Poirier's book does much to successfully fill this gap. The present volume is written for advanced undergraduate and . I found this book excellent in all respects. It brings under one cover a set of topics that are dispersed in the literature, and it does so with great clarity and consistency.

Poirier's book does much to successfully fill this gap. The present volume is written for advanced undergraduate and graduate students without previous exposure to mineralogical and petrological physics. It will prepare readers for more advanced book. Gerado G. Tango, Geophysics. It should form part of the library of anyone with a serious interest in the physics of the Earth's interior. Giorgio Ranalli, Geoscientist.

Langenhorst, Falko and Poirier, Jean-Paul 2000 Metrics.

Langenhorst, Falko and Poirier, Jean-Paul 2000. Anatomy of black veins in Zagami: clues to the formation of high-pressure phases. Earth and Planetary Science Letters, Vol. 184, Issue. Introduction to the Physics of the Earth's Interior describes the structure, composition and temperature of the deep Earth in one comprehensive volume. For courses that include these topics, this book would be an excellent reference tex. ighly recommended for the equations of state and melting relations for the Earth’s interior. Donald L. Turcotte Source: Journal of Geological Education.

Поставляется из: Англии Описание: Introduction to the Physics of the Earth’s Interior describes the structure, composition and temperature of the deep Earth in one comprehensive volume. The book closes with a discussion of current seismological, thermal and compositional models of the Earth.

Jean-Paul Poirier is Professor of Geophysics at the Institut de Physique du Globe de Paris, and a corresponding member of the Acade´ mie des Sciences.

Cambridge University Press. Jean-Paul Poirier is Professor of Geophysics at the Institut de Physique du Globe de Paris, and a corresponding member of the Acade´ mie des Sciences. He is the author of over ty articles and six books on geophysics and mineral physics, including Creep of Crystals (Cambridge University Press, 1985) and Crystalline Plasticity and Solid-state ow of Metamorphic Rocks with A. Nicolas (Wiley, 1976). This Page Intentionally Left Blank. Introduction to the physics of the earth’s.

Earth's Interior (Cambridge Topics in Mineral Physics & Chemistry). Be the first to ask a question about Introduction to the Physics of the Earth's Interior. Lists with This Book.

Introduction to the Physics of the Earth's Interior describes the structure, composition and temperature of the deep Earth. Introduction to the Physics of the Earth's Interior (Cambridge Topics in Mineral Physics & Chemistry). 052166313X (ISBN13: 9780521663137).

The first chapter provides a brief overview of the thermodynamics of solids. The second introduces elastic moduli and their derivation, and issues of thermodynamic coupling. Once these preliminaries have been covered, the book moves on to a general discussion of solid-state physics.

Main Author: Poirier, Jean Paul. Cambridge ; New York : Cambridge University Press, 1991. Series: Cambridge topics in mineral physics and chemistry ; 3. Published: Cambridge ; New York : Cambridge University Press, 1991. Subjects: Geophysics.

Mineral physics is the science of materials that compose the interior of planets, particularly the Earth. It overlaps with petrophysics, which focuses on whole-rock properties. It provides information that allows interpretation of surface measurements of seismic waves, gravity anomalies, geomagnetic fields and electromagnetic fields in terms of properties in the deep interior of the Earth

Mineral physics is the science of materials that compose the interior of. .Poirier, Jean-Paul (2000). Introduction to the Physics of the Earth's Interior. Cambridge Topics in Mineral Physics & Chemistry. Many of the pioneering studies in mineral physics involved explosions or projectiles that subjected a sample to a shock. For a brief time interval, the sample is under pressure as the shock wave passes through. Pressures as high as any in the Earth have been achieved by this method. However, the method has some disadvantages.

The volume closes with a discussion of current seismological, thermal and compositional models of the Earth. About 250 new references have been added. The volume closes with a discussion of current seismological, thermal and compositional models of the Earth.