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Field Description of Metamorphic Rocks 2nd edition [Mīkstie vāki]

(Virginia Polytechnic Institute and State University, Blacksburg, VA, USA), (University of Olso, Norway)
  • Formāts: Paperback / softback, 192 pages, height x width x depth: 213x140x13 mm, weight: 272 g
  • Sērija : Geological Field Guide
  • Izdošanas datums: 24-Mar-2022
  • Izdevniecība: Wiley-Blackwell
  • ISBN-10: 1118618750
  • ISBN-13: 9781118618752
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  • Mīkstie vāki
  • Cena: 36,44 €
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  • Bibliotēkām
  • Formāts: Paperback / softback, 192 pages, height x width x depth: 213x140x13 mm, weight: 272 g
  • Sērija : Geological Field Guide
  • Izdošanas datums: 24-Mar-2022
  • Izdevniecība: Wiley-Blackwell
  • ISBN-10: 1118618750
  • ISBN-13: 9781118618752
Citas grāmatas par šo tēmu:
"Metamorphic rocks form a substantial proportion of the material that makes up the Earth's crust, and metamorphic processes have been almost continually occurring throughout geological time since the origin of that crust. Metamorphism can be defined simply as the process by which sedimentary or igneous rocks are transformed (metamorphosed) by re-crystallisation due to changes in pressure, temperature, or fluid conditions. To complicate matters somewhat, metamorphism can of course also act on rocks that have already been metamorphosed previously, building layer upon layer of complexity into those rocks that record field evidence of some of Earth's most dynamic processes. Our understanding of metamorphism is somewhat limited by the fact that we are unable to directly observe it happening to the rocks. As you read this, metamorphism is in action all around the planet, in all aspects of the Earth's plate tectonic system (e.g. Figure 1.1), but we cannot directly see it (generally because it happens at depth and very slowly). In order to understand the processes and products of metamorphism and alteration in rocks, detailed fieldwork, petrography, experimental studies, and numerical modelling are required. It is important to note, however, that the very originof metamorphic petrology (the science of understanding the distribution, structure, and origin of metamorphic rocks) is rooted in a tradition of careful and systematic field observation, and that this remains an absolute cornerstone of the discipline today"--

This hand pocket-sized field guide describes how metamorphic rocks and rock masses maybe observed, recorded and mapped in the field. Written at a level suitable for earth science undergraduate students, this book is an essential tool for any geologist—student, professional or amateur—faced with the task of making a general description of an area of metamorphic rocks. A clear, systematic framework, together with numerous colour diagrams, illustrations and checklists, enables readers to produce useful and broadly similar descriptions, despite possible differences of background or specialist interest. Additional information is also provided to aid those who are undertaking a field mapping and report course.

  • Shows the reader how to observe metamorphic rocks in the field, from the outcrop to the hand specimen scale
  • Fully revised and updated to incorporate new developments in the field
  • User-friendly and accessible writing style Including a revised format with tabbed sections for easy navigation
  • Key topics covered include; classification and mapping of metamorphic rocks, understanding key textures and fabrics, and details on contacts and fault zones.
Preface vii
Acknowledgments ix
1 Introduction and Occurrence 1(16)
1.1 The Importance of Fieldwork in Metamorphic Terrains
1(3)
1.2 Understanding Metamorphism; Pressure/Temperature Relationships
4(1)
1.3 Mode of Occurrence of Metamorphic Bodies
4(9)
1.4 Summary
13(4)
2 Field Skills and Mapping Outcrop Structures 17(20)
2.1 Equipment
17(2)
2.2 Preparing Maps and Basic Mapping
19(1)
2.3 Notebooks and Data Recording
20(13)
2.4 Digital 3D Outcrop Mapping
33(4)
3 Metamorphic Minerals, Rock Types, and Classification 37(30)
3.1 Minerals
37(9)
3.2 The Basic Classification of Metamorphic Rocks in P-T
46(2)
3.3 Metamorphic Rock Names
48(2)
3.4 Reporting Rock Types
50(4)
3.5 Compositional Category and Metamorphic Grade
54(13)
4 Understanding Textures and Fabrics 1: Banding, Cleavage, Schistosity, and Lineations 67(28)
4.1 General Terminology
67(4)
4.2 Rocks without a Metamorphic Directional Fabric
71(1)
4.3 Banding
71(8)
4.4 The Development of Fabric, Cleavage, Schistosity, and Lineations
79(9)
4.5 Refraction, Kinking, and Shearing of Fabrics
88(1)
4.6 Deformation Fabrics and Folds
89(6)
5 Understanding Textures and Fabrics 2: Metamorphic Crystals, Pseudomorphs, and Scattered Entities 95(20)
5.1 Recording Metamorphic Textures
95(2)
5.2 Metamorphic Crystal Growth and Porphyroblasts
97(12)
5.3 Boudins, Shear Pods, and Knockers
109(6)
6 Contacts, Reaction Zones, and Veins 115(22)
6.1 Igneous Contacts - Aureoles and Metasomatism
115(9)
6.2 Veins and Pegmatites
124(6)
6.3 Reaction Zones and Chemical Changes at Contacts
130(7)
7 Faults, Mylonites, and Cataclasites 137(14)
7.1 Fault and Shear Zone Types
137(1)
7.2 Faults and Fault Breccias
138(3)
7.3 Cataclasites and Pseudotachylites
141(3)
7.4 Mylonites and Shear Zones
144(7)
8 Summary Tables, Checklists, and Mapping Report Advice 151(20)
8.1 Compositional Categories and Their Grade Indicators
151(6)
8.2 Minerals
157(7)
8.3 Further Mapping Advice; Formations, Markers, and a Final Report
164(7)
Checklist of Rock Features 171(2)
Further Reading Suggestions 173(2)
Index 175
Dougal Jerram, University of Oslo, Norway and DougalEARTH Ltd, Solihull, UK.

Mark Caddick, Virginia Tech, Blacksburg, VA, USA.