Document Type : Original Research Paper
Authors
1 Assistant Professor, Department of Geology, Islamic Azad University, Lahijan Branch, Lahijan, Iran
2 Assistant Professor, Department of Geology, Islamic Azad University, Damavand Branch, Damavand, Iran
3 Ph. D., Department of Geology, Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran
Abstract
The pillow basalts, Cretaceous in age, outcrop in the northern part of Alborz in the East of Guilan province (north of Iran). The pillow lavas are mainly olivine basalts. From geochemical point of view, these rocks are transitional or mildly alkalic series and negative anomaly of Nb-Ta, Zr, Ba; positive anomaly of Kand Pb; low ratios of Ce/Pb, Nb/U and high ratios of Th/Nb and Ba/Zr are geochemical evidences of crustal contamination. In tectonic setting diagrams, the pillow lavas plots in intra-continental rift Basalts terrain and is comparable with the Transitional Ethiopian Rift Basalts. The geochemical studies show that the pillow basalts are derived from the spinel-lherzolite mantle source and originated from less than 60km depth with less than %15 partial melting.
Keywords
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