Institut für Erdsystemwissenschaften

Jul 9, 2024 | academic.oup.com | Leibniz Universität Hannover |Mineral Resources |Institut für Erdsystemwissenschaften |Abteilung Mineralogie

High-Ti basalts are commonly believed to represent parental magmas leading to the formation of mafic-ultramafic layered intrusions, such as Late Permian Panzhihua and Hongge in the Emeishan Large Igneous Province (SW China). Consequently, elucidation of the crystallisation and crustal differentiation of high-Ti basalts is critical for our understanding of the petrogenesis of these layered intrusions and the associated oxide ore mineralisation.