这是一本地理地壳学专著。全书详实分析了岩石的形成,地壳变化,地质压力的变化对岩层的影响等。本书为全英文版,原汁原味,图文并茂。资料翔实,数据精确,分析独到,观点新颖。本书具有极高的学术价值及科研参考价值。
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书名 | STRUCTURAL AND METAMORPHIC EVOLUTION OF THE ARCHAEAN HIGH-PRESSURE GRANULITE(精) |
分类 | 生活休闲-旅游地图-地图 |
作者 | 本社编 |
出版社 | 科学出版社 |
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介绍 |
内容推荐 这是一本地理地壳学专著。全书详实分析了岩石的形成,地壳变化,地质压力的变化对岩层的影响等。本书为全英文版,原汁原味,图文并茂。资料翔实,数据精确,分析独到,观点新颖。本书具有极高的学术价值及科研参考价值。 目录 ABSTRACT 摘要(ABSTRACT IN CHINESE) PARTⅠINTRODUCTION CHAPTER 1 INTRODUCTION CHAPTER 2 GEOLOGY OF NORTH CHINA AND THE STUDY AREA PART Ⅱ STRUCTURAL ANALYSIS CHAPTER 3 ROCK ASSOCIATIONS AND LITHO-TECTONIC DOMAINS CHAPTER 4 STRUCTURAL FRAMEWORK AND TECTONO-METAMORPHIC CHAPTER 5 STRUCTURES RELATED TO D3 DEFORATION CHAPTER 6 SHEAR SENSE INDICATORS IN MEDIUM TO HIGH GRADE ROCKS CHAPTER 7 KINEMATICS OF THE D3 DEFORMATION PART Ⅲ PETROLOGICAL AND PALAEOMAGNETIC STUDIES CHAPTER 8 PETROLOGICAL STUDIES CHAPTER 9 MAGNETIC FABRICS CHAPTER 10 PALAEOMAGNETISM OF THE HIGH-GRADE ROCKS PART Ⅳ DISCUSSION AND CONCLUSION CHAPTER 11 DISCUSSION AND CONCLUSIONS ACKNOWLEDGEMENTS CURRICULUM VITAE REFERENCES APPENDIX 试读章节 Anohter important element of MHGR is the crystallographic preferred orientation of mineral.In equidimensional grains like quartz or feldspar this is only evident in this sections or by using special detection techniques.These fabrics can be important to determine the nature of deformation in the rock,but cannot be determined in the field and are not treated here. |
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