Petrology of Igneous and Metamorphic Rocks

Petrology of Igneous and Metamorphic Rocks
Author: Donald W. Hyndman
Publisher: McGraw-Hill Science, Engineering & Mathematics
Total Pages: 552
Release: 1972
Genre: Nature
ISBN:

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Petrogenesis of Metamorphic Rocks

Petrogenesis of Metamorphic Rocks
Author: Kurt Bucher
Publisher: Springer Science & Business Media
Total Pages: 434
Release: 2011-07-14
Genre: Science
ISBN: 3540741682

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Petrogenesis of Metamorphic Rocks presents a large number of diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given set of metamorphic rocks may have formed. Other parameters that control metamorphic mineral assemblages are also discussed and pitfalls resulting from simplifications and generalizations are highlighted. The book discusses the most common metamorphic rock types, their nomenclature, structure and graphical representation of their mineral assemblages. Part I defines basic principles of metamorphism, introduces metamorphic processes, geologic thermometry and barometry and defines metamorphic grade. Part II presents in a systematic way mineralogical changes and assemblages found in the most common types of metamorphic rocks. The computation of diagrams is based on recent advances in quantitative petrology and geochemistry. An extensive bibliography, including the key contributions and classic papers in the field, make it an invaluable source book for graduate students and professional geologists.

The Bookseller

The Bookseller
Author:
Publisher:
Total Pages: 616
Release: 1952
Genre: Bibliography
ISBN:

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Flow Processes in Faults and Shear Zones

Flow Processes in Faults and Shear Zones
Author: G. Ian Alsop
Publisher: Geological Society of London
Total Pages: 396
Release: 2004
Genre: Science
ISBN: 9781862391536

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Faults and their deeper level equivalents, shear zones, are localized regions of intense deformation within the Earth. They are recognized at all scales from micro to plate boundary, and are important examples of the nature of heterogeneous deformation in natural rocks. Faults and shear zones are significant as they profoundly influence the location, architecture and evolution of a broad range of geological phenomenao The topography and bathymetry of the Earth's surface is marked by mountain belts and sedimentary basins that are controlled by faults and shear zoneso In addition, faults and shear zones control fluid migration and transport including hydrothermal and hydrocarbon systems. Once faults and shear zones are established, they are often long-lived features prone to multiple reactivation over very large time-scales. This collection of papers addresses lithospheric deformation and the rheology of shear zones, together with processes of partitioning and the unravelling of fault and shear zone histories.