Browse content
Table of contents
Actions for selected chapters
- Full text access
- Book chapterNo access
CHAPTER 1 - INTRODUCTION
Pages 1-3 - Book chapterNo access
CHAPTER 2 - RADIOACTIVITY
Pages 4-14 - Book chapterNo access
CHAPTER 3 - EXPERIMENTAL METHODS
Pages 15-41 - Book chapterNo access
CHAPTER 4 - THE DATING OF UNDISTURBED MINERALS AND ROCKS
Pages 42-74 - Book chapterNo access
CHAPTER 5 - DATING DISTURBED MINERALS AND ROCKS
Pages 75-92 - Book chapterNo access
CHAPTER 6 - LEAD ISOTOPE METHODS
Pages 93-99 - Book chapterNo access
CHAPTER 7 - THE GENERAL PROBLEM OF INTERPRETATION
Pages 100-108 - Book chapterNo access
CHAPTER 8 - THE PHANEROZOIC TIME-SCALE
Pages 109-115 - Book chapterNo access
CHAPTER 9 - THE PULSE OF THE EARTH
Pages 116-126 - Book chapterNo access
CHAPTER 10 - REVERSALS OF THE EARTH'S MAGNETIC FIELD
Pages 127-134 - Book chapterNo access
CHAPTER 11 - METEORITES
Pages 135-149 - Book chapterNo access
CHAPTER 12 - THE AGE OF THE EARTH
Pages 150-166 - Book chapterNo access
REFERENCES
Pages 167-176 - Book chapterNo access
INDEX
Pages 177-178
About the book
Description
The Earth's Age and Geochronology provides an outline of geochronological methods, applications, and interpretations. This book discusses the fossil fission track method of dating. Organized into 12 chapters, this book begins with an overview of an accurate chronometer for measuring time intervals that must contain some sort of mechanism in which it operates at a predictable or known rate. This text then discusses the methodology of dating as well as the importance of long cooling histories. Other chapters consider the application of the experimental method to idealized, undisturbed systems. This book discusses as well the concept that in plutonic environments daughter isotope retention may often not commence until long after crystallization, or the peak of metamorphism. The final chapter deals with the applications of geochronology wherein the effects of selectivity will be particularly evident. This book is a valuable resource for nuclear physicists, astronomers, geologists, cosmologists, geochronologists, experimentalists, and scientists.
The Earth's Age and Geochronology provides an outline of geochronological methods, applications, and interpretations. This book discusses the fossil fission track method of dating. Organized into 12 chapters, this book begins with an overview of an accurate chronometer for measuring time intervals that must contain some sort of mechanism in which it operates at a predictable or known rate. This text then discusses the methodology of dating as well as the importance of long cooling histories. Other chapters consider the application of the experimental method to idealized, undisturbed systems. This book discusses as well the concept that in plutonic environments daughter isotope retention may often not commence until long after crystallization, or the peak of metamorphism. The final chapter deals with the applications of geochronology wherein the effects of selectivity will be particularly evident. This book is a valuable resource for nuclear physicists, astronomers, geologists, cosmologists, geochronologists, experimentalists, and scientists.
Details
ISBN
978-0-08-016387-1
Language
English
Published
1972
Copyright
Copyright © 1972 Elsevier Ltd. All rights reserved.
Imprint
Pergamon