Composition of the Chilled Marginal Rocks of the Panzhihua Layered Intrusion, Emeishan Large Igneous Province, SW China: Implications for Parental Magma Compositions, Sulfide Saturation History and Fe–Ti Oxide Mineralization

Volume: 60, Issue: 3, Pages: 619 - 648
Published: Feb 7, 2019
Abstract
The chilled marginal rocks of the Panzhihua layered intrusion of the Emeishan Large Igneous Province (ELIP), SW China, including microgabbros and olivine–phyric gabbros, are similar to coeval high-Ti basalts in the Panzhihua area in both major and trace element compositions. The olivine–phyric gabbros are characterized by depleted Nd isotopic compositions (εNd(t) = +1·15 to +4·18) and initial 87Sr/86Sr (0·7043–0·7052) similar to those of the...
Paper Details
Title
Composition of the Chilled Marginal Rocks of the Panzhihua Layered Intrusion, Emeishan Large Igneous Province, SW China: Implications for Parental Magma Compositions, Sulfide Saturation History and Fe–Ti Oxide Mineralization
Published Date
Feb 7, 2019
Volume
60
Issue
3
Pages
619 - 648
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