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Lower Oligocene Calc-Alkaline Spessartitic Lamprophyres from Central Iran (East of Anarak Area); an Evidence from the Eastern Branch of Neotethys Subduction-Related Mantle Enrichment |
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| Authors: | Nazari Gh. H. Torabi Gh. Arai Sh. Morishita T. |
| Affiliation: | 1.Department of Geology, University of Isfahan, 8174673441, Isfahan, Iran ;2.Institute of Liberal Arts and Science, Kanazawa University, 920‒1192, Kanazawa, Japan ;3.College of Science and Engineering, School of Natural System, Kanazawa University, 920‒1192, Kanazawa, Japan ; |
| Abstract: | Geotectonics - The Lower Oligocene Kal-e-kafi (East of Anarak, Central Iran) lamprophyres occur as stocks and dikes, which cross-cut the Eocene volcanic and Cretaceous sedimentary rocks. The... |
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