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Mud Volcanoes in an Active Fore-Arc Setting: A Case Study from the Makran Coastal Belt, SW Pakistan

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Book cover Tsunamis and Earthquakes in Coastal Environments

Part of the book series: Coastal Research Library ((COASTALRL,volume 14))

Abstract

The Makran coastal belt is over 1000 km long stretching from Iran to east of Karachi in Pakistan. A major active subduction zone known as Makran subduction zone defined by the under thrusting of the Arabian plate beneath the Eurasian plate runs parallel to the coastline. The subduction zone is associated with a thick accretionary sedimentary wedge deposited in an active fore-arc basin containing very thick detrital sediments contributed by the accretion of the subducting plate since Late Eocene time. The sediments in the fore-arc basin are fine-grained usually of clay size fraction deposited in highly fluidized conditions trapping methane gas. The fluidized mud diapirically moves upward along weak zones as mud volcanoes due to high sedimentation rates and escaping gas pressure piercing through the overlying sediment layers. The development of mud volcanoes shows a close relationship between the sedimentation rates, gas escape from sediments and tectonic activity. Mud volcanoes are found in abundance both onshore and offshore of the Makran Coast. Most of the onshore mud volcanoes are associated with active fault zones and are believed to be triggered by tectonic activity. Located in the hanging wall of an active subduction zone, the region is seismically highly active and occurrence of major earthquakes exceeding magnitude 7 is a common phenomenon (e.g., Mw = 7.7 2013 Awaran, Mw = 8.2 1945 Makran). The seismic activity of this scale is likely the major triggerer for the emergence of new islands off the Makran coast in the Arabian Sea on regular basis in the past history. The latest of these emerged in 2013 immediately after the Mw = 7.7 Awaran earthquake.

In this chapter we review major mud volcanoes formed along the Makran coastal region by describing their distribution, evolutionary history and mechanism of their formation. The chapter also describes the sudden appearance of islands off Makran coast since 1945 major earthquake and their importance in the geological history of the coastal regions.

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References

  • Barber A, Tjokrosapoetro S, Charlton T (1986) Mud volcanoes, shale diapirs, wrench faults, and mélanges in accretionary complexes, Eastern Indonesia. AAPG Bull 70(11):1729–1741

    Google Scholar 

  • Basov E, Ivanov M (1996) The Late Quaternary mud volcanism in the Black Sea. Lithol Min Res 31(2):191–197

    Google Scholar 

  • Bilham R, Lodi S, Hough S, Bukhary S, Murtaza Khan A, Rafeeqi SFA (2007) Seismic hazard in Karachi, Pakistan: uncertain past, uncertain future. Seismol Res Lett 78(6):601–613

    Article  Google Scholar 

  • Breen NA, Silver EA, Hussong DM (1986) Structural styles of an accretionary wedge south of the Island of Sumba, Indonesia, revealed by Sea MarcII side-scan sonar. Geol Soc Am Bull 97:1250–1261

    Article  Google Scholar 

  • Byrne DE, Sykes LR, Davis DM (1992) Great thrust earthquakes and aseismic slip along the plate boundary of the Makran subduction zone. J Geophys Res 97(B1):449–478

    Article  Google Scholar 

  • Calves G, Schwab AM, Huuse M, Van Rensbergen P, Clift PD, Tabrez AR, Inam A (2010) Cenozoic mud volcano activity along the Indus Fan: offshore Pakistan. Basin Res 22(4):398–413

    Article  Google Scholar 

  • Collier JS, White RS (1990) Mud diapirism within Indus fan sediments: Murray Ridge, Gulf of Oman. Geophys J Int 101:345–353

    Article  Google Scholar 

  • DeJong KA (1982) Tectonics of the Persian Gulf, Gulf of Oman, and southern Pakistan region. In: Nain AEM, Staehli FG (eds) The ocean basins and margins, vol 6, The Indian Ocean. Plenum Press, New York, pp 315–351

    Google Scholar 

  • Delisle G (2004) The mud volcanoes of Pakistan. Environ Geol 46:1024–1029

    Article  Google Scholar 

  • Delisle G, Von Rad U, Andruleit H, Von Daniels CH, Tabrez AR, Inam A (2002) Active mud volcanoes on- and offshore eastern Makran, Pakistan. Int J Earth Sci 91:93–110

    Article  Google Scholar 

  • DeMets C, Gordon RG, Argus DF, Stein S (1990) Current plate motions. Geophys J Int 101:425–478

    Article  Google Scholar 

  • Elliot HM (1857) The history of India as told by its own historians: The Muhammadan period In: Dowson J (ed) 3rd edn. London, Trubner. Reprinted AMS Press, New York 1966

    Google Scholar 

  • Gaedicke C, Schulter H, Roeser HA, Prexl A, Schreckenberger B, Meyer H, Reichert C, Clift P, Amjad S (2002) Origin of the northern Indus Fan and Murray Ridge, Northern Arabian Sea: interpretation from seismic and magnetic imaging. Tectonophysics 355:127–143

    Article  Google Scholar 

  • Harms JC, Chapel HN, Francis DC (1984) The Makran coast of Pakistan: its stratigraphy and hydrocarbon potential. In: Haq BU, Milliman JD (eds) Marine geology and oceanography of Arabian Sea and Coastal Pakistan. Van Nostr and Reinhold, New York, pp 3–26

    Google Scholar 

  • Henry P, Le Pichon X, Lallemant S, Foucher J-P, Westbrook G, Hobart M (1990) Mud volcano field seaward of the Barbados accretionary complex: a deep-towed side scan sonar survey. J Geophys Res 95(B):8917–8929

    Article  Google Scholar 

  • Higgins G, Saunders JB (1974) Mud volcanoes-their nature and origin. In: Jung P, Bolli H, Panchaud R, Saunders J, Schaefer H, Wiedenmayer F (eds) Contributions to the geology and paleobiology of the Caribbean and adjacent areas, vol 84(1). Verhandlungen der Naturforschenden Gesellschaft, Basel, pp 101–152

    Google Scholar 

  • Hunting Survey Corporation Ltd (1961) Reconnaissance geology of part of West Pakistan. Miracle Press, Ottawa, pp 1–550

    Google Scholar 

  • Kassi AM, Khan SD, Bayraktar H, Kasi AM (2014) Newly discovered mud volcanoes in the Coastal Belt of Makran, Pakistan-tectonic implications. Arab J Geosci 7(11):4899–4909

    Article  Google Scholar 

  • Kazmi AH, Abbasi IA (2008) Stratigraphy and historical geology of Pakistan. Department and NCE in Geology, University of Peshawar, Pakistan, 551p

    Google Scholar 

  • Khan MA, Siddiqui RH, Jan MQ (2010) Temporal evolution of Cretaceous to Pleistocene Magmatism in the Chagai Arc, Balochistan. In: Pakistan. 125th Himalaya-Karakoram-Tibet workshop, San Francisco, USA

    Google Scholar 

  • Kukowski N, Schillhorn T, Flueh ER, Huhn K (2000) Newly identified strike-slip plate boundary in the northeastern Arabian Sea. Geology 28(4):355–358

    Article  Google Scholar 

  • Kukowski N, Schillhorn T, Huhn K, von Rad U, Husen S, Flueh ER (2001) Morphotectonics and mechanics of the central Makran accretionary wedge of Pakistan. Mar Geol 173:1–19

    Article  Google Scholar 

  • Leggett JK, Platt J (1984) Structural features of the Makran fore-arc on Landsat imagery. In: Haq BU, Milliman JD (eds) Marine geology and oceanography of Arabian Sea and Coastal Pakistan. Van Nostr and Reinhold, New York, pp 33–43

    Google Scholar 

  • Martin JB, Kastner M, Henry P, Le Pichon X, Lallement S (1996) Chemical and isotopic evidence for sources of fluids in a volcano field seaward of the Barbados accretionary wedge. J Geophys Res 101:20325–20345

    Article  Google Scholar 

  • Minshull TA, White RS (1989) Sediment compaction and fluid migration in the Makran accretionary prism. J Geophys Res 94:7387–7402

    Article  Google Scholar 

  • Platt JP, Leggett JK, Young J, Raza H, Alam S (1985) Large-scale under plating in the Makran accretionary prism, southwest Pakistan. Geology 13:507–511

    Article  Google Scholar 

  • Reimann KU (1989) Makran coastal range, Field report no. 8. Hydrocarbon Development Institute of Pakistan, German Advisory Group, Islamabad (BGR Archive No. 0115480)

    Google Scholar 

  • Schluter HU, Prexl A, Gaedicke C, Roeser H, Reichert C, Meyer H, von Daniels C (2002) The Makran accretionary wedge: sediment thicknesses and ages and the origin of mud volcanoes. Mar Geol 185:219–232

    Article  Google Scholar 

  • Siddiqui RH (2004) Crustal evolution of the Chagai–Raskoh Arc Terrane, Balochistan, Pakistan. Unpublished PhD thesis, National Centre of Excellence in Geology, University of Peshawar, Pakistan

    Google Scholar 

  • Snead RE (1964) Active mud volcanoes of Baluchistan, West Pakistan. Geogr Rev 54:546–560

    Article  Google Scholar 

  • Sondhi VP (1947) The Makran earthquake of 28th November 1945: the birth of new islands. Indian Min 1:154–156

    Google Scholar 

  • Stride AH, Belderson R, Kenyon N (1982) Structural grain, mud volcanoes and other features on the Barbados ridge complex revealed by GLORIA long-range side-scan sonar. Mar Geol 49:187–196

    Article  Google Scholar 

  • Tabrez AR, Inam A (2012) Hydrocarbon potential in the Makran offshore area. Search and Discovery Article #80218 (2012)

    Google Scholar 

  • Tabrez AR, Inam A, Amjad S (1999) Birth of an island “Malan” off Hingol River, Makran, Balochistan. Biogeosciences 8:14–15

    Google Scholar 

  • von Rad U, Schulz H, Riech V, Den Dulk M, Berner U, Sirocko F (1999) Multiple monsoon- controlled break down of oxygen-minimum conditions during the past 30,000years documented in laminated sediments of Pakistan. Palaeogeogr Palaeoclimatol Palaeoecol 152:129–161

    Article  Google Scholar 

  • von Rad U, Berner U, Delisle G, Doose-Rolinski H, Fechner N, Linke P, Lückge A, Roeser HA, Schmaljohann R, Wiedicke M, Sonne 122/130 Scientific Parties (2000) Gas and fluid venting at the Makran accretionary wedge off Pakistan. Geo-Mar Lett 20:10–19

    Article  Google Scholar 

  • Westbrook GK, Smith MJ (1983) Long decollements and mud volcanoes: evidence from the Barbados ridge complex for the role of high pore fluid pressure in the development of an accretionary complex. Geology 11:279–283

    Article  Google Scholar 

  • White RS, Louden KE (1982) The Makran continental margin: Structure of a thickly sedimented convergent plate boundary. In: Watkins JS, Drake CL (eds) Studies in continental margin geology, vol 34. American Association of Petroleum Geologists Memoir, Tulsa, pp 499–518

    Google Scholar 

  • Wiedicke M, Neben S, Spiess V (2001) Mud volcanoes at the front of the Makran accretionary complex, Pakistan. Mar Geol 172:57–73

    Article  Google Scholar 

Download references

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Authors and Affiliations

  1. Department of Earth Science, College of Science, Sultan Qaboos University, Muscat, Sultanate of Oman

    Iftikhar Ahmed Abbasi

  2. Department of Geology, Baluchistan University, Sariab Road, Quetta, Baluchistan, Pakistan

    Din Mohammed Kakar

  3. Karakorum International University, Gilgit, Pakistan

    Mohammed Asif Khan

  4. Department of Civil Engineering, College of Engineering, Sultan Qaboos University, Muscat, Sultanate of Oman

    Ahmed Sana

Authors
  1. Iftikhar Ahmed Abbasi
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  2. Din Mohammed Kakar
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  3. Mohammed Asif Khan
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  4. Ahmed Sana
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Correspondence to Iftikhar Ahmed Abbasi .

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Editors and Affiliations

  1. Villaviciosa, Asturias, Spain

    V. Santiago-Fandiño

  2. Department of Civil Engineering, Tohoku University, Sendai, Japan

    H. Tanaka

  3. Department of Geology and Paleontology, Westfälische Wilhelms-University, Münster, Germany

    M. Spiske

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Abbasi, I.A., Kakar, D.M., Khan, M.A., Sana, A. (2016). Mud Volcanoes in an Active Fore-Arc Setting: A Case Study from the Makran Coastal Belt, SW Pakistan. In: Santiago-Fandiño, V., Tanaka, H., Spiske, M. (eds) Tsunamis and Earthquakes in Coastal Environments. Coastal Research Library, vol 14. Springer, Cham. https://doi.org/10.1007/978-3-319-28528-3_6

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