Data for: Geochemistry, petrogenesis, zircon U-Pb geochronology and Sr-Nd isotopic composition of Kuh-e-Shah volcanic rocks: Implications for an active continental margin along with eastern Iran during the Paleogene

In this study, we present new geochemical (whole-rock major and trace element), isotopic (Rb-Sr and Sm-Nd) and geochronological (U-Pb) data from the Kuh-e-Shah volcanic rocks with a comparison to other scattered volcanic rocks throughout the Lut Block (Pang et al., 2013; Saadat & Stern, 2016; Javidi Moghaddam et al., 2019) in order to better understanding the Paleogene magmatism evolution of the Lut Block and to place constraints to the timing and onset of volcanism, its tectonic implications, the geochemical features of the mantle source involved in volcanic rocks genesis, petrogenetic processes and the controls of magma generation processes, the probable effects of fractional crystallization and crustal contamination, and geodynamic evolution of volcanic rocks which exposed in the western part of the Kuh-e-Shah volcano-plutonic complex.