Such a gap limits the understanding of magma evolution and tectonic activity after rifting. In this study, by examining the ∼126–121 Ma basalts and diabases of the post-rift stage, we provide ...

Though the volcano’s magma chambers could hold enough material for a caldera-forming event, none of them are likely to erupt soon.

This results in an increase of the Fe/Mg-ratio during the initial stages of magma evolution, the tholeiitic suite of rocks. Oxidising conditions in a parent magma promote the crystallisation of ferric ...

Understand and interpret the origin and evolution of magma as it passes through the volcanic system, and how its physical and chemical properties influence eruption. Understand how eruptions construct ...

Key questions remain about the timing, volume, and structural controls on magma emplacement. We present new high resolution aeromagnetic data across Adelaide Island, on the western margin of the AP ...

Natalie Accardo, postdoc at PennState University, will present her lecture at 11 a.m. EDT on November 1, 2018, in the Greenewalt Lecture Hall as part of DTM's Weekly Seminar Series. Coffee, tea, and a ...

My current objective is to understand how magma chambers grow and solidify with varying magma fluxes. I plan to couple thermal and mechanical models to gain further insight in the temporal evolution ...

Yanhao Lin from the Center for High Pressure Science and Technology Advanced Research, China, investigated the effects of oxygen fugacity on magma ocean formation during early Earth evolution.