<p><p>The second half of the past century witnessed a remarkable paradigm shift in approach to the understanding of igneous rocks. Global literature records a change from a classical petrographic approach to emphasis on mineral chemistry, trace element characteristics, tectonic setting, phase relati
Igneous Petrology
β Scribed by CHARLES J. HUGHES (Eds.)
- Publisher
- Academic Press, Elsevier
- Year
- 1982
- Leaves
- 552
- Series
- Developments in Petrology 7
- Category
- Library
No coin nor oath required. For personal study only.
β¦ Table of Contents
Content:
Developments in Petrology
Page ii
Front Matter
Page iii
Copyright page
Page iv
Preface
Pages v-vi
CHARLES J. HUGHES
Glossary
Pages vii-ix
Chapter 1 - Mineralogy of Igneous Rocks
Pages 1-27
Chapter 2 - Volcanic Activity
Pages 29-56
Chapter 3 - Forms and Structures of Intrusive Rocks
Pages 57-87
Chapter 4 - Classification of Igneous Rocks
Pages 89-124
Chapter 5 - Petrography of Igneous Rocks
Pages 125-146
Chapter 6 - Physical Properties and Physical Chemistry of Magmas
Pages 147-198
Chapter 7 - Differentiation of Igneous Rocks
Pages 199-249
Chapter 8 - Igneous Rock Series
Pages 251-270
Chapter 9 - Igneous Rocks of Oceanic Areas
Pages 271-311
Chapter 10 - Igneous Rocks of Continental Areas
Pages 313-368
Chapter 11 - Igneous Rocks Above Benioff Seismic Zones
Pages 369-413
Chapter 12 - Igneous Rocks of the Precambrian
Pages 415-443
Chapter 13 - Petrogenesis of Igneous Rocks
Pages 445-472
Chapter 14 - Degradation of Igneous Rocks
Pages 473-488
Epilogue
Page 488
Clarence Tracy
References
Pages 489-519
Name Index
Pages 521-528
Locality Index
Pages 529-533
General Index
Pages 535-551
π SIMILAR VOLUMES
Igneous and metamorphic petrology has over the last twenty years expanded rapidly into a broad, multifaceted and increasingly quantitative science. Advances in geochemistry, geochronology, and geophysics, as well as the appearance of new analytical tools, have all contributed to new ways of thinking
<p>Igneous petrology was to some extent essentially a descriptive sciΒ ence until about 1960. The results were mainly obtained from field work, major element analyses, and microscopical studies. During the 1960's two simultaneous developments took place, plate tectonics became generally accepted, an
<p><p>The second half of the past century witnessed a remarkable paradigm shift in approach to the understanding of igneous rocks. Global literature records a change from a classical petrographic approach to emphasis on mineral chemistry, trace element characteristics, tectonic setting, phase relati
Igneous and metamorphic petrology has over the last twenty years expanded rapidly into a broad, multifaceted and increasingly quantitative science. Advances in geochemistry, geochronology, and geophysics, as well as the appearance of new analytical tools, have all contributed to new ways of thinking