The eruptive history and chemical stratigraphy of a post-caldera, steady-state volcano: Yasur, Vanuatu
详细信息 查看全文
- 作者：Chris W. Firth (1)
Heather K. Handley (1)
Shane J. Cronin (2)
Simon P. Turner (1) - 关键词：Tephra chronology ; Volcanic history ; Steady ; state magma chamber ; Thermobarometry ; Yasur
- 刊名：Bulletin of Volcanology
- 出版年：2014
- 出版时间：July 2014
- 年：2014
- 卷：76
- 期：7
- 全文大小：
- 参考文献：1. Albarede F (1985) Regime and trace-element evolution of open magma chambers. Nature 318:356-58 CrossRef
2. Albarede F, Tamagnan V (1988) Modeling the recent geochemical evolution of the Piton de la Fournaise Volcano, Reunion Island 1931-986. J Petrol 29:997-030 CrossRef
3. Albarede F, Luais B, Fitton G, Semet M, Kaminski E, Upton BGJ, Bachelery P, Cheminee J-L (1997) The geochemical regimes of Piton de la Fournaise Volcano (Reunion) during the last 530 000 years. J Petrol 38:171-01 CrossRef
4. Allen SR (2004) Complex spatter- and pumice-rich pyroclastic deposits from an andesitic caldera-forming eruption: the Siwi pyroclastic sequence, Tanna, Vanuatu. Bull Volcanol 67:27-1 CrossRef
5. Allibone R, Cronin SJ, Charley DT, Neall VE, Stewart RB, Oppenheimer C (2012) Dental fluorosis linked to degassing of Ambrym volcano, Vanuatu: a novel exposure pathway. Environ Geochem Health 34:155-70 CrossRef
6. Arrighi S, Principe C, Rosi M (2001) Violent Strombolian and sub-plinian eruptions at Vesuvius during post-1631 activity. Bull Volcanol 63:126-50 CrossRef
7. Boygle J (1999) Variability of tephra in lake and catchment sediments, Svínavatn, Iceland. Glob Planet Chang 21:129-49 CrossRef
8. Burnham CW (1975) Water and magmas; a mixing model. Geochim Cosmochim Acta 39:1077-084 CrossRef
9. Campbell FA (1888) The active volcano on Tanna, New Hebrides, with some remarks on the cause of volcanic action. Proc Roy Soc Victoria 1:73-3
10. Carney JN, McFarlane A (1979) Geology of Tanna, Aneityum, Futuna and Aniwa. New Hebrides Government Geol Survey, pp 5-9
11. Chen JK, Taylor FW, Edwards RL, Cheng H, Burr GS (1995) Recent emerged reef terraces of the Yenkahe resurgent block, Tanna, Vanuatu: implications for volcanic, landslide and tsunami hazards. J Geol 103:577-90 CrossRef
12. Cole JW, Milner DM, Spinks KD (2005) Calderas and caldera structures: a review. Earth-sci Rev 69:1-6
13. Cook J (1777) A voyage round the world, performed in His Britannic Majesty’s ships the Resolution and Adventure, in the years 1772, 1773, 1774 and 1775. 523 pp
14. Cronin SJ, Sharp DS (2002) Environmental impacts on health from continuous volcanic activity at Yasur (Tanna) and Ambrym, Vanuatu. Int J Environ Health Res 12:109-23 CrossRef
15. Eissen J, Blot C, Louat R (1991) Chronologie de l’activite volcanique historique de l’arc insulaier des Nouvelles-Hebrides de 1595 a 1991. ORSTOM Rep:68 pp
16. Francalanci L, Tommasini S, Conticelli S (2004) The volcanic activity of Stromboli in the 1906-998 AD period: mineralogical, geochemical and isotope data relevant to the understanding of the plumbing system. J Volcanol Geotherm Res 131:179-11 CrossRef
17. Francis P, Oppenheimer C, Stevenson D (1993) Endogenous growth of persistently active volcanoes. Nature 366:554-57 CrossRef
18. Frater M (1917) The volcanic eruption of 1913 on Ambrym Island, New Hebrides. Geol Mag 6:496-03 CrossRef
19. Gorman MK, Quinn TM, Taylor FW, Partin JW, Cabioch G, Austin JA, Pelletier B, Ballu V, Maes C, Saustrup S (2012) A coral-based reconstruction of sea surface salinity at Sabine Bank, Vanuatu from 1842 to 2007 CE. Palaeooceanography. doi:10.1029/2012PA002302
20. Grove RH (2007) The great El Ni?o of 1789-3 and its global consequences: reconstructing an extreme climate event in world environmental history. Mediev Hist J 10:75-8 CrossRef
21. GVN Bulletin (1990) Glob Volcan Netw Bull 15(11)
22. GVN Bulletin (1999) Glob Volcan Netw Bull 24(07)
23. Harrison DE, Luther DS (1990) Surface winds from tropical pacific islands-climatological statistics. J Clim 3:251-71 CrossRef
24. Hendy EJ, Gagan MK, Albert CA, McCulloch MT, Lough JM, Isdale PJ (2002) Abrupt decrease in tropical Pacific sea surface salinity at the end of Little Ice Age. Science 295:1511-514 CrossRef
25. Hogg AG, Hua Q, Blackwell PG, Niu M, Buck CE, Guilderson TP, Heaton TJ, Palmer JG, Reimer PJ, Reimer RW, Turney CSM, Zimmerman SRH (2013) SHCAL13 southern hemisphere calibration, 0-0,000?years cal BP. Radiocarbon 55:1889-903 CrossRef
26. Hurles ME, Matisoo-Smith E, Gray RD, Penny D (2003) Untangling oceanic settlement: the edge of the knowable. TRENS Ecol Evol 18:531-40 CrossRef
27. Kanas T, Nango I, Fransser J, Morris S (2000) Lake Siwi to River Siwi. Vanuatu Dept Land Surv 27 pp
28. Keiding JK, Sigmarsson O (2012) Geothermobarometry of the 2010 Eyjafjallj?kull eruption: new constraints on Icelandic magma plumbing systems. J Geophys Res. doi:10.1029/2011JB008829
29. Kelley JL (2008) Glassy tephra of Yasur Volcano, Vanuatu: a magnetic, petrographic and crystallographic study and implications for devitrification. MSc Thesis, Southern Illinois University
30. Kelley PJ, Kyle PR, Dunbar NW, Sims KWW (2008) Geochemistry and mineralogy of the phonolite lava lake, Erebus volcano, Antarctica: 1972-004 and comparison with older lavas. J Volcanol Geotherm Res 177:589-05 CrossRef
31. Kremers S, Lavallee Y, Hanson J, Hess K, Chevrel MO, Wassermann J, Dingwell DB (2012) Shallow magma-mingling-driven Strombolian eruptions at Mt. Yasur volcano, Vanuatu. Geophys Res Lett 39. doi:10.1029/2012GL053312
32. Labillardiere J (1800) Voyage in search of La Perouse. London 655 pp
33. Landi P, Métrich N, Bertagnini A, Rosi M (2004) Dynamics of magma mixing and degassing recorded in plagioclase at Stromboli (Aeolian Archipelago, Italy). Contrib Mineral Petrol 147:213-27 CrossRef
34. Landi P, Corsaro RA, Francalanci L, Civetta L, Miraglia L, Pompilio M, Tesoro R (2009) Magma dynamics during the 2007 Stromboli eruption (Aeolian Islands, Italy): mineralogical, geochemical and isotopic data. J Volcanol Geotherm Res 182:255-68 CrossRef
35. Lowe DJ (2011) Tephrochronology and its application: a review. Quat Geochronol 6:107-53 CrossRef
36. Mastin LG (2001) A simple calculator of ballistic trajectories for blocks ejected during volcanic eruptions. U.S. Geol Survey Open-File Report 01-5, U.S. Geological Survey
37. Merle O, Brothelande E, Lenat JF, Bachelery P, Garaebiti E (2013) A structural outline of the Yenkahe volcanic resurgent dome (Tanna Island, Vanuatu Arc, South Pacific). J Volcanol Geotherm Res 268:64-2 CrossRef
38. Métrich N, Bertagnini A, Di Muro A (2010) Conditions of magma storage, degassing and ascent at Stromboli: new insights into the volcano plumbing system with inferences on the eruptive dynamics. J Petrol 51:603-26 CrossRef
39. Métrich N, Allard P, Aiuppa A, Bani P, Bertagnini A, Shinohara H, Parello F, Di Muro A, Garaebiti E, Belhadj O, Massare D (2011) Magma and volatile supply to post-collapse volcanism and block resurgence in Siwi caldera (Tanna Island, Vanuatu Arc). J Petrol 52:1077-105 CrossRef
40. Moromoto N (1989) Nomenclature of pyroxenes. Can Mineral 27:143-56
41. Nairn IA, Scott BJ, Giggenbach WF (1988) Yasur volcano investigations, Vanuatu. N Z Geol Surv Rep Geol 134, 74 pp
42. Neef G, Zhao JX, Collerson KD, Zhang FS (2003) Late Quaternary uplift and subsidence of the west coast of Tanna, south Vanuatu, southwest Pacific: U-Th ages of raised coral reefs in the Median Sedimentary Basin. Aust J Earth Sci 50:39-8 CrossRef
43. Nimis P (1995) A clinopyroxene geobarometer for basaltic systems based on crystal-structure modelling. Contrib Mineral Petrol 121:115-25 CrossRef
44. Nunn P (2007) Climate, environment and society in the pacific during the last millennium. Dev Earth Environ Sci 6
45. O’Hara MJ (1977) Geochemical evolution during fractional crystallisation of a periodically refilled magma chamber. Nature 266:503-07 CrossRef
46. O’Neill HC, Jenner FE (2012) The global pattern of trace-element distributions in ocean floor basalts. Nature 491:698-04 CrossRef
47. Oppenheimer C, Bani P, Calkins JA, Burton MR, Sawyer GM (2006) Rapid FTIR sensing of volcanic gasses released by Strombolian explosions at Yasur volcano, Vanuatu. Appl Phys B 85:453-60 CrossRef
48. Oppenheimer C, Lomakina AS, Kyle PR, Kingsbury NG, Boichu M (2009) Pulsatory magma supply to a phonolite lava lake. Earth Planet Sci Lett 284:392-98 CrossRef
49. Peltier A, Finizola A, Douillet GA, Brothelande E, Garaebiti E (2012) Structure of an active volcano associated with a resurgent block inferred from thermal mapping: the Yasur-Yenkahe volcanic complex (Vanuatu). J Volcanol Geotherm Res 243-44:59-8 CrossRef
50. Platz T, Cronin SJ, Smith IEM, Turner MB, Stewart RB (2007) Improving the reliability of microprobe based analyses of andesitic glasses for tephra correlation. The Holocene 17:573-83 CrossRef
51. Putirka KD (2008) Thermometers and barometers for volcanic systems. Rev Mineral Geochem 69:61-20 CrossRef
52. Pyle DM (1992) The volume and residence time of magma beneath active volcanoes determined by decay series equilibria methods. Earth Planet Sci Lett 112:61-3 CrossRef
53. Robin C, Eissen JP, Monzier M (1994) Ignimbrites of basaltic andesite and andesite compositions from Tanna, New Hebrides Arc. Bull Volcanol 56:10-2 CrossRef
54. Rosi M, Bertagnini A, Landi P (2000) Onset of the persistent activity at Stromboli Volcano (Italy). Bull Volcanol 62:294-00 CrossRef
55. Stevenson DS, Blake S (1998) Modelling the dynamics and thermodynamics of volcanic degassing. Bull Volcanol 60:307-17 CrossRef
56. Streck MJ, Dungan MA, Malavassi E, Reagan MK, Bussy F (2002) The role of basalt replenishment in the generation of basaltic andesites of the ongoing activity at Arenal volcano, Costa Rica: evidence from clinopyroxene and spinel. Bull Volcanol 64:316-27 CrossRef
57. Taddeucci J, Scarlato P, Capponi A, Del Bello E, Cimarelli C, Palladino DM, Kueppers U (2012) High-speed imaging of Strombolian explosions: the ejection velocity of pyroclasts. Geophys Res Lett 39. doi:10.1029/2011GL050404
58. Turner SP, Peate DW, Hawkesworth CJ, Eggins SM, Crawford AJ (1999) Two mantle domains and the time scales of fluid transfer beneath the Vanuatu Arc. Geology 27:963-66 CrossRef
59. Turner MB, Cronin SJ, Stewart RB, Bebbington M, Smith IEM (2008) Using titanomagnetite textures to elucidate volcanic eruption histories. Geology 36:31-4 CrossRef
60. van Achterbergh E, Ryan CG, Jackson SE, Griffin WL (2001) Data reduction software for LA-ICP-MS. In: Sylvester P (ed) Laser-ablation ICP-MS in the earth sciences: principles and applications. Mineralogical Association of Canada 29:239-43
61. Vanderkluysen L, Harris AJL, Kelfoun K, Bonadonna C, Rieppe M (2012) Bombs behaving badly: unexpected trajectories and cooling of volcanic projectiles. Bull Volcanol 74:1849-858 CrossRef
62. Wadge G (1981) The magma budget of Volcan Arenal, Costa Rica from 1968-980. J Volcanol Geotherm Res 19:281-02 CrossRef
63. Wadge G (1982) Steady-state volcanism: evidence from eruption histories of polygenetic volcanoes. J Geophys Res 87:4035-049 CrossRef
64. Wallace PJ (2005) Volatiles in subduction zone magmas: concentrations and fluxes based on melt inclusion and volcanic gas data. J Volcanol Geotherm Res 140:217-40 CrossRef - 作者单位：Chris W. Firth (1)
Heather K. Handley (1)
Shane J. Cronin (2)
Simon P. Turner (1)
1. GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW, 2109, Australia
2. Volcanic Risk Solutions, IAE, Massey University, Palmerston North, New Zealand - ISSN：1432-0819
文摘
The persistent activity of Yasur volcano, a post-caldera scoria cone in the southern Vanuatu Arc, along with the uniformity exhibited by its eruptive products, indicates that it is a “steady-state-volcano. This implies that rates of magma replenishment and tapping are in equilibrium. Examination of recently exposed tephra sequences suggests that Strombolian-style activity at Yasur has persisted in its current form for the last 630-50?years. Eruption of tephra with uniform grain size and texture throughout this period indicates invariant eruption magnitude and style. Based on tephra accumulation rates, a uniform, time-averaged eruption flux of ?10-80?m3?days? is estimated. Major and trace element analyses of glass shards and mineral grains from these tephra deposits show limited variation in magma composition throughout that time, consistent with a chemically buffered magma reservoir and models for steady-state volcanism. Similarly, mineral crystallisation temperature estimates are within error, suggesting the magma reservoir has retained a constant temperature through this time, while pressure estimates suggest shallow crystallisation. Eruptions appear to be driven by gas release, with small fluctuations in magma chemistry and eruptive behaviour governed by perturbations in volatile flux. This period of steady-state activity was preceded by ?00?years of higher-magnitude, lower-frequency eruptions during which less evolved compositions were erupted. Variation between these two styles of eruptive behaviour may be explained by a shift from a periodically closed to fully opened conduit, allowing more regular magma release and changes to degassing regimes. New radiocarbon ages suggest a period of irregular eruptive behaviour extending >1,400?year?B.P. Overall, a transition from an irregular to a very steady magmatic system has occurred over the past ??kyr. Previously determined tectonic indicators for caldera resurgence in the area suggest revived magma replenishment after a hiatus following the caldera-forming Siwi eruption. This replenishment, while now supplying today’s constant activity, has not yet manifested itself in variations in composition or style/magnitude of eruptions.