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International Journal of Geography and Geology

February 2014, Volume 3, 2, pp 30-44

Tectomagmatic Origin of the Zahedan Batholiths – South East Iran (Reling on Intergrated Outcrop Study of the Petrology of High Mass in Loochan, Southwest Zahedan)

Behrooz Sahebzadeh

Behrooz Sahebzadeh 1

  1. Department of Geosciences, Farhangian University, Shahhid Motahhari Campus, Zahedan, Iran 1

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Abstract:

Zahedan batholiths, the largest intrusive igneous mass in Sistan Suture zone, in Southeast of Iran during the Eocene - Oligocene is formed in this zone. The mass of igneous outcrops in a narrow mass with scattered outcrops Larger populations with continuous advice, The Afghan Block of East and West Blocks of Lout outcrop at the surface, Granitoid batholiths magma intrusion in the petrographical Zahedan region specific and that the mass of Tectomagmatic origin of calc-alkaline and per aluminous igneous intrusion that is Melting of continental sedimentary rocks in the shallow crust Lateral movement of the compression zone includes the land area is under construction .

Contribution/ Originality

Keywords:

Southeast of Iran, Sistan Suture zone, Zahedan igneous intrusions, Loochan batholiths, Tectomagmatic origin, Melting of the continental crust, Petrological diagrams

Reference:

  1. Berberian, M. and G.C. King, 1981. Towards a paleogeography and tectonic evolution of Iran. Canadian Journal of Earth-Sciences, Reviews, 18(2): 210-265.
  2. Boomeri, M. and G.R. Lashkaripour, 2003. Granite of Zahedan, Southeastern Iran. European Geophysical Research Abstracts, 5: 04933.
  3. Boomeri, M., G.R. Lashkaripour and M.N. Gorgich, 2004. Geochemistry and petrography of Zahedan granitic rocks, research project. Zahedan: Sistan and Baluchistan University. pp:187
  4. Camps, V.E. and R.J. Griffis, 1982. Character, genesis and tectonic setting of igneous rocks in the Sistan suture zone, Eastern Iran, Lithos.15 September 1982, 15(3): 221-239.
  5. Klinic, I.A., 1972. Experimental study of partial melting of coastal rocks and formation of migmatite, congers. Repot 24th Session, Montreal2. pp: 109-113.
  6. Ebrahimzadeh, E., 2007. Fundamentals of Iran South-East longitude. Zahedan: Printing, Publishing, Sistan and Baluchistan University. pp: 473.
  7. Kuno, H., 1968. Differentiation of basaltic magma, In Hess, H. H. et Poldervaart, A. Edit, Basalts. New York: Interscience Pull. 2: 623- 688.
  8. Maniar, P. and P.M. Piccoli, 1989. Tectonic discrimination of granitoid. Geological Society of America Bulletin, 101(5): 635-643.  [Accessed May 1989].
  9. MoinVazeri, H. and A. Ahmadi, 2002. Petrography and petrology of igneous rocks. Tehran: Printing, Publishing, Teacher Training University. pp: 539.
  10. Sadeghian, M. and M.V. Valizadeh, 2007. Granitoid emplacement mechanism of Zahedan in light of the methodology AMS. Journal of Earth Sciences, Geological Survey of Title, (66): 134-159.
  11. Tirrul, R., I.R. Bell, R. Griffis and V.E. Camps, 1983. The Sistan suture zone of Eastern Iran. Geological society of American. Bulletin; January 1983, 94(1): 134-150.
  12. Wright, J.B., 1969. A simple alkalinity ratio and its application to questions of non-orogenic granite gneiss. Geol. Mag, 106: 370–384.

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