變質地質學

變質地質學

《變質地質學》是2007年10月中國地質大學出版社出版的圖書,作者是梅森。

基本介紹

  • 書名:變質地質學
  • 作者:梅森
  • ISBN:9787562522072
  • 頁數:153
  • 定價:50.00元
  • 出版社:中國地質大學出版社
  • 出版時間:2007-10
內容簡介,目錄,

內容簡介

《中國地質大學十一五規劃教材·變質地質學》是隨著20世紀60年代板塊構造學興起而迅速發展起來的地質學科,作為課程,它屬於地質專業課程性質,具有顯著的地質前沿和岩石學與構造學學科交叉特點。《中國地質大學十一五規劃教材·變質地質學》全面介紹了變質岩石學和變質地質學的基礎理論、基礎知識和基本技能。內容主要包括變質作用通論、接觸變質、動力變質和區域變質及地外變質五大部分。

目錄

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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