Mafic–Ultramafic Tyulkulam Massif, West–Central Asian Orogenic Belt (Central Kazakhstan): Mineralogical and Geochemical Evidence for Transition from Forearc to Island-Arc Magmatism during the Evolution of the Junggar–Balkhash Ocean
This study presents the first comprehensive mineralogical and geochemical analysis of the Tyulkulam Massif in Central Kazakhstan, revealing that its ultramafic-mafic rocks record a tectonomagmatic evolution from forearc to island-arc settings during the early development of the Junggar–Balkhash Ocean.