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The Earth's core : structure, properties, and dynamics /
| Clasificación: | Libro Electrónico |
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| Otros Autores: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
New York :
Nova Science Publishers, Inc.,
[2012]
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| Colección: | Earth sciences in the 21st century series.
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| Temas: | |
| Acceso en línea: | Texto completo |
Tabla de Contenidos:
- THE EARTH'S CORE; STRUCTURE, PROPERTIES AND DYNAMICS; EARTH SCIENCES IN THE 21ST CENTURY; Library of Congress Cataloging-in-Publication Data; CONTENTS; PREFACE; COMPUTER MODELING OF LIQUIDIRON SOLUTIONS IN THE EARTH'S CORE; ABSTRACT; 1. INTRODUCTION; 2. EMBEDDED ATOM MODEL; 3. EAM POTENTIALS FOR IRON; 3.1. General Description; 3.2. Pure Liquid Iron at Normal Pressure; 3.3. Compressed States of Pure Iron; 3.4. The Simulation at Conditions in the Earth Centre; 4. THE USING OF SHOCK COMPRESSION DATA OF IRON; 4.1. Correcting of EAM Potential.
- 4.2. Properties of Iron Models with the Corrected EAM Potential4.3. Estimation of Melting Temperature of Iron with EAM Potential; 4.4. Situation in the Earth Centre; 4.5. Verification of Grüneisen Model; 5. MODELING OF SYSTEM IRON
- SULPHUR; 5.1. EAM Potential; 5.2. Results of Simulation of Fe
- S System; CONCLUSION; REFERENCES; ORIGIN AND DEVELOPMENT OF CORESOF THE TERRESTRIAL PLANETS:EVIDENCE FROM THEIR TECTONOMAGMATICEVOLUTION AND PALEOMAGNETIC DATA; ABSTRACT; 1. GENERAL INFORMATION ON THE PRESENT EARTH'S CORE; 2. GENERAL INFORMATION ABOUT TECTONOMAGMATICDEVELOPMENT OF THE EARTH AND MOON.
- 2.1. Tectonomagmatic Development of the Earth2.1.1. Tectonomagmatic processes in the Early Precambrian; 2.1.2. Cardinal change of tectonomagmatic processes in mid-Paleoproterozoic; 2.2. Tectonomagmatic Evolution of the Moon, Venus and Mars; 3. REASONS FOR THE EVOLUTION OF THE EARTH AND TERRESTRIAL PLANETSAND THE ROLE OF THEIR CORESIN THESE PROCESSES; 3.1. Possible Reasons for the Differences in the Magmatic Evolution of theEarth and Moon; 3.2. Similarities and Differences in the Initial Composition of TerrestrialPlanets.
- 3.3. Causes of Irreversible Tectonomagmatic Evolution of the TerrestrialPlanets3.3.1. The reason for the centripetal heating of the terrestrial planets; 3.4. The Evolution of the Terrestrial Planets Cores; 3.4.1. Evolution of the Earth's core; 3.4.2. The evolution of terrestrial planets' cores; CONCLUSION; REFERENCES; A REVIEW OF THE SLICHTER MODES:AN OBSERVATIONAL CHALLENGE; ABSTRACT; INTRODUCTION; THEORETICAL EIGENPERIOD FOR THE SLICHTER MODE; DAMPING OF THE INNER CORE MOTION; EXCITATION OF THE SLICHTER MODE; SEARCH FOR THE SLICHTER TRIPLET; CONCLUSION; REFERENCES.
- MANIFESTATIONS OF UPWELLINGMANTLE FLOW ON THE EARTH'S SURFACEABSTRACT; 1. INTRODUCTION; 2. GEOLOGICAL BACKGROUND; 3. Magnetotelluric Soundings; 3.1. Observations and Data Analysis; 3.2. Two-Dimensional Magnetotelluric Modeling; 3.3. Resistivity Structure Beneath the Asahi Mountains; 4. HELIUM ISOTOPES OF HOT SPRINGS; 5. DISCUSSION; 5.1. Geophysical and Geochemical Evidence for Latent Magmatism; 5.2. Anelastic Crustal Uplift Caused by Latent Magmatism; 6. CONCLUSIONS; ACKNOWLEDGMENTS; REFERENCES; ON SOLIDIFICATION AND FLUCTUATIONS AT THEBOUNDARY OF THE EARTH'S INNER CORE; Abstract.