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Characterization of some selected mud volcanoes of southern Taiwan

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In the present study, some mud volcanoes in Pingtung and Kaohsiung areas were selected. The selected mud volcanoes are located above the mud diaper system in southern Taiwan. Three different sampling techniques were used to collect samples in and around the said mud volcanoes. The results show that river water samples from different places fall on the meteoric line. Mud samples are found to be heavier in oxygen isotope while hydrogen isotope remains the same. Soil gas samples were also collected at the depth of 1 m and dissolved gases from the mud volcanic site (or nearby) were collected for gas chromatography analyses. Soil gas samples and dissolved gas from mud pool and groundwater were analyzed for radon concentration using RAD7 (solid-state nuclear track detector) bi-weekly. Long-term investigation will be needed to understand the relationship of mud volcanoes the eruption cycle with gas composition variations. It will also help to understand their relationship with tectonic activities in the region.
Czasopismo
Rocznik
Strony
1257--1265
Opis fizyczny
Bibliogr. 23 poz.
Twórcy
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
  • Department of Geosciences National Taiwan University Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
autor
  • National Center for Research on Earthquake Engineering NARL Taipei Taiwan
  • Department of Earth Sciences and Institute of Geophysics National Central University Jhongli Taiwan
Bibliografia
  • 1. Albarello D (2005) Physical models of mud volcanoes, mud volcanoes as natural strainmeters: a working hypothesis. In: Martinelli G, Panahi B (eds) Mud volcanoes, geodynamics, and seismicity. Springer, Dordrecht, pp 239–249
  • 2. Chow J, Lee JS, Liu CS, Lee BD, Watkins JS (2001) A submarine canyon as the cause of a mud volcano: Liuchieuyu Island in Taiwan. Mar Geol 176:55–63
  • 3. Dimitrov LI (2002) Mud volcanoes-the most important pathway for degassing deeply buried sediments. Earth Sci Rev 59:49–76
  • 4. Etiope G, Klusman RW (2002) Geologic emissions of methane to the atmosphere. Chemosphere 49:777–789
  • 5. Etiope G, Caracausi A, Favara R, Italiano F (2002) Methane emission from the mud volcanoes of Sicily (Italy). Geophys Res Lett 29(14):340–343
  • 6. Higgins GE, Saunders JB (1974) Mud volcanoes—their nature and origin. Verh Naturforsch Ges Basel 84:101–152
  • 7. Judd A, Davies G, Wilson J, Homes R, Baron G, Bryden L (1997) Contribution to atmospheric methane by natural seepages on the UK continental shelf. Mar Geol 137:165–189
  • 8. Judd AG, Hovland M, Dimitrov LI, Gil SG, Jukes V (2002) The geological methane budget at continental margins and its influence on climate change. Geofluids 2:109–126
  • 9. Kopf AJ (2002) Significance of mud volcanism. Rev Geophys 40(2):1,005. https://doi.org/10.1029/2000rg000093
  • 10. Kopf AJ (2003) Comment on the paper ‘‘Methane emission from the mud volcanoes of Sicily (Italy)’’ by Etiope et al. Geophys Res Lett. https://doi.org/10.1029/2000gl015821
  • 11. Kopf A, Deyhle A, Lavrushin VY, Polyak BG, Gieskes JM, Buadnidze GI, Wallmann K, Eisenhauer A (2003) Isotopic evidence (He, B, C) for deep fluid and mud mobilization from mud volcanoes in the Caucasus continental collision zone. Int J Earth Sci (Geol Rund). https://doi.org/10.1007/s00531-003-0326-y
  • 12. Kopf A, Delisle G, Faber E, Panahi B, Aliyev CS, Guliyev I (2010) Long term in situ monitoring at Dashgil mud volcano, Azerbaijan: a link between seismicity, pore-pressure transients and methane emission. Int J Earth Sci (Geol Rundsch) 99(suppl 1):S227–S240. https://doi.org/10.1007/s00531-009-0487-4
  • 13. Lee H-F, Yang TF, Tefang Faith Lan TF, Song S-R, Tsao S (2005) Fumarolic gas composition of the Tatun Volcano Group, Northern Taiwan. TAO 16(4):843–864
  • 14. Liu CS, Huang IL, Teng LS (1997) Structural features off southwestern Taiwan. Mar Geol 137:305–319
  • 15. Martinelli G, Panahi B (2005) Mud volcanoes, geodynamics, and seismicity. Springer, Dordrecht
  • 16. Milkov AV (2000) Worldwide distribution of submarine mud volcanoes and associated gas hydrates. Mar Geol 167:29–42
  • 17. Milkov AV, Sassen R, Apanasovich TV, Dadashev FG (2003) Global gas flux from mud volcanoes: a significant source of fossil methane in the atmosphere and the ocean. Geophys Res Lett 30(2):1,037. https://doi.org/10.1029/2002gl016358
  • 18. Rhakmanov RR (1987) Mud volcanoes and their importance in forecasting of subsurface petroleum potential. Nedra, Moscow, p 1987 (in Russian)
  • 19. Shih TT (1967) A survey of the active mud volcanoes in Taiwan and a study of their types and the character of the mud. Petrol Geol Taiwan 5:259–311
  • 20. Wang S, Hsu ML, Yang CF (1988) Mud volcanoes of Taiwan. Ann Taiwan Mus 31:31–49 (in Chinese with English abstract)
  • 21. Yang TF (2002) 3He/4He ratios of fluid samples around Taiwan. Geochim Cosmochim Acta 66:A859
  • 22. Yang TF, Yeh G-H, Fu C-C, Wang C-C, Lan T-F, Lee H-F, Chen C-H, Walia V, Quo-Cheng Sung Q-C (2004) Composition and exhalation flux of gases from mud volcanoes in Taiwan. Environ Geol 46:1003–1011
  • 23. Yassir NA (1987) Mud volcanoes: evidence of neotectonic activity. Memoir Geol Soc China 9:513–524
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-32080515-56ce-4128-b41a-fbb1d15b07a8
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