Jodie A. Miller

TL;DR: In this paper, the authors show that the current volume constraints for the silicic ignimbrite eruptions may be considerably underestimated due to considerable volumes residing as co-ignimblite ash deposits.

TL;DR: In contrast to oceanic lithosphere, the continents are manifestly composed of the products of tectonic processes whose cumulative duration spans much of the Earths history as discussed by the authors, and the character of the continents is significantly influenced by the way in which the existing lithosphere responds to new tectonothermal events that follow geologically significant cessations of activity.

TL;DR: The authors presented a combination of review and research papers, which highlight some of the issues and problems associated with the characterization and modelling of continental reactivation and reworking, and provided a crucial data set with which to evaluate the spatial patterns, temporal evolution and dynamic controls of tectonic rejuvenation of the continents and continental lithosphere.

TL;DR: For example, the authors showed that melting mud in Earth's mantle from extreme oxygen isotope signatures in zircon can be inferred from the presence of oxygen isotopes in Zircon.

TL;DR: In this article, the authors studied the lower Cambrian Naukluft Thrust which crops out in central Namibia and found that it contains a cataclastic dolomite fault rock, referred to as "gritty dolomerite" which they interpret as a signature of coseismic carbonate dissociation and subsequent fluid-rock interactions.