Reactive Transport in Porous Media
Reactive Transport in Porous Media

Author: Peter C. Lichtner

Publisher: Walter de Gruyter GmbH & Co KG

Published: 2018-12-17

Total Pages: 452

ISBN-13: 1501509799

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Volume 34 of Reviews in Mineralogy focuses on methods to describe the extent and consequences of reactive flow and transport in natural subsurface systems. Since the field of reactive transport within the Earth Sciences is a highly multidisciplinary area of research, including geochemistry, geology, physics, chemistry, hydrology, and engineering, this book is an attempt to some extent bridge the gap between these different disciplines. This volume contains the contributions presented at a short course held in Golden, Colorado, October 25-27, 1996 in conjunction with the Mineralogical Society of America's (MSA) Annual Meeting with the Geological Society of America in Denver, Colorado.

Geochemistry and Fluid Flow
Geochemistry and Fluid Flow

Author: Larry W. Lake

Publisher: Gulf Professional Publishing

Published: 2002

Total Pages: 258

ISBN-13: 9780444505699

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This book is a culmination of a research project conducted at The University of Texas at Austin (UT) over the past 20 years. It has also been used as a text in a graduate course at UT on geochemistry and flow, taught by each of the editors over a period of 10 years. The reader will undoubtedly benefit from the knowledge flow that this progression from research project, via classroom, to text represents.

Metasomatism and the Chemical Transformation of Rock
Metasomatism and the Chemical Transformation of Rock

Author: Daniel Harlov

Publisher: Springer Science & Business Media

Published: 2012-08-14

Total Pages: 804

ISBN-13: 3642283934

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Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.