Fluid-magmatic interactions at oceanic islands as a possible source for the sodic agpaitic Trend A. G. SimakinT. P. SalovaV. I. Kovalenko OriginalPaper 18 November 2011 Pages: 641 - 652
Visual in-situ monitoring of the behavior and phase states of water-hydrocarbon inclusions at high temperatures and pressures V. S. BalitskyS. V. PenteleyT. M. Bublikova OriginalPaper 18 November 2011 Pages: 653 - 674
Middle Eocene volcanic shoshonites from western margin of Central-East Iranian Microcontinent (CEIM), a mark of previously subducted CEIM-confining oceanic crust Ghodrat Torabi OriginalPaper 18 November 2011 Pages: 675 - 689
Alkaline basalt from the Central Iran, a mark of previously subducted Paleo-Tethys oceanic crust Ghodrat TorabiOmid Hemmati OriginalPaper 18 November 2011 Pages: 690 - 704
