Geomorphological and Geochemical Characteristics Mud Volcanoes Near Zendan Fault ,Iran

Document Type : Original Research Article

Author

Department of Geography, Faculty of Human Sciences, Jiroft University, Jiroft, Iran

Abstract

Mud volcanism is a global phenomenon usually associated with compressional tectonics that favor extrusion of fluid- and clay mineral-rich sediment both on land and offshore. Iran's coastal, bordering the western Makran Coast, has more than 50prominent onshore MVs. In this research, after data collection, including topography and geology maps, IRS satellite data and aerial photos, remote sensing verifications were implemented. Then, mud volcanoes determination was completed by field work studies and checking. Their geomorphology characteristic such as area and height were measured. One sediment and one water samples were taken from each mud volcano in the field work, then analyses of major, minor and trace elements were carried out through ICP-OES. About 20 small or big mud volcanoes were determined in Hormozgan province that they have not been introduced before. In the meantime, hydrogeochemistry studies or determination of the percentage of available elements in water for all mud volcanoes were implemented. Since this geomorphological phenomenon indicates tectonic activity of a region, hence there is a possibility of mild earthquake and faulting occurrence. After determine correlation analysis cluster and factor analyiss determine between different factors from scoter plot map characterized that source of elements Al, Fe, Ni, V, Sc, Ti, Cr, Zn, Cu, Mn, Na, K, Li, Be is geogenic and source of elements Ca,Mn and S is biogenic.

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References

Kopp, C., Fruehn, J., Flueh, E.R., Reichet, C., Kukowski, N., Bialas, J. & Klaeschen, D., 2000. Structure of the Makran subduction zone from wide-angle and reflection seismic data, Tectonophysics, 329, 171-191.
Harms, J.C., Cappel, R.N. & Francis, D.C., 1984. The Makran coast of Pakistan: its stratigraphy and hydrocarbon potential. In: Haq, B.U. & Milliman, J.D. (eds) Marine Geology and Oceanography of the Arabian Sea and Coastal Pakistan. Van Nostrand Reinhold, New York, 3-26.
Snead, R., 1964. Active mud-volcanoes of Balochistan, West Pakistan, Geography Review 4, 546-560.
Higgins, G.E. & Saunders, J.B., 1974. Mud volcanoes— their nature and origin. Verh Naturf Ges Basel, 84, 101-152.
Barber, A.J., Tjokrosapoetro, S. & Charlton, T.R., 1986. Mud volcanoes, shale diapirs, wrench faults and me´langes in accretionary complexes, eastern Indonesia, AAPG Bull, 70, 1729-1741.
Kopf, A., Robertson, A.H.F., Clennell, M.B. & Flecker, R., 1998. Mechanism of mud extrusion on the Mediterranean Ridge, Geomarine Lett, 18, 97-114.
Yassir, N.A., 1989. Mud volcanoes and the behaviour of overpressured clays and silts, PhD thesis, University College London, 249.
Hedberg, H., 1974. Relation of methane generation to undercompacted shales, shale diapirs and mud volcanoes, AAPG Bull, 58, 661-673.
Moore, J.C. & Vrolijk, P., 1992. Fluids in accretionary prisms. Rev Geophys, 30, 113-135.
Mellors, R., Kilb, D., Aliyev, A., Gasamov, A. & Yetirmishli, G., 2007. Correlations between earthquakes and large mud volcano eruptions, J Geophys Res, 112, B04304. doi:10.1029/2006JB004489.
Moore, J.C. & Vrolijk, P., 1992. Fluids in accretionary prisms. Rev Geophys, 30, 113-135. Milkov, A.V., 2000. Worldwide distribution of submarine mud volcanoes and associated gas hydrates, Mar Geol, 167, 29-42.
Robertson, A.H.F., 1996. Scientific Party of ODP Leg 160, Mud volcanism on the Mediterranean Ridge: initial results of Ocean Drilling Program Leg 160. Geology, 24, 239-242.
Kopf, A., Stegmann, S., Delisle, G., Panahi, B., Aliyev, C.S. & Guliyev, I., 2009. In situ CPTU experiments at active Dashgil mud volcano, Azerbaijan: evidence for excess fluid pressure, updoming, and possible future violent eruption, Mar Petrol Geol doi: 10.1016/j.marpetgeo.2008.11.005.
Judd. A.G. & Hovland, M., 2007. Submarine fluid flow, the impact on geology, biology, and the marine environment, Cambridge University Press, 475.
Brown, K.M., 1990. The nature and hydrogeologic significance of muddiapirs and diatremes for accretionary systems. J Geophys Res, 95, 8969-8982.
Dimitrov, L.I., 2002. Mud volcanoes—the most important pathway for degassing deeply buried sediments, Earth Sci. Rev., 59, 49-76.
Huguen, C., Mascle, J., Chaumillon, E., Kopf, A., Woodside, J. & Zitter, T., 2004. Structural setting and tectonic control of the mud volcanoes from the central Mediterranean Ridge (Eastern Mediterranean), Mar. Geol. 209, 245-263.
Panahi, B.M., 2005. Mud volcanism, geodynamics and seismicity of Azerbaijan and the Caspian Sea region. In: G. Martinelli and B. Panahi, Editors, Mud Volcanoes, Geodynamics and Seismicity, NATO Science Series, Springer, The Netherlands, 89-104.
Milkov, A.V., 2000. Worlwide distribution of submarine mud volcanoes and associated gas hydrates, Mar. Geol. 167, 29-42.
Feyzullayev, A.A., Kadirov, F.A. and Aliyev, C.S., 2005. Mud volcano model resulting from geophysical and geochemical research. In: G. Martinelli and B. Panahi, Editors, Mud Volcanoes, Geodynamics and Seismicity, NATO Science Series, Springer, The Netherlands, 251-262.
Guliyev, I.S. & Feizullayev, A.A., 1997. All about mud volcanoes, NAFTA Press Publ. House, Baku, 120.
Yusifov, M. & Rabinowitz, P.D., 2004. Classification of mud volcanoes in the South Caspian Basin, offshore Azerbaijan, Mar. Pet. Geol. 21, 965-975.
Byrne, D.E., Sykes, L.R. & Davis, D.M., 1992. Great thrust earthquakes and aseismic slip along the plate boundary of the Makran subduction zone. J. Geophys. Res. 97 (B1), 449-478.
DeMets, C., Gordon, R.G., Argus, D.F. & Stein, S., 1990. Current plate motions. Geophys. J. 101, 425^478.
Harms, J.C., Cappel, H.N. & Francis, D.C., 1982. Geology and petroleum potential of the Makran Coast, Pakistan. Off- shore, SE-Asia Conference, Geology Session 1- 9, 9-12 Febr., Singapore.
Flueh, E.R., Kukowski, N. & Reichert, C., 1997. FS Sonne Cruise Report SO123, Makran-Murray Traverse. GEOMAR Report ISSN 0936-5788, 292. Kopp, C., Fruhn, J., Fluh, E.R., Reichert, C., Kukowski, N., Bialas, J. & Klaeschen, D., 2001. Structure of the Makran subduction zone from wide-angle and reflection seismic data. Tectonophysics 329, 171-191.
Mountain, G.S. & Prell, W.L., 1990. A multiphase plate tectonic history of the southeast continental margin of Oman. In: Robertson, A.H.F., Searle, M.P., Ries, A.C. (Eds.), TheGeology and Tectonics of the Oman Region. Geol. Soc. Spec. Publ. 49, London, 725-743.
Hutchinson, I., Louden, K.E., White, R.S. & Von Herzen, R.P., 1981. Heat flow and age of the Gulf of Oman. Earth Planet. Sci. Lett., 56, 252-262.
Kukowski, N., Schillhorn, T., Huhn, K., Von Rad, U., Husen, S. & Flueh, E.R., 2001. Morphotectonics and mechanics of the central Makran accretionary wedge off Pakistan. Mar.Geol., 173, 1-19.
Quittmeyer, R.C. & Kafka, A.L., 1984. Constraints on plate motions in southern Pakistan and the northern Arabian Sea from the focal mechanisms of small earthquakes.
Von Rad, U., Berner, U., Delisle, G., Doose, H., Fechner, N., Linke, P., Luckge, A., Roeser, H.A., Schmaljohann, R., Wiedicke, M. & Sonne 122/130 Scientific Parties, 2000. Gasand fluid venting at the Makran accretionary wedge off Pakistan: initial results. GeoMar. Lett., 20, 10-19.
Wilson, C.C. & Birchwood, K.M., 1965. The Trinidad Mud Volcano Island of 1964. Proceedings Geological Society of London, vol., 1626, 169-174.
Williams, P.R., Pigram, C.J. & Amiruddin, D.B., 1984. Melangeproduction and the importance of shale diapirism in accretionary terranes, 309, 145-146.
Burg, J.P. & Dolati, A., Geological Ins titute, ETH Zurich, Sonneggstrasse 5, CH‐8092 Zürich.
Sustainable Earth Trends
Volume 2, Issue 4 - Serial Number 4
October 2022
Pages 48-54

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