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9780195109207

Geochronology and Thermochronology by the 40ar/39ar Method

by ;
  • ISBN13:

    9780195109207

  • ISBN10:

    0195109201

  • Edition: 2nd
  • Format: Hardcover
  • Copyright: 1999-08-05
  • Publisher: Oxford University Press

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Summary

Argon isotopic dating is one of the most important techniques for estimating the ages of rocks and can be used on very small samples. It has been used to assign reliable ages to the Earth and numerous meteorites. This second edition covers the standard principles and methods and incorporates many of new developments from the last decade. It covers the basis of the method, technical aspects, data presentation, diffusion theory, thermochronology, and many applications and case studies.

Table of Contents

Historical Introduction
3(6)
General comments
3(1)
Historical outline
4(5)
Basis of the 40Ar/39Ar Dating Method
9(35)
Potassium-argon dating
9(3)
40Ar/39Ar dating
12(2)
Potassium and its isotopes
14(1)
The 40K decay scheme and constants
15(1)
Derivation of age equations
16(3)
Atmospheric argon
19(1)
Materials suitable for dating
20(19)
Range of applicability
39(5)
Technical Aspects
44(65)
Introduction
44(1)
Sample preparation
44(1)
Monitor minerals
45(5)
Nuclear reactions
50(1)
Nuclear reactors as a neutron source
51(3)
The 39K(n,p)39 Ar reaction
54(3)
Interfering nuclear reactions and correction factors
57(8)
Optimization of irradiation parameters
65(5)
Neutron flux gradients
70(4)
Self-shielding
74(1)
Temperature effects
74(1)
Lattice damage
74(1)
Decay factors
75(1)
Total sample activity
75(1)
Safety aspects
76(1)
Argon extraction systems
76(6)
Mass spectrometry
82(11)
Laser microprobes
93(16)
40Ar/39Ar Data Presentation and Interpretation
109(28)
Introduction
109(1)
Simple behavior (closed system)
109(6)
Complex behavior (open sytem)
115(5)
Mixed phases
120(3)
Excess argon
123(7)
Nuclear recoil
130(1)
Grain size and distribution
131(1)
Phase changes in vacuum
132(1)
Resolution within the age spectrum
133(4)
Appendix 4.A.1 Isochron analysis
134(3)
Diffusion Theory and Measurements
137(28)
Introduction
137(1)
The process of diffusion
137(1)
The phenomenological basis of diffusion theory
138(1)
Methods of solution for constant D
139(1)
Episodic 40Ar loss
140(3)
Diffusion mechanisms
143(2)
Measurement of argon diffusion in silicates
145(20)
Appendix 5.A.1 Derivation of the diffusion equation
159(2)
Appendix 5.A.2 Separation-of-variables solution for a plane sheet
161(2)
Appendix 5.A.3 Translation to spherical coordinates
163(1)
Appendix 5.A.4 Sample diffusion calculation
164(1)
40Ar/39Ar Thermochronology
165(26)
Introduction
165(1)
The closure temperature concept
165(8)
Models for complex argon diffusion behavior of silicates
173(7)
Evaluation of the multidiffusion domain and multipath models
180(5)
Nonmonotonic thermal histories
185(6)
Appendix 6.A.1 Closure temperature for first-order loss
185(2)
Appendix 6.A.2 Closure temperature for volume diffusion
187(1)
Appendix 6.A.3 Closure profiles
188(1)

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