During Shakespeare's lifetime, John Lyly was repeatedly described as the central figure in contemporary English literature. This book takes that claim seriously, asking how and why Lyly was considered the most important writer of his time. Kesson traces Lyly's work in prose fiction and the theatre, demonstrating previously unrecognised connections between these two forms of entertainment. The final chapter examines how his importance to early modern authorship came to be forgotten in the late seventeenth century and thereafter. This book serves as an introduction to Lyly and early modern literature for students, but its argument for the central importance of Lyly himself and 1580s literary culture makes it a significant contribution to current scholarly debate. Its investigation of the relationship between performance and print means that it will be of interest to those who care about, watch or work in early modern performance.
During Shakespeare's lifetime, John Lyly was repeatedly described as the central figure in contemporary English literature. This book takes that claim seriously, asking how and why Lyly was considered the most important writer of his time. Kesson traces Lyly's work in prose fiction and the theatre, demonstrating previously unrecognised connections between these two forms of entertainment. The final chapter examines how his importance to early modern authorship came to be forgotten in the late seventeenth century and thereafter. This book serves as an introduction to Lyly and early modern literature for students, but its argument for the central importance of Lyly himself and 1580s literary culture makes it a significant contribution to current scholarly debate. Its investigation of the relationship between performance and print means that it will be of interest to those who care about, watch or work in early modern performance.
The Earth's rocky mantle convects to lose heat, which comes from the liquid iron core below. The mantle's interfaces - the core-mantle boundary, and the lithosphere - may hold the key to understanding mantle motion because of the seismic anisotropy present in these parts of the Earth. In this thesis, Andy Nowacki presents a precise but comprehensive review of the current state of the art in studying flow with anisotropy, mineral physics and geodynamics. New measurements of shear wave anisotropy in the lowermost mantle and at mid-ocean ridges are used to constrain mechanisms of creep and melt extraction in the mantle. A model of global flow is used to predict anisotropy in the deep Earth, and novel methods to forward model shear wave splitting are described. Future studies of mantle flow must incorporate the understanding gained in this thesis. The thesis contains a substantive introduction to the structure of the Earth, seismic anisotropy in general and in the core-mantle boundary region, and mid-ocean ridge processes. It also describes novel methods for forward modelling and interpreting shear wave splitting data. Three chapters present timely research into dynamics at divergent plate boundaries and at the core-mantle boundary.
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