Sci Lett 202:133–145
Wallace PJ, Anderson AT et al (1995) Quantification of pre-eruptive exsolved gas contents in silicic magmas. Nature 377:612–616
Wark DA, Watson EB (2006) TitaniQ: a titanium-in-quartz geothermometer. Contrib Mineral Petrol 152:743–754. https://doi.org/10.1007/s00410-006-0132-1
Wark DA, Hildreth W, Spear FS et al (2007) Pre-eruption recharge of the Bishop magma system. Geology 35:235–238. https://doi.org/10.1130/G23316A.1
Watts KE, Bindeman IN, Schmitt AK (2012) Crystal scale anatomy of a dying supervolcano: an isotope and geochronology study of individual phenocrysts from voluminous rhyolites of the Yellowstone caldera. Contrib Mineral Petrol 164(1):45–67
Wilke S, Holtz F, Neave DA, Almeev R (2017) The effect of anorthite content and water on quartz-feldspar cotectic compositions in the rhyolitic system and implications for geobarometry. J Petrol 58:789–818. https://doi.org/10.1093/petrology/egx034
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 47:35–69. https://doi.org/10.1093/petrology/egi066
Wilson CJN, Stelten ME, Lowenstern JB (2018) Contrasting perspectives on the Lava Creek Tuff eruption, Yellowstone, from new U-Pb and 40Ar/39Ar age determinations. Bull Volcanol 80(6):53
Wotzlaw JF, Bindeman IN, Stern RA et al (2015) Rapid heterogeneous assembly of multiple magma reservoirs prior to Yellowstone supereruptions. Sci Rep 5:1–10. https://doi.org/10.1038/srep14026
Zellmer GF, Clavero JE (2006) Using trace element correlation patterns to decipher a sanidine crystal growth chronology: an example from Taapaca volcano, Central Andes. J Volcanol Geotherm Res 156:291–301. https://doi.org/10.1016/j.jvolgeores.2006.03.004
Zhang Y (2008) Geochemical kinetics. Princeton University Press, Princeton, p 656
Acknowledgements
Thanks to the National Park Service for the scientific permit (YELL-2015-SCI-6078) that made this research possible. We thank Matt Coble (Stanford-U.S. Geological Survey SHRIMP-RG lab) for assistance during CL imaging as well as Axel Wittman and Maitrayee Bose (Arizona State University) for assistance with the electron microprobe and NanoSIMS analyses respectively. Thank you to Mark Ghiorso for helpful discussions regarding rhyolite-MELTS modeling. The authors would also like to thank Tim Druitt and Mary Reid for their thoughtful and constructive comments that improved this manuscript. This study was supported by an NSF CAREER Grant EAR-1654584 to Till.
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Shamloo, H.I., Till, C.B. Decadal transition from quiescence to supereruption: petrologic investigation of the Lava Creek Tuff, Yellowstone Caldera, WY. Contrib Mineral Petrol 174, 32 (2019). https://doi.org/10.1007/s00410-019-1570-x
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DOI: https://doi.org/10.1007/s00410-019-1570-x