变质地质学

作者简介

《中国地质大学十一五规划教材·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。《中国地质大学十一五规划教材·变质地质学》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。

书籍目录

Chapter 1 Definition of metamorphism, classification of metamorphic rocks1.1 Definition of metamorphism1.2 Classification and nomenclature of metamorphic rocks1.3 The minerals of metamorphic rocks1.4 English mineral names1.5 Description of thin sections of metamorphic rocksHOMEWORKChapter 2 Conditions of metamorphism, P-T-t paths, the Phase Rule, composition-assemblage diagrams, metamorphic facies2.1 Limits of metamorphism2.2 P-T-t paths2.3 Equilibrium2.4 The Phase Rule2.5 Using the Phase Rule to fix P- T Conditions2.6 AFM diagrams2.7 Metamorphic faciesHOMEWORKChapter 3 Contact metamorphism 1 : the role of heat3.1 Introduction3.2 Contact aureole of the Markfield Diorite, Leicestershire, England3.3 Contact aureole of the Skiddaw Granite, Lake District, England3.4 Heat transfer at the contacts of intrusions3.5 Effect of intrusion size and shape on aureole size and shape3.6 Thermal conduction models of contact aureoles3.7 Thermal convection models of contact aureoles3.8 Facies series in contact metamorphismHOMEWORKChapter 4 Contact metamorphism 2: the role of fluids4.1 Introduction4.2 Contact metamorphism of limestone4.3 Buffering of H2O and CO2 in calcareous skarns4.4 Very high temperature reactions between calcite and quartz4.5 DiscussionHOMEWORKChapter 5 Dynamic metamorphism5.1 Introduction and definition5.2 Strain5.3 Classification of dynamic metamorphic rocks5.4 The Lochseiten Mylonite, Switzerland5.5 Dynamic metamorphism in Dengfeng County, Henan Province5.6 Dynamic metamorphism in relation to depth5.7 Microstructures of metamorphic rocksHOMEWORKChapter 6 Regional metamorphism 1: Barrows Metamorphic Zones6.1 Introduction6.2 Barrows Zones in pelitic rocks6.3 Changes in mineral assemblages with metamorphic grade6.4 The Sulitjelma District, Norway and Sweden6.5 Garnet growth and zoning at Sulitjelma6.6 Geothermal gradients and metamorphic field gradientsHOMEWORKChapter 7 Regional metamorphism 2: basic igneous rocks7.1 Sulitjelma greenstones and amphibolites7.2 The boundary between the greenschist and amphibolite facies7.3 ACF triangular diagrams to represent mineral assemblages of metabasites7.4 Plotting ACF triangular diagrams7.5 Metamorphic temperature gradients in sedimentary basinsHOMEWORKChapter 8 Regional metamorphism 3: ocean floor metamorphism8.1 Metamorphism at spreading ocean ridges8.2 The Troodos Ophiolite, Cyprus8.3 Petrology of the Ophiolite8.4 Structure and geothermal gradients of oceanic ridges8.5 Hydrothermal activity near spreading ridges8.6 ConclusionsHOMEWORKChapter 9 Regional metamorphism 4: high temperature metamorphism9.1 Partial melting and migmatites9.2 Structural varieties of migmatite9.3 Field relations of migmatites9.4 The granulite facies9.5 Why are granulites so dry?9.6 The Adirondack Mountains, New York State, USA9.7 Ultra-high temperature metamorphismHOMEWORKChapter 10 Regional metamorphism 5: HP and UHP metamorphism10.1 High pressure metamorphism10.2 The Franciscan metamorphic belt of California10.3 Eclogites and the eclogite facies10.4 Ultra high pressure metamorphism10.5 How did HP and UHP rocks get back to the surface?10.6 UHP rocks, the range of conditions of metamorphism and implications for metamorphic faciesHOMEWORKChapter 11 Extra-terrestrial metamorphism11.1 Impact metamorphism11.2 Meteor Crater, Arizona, USA11.3 Shock metamorphism at the N6rdlinger Ries Crater, Germany

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