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

International Journal of Geography and Geology, 2014, vol. 3, issue 2, 30-44

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.

Keywords: Southeast of Iran; Sistan suture zone; Zahedan igneous intrusions; Loochan batholiths; Tectomagmatic origin; Melting of the continental crust; Petrological diagrams. (search for similar items in EconPapers)
Date: 2014
References: Add references at CitEc
Citations:

Downloads: (external link)
https://archive.conscientiabeam.com/index.php/10/article/view/1918/2727 (application/pdf)

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:pkp:ijogag:v:3:y:2014:i:2:p:30-44:id:1918

Access Statistics for this article

More articles in International Journal of Geography and Geology from Conscientia Beam
Bibliographic data for series maintained by Dim Michael ().