Characterization of copper ± (gold) vein‐type mineralization along terrain boundary fault, Dubarpeth in Central India: Constraints from fluid inclusion, stable isotope, and in situ trace element geochemistry of sulphides

We present the findings on in situ trace element geochemistry of sulphides by LA‐ICPMS, sulphur isotope, and hydrothermal fluid evolution of copper ± gold mineralization at Dubarpeth, Central India. Mineralization is associated with chloritized‐silicified alteration zones, structurally localized along the terrain boundary fault between Archean TTG quartz diorite (2.5 Ga) of Western Bastar Craton and Paleo‐Mesoproterozoic cover sediments of...