Bronislav Gongalsky,
Nadezhda A. Krivolutskaya,
Nadezhda Krivolutskaya
Springer International Publishing
e druk, 2019
9783030035587
World-Class Mineral Deposits of Northeastern Transbaikalia, Siberia, Russia
Specificaties
Gebonden, blz.
|
Engels
Springer International Publishing |
e druk, 2019
ISBN13: 9783030035587
Rubricering
Onderdeel van serie
Modern Approaches in Solid Earth Sciences
Verwachte levertijd ongeveer 9 werkdagen
Samenvatting
This book describes for the first time the complexity of the Northeastern Transbaikalia province of Russia. This province is one of the largest Early Proterozoic metallogenic provinces on Earth. It comprises three extra large deposits: Cu-sandstones Udokan, Fe-Ti-V and Cu-PGE Chiney, and REE Katugin. This book is a research study and includes geological, mineralogical, and geochemical data obtained by the authors from 30 field trips in the region, using XRF, ICP-MS, La-ICP-MS, EPMA, and the study of Sr, Nd, U-Pb isotopes in rocks and minerals. It demonstrates the complicated origin of Cu deposits comprising 50 Mt copper concentrated in sedimentary and magmatic rocks in this area.
Specificaties
ISBN13:9783030035587
Taal:Engels
Bindwijze:gebonden
Uitgever:Springer International Publishing
Inhoudsopgave
Foreword<div><br></div><div>Part I. Overview</div><div><br></div><div>Chapter 1. Introduction</div><div>1.1 History of Study of the Northern Transbaikalia</div><div>1.2 Material and Methods</div><div>1.3 Acknowledgements</div><div><br></div><div>Chapter 2. Regional Geology of the Kodar-Udokan Ore District</div><div>2.1 General Characterization of Territory</div><div>2.2 Basement Rocks</div><div>2.3 Platform Cover Rocks</div><div>2.4 Intrusive Rocks</div><div><br></div><div>Part II. Deposits in Magmatic Rocks</div><div><br></div><div>Chapter 3. Chineysky Layered Pluton: Structure, Formation Conditions</div><div>3.1 General Characterization of Pluton</div><div>3.2 Internal Structure of Pluton</div><div>3.2.1 Coarse-Grained Anorthosite and Monzodiorite</div><div>3.2.2 High-Ti Gabbro Rocks</div><div>3.2.3 Low-Ti Gabbro Rocks</div><div>3.2.4 Fluid-Magmatic Breccia with Lamprophyre Cement</div><div>3.2.5 Detailed Sections of the Chineysky Pluton</div><div>3.3 Chemistry and General Typification of Intrusive Rocks</div><div>3.4 Temperature and Composition of Magmas Based on COMAGMAT Program Modelling</div><div>3.5 Trace Elements in Intrusive Rocks</div><div>3.6 Formation of the Chineysky Pluton</div><div><br></div><div>Chapter 4. Titanomagnetite Ore in Chineysky Pluton</div><div>4.1 General Characteristics of Titanomagnetite Mineralization</div><div>4.2 Chemical Composition of Ore</div><div>4.3 Mineral Composition of Ore</div><div>4.4 Conditions of Titanomagnetite Ore Crystallization</div><div><br></div><div>Chapter 5. Sulfide Mineralization Spatially Related to Plutons of Chineysky Pluton</div><div>5.1 Sulfide Deposits and Prospects in Marginal Zone of the Chineysky Pluton</div><div>5.1.1 General Characterization</div><div>5.1.2 Rudny Deposit</div><div>5.1.3 Kontaktovy Deposit</div><div>5.1.4 Sulfide Mineralization in Titanomagnetite Ore</div><div>5.1.5 Sulfide Mineralization Related to Tectonic Disturbances</div><div>5.1.6 Mode of Occurrence and Distribution of Trace Elements (Ni, Co) in Copper Ore</div><div>5.1.7 PGE Distribution in Rocks and Ore</div><div>5.1.8 T-Log S2 Parameters of Sulfide Ore Formation</div><div><br></div><div><div>Chapter 6. Sulfide Mineralization Spatially Related to Massifs of Chineysky Complex</div><div>6.1 Sulfide Deposits of Luktur Pluton</div><div>6.2 Cu-Ni Prospects in Gabbro Rocks of the Mylovsky Pluton</div></div><div><br></div><div>Part III. Sandstone-Hosted Cu Deposits</div><div><br></div><div>Chapter 7. Unique Udokan Cu-Ag-Fe Deposit</div><div>7.1 Geological Position of Deposit</div><div>7.2 Structure and Composition of Ore Units</div><div>7.3 Composition of Sulfide Ore</div><div>7.3.1 Chemical Composition of Ore</div><div>7.3.2 Structure and Texture of Ore</div><div>7.3.3 Mineralogy of Ore</div><div>7.4 Oxided Ore of Udokan Deposit</div><div>7.4.1 Mineral Composition and Associations</div><div>7.4.2 Localization of Ore Types</div><div>7.5 Metamorphism of Rocks and Ore</div><div>7.6 Conclusions</div><div><br></div>Chapter 8. Sandstone-Hosted Hydrothermal Cu-Ag-Fe Deposits in Kodar-Udokan Ore District<div>8.1 Pravoingamakitsky Deposit</div><div>8.2 Krasnoe Deposit</div><div>8.3 Burpala Deposit</div><div>8.4 Unkur Deposit</div><div>8.5 Sakinskoe</div><div>8.6 Conclusions</div><div><br></div><div>Part IV. Deposits in Metasomatic Rocks</div><div><br></div><div>Chapter 9. Katugin Nb-Ta-Zr-REE-Y Deposits</div><div>9.1 Geological Structures</div><div>9.2 Isotope Composition of Granite</div><div>9.3 Isotope Composition of Zircon</div><div>9.4 Mineral Composition of Ore</div><div>9.5 Genesis of Ore</div><div><br></div><div>Chapter 10. Prospects and Uranium Mineralization</div><div>10.1 Chitkanda Uranium Prospect</div><div>10.2 Uranium Prospects Hosted in the Chineysky Pluton</div><div>10.2.1 Geology of the U-Hosted Rocks</div><div>10.2.2 Mineralogy of U Ores</div><div>10.2.3 Genesis of Mineralization</div><div><br></div><div>Conclusions. Paleoproterozoic Ore-Magmatic System of Kodar-Udokan Ore District: A Synthesis</div><div><br></div><div>Chapter 11. </div><div>11.1 Historical Overview</div><div>11.2 Staged System of Ore Types</div><div>11.3 Regional Tectonic Evolution and Metallogeny</div><div><br></div><div>References</div><div><br></div><div>Appendix</div>