Physics and Chemistry of Minerals

, Volume 44, Issue 6, pp 431–444 | Cite as

A Brillouin scattering study of hydrous basaltic glasses: the effect of H2O on their elastic behavior and implications for the densities of basaltic melts

  • Lei Wu
  • De-Bin Yang
  • Jun-Xiu Liu
  • Bo Hu
  • Hong-Sen Xie
  • Fang-Fei Li
  • Yang Yu
  • Wen-Liang Xu
  • Chun-Xiao Gao
Original Paper
First Online:
Received:
Accepted:
  • 196 Downloads

Abstract

Hydrous basalt glasses with water contents of 0–6.82% were synthesized using a multi-anvil press at 1.0–2.0 GPa and 1200–1400 °C. The starting materials were natural Mesozoic basalts from the eastern North China Craton (NCC). Their sound velocities and elastic properties were measured by Brillouin scattering spectroscopy. The longitudinal (V P) and shear (V S) wave velocities decreased with increasing water content. Increasing the synthesis pressure resulted in the glass becoming denser, and finally led to an increase in V P. As the degree of depolymerization increased, the V P, V S, and shear and bulk moduli of the hydrous basalt glasses decreased, whereas the adiabatic compressibility increased. The partial molar volumes of water (\(\nu\)) under ambient conditions were independent of composition, having values of 11.6 ± 0.8, 10.9 ± 0.6 and 11.5 ± 0.5 cm3/mol for the FX (Feixian), FW (Fuxin), and SHT (Sihetun) basalt glasses, respectively. However, the \({{V}_{{{\text{H}}_{\text{2}}}\text{O}}}\) values measured at elevated temperatures and pressures are increasing with increasing temperature or decreasing pressure. The contrasting densities of these hydrous basalt melts with those previously reported for mid-ocean ridge basalt and preliminary reference Earth model data indicate that hydrous basalt melts may not maintain gravitational stability at the base of the upper mantle.

Keywords

Brillouin scattering North China Craton Hydrous basalt glass 
This is a preview of subscription content, log in to check access.

Notes

Acknowledgements

We thank Professor Xia Qun-ke for technical support on the electron microprobe and infrared absorption spectroscopy experiments. We also thank Professor Liu Qiong for hospitality and stimulating discussions. This work was financially supported by (Grant No. 91014004, 11374121 and 11074094), China Postdoctoral Science Foundation (Grant No. 2013M540243), the Fundamental Research Funds for Jilin University, China (Grant No. 450060491500) and the Special fund of the West Light Foundation of CAS.

References

  1. Agee CB (1998) Crystal-liquid density inversions in terrestrial and lunar magmas. Phys Earth Planet Inter 107:63–74CrossRefGoogle Scholar
  2. Armstrong J (1989) CITZAF: combined ZAF and phi-rho (Z) electron beam correction programs. California Institute of Technology, PasadenaGoogle Scholar
  3. Bercovici D, Karato, S-i (2003) Whole-mantle convection and the transition-zone water filter. Nature 425(6953):39–44CrossRefGoogle Scholar
  4. Bouhifd AM, Whittington A, Richet P (2001) Partial molar volume of water in phonolitic glasses and liquids. Contrib Mineral Petrol 142(2):235–243CrossRefGoogle Scholar
  5. Chopelas A, Boehler R (1989) Thermal expansion measurements at very high pressure, systematics, and a case for a chemically homogeneous mantle. Geophys Res Lett 16(11):1347–1350CrossRefGoogle Scholar
  6. Fan W and Menzies M (1992) Destruction of aged lower lithosphere and accretion of asthenosphere mantle beneath eastern China. Geotecton et Metallog 16:171–180Google Scholar
  7. Gao S, Rudnick RL, Carlson RW, McDonough WF, Liu Y-S (2002) Re–Os evidence for replacement of ancient mantle lithosphere beneath the North China craton. Earth Planet Sci Lett 198:307–322CrossRefGoogle Scholar
  8. Gao S, Rudnick RL, Xu W-L, Yuan H-L, Liu Y-S, Walker RJ, Puchtel IS, Liu X, Huang H, Wang X-R (2008) Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China Craton. Earth Planet Sci Lett 270:41–53CrossRefGoogle Scholar
  9. Guillermet AF (1986) The pressure dependence of the expansivity and of the Anderson–Grüneisen parameter in the Murnaghan approximation. J Phys Chem Solids 47:605–607CrossRefGoogle Scholar
  10. Hirschmann MM (2006) Water, melting, and the deep Earth H2O cycle. Annu Rev Earth Planet Sci 34:629–653CrossRefGoogle Scholar
  11. Ihinger PD, Zhang Y, Stolper EM (1999) The speciation of dissolved water in rhyolitic melt. Geochim Cosmochim Acta 63:3567–3578CrossRefGoogle Scholar
  12. Karato SI (1995) Effects of water on seismic wave velocities in the upper mantle. Proceedings of the Japan Academy. Ser B Phys Biol Sci 71(2):61–66Google Scholar
  13. Karato SI, Jung H (1998) Water, partial melting and the origin of the seismic low velocity and high attenuation zone in the upper mantle. Earth Planet Sci Lett 157(3–4):193–207CrossRefGoogle Scholar
  14. Kawamoto T, Holloway JR (1997) Melting temperature and partial melt chemistry of H2O-saturated mantle peridotite to 11 gigapascals. Science 276(5310):240–243CrossRefGoogle Scholar
  15. Lee SK, Yi YS, Cody GD, Mibe K, Fei Y, Mysen BO (2011) Effect of network polymerization on the pressure-induced structural changes in sodium aluminosilicate glasses and melts: 27Al and 17O solid-state NMR study. J Phys Chem C 116(3):2183–2191CrossRefGoogle Scholar
  16. Litasov K, Ohtani E (2002) Phase relations and melt compositions in CMAS–pyrolite–H2O system up to 25 GPa. Phys Earth Planet Inter 134(1):105–127CrossRefGoogle Scholar
  17. Liu DY, Nutman AP, Compston W, Wu JS, Shen QH (1992) Remmants of ≥ 3800 Ma crust in the Chinese part of the Sino-Korean craton. Geology 20:339–342CrossRefGoogle Scholar
  18. Malfait WJ, Xue X (2010) The nature of hydroxyl groups in aluminosilicate glasses: Quantifying Si–OH and Al–OH abundances along the SiO2–NaAlSiO4 join by 1H, 27Al–1H and 29Si-1H NMR spectroscopy. Geochim Cosmochim Acta 74:719–737CrossRefGoogle Scholar
  19. Malfait WJ, Sanchez-Valle C, Ardia P, Medard E, Lerch P (2011) Amorphous materials: properties, structure, and durability: compositional dependent compressibility of dissolved water in silicate glasses. Am Mineral 96:1402–1409CrossRefGoogle Scholar
  20. Malfait WJ, Seifert R, Petitgirard S, Mezouar M, Sanchez-Valle C (2014a) The density of andesitic melts and the compressibility of dissolved water in silicate melts at crustal and upper mantle conditions. Earth Planet Sci Lett 393:31–38Google Scholar
  21. Malfait WJ, Seifert R, Petitgirard S, Perrillat J P, Mezouar M, Ota T, Sanchez-Valle C (2014b) Melt buoyancy in large silicic magma chambers as a viable trigger of supervolcano eruptions. Nat Geosci 7:122–125Google Scholar
  22. Manghnani MH, Williams Q, Dingwell DB (2013) A high-temperature Brillouin scattering study on four compositions of haplogranitic glasses and melts: high-frequency elastic behavior through the glass transition. Am Mineral 98:367–375CrossRefGoogle Scholar
  23. Matsukage KN, Jing Z, Karato S-i (2005) Density of hydrous silicate melt at the conditions of Earth’s deep upper mantle. Nature 438:488–491CrossRefGoogle Scholar
  24. Menzies MA, Fan WM, Zhang M (1993) Palaeozoic and Cenozoic lithoprobes and the loss of >120 km of Archaean lithosphere, Sino-Korean craton, China. In: Prichard HM, Alabaster T, Harris NBW (eds.) Magmatic Processes and Plate Tectonics. Geological Society London Special Publications, London 76:71–81Google Scholar
  25. Mock R, Hillebrands B, Sandercock R (1987) Construction and performance of a Brillouin scattering set-up using a triple-pass tandem Fabry-Perot interferometer. J Phys E Sci Instrum 20(6):656CrossRefGoogle Scholar
  26. Ochs FA, Lange RA (1997) The partial molar volume, thermal expansivity, and compressibility of H2O in NaAlSi3O8 liquid: new measurements and an internally consistent model. Contrib Mineral Petrol 129(2–3):155–165CrossRefGoogle Scholar
  27. Ochs FA, Lange RA (1999) The density of hydrous magmatic liquids. Science 283(5406):1314–1317CrossRefGoogle Scholar
  28. Ohlhorst S, Behrens H, Holtz F (2001) Compositional dependence of molar absorptivities of near-infrared OH-and H2O bands in rhyolitic to basaltic glasses. Chem Geol 174:5–20CrossRefGoogle Scholar
  29. Ohtani E, Maeda M (2001) Density of basaltic melt at high pressure and stability of the melt at the base of the lower mantle. Earth Planet Sci Lett 193(1):69–75CrossRefGoogle Scholar
  30. Pei F, Xu W, Wang Q, Wang D, Lin J (2004) Mesozoic basalt and mineral chemistry of the mantle-derived xenocrysts in Feixian, Western Shandong, China: constraints on nature of Mesozoic lithospheric mantle. Geological Journal of China Universities 10:88Google Scholar
  31. Peslier AH, Luhr JF, Post J (2002) Low water contents in pyroxenes from spinel-peridotites of the oxidized, sub-arc mantle wedge. Earth Planet Sci Lett 201:69–86CrossRefGoogle Scholar
  32. Revenaugh J, Sipkin S (1994) Seismic evidence for silicate melt atop the 410-km mantle discontinuity. Nature 369:474–476CrossRefGoogle Scholar
  33. Richet P, Whittington A, Holtz F, Behrens H, Ohlhorst S, Wilke M (2000) Water and the density of silicate glasses. Contrib Mineral Petrol 138(4):337–347CrossRefGoogle Scholar
  34. Sakamaki T, Suzuki A, Ohtani E (2006) Stability of hydrous melt at the base of the Earth’s upper mantle. Nature 439:192–194CrossRefGoogle Scholar
  35. Sakamaki T, Ohtani E, Urakawa S, Suzuki A, Katayama Y (2009) Measurement of hydrous peridotite magma density at high pressure using the X-ray absorption method. Earth Planet Sci Lett 287:293–297CrossRefGoogle Scholar
  36. Seifert WK, Moldowan JM (1981) Paleoreconstruction by biological markers. Geochim Cosmochim Acta 45:783–794CrossRefGoogle Scholar
  37. Seifert R, Malfait WJ, Petitgirard S, Sanchez-Valle C (2013) Density of phonolitic magmas and time scales of crystal fractionation in magma chambers. Earth Planet Sci Lett 381:12–20CrossRefGoogle Scholar
  38. Stolper E (1982) Water in silicate glasses: an infrared spectroscopic study. Contrib Mineral Petrol 81:1–17CrossRefGoogle Scholar
  39. Suzuki A, Ohtani E, Kato T (1998) Density and thermal expansion of a peridotite melt at high pressure. Phys Earth Planet Inter 107:53–61CrossRefGoogle Scholar
  40. Tammann G, Jenckel E (1929) Die Zunahme der Dichte von Gläsern nach Erstarrung unter erhöhtem Druck und die Wiederkehr der natürlichen Dichte durch Temperatursteigerung. Zeitschrift für anorganische allgemeine Chemie 184:416–420CrossRefGoogle Scholar
  41. Tkachev S, Manghnani M, Williams Q (2005) In situ brillouin spectroscopy of a pressure-induced apparent second-order transition in a silicate glass. Phys Rev Lett 95:57402CrossRefGoogle Scholar
  42. Wan Y, Wang S, Liu D, Wang W, Kröner A, Dong C, Yang E, Zhou H, Hangqian X, Ma M (2012) Redefinition of depositional ages of Neoarchean supracrustal rocks in western Shandong Province, China: SHRIMP U–Pb zircon dating. Gondwana Res 21:768–784CrossRefGoogle Scholar
  43. Wang D, Xu W, Feng H, Lin J, Zheng C (2002) Nature of Late Mesozoic lithospheric mantle in western Liaoning Province: evidences from basalt and the mantle-derived xenoliths. J Jilin Univ 32:319 (Chinese)Google Scholar
  44. Wang W, Yang EX, Zhai MG, Wang SJ, Santosh M, Du LL, Xie HQ, Lv B, Wan YS (2013) Geochemistry of ~2.7 Ga basalts from Taishan area: constraints on the evolution of early Neoarchean granite-greenstone belt in western Shandong Province, China. Precambrian Res 224:94–109CrossRefGoogle Scholar
  45. Whitfield CH, Brody EM, Bassett WA (1976) Elastic moduli of NaCl by Brillouin scattering at high pressure in a diamond anvil cell. Rev Sci Instrum 47:942–947CrossRefGoogle Scholar
  46. Whittington AG, Richet P, Polian A (2012) Water and the compressibility of silicate glasses: a Brillouin spectroscopic study. Am Mineral 97:455–467CrossRefGoogle Scholar
  47. Williams Q, Garnero EJ (1996) Seismic evidence for partial melt at the base of Earth’s mantle. Science 273:1528CrossRefGoogle Scholar
  48. Wu F-Y, Ge W-C, Sun D-Y (2003) Discussions on the lithospheric thinning in eastern China. Earth Sci Front 10:51–60 (in Chinese).Google Scholar
  49. Wu L, Yang D-B, Xie H-S, Li F-F, Hu B, Yu Y, Xu W-L, Gao C-X (2014) Pressure-induced elastic and structural changes in hydrous basalt glasses: the effect of H2O on the gravitational stability of basalt melts at the base of the upper mantle. Earth Planet Sci Lett 406:165–173CrossRefGoogle Scholar
  50. Xia Q-K, Hao Y, Li P, Deloule E, Coltorti M, Dallai L, Yang X, Feng M (2010) Low water content of the Cenozoic lithospheric mantle beneath the eastern part of the North China Craton. J Geophys Res 115:B07207CrossRefGoogle Scholar
  51. Xie H-S, Zhang Y-M, Xu H-G, Hou W, Guo J, Zhao H (1993) A new method of measurement for elastic-wave velocities in minerals and rocks at high-temperature and high-pressure and its significance. Sci China Ser B-Chem 36(10):1276–1280Google Scholar
  52. Xu Y-G (2001) Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in China: evidence, timing and mechanism. Phys Chem Earth Part A Solid Earth Geod 26:747–757.CrossRefGoogle Scholar
  53. Xu WL, Zheng CQ, Wang DY (1999) Discovery of mantle- and lower crust-derived xenoliths in Mesozoic trachybasalts from western Liaoning, and their geological implications. Geol Rev 45:444–449 (in Chinese).Google Scholar
  54. Xu YG, Huang X-L, Ma J-L, Wang Y-B, Iizuka Y, Xu J-F, Wang Q, Wu X-Y (2004) Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton: constraints from SHRIMP zircon U–Pb chronology and geochemistry of Mesozoic plutons from western Shandong. Contrib Mineral Petrol 147:750–767CrossRefGoogle Scholar
  55. Xu WL, Hergt JM, Gao S, Pei FP, Wang W, Yang DB (2008) Interaction of adakitic melt–peridotite: implications for the high-Mg# signature of Mesozoic adakitic rocks in the eastern North China Craton. Earth Planet Sci Lett 265:123–137CrossRefGoogle Scholar
  56. Xu WL, Yang DB, Gao S, Pei FP, Yu Y (2010) Geochemistry of peridotite xenoliths in Early Cretaceous high-Mg# diorites from the Central Orogenic Block of the North China Craton: the nature of Mesozoic lithospheric mantle and constraints on lithospheric thinning. Chem Geol 270:257–273CrossRefGoogle Scholar
  57. Xu W-L, Zhou Q-J, Pei F-P, Yang D-B, Gao S, Li Q-L, Yang Y-H (2013) Destruction of the North China Craton: delamination or thermal/chemical erosion? Mineral chemistry and oxygen isotope insights from websterite xenoliths. Gondwana Res 23:119–129CrossRefGoogle Scholar
  58. Yan Z-T (2000) An approximate relation between cubical thermal expansion coefficient of solids and pressure. Chin J High Press Phys 14:4Google Scholar
  59. Yang W, Li S (2008) Geochronology and geochemistry of the Mesozoic volcanic rocks in Western Liaoning: implications for lithospheric thinning of the North China Craton. Lithos 102:88–117CrossRefGoogle Scholar
  60. Yang D-B, Xu W-L, Pei F-P, Yang C-H, Wang Q-H (2012) Spatial extent of the influence of the deeply subducted South China Block on the southeastern North China Block: constraints from Sr–Nd–Pb isotopes in Mesozoic mafic igneous rocks. Lithos 136–139:246–260CrossRefGoogle Scholar
  61. Yin CQ, Zhao GC, Guo JH, Sun M, Zhou XW, Zhang J, Xia XP, Liu CH (2011) U-Pb and Hf isotopic study of zircons of the Helanshan Complex: constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Lithos 122:25–38CrossRefGoogle Scholar
  62. Yoshino T, Manthilake G, Matsuzaki T, Katsura T (2008) Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite. Nature 451:326–329CrossRefGoogle Scholar
  63. Zhai M, Guo J, Liu W (2005) Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton: a review. J Asian Earth Sci 24:547–561CrossRefGoogle Scholar
  64. Zhang Y, Stolper EM (1991) Water diffusion in a basaltic melt. Nature 351:306–309CrossRefGoogle Scholar
  65. Zhang H-F, Zheng J-P (2003) Geochemical characteristics and petrogenesis of Mesozoic basalts from the North China Craton: a case study in Fuxin, Liaoning Province. Chin Sci Bull 48(9):924–930CrossRefGoogle Scholar
  66. Zhao G-C, Guo J-H (2012) Precambrian geology of China: preface. Precambrian Res 221–222:1–12CrossRefGoogle Scholar
  67. Zhao GC, Wilde SA, Cawood PA, Sun M (2002) SHRIMP U-Pb zircon ages of the Fuping Complex: implications for accretion and assembly of the North China Craton. Am J Sci 302:191–226CrossRefGoogle Scholar
  68. Zhao GC, Wilde SA, Sun M, Li SZ, Li XP, Zhang J (2008) SHRIMP U-Pb zircon ages of granitoid rocks in the Lüliang Complex: implications for the accretion and evolution of the Trans-North China Orogen. Precambrian Res 160:213–226CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2017

Authors and Affiliations

  • Lei Wu
    • 1
    • 2
  • De-Bin Yang
    • 1
  • Jun-Xiu Liu
    • 1
  • Bo Hu
    • 1
  • Hong-Sen Xie
    • 2
  • Fang-Fei Li
    • 1
  • Yang Yu
    • 1
  • Wen-Liang Xu
    • 1
  • Chun-Xiao Gao
    • 1
  1. 1.State Key Laboratory of Superhard Materials, College of Earth SciencesJilin UniversityChangchunChina
  2. 2.Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of GeochemistryChinese Academy of SciencesGuiyangChina

Personalised recommendations