Geochemistry and Tectonic Setting of Pleistocene Basaltic Lava Flows in the Shahre-Babak Area, NW of Kerman, Iran: Implication for the Evolution of Urumieh- Dokhtar Magmatic Assemblage

Pleistocene basaltic lava flows, consisting of trachybasalt and basaltic trachyandesite, cover an area north-northwest of Shahre-Babak in southeastern Iran. The whole rock chemistry indicates that the lavas are dominantly alkaline and mildly calc-alkaline. Variation diagrams of SiO2 with major and t...

Full description

Saved in:
Bibliographic Details
Main Author: S.Z. Hosseini
Format: Article
Language:English
Published: University of Tehran 2009-12-01
Series:Journal of Sciences, Islamic Republic of Iran
Subjects:
Online Access:https://jsciences.ut.ac.ir/article_20130_3e0e1889d798650d2d7304a0207d00c7.pdf
Tags: Add Tag
No Tags, Be the first to tag this record!