This PowerPoint presentation is part of the Whitman College petrology course. This 50-slide presentation introduces layered mafic intrusions around the world. The chapter discusses various layered mafic complexes in cross section and plan view, and also describes stratigraphy within the complexes. The presentation further describes processes within the complexes, such as crystallization, differentiation, layering, convective overturn, in-situ processes, compositional convection, and density currents. This resource is part of the Teaching Petrology collection. http://serc.carleton.edu/NAGTWorkshops/petrology03/index.html
Part of the Cutting Edge collection. The NAGT/DLESE On the Cutting Edge project helps geoscience faculty stay up-to-date with both geoscience research and teaching methods.
Subject: Geoscience:Geology:Igneous and Metamorphic Petrology:Igneous Processes, Geoscience:Geology:Mineralogy:Phase Equilibria/Thermodynamics, Geoscience:Geology:Igneous and Metamorphic Petrology:Igneous Associations and Tectonic Settings, Thermodynamics and Phase Equilibria, Geoscience:Geology:Tectonics, Geochemistry:Phase Equilibria/Thermodynamics, Geoscience:Geology:Geochemistry Resource Type: Course Information:Course Site:Course Notes, Audio/Visual:Images/Illustrations Grade Level: Graduate/Professional, College Lower (13-14), College Upper (15-16) Classes of Earth Materials: Plutonic Rocks Course Type: Upper Level:Mineralogy, Petrology Geochemistry Applications: Chemical Differentiation:Earth Topics: Solid Earth:Geochemistry:Phase Equilibria/Thermodynamics, Chemistry/Physics/Mathematics, Solid Earth:Geochemistry, Solid Earth, Mineralogy:Phase Equilibria/Thermodynamics, Solid Earth:Petrology:Igneous Processes, Thermodynamics and Phase Equilibria, Igneous Associations and Tectonic Settings Solid Earth Processes: Alteration (Hydrothermal), Volcanism, PlutonismKeywords: modal layering, phase layering, cryptic layering, rhythmic layering, intermittent layering, compositional convection, vortex model
CMS authors: link to this resource in your page using [resource 22090]