Evolution Of Phyllosilicates Through Diagenesis And Low Grade Metamorphism In A Prograde Sequence Of Pelitic Rocks From Southern New Zealand

Low-Grade Metamorphism explores processes and transformations in rocks during the early stages of metamorphic recrystallization. There has been little analysis and documentation of this widespread phenomenon, especially of the substantial and exciting advances that have taken place in the subject over the last decade. This book rectifies that shortfall, building on the foundations of Low-Temperature Metamorphism by Martin Frey (1987). The editors have invited contributions from an internationally acknowledged team of experts, who have aimed the book at advanced undergraduate and graduate students as well as researchers in the field. Contributions from internationally acknowledged experts. Documents the substantial and exciting advances that have taken place in the subject over the last decade.

The collective outgrowth of presentations at a September 1992 meeting titled The Transition from Basalt to Metabasalt: Environments, Processes, and Petrogenesis, held in Davis, California under the auspices of IGCP Project 294, to discuss recent advances and to identify important areas for further

Developments in Petrology, Volume 10: Shale-Slate Metamorphism in Southern Appalachians provides information pertinent to shale-slate metamorphism. This book aims to develop a paleothermometer for shales and to be able to predict the reactions that would arise in response to an increase in temperature. Organized into 10 chapters, this volume begins with an overview of the mineral, isotopic, chemical, petrographic, and structural changes that occur during late-stage diagenesis. This text then examines the petrology and texture of a series of physilites ranging from the middle diagenesis zone to the greenschist facies. Other chapters consider the X-ray analyses of the Conasauga samples, which show that most of the parameters that can be measured have a systematic trend that can be related to increasing grade of metamorphism. This book discusses as well chlorite as a common component of shales and low-grade metamorphic rocks. The final chapter deals with the carbonate rocks. This book is a valuable resource for petrologists.

This second volume in the new series produced by the Mineralogical Society is concerned with the study of rocks from the deep continental crust. It is, we hope, timely to summarize recent petrological advances contributing to this field of active interest. Based mainly on review papers read at a conference, the chapters have subsequently been revised and expanded, while the editors have produced an introductory overview as Chapter 1. The conference was the Winter Meeting of the Mineralogical Society on 15 December 1988, at wh ich Prof. R. C. Newton delivered the 20th Hallimond Lecture of the Society (which forms the basis of Ch. 7). The editors are grateful to all who contrib uted to the smooth running of the meeting at Kingston Polytechnic, and in the ensuing preparation of the volume: in particular, we sincerely thank all of the following for their labours as referees: A. J. Baker, L. M. Barron, M. J. Bickle, A. D. Chambers, J. D. Clemens, J. S. Daly, G. T. R. Droop, C. R. L. Friend, E. S. Grew, S. L. Harley, R. S. Harmon, N. B. W. Harris, B. Harte, T. J. B. Holland, N. F. C. Hudson, W. S. MacKenzie, W. Perkins, H. R. Rollinson, J. W. Sheraton, D. J. Waters, R. H. Worden and B. W. D. Yardley. John R.