更新时间：2023-07-16 16:04
《变质地质学》是2007年10月中国地质大学出版社出版的图书，作者是梅森。
《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。
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