变质地质学(中国地质大学十一五规划教材)pdf/txt下载_在线阅读全文

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《变质地质学》是随着20世纪60年代板块构造学兴起而迅速发展起来的地质学科，作为课程，它属于地质专业课程性质，具有显著的地质前沿和岩石学与构造学学科交叉特点。本书全面介绍了变质岩石学和变质地质学的基础理论、基础知识和基本技能。内容主要包括变质作用通论、接触变质、动力变质和区域变质及地外变质五大部分。

内容简介

《变质地质学》是随着20世纪60年代板块构造学兴起而迅速发展起来的地质学科，作为课程，它属于地质专业课程性质，具有显著的地质前沿和岩石学与构造学学科交叉特点。由英国著名岩石学家R．Mason教授和我校桑隆康教授合著的该课程双语教学教材《Metamorphic Geoloy》全面介绍了变质岩石学和变质地质学的基础理论、基础知识和基本技能。内容主要包括变质作用通论、接触变质、动力变质和区域变质及地外变质五大部分。与国内其他类似教材的内容相比，本课程具有明显的先进性，介绍了包括P-T-t轨迹、缓冲平衡、超高压变质、超高温变质、地外变质等前沿课题。其中，缓冲平衡、超高温变质、地外变质等课题国内教材很少涉及。此外，教材强调用AFM图对变泥质岩进行共生分析，对世界著名的Barrow变质带、Sulitjelma变质带、Skiddaw接触晕和塞浦路斯蛇绿岩带等经典的介绍比较详细、生动。与国外类似教材相比，该教材介绍了国外课程通常没有的我国周口店、北戴河、三峡、秦岭、嵩山、大别山变质作用方面的内容，具有明显的中国特色。该教材的出版是双语教材建设方面取得的突破性进展。

作者简介

梅森1941年5月4日生于英国伦敦，1963年获剑桥大学理学学士学位，1967年获剑桥大学哲学博士学位，1990年获英国Hertfordshire大学教育学研究生证书。1966—1996年，先后在在英国伦敦大学大学学院、伦敦大学Birkbeck学院、Luton大学讲授《变质岩岩石学》、《构造地质学》和《地质学》等课程，其中1986年在武汉地质学院讲授《变质岩石学》。1996年起，在中国地质大学(武汉)为国家理科基地班和工科基地班讲授双语课程《变质岩石学》和《变质地质学》。现为中国地质大学(武汉)矿物学岩石学矿床学教授、英国伦敦教育顾问。主要研究领域包括变质岩石学、变质地质学、双语教育。他的《变质岩岩石学(第一版，1978)》于1981年被译成俄文在苏联世界出版社出版。他的《变质岩岩石学(第二版，1990)》被英、美、中、俄众多岩石学教材引用。由于他在双语教学和中英交流所作的突出贡献，2001年获得我国政府授予外籍专家的最高奖——友谊奖。桑隆康1945年10月25日生于江西省九江市，1969年毕业于合肥工业大学地质系，1982年获武汉地质学院理学硕士学位，1970一1979年在安徽省地质局311地质队从事变质磷矿地质调查和找矿勘探工作。1982年起，在中国地质大学(武汉)讲授《岩石学》、《变质岩石学》和《变质地质学》等课程。现为中国地质大学(武汉)矿物学岩石学矿床学教授、博士生导师、精品课程《岩石学》负责人，俄罗斯自然科学院外籍院士。主要研究领域包括岩石学、变质地质学、地学教育。多次获得省部级教学和科研奖励。他与路凤香教授联合主编的教材《岩石学》作为高等教育面向21世纪课程教材于2002年在地质出版社出版。

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目　　录

Chapter 1 Definition of metamorphism, classification ofmetamorphic rocks 1.1 Definition of metamorphism 1.2 Classification and nomenclature of metamorphic rocks 1.3 The minerals of metamorphic rocks 1.4 English mineral names 1.5 Description of thin sectio of metamorphic rocks HOMEWORKChapter 2 Conditio of metamorphism, P-T-t paths, the Phase Rule,composition-assemblage diagrams, metamorphic facies 2.1 Limits of metamorphism 2.2 P-T-t paths 2.3 Equilibrium 2.4 The Phase Rule 2.5 Using the Phase Rule to fix P- T Conditio 2.6 AFM diagrams 2.7 Metamorphic facies HOMEWORKChapter 3 Contact metamorphism 1 : the role of heat 3.1 Introduction 3.2 Contact aureole of the Markfield Diorite, Leicestehire,England 3.3 Contact aureole of the Skiddaw Granite, Lake District,England 3.4 Heat trafer at the contacts of intrusio 3.5 Effect of intrusion size and shape on aureole size and shape 3.6 Thermal conduction models of contact aureoles 3.7 Thermal convection models of contact aureoles 3.8 Facies series in contact metamorphism HOMEWORKChapter 4 Contact metamorphism 2: the role of fluids 4.1 Introduction 4.2 Contact metamorphism of limestone 4.3 Buffering of H2O and CO2 in calcareous skar 4.4 Very high temperature reactio between calcite and quartz 4.5 Discussion HOMEWORKChapter 5 Dynamic metamorphism 5.1 Introduction and definition 5.2 Strain 5.3 Classification of dynamic metamorphic rocks 5.4 The Lochseiten Mylonite, Switzerland 5.5 Dynamic metamorphism in Dengfeng County, Henan Province 5.6 Dynamic metamorphism in relation to depth 5.7 Microstructures of metamorphic rocks HOMEWORK Chapter 6 Regional metamorphism 1: Barrow's Metamorphic Zones 6.1 Introduction 6.2 Barrow's Zones in pelitic rocks 6.3 Changes in mineral assemblages with metamorphic grade 6.4 The Sulitjelma District, Norway and Sweden 6.5 Garnet growth and zoning at Sulitjelma 6.6 Geothermal gradients and metamorphic field gradients HOMEWORKChapter 7 Regional metamorphism 2: basic igneous rocks 7.1 Sulitjelma greetones and amphibolites 7.2 The boundary between the greechist and amphibolite facies 7.3 ACF triangular diagrams to represent mineral assemblages ofmetabasites 7.4 Plotting ACF triangular diagrams 7.5 Metamorphic temperature gradients in sedimentary basi HOMEWORKChapter 8 Regional metamorphism 3: ocean floor metamorphism 8.1 Metamorphism at spreading ocean ridges 8.2 The Troodos Ophiolite, Cyprus 8.3 Petrology of the Ophiolite 8.4 Structure and geothermal gradients of oceanic ridges 8.5 Hydrothermal activity near spreading ridges 8.6 Conclusio HOMEWORKChapter 9 Regional metamorphism 4: high temperature metamorphism 9.1 Partial melting and migmatites 9.2 Structural varieties of migmatite 9.3 Field relatio of migmatites 9.4 The granulite facies 9.5 Why are granulites so dry? 9.6 The Adirondack Mountai, New York State, USA 9.7 Ultra-high temperature metamorphism HOMEWORKChapter 10 Regional metamorphism 5: HP and UHP metamorphism 10.1 High pressure metamorphism 10.2 The Franciscan metamorphic belt of California 10.3 Eclogites and the eclogite facies 10.4 Ultra high pressure metamorphism 10.5 How did HP and UHP rocks get back to the surface?10.6 UHP rocks, the range of conditio of metamorphism andimplicatio for metamorphic facies HOMEWORKChapter 11 Extra-terrestrial metamorphism 11.1 Impact metamorphism 11.2 Meteor Crater, Arizona, USA 11.3 Shock metamorphism at the N6rdlinger Ries Crater, Germany 11.4 Metamorphism in Moon rocksReferences

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Chapter 1  Definition of metamorphism, classification of
metamorphic rocks
  1.1  Definition of metamorphism
  1.2  Classification and nomenclature of metamorphic rocks
  1.3  The minerals of metamorphic rocks
  1.4  English mineral names
  1.5  Description of thin sectio of metamorphic rocks
  HOMEWORK
Chapter 2  Conditio of metamorphism, P-T-t paths, the Phase Rule,
composition-assemblage diagrams, metamorphic facies
  2.1  Limits of metamorphism
  2.2  P-T-t paths
  2.3  Equilibrium
  2.4  The Phase Rule
  2.5  Using the Phase Rule to fix P- T Conditio
  2.6  AFM diagrams
  2.7  Metamorphic facies
  HOMEWORK
Chapter 3  Contact metamorphism 1 : the role of heat
  3.1  Introduction
  3.2  Contact aureole of the Markfield Diorite, Leicestehire,
England
  3.3  Contact aureole of the Skiddaw Granite, Lake District,
England
  3.4  Heat trafer at the contacts of intrusio
  3.5  Effect of intrusion size and shape on aureole size and shape
  3.6  Thermal conduction models of contact aureoles
  3.7  Thermal convection models of contact aureoles
  3.8  Facies series in contact metamorphism
  HOMEWORK
Chapter 4  Contact metamorphism 2: the role of fluids
  4.1  Introduction
  4.2  Contact metamorphism of limestone
  4.3  Buffering of H2O and CO2 in calcareous skar
  4.4  Very high temperature reactio between calcite and quartz
  4.5  Discussion
  HOMEWORK
Chapter 5  Dynamic metamorphism
  5.1  Introduction and definition
  5.2  Strain
  5.3  Classification of dynamic metamorphic rocks
  5.4  The Lochseiten Mylonite, Switzerland
  5.5  Dynamic metamorphism in Dengfeng County, Henan Province
  5.6  Dynamic metamorphism in relation to depth
  5.7  Microstructures of metamorphic rocks
  HOMEWORK
 Chapter 6  Regional metamorphism 1: Barrow's Metamorphic Zones
  6.1  Introduction
  6.2  Barrow's Zones in pelitic rocks
  6.3  Changes in mineral assemblages with metamorphic grade
  6.4  The Sulitjelma District, Norway and Sweden
  6.5  Garnet growth and zoning at Sulitjelma
  6.6  Geothermal gradients and metamorphic field gradients
  HOMEWORK
Chapter 7  Regional metamorphism 2: basic igneous rocks
  7.1  Sulitjelma greetones and amphibolites
  7.2  The boundary between the greechist and amphibolite facies
  7.3  ACF triangular diagrams to represent mineral assemblages of
metabasites
  7.4  Plotting ACF triangular diagrams
  7.5  Metamorphic temperature gradients in sedimentary basi
  HOMEWORK
Chapter 8  Regional metamorphism 3: ocean floor metamorphism
  8.1  Metamorphism at spreading ocean ridges
  8.2  The Troodos Ophiolite, Cyprus
  8.3  Petrology of the Ophiolite
  8.4  Structure and geothermal gradients of oceanic ridges
  8.5  Hydrothermal activity near spreading ridges
  8.6  Conclusio
  HOMEWORK
Chapter 9  Regional metamorphism 4: high temperature metamorphism
  9.1  Partial melting and migmatites
  9.2  Structural varieties of migmatite
  9.3  Field relatio of migmatites
  9.4  The granulite facies
  9.5  Why are granulites so dry?
  9.6  The Adirondack Mountai, New York State, USA
  9.7  Ultra-high temperature metamorphism
  HOMEWORK
Chapter 10  Regional metamorphism 5: HP and UHP metamorphism
  10.1  High pressure metamorphism
  10.2  The Franciscan metamorphic belt of California
  10.3  Eclogites and the eclogite facies
  10.4  Ultra high pressure metamorphism
  10.5  How did HP and UHP rocks get back to the surface?
10.6  UHP rocks, the range of conditio of metamorphism and
implicatio for metamorphic facies
  HOMEWORK
Chapter 11  Extra-terrestrial metamorphism
  11.1  Impact metamorphism
  11.2  Meteor Crater, Arizona, USA
  11.3  Shock metamorphism at the N6rdlinger Ries Crater, Germany
  11.4  Metamorphism in Moon rocks
References
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变质地质学(中国地质大学十一五规划教材)

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