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Geo-Marine Letters

, Volume 23, Issue 3–4, pp 258–268 | Cite as

Mud and fluid migration in active mud volcanoes in Azerbaijan

  • S. Planke
  • H. Svensen
  • M. Hovland
  • D. A. Banks
  • B. Jamtveit
Original

Abstract

Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed.

Keywords

Azerbaijan Dormant Period Petroleum Migration South Caspian Basin Oilfield Brine 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

This work was partly financed by the Norwegian Research Council grant 120897 to B. Jamtveit/H. Svensen. We would like to thank Statoil for logistic assistance during fieldwork, and Achim Kopf for a constructive review.

References

  1. Abrams MA, Narimanov AA (1997) Geochemical evaluation of hydrocarbons and their potential sources in the western South Caspian depression, Republic of Azerbaijan. Mar Petrol Geol 14:451–468CrossRefGoogle Scholar
  2. Aliyev A, Guliev I, Panahi B (2000) Mud volcanoes’ hazards. Nafta Press, BakuGoogle Scholar
  3. Aliyev A, Guliyev IS, Belov IS (2002) Catalogue of recorded eruptions of mud volcanoes of Azerbaijan. Nafta Press, BakuGoogle Scholar
  4. Balakishiyeva BA, Rashidova TN (1980) Chemical model of Caspian Sea water. Geochem Int 17:133–147Google Scholar
  5. BBC (2001) Azeri mud volcano flares. http://news.bbc.co.uk/1/hi/sci/tech/1626310.stm (link operating in July 2003)
  6. Bottrell SH, Yardley BWD (1991) The distribution of Fe and Mn between chlorite and fluid: evidence from fluid inclusions. Geochim Cosmochim Acta 55:241–244CrossRefGoogle Scholar
  7. Brown KM (1990) The nature and hydrogeologic significance of mud diapirs and diatremes for accretionary systems. J Geophys Res 95:8969–8982Google Scholar
  8. Carpenter AB, Miller JC (1969) Geochemistry of saline subsurface water, Saline County (Missouri). Chem Geol 4:135–167CrossRefGoogle Scholar
  9. Collins AG (1975) Geochemistry of oilfield waters. Elsevier, New YorkGoogle Scholar
  10. Cooper C (2001) Mud volcanoes of Azerbaijan visualized using 3D seismic depth cubes: the importance of overpressured fluid and gas instead of non extant diapirs. In: Abstr Vol Subsurface Sediment Mobilization Conf, 10–13 September, Ghent, Belgium, p 71Google Scholar
  11. Davidson J, De Silva S (2000) Composite volcanoes. In: Sigurdsson H (ed) Encyclopedia of volcanoes. Academic Press, New York, pp 663–681Google Scholar
  12. Devlin WJ et al. (1999) South Caspian Basin: young, cool, and full of promise. GSA Today 9:1–9Google Scholar
  13. Dia AN, Castrec-Rouelle M, Boulègue J, Comeau P (1999) Trinidad mud volcanoes: where do the expelled fluids come from? Geochim Cosmochim Acta 63:1023–1038CrossRefGoogle Scholar
  14. Dimitrov LI (2002) Mud volcanoes—the most important pathway for degassing deeply buried sediments. Earth Sci Rev 59:49–76CrossRefGoogle Scholar
  15. Fitts TG, Brown KM (1999) Stress-induced smectite dehydration: ramifications for patterns of freshening and fluid expulsion in the N. Barbados accretionary wedge. Earth Planet Sci Lett 172:179–197CrossRefGoogle Scholar
  16. Fontes JCh, Matray JM (1993) Geochemistry and origin of formation brines from the Paris Basin, France. 1. Brines associated with Triassic salts. Chem Geol 109:149–175Google Scholar
  17. Fournier RO, Truesdell AH (1973) An empirical Na-K-Ca chemical thermometer for natural waters. Geochim Cosmochim Acta 37:1255–1275CrossRefGoogle Scholar
  18. Fowler SR, Mildenhall J, Zalova S, Riley G, Elsley G, Desplanques A, Guliyev F (2000) Mud volcanoes and structural development on Shah Deniz. J Petrol Sci Eng 28:189–206CrossRefGoogle Scholar
  19. Guliyev IS (2002) South-Caspian depression—an intensive area of hydrocarbon fluid formation and migration. In: Abstr Vol 7th Int Conf Gas in Marine Sediments, 7–12 October 2002, Baku, Azerbaijan. Nafta Press, Baku, pp 66–69Google Scholar
  20. Guliyev IS, Feizullayev AA (1994) Natural hydrocarbon seepages in Azerbaijan. In: Proc AAPG Hedberg Research Conf, 24–28 April, Vancouver, Canada, pp 76–79Google Scholar
  21. Guliyev IS, Feizullayev AA (1996) Geochemistry of hydrocarbon seepages in Azerbaijan. In: Schumacher D, Abrams MA (eds) Hydrocarbon migration and its near surface expression. AAPG Mem 66:63–70Google Scholar
  22. Guliyev IS, Feizullayev AA (1997) All about mud volcanoes. Nafta Press, BakuGoogle Scholar
  23. Guliyev IS, Feizullayev AA, Kadirov FA (2002) Petroleum system in dis-equilibrium basins (in case of South Caspian Basin). Azerbaijan Natl Acad Sci, Geol Inst, Nafta Press, BakuGoogle Scholar
  24. Hanor JS (1994) Origin of saline fluids in sedimentary basins. In: Parnell J (ed) Geofluids: origin, migration and evolution of fluids in sedimentary basins. Geol Soc Spec Publ 78:151–174Google Scholar
  25. Harder H (1970) Boron content of sediments as a tool in facies analysis. Sediment Geol 4:153–175CrossRefGoogle Scholar
  26. Hedberg HD (1974) Relation of methane generation to undercompacted shales, shale diapirs, and mud volcanoes. Am Assoc Petrol Geol Bull 58:661–673Google Scholar
  27. Helios Rybicka E, Calmano W, Breeger A (1995) Heavy metals sorption/desorption on competing clay minerals; and experimental study. Appl Clay Sci 9:369–381CrossRefGoogle Scholar
  28. Higgins GE, Saunders JB (1974) Mud volcanoes—their nature and origin. Verhandl Naturf Ges Basel 84:101–152Google Scholar
  29. Hovland M, Hill A, Stokes D (1997) The structure and geomorphology of the Dashgil mud volcano, Azerbaijan. Geomorphology 21:1–15CrossRefGoogle Scholar
  30. Inan S, Namik Yalcin M, Guliev IS, Kuliev K, Feizullayev AA (1997) Deep petroleum occurrences in the Lower Kura Depression, South Caspian Basin, Azerbaijan: an organic geochemical and basin modelling study. Mar Petrol Geol 14:731–762CrossRefGoogle Scholar
  31. Ishikawa T, Nakamura E (1993) Boron isotope systematics of marine sediments. Earth Planet Sci Lett 117:567–580CrossRefGoogle Scholar
  32. Jakubov AA, Ali-Zade AA, Zeinalov MM (1971) Mud volcanoes of the Azerbaijan SSR: atlas (in Russian). Azerbaijan Academy of Sciences, BakuGoogle Scholar
  33. Jamtveit B, Svensen H, Podladchikov YY, Planke S (2003) Hydrothermal vent complexes associated with sill intrusions in sedimentary basins. J Geol Soc Lond Spec Publ (in press)Google Scholar
  34. Kadirov F, Guliyev IS, Kadirov A, Feyzullayev A, Mukhtarov A (2002) Model of mud volcano by the geophysical, geodetic and geochemical data. In: Abstr Vol 7th Int Conf Gas in Marine Sediments, 7–12 October 2002, Baku, Azerbaijan. Nafta Press, Baku, pp 105–107Google Scholar
  35. Katz B, Richards D, Long D, Lawrence W (2000). A new look at the components of the petroleum system of the South Caspian Basin, J Petrol Sci Eng 28:161–182Google Scholar
  36. Kopf A (2002) Significance of mud volcanism. Rev Geophys 40(2):1005 DOI 10.1029/2000RG000093CrossRefGoogle Scholar
  37. Kopf A, Behrmann JH (2000). Extrusion dynamics of mud volcanoes on the Mediterranean Ridge accretionary complex. Geol Soc Spec Publ 174:169–204Google Scholar
  38. Kopf A, Deyhle A (2002) Back to the roots: boron geochemistry of mud volcanoes and its implications for mobilization depth and global B cycling. Chem Geol 192:195–210CrossRefGoogle Scholar
  39. Lagunova IA (1974) On the origin of carbon dioxide in the gases of mud volcanoes of the Kerch’-Taman’ region. Geochem Int 11:1209–1214Google Scholar
  40. Lagunova IA (1976) Origin of boron in waters of mud volcanoes. Int Geol Rev 18:929–934Google Scholar
  41. Martin JB, Kastner M, Henry P, Le Pichon X, Lallement S (1996) Chemical and isotopic evidence for sources of fluids in a mud volcano field seaward of the Barbados accretionary wedge. J Geophys Res 101:20,325–20,345Google Scholar
  42. Mason B (1966) Principles of geochemistry, 3rd edn. Wiley, New YorkGoogle Scholar
  43. McCaffrey MA, Lazar B, Holland HD (1987) The evaporation path of seawater and the coprecipitation of Br− and K+ with halite. J Sediment Petrol 57:928–937Google Scholar
  44. Milkov AV (2000) Worldwide distribution of submarine mud volcanoes and associated gas hydrates. Mar Geol 167:29–42CrossRefGoogle Scholar
  45. Moore C, Vrolijk P (1992) Fluids in accretionary prisms. Rev Geophys 30:113–135Google Scholar
  46. Nadirov RS, Bagirov E, Tagiyev M (1997) Flexural plate subsidence, sedimentation rates, and structural development of the super-deep South Caspian Basin. Mar Petrol Geol 14:383–400CrossRefGoogle Scholar
  47. Narimanov AA, Akperov NA, Abdullaev TI (1998) The Bahar oil and gas-condensate field in the South Caspian Basin. Petrol Geosci 4:253–258Google Scholar
  48. Ransom B, Helgeson HC (1995) A chemical and thermodynamical model of dioctahedral 2:1 layer clay minerals in diagenetic processes: dehydration of dioctahedral aluminous smectite as a function of temperature and depth in sedimentary basins. Am J Sci 295:245–281Google Scholar
  49. Rittenhouse G (1967) Bromine in oil-field waters and its use in determining possibilities of origin of these waters. Am Assoc Petrol Geol Bull 51:2430–2440Google Scholar
  50. Sigurdsson H (ed) (2000) Encyclopedia of volcanoes. Academic Press, New YorkGoogle Scholar
  51. Sjögren H (1886) Meddelande om slamvulkanerna i Baku. Geol För För Stockh 8:417–429Google Scholar
  52. Sjögren H (1891) Preliminära meddelande om de kaukasiska naftafälten. Geol För För Stockh 13:223–255Google Scholar
  53. Sokolov VA, Buniat-Zade ZA, Goedekian AA, Dadashev FG (1968) The origin of gases of mud volcanoes and the regularities of their powerful eruptions. In: Advances in organic geochemistry 1968. Pergamon Press, New York, pp 473–484Google Scholar
  54. Svensen H, Planke S, Jamtveit B, Pedersen T (2003) Seep carbonate formation controlled by hydrothermal vent complexes: a case study from the Vøring Basin, the Norwegian Sea. Geo-Mar Lett (in press) DOI 10.1007/s00367-003-0141Google Scholar
  55. Tagiyev MF, Nadirov RS, Bagirov EB (1997) Geohistory, thermal history and hydrocarbon generation history of the north-west South Caspian Basin. Mar Petrol Geol 14:363–382CrossRefGoogle Scholar
  56. Valyaev BM, Grinchenko YI, Erokhin VE, Prokhorov VS, Titkov GA (1985) Isotopic composition of gases from mud volcanoes. Lithol Miner Resources 20:62–75Google Scholar
  57. Williams LB, Hervig RL, Wieser ME, Hutcheon I (2001) The influence of organic matter on the boron isotope geochemistry of the gulf coast sedimentary basins, USA. Chem Geol 174:445–461CrossRefGoogle Scholar
  58. Worden RH (1996) Controls on halogen concentrations in sedimentary formation waters. Mineral Mag 60:259–274Google Scholar
  59. You CF, Spivack AJ, Smith JH, Gieskes JM (1993) Mobilization of boron at convergent margins: implications for boron geochemical cycle. Geology 21:207–210CrossRefGoogle Scholar
  60. You CF, Castillo PR, Gieskes JM, Chan LH, Spivack AJ (1996) Trace element behavior in hydrothermal experiments: implications for fluid processes at shallow depths in subduction zones. Earth Planet Sci Lett 140:41–52Google Scholar

Copyright information

© Springer-Verlag 2003

Authors and Affiliations

  • S. Planke
    • 1
    • 2
  • H. Svensen
    • 2
  • M. Hovland
    • 3
  • D. A. Banks
    • 4
  • B. Jamtveit
    • 2
  1. 1.Volcanic Basin Petroleum Research (VBPR)OsloNorway
  2. 2.Physics of Geological ProcessesUniversity of OsloOsloNorway
  3. 3.StatoilStavangerNorway
  4. 4.School of Earth SciencesUniversity of LeedsLeedsUK

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