Contact Metamorphism 0939950316
395 21 338MB
English Pages 864 Year 1991
Table of contents :
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Titles
CONTACT
DERRILL M. KERRICK, Editor
The authors, by affiliation:
The Series Editor:
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Titles
Copyright 1991
ISSN 0275-0279
Volume 26: CONTACT METAMORPHISM
Tables
Table 1
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CONTACT METAMORPHISM
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TABLE OF CONTENTS
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v
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Chapter 5 R.J. Tracy & B.R. Frost
PHASE EQUILIBRIA AND THERMOBAROMETRY OF CALCAREOUS,
ULTRAMAFIC AND MAFIC ROCKS, AND IRON FORMATIONS
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Chapter 6 James Brenan
DEVELOPMENT AND MAINTENANCE OF METAMORPHIC
PERMEABILITY: IMPLICATIONS FOR FLUID TRANSPORT
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x
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Chapter 9
STABLE ISOTOPE MONITORS
Peter I. Nabelek
Chapter 10
K.P. Furlong, R.B. Hanson & J.R. Bowers
MODELING THERMAL REGIMES
xi
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xu
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xiii
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Chapter 13
S.R. Paterson, R.H. Vernon & T.K. Fowler, Jr.
AUREOLE TECTONICS
701 Pluton shapes
706 PMR's in contact aureoles without regional deformation
706 PMR's in contact auireoles with concurrent regional deformation
Chapter 14
M.D. Barton, J-M. Staude, E.A. Snow & D.A. Johnson
AUREOLE SYSTEMATICS
xv
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xvi
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Chapter 1
Derrill M. Kerrick
OVERVIEW OF CONTACT METAMORPHISM
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•
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Tables
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N
.-~"
/
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Table 1
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r
SOUTH OF GWEEBARRA BAY
/,
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b
DfD/"Q
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Gl '-'!0
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---- /' a
Tables
Table 1
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REFERENCES
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Tables
Table 1
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Table 1
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Table 1
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Chapter 3
Theodore C. Labotka
CHEMICAL AND PHYSICAL PROPERTIES OF FLUIDS
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Tables
Table 1
Table 2
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Figure 1. The p- V - T properties of H20. derived from the
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Table 1
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Table 1
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V sr P (a V ap T
Cp = a + b T2 + cT + ~ + s: + .L:
IT T T2
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G - GO = f: V dp = RT In (to)
G- GO= RTln(fo)
f r
RTlnr=)p'VdP.
Tables
Table 1
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lnf=_b_- a + In(_lIT_) + a In(~)
V-b RTl.5(V+b) V-b bRT1.5 V+b
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Table 1
Table 2
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V= Vo- VoCln(BB+p)+(aVT) (T-To)-(aVT) (T-To)C1ln(Bl+P)
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I Volumetric Properties of CO2
I Isobars (MPa) I
...
x
III
i
a
::s
~
Temperature °C
I Isotherms (OC) I
Pressure (MPa)
of
III
~
§
~
II'::
Temperature °C
Figure 4. The p-V-T properties of eCh. derived from the equation of state of Shmonov and Shmulovich (1974).
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Tables
Table 1
Table 2
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Table 4. Specific Volume of C02 (m3lkg x 10-3)
Table 5. Fugacity of C02 (MPa)
_ RT a (T)
P-V-b - YTV(V+b)
p=RT(1+y+yLy3) a(T. V) a(T. V)=e+#-+ ~2
V(1_y)3 YTV(V+b) y=...b...
4V
RT in !H,O = a + b T + e T2
b2 ~+k
c = el + e2 P + ~ +.£1..
Tables
Table 1
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Fugacity of CO2 Comparison
Tables
Table 1
Table 2
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.c~h:H2Q mixtures
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µi(T,p) = µ(T,l) + RTIn Ii = µiO(T,l) + RTIn aj[( = µt(T,l) + RT
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Table 8. MRK Equations of State for CH4 and other COHS Gases
Tables
Table 1
Table 2
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a
a
NaCI Dissociation Constant
Isobars (MPa)
o --- --- --- --- ---
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Table 1
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Tables
Table 1
Table 2
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OuartZ- H2Q
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Tables
Table 1
Table 2
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log m = A + B (log V) + C(log V)2
T 'rZ +
T
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~
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oS
Solubility of Calcite
fH,fo~ T
f~ T T
fo~ T T
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Table 1
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Temperature COC)
Closed System Graphite + H20
-----
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Temperature COC)
-20
9
~
- -25
Temperature COC)
REV026C003_p75-104.pdf
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A I p = 150MPa
-20
s
b.O
...
-40~------~------~----~------~------~------_J
Temperature CCC)
B
p = 150 MPa
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(a~=(x~2 .
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A
Temperature CCC)
B
-
o
e
=
E-c
1.0 - XH20
KD is the ratio
which is assumed to be 1.5 in Figure 18.
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(Kff1 + (1- Kgu) x~t ftho
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1.00 r--~--..,..--'T"""-_'!"'"--~--"
Wollastonite + Calcite + Quartz + Graphite
600
0.00 I I I --- I I I I
300 400 500
Temperature (OC)
1150 MPal
0.20
~
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....
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XC02
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/ .
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,-..
o
B
550
500
450
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400°C Solvus
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dv;
Q=v=-Kq(Vp - pg)
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Tables
Table 1
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Daa = _.KT_(~)1{3
2 It 11a v.
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!lI. = 1( v2r ,
95
Dt
dt
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Table 1
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REFERENCES
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Chapter 4 D.R.M. Pattison & R.J. Tracy
PHASE EQUILIBRIA AND THERMOBAROMETRY
OF METAPELITES
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Table 1
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Tables
Table 1
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Tables
Table 1
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Zones I 810
Zones JI8 ill
~ W ~ ~ ~ w m
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M/FM
Zone N(a)
Zone N:(bl
M/FM
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Zones 'I. 8 'I.o
Zone Yb
Tables
Table 1
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Tables
Table 1
Table 2
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Table 1
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m:
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Fe
Zone I
Mg
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Zone JI[
Zone II
Zone II
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Fe
Zone IT
Mg
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Zone ill
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Table 1
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Tables
Table 1
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T
MSIAIS
L
22
Btl Grt
L
V
Ms
V :
: M~Srt
.
KMASH
KFASH
p
V
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KFMASH
p
/
/ Sil
T
22
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Average pelite P = 5 kbars
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Table 1
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Table 1
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Table 1
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Table 1
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r
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700
650
600
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-
-
600
P=3kbar
/
0.4
0.5
0.6
0.9
a H 0
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-
u
a,
I-
550
p = 3 kbar
-'.---- --
/:_ - Crd -
i: \ __ -........ Kf
/ \_: . Ms ----B ~ H20
• / ~ 1 - """
fIr\\ : / : a. = 0 84 alz~
/~. . H20 .
1
· ..-0
· : rd
500~~~~--~~~--~~~~
0.1 0.3 0.5 0.7 0.9
Mg/(Mg+Fe)
Table 5. Pressure ranges of facies series (in kbar), using different And = Sil curves.
Tables
Table 1
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-
o
-
t-
---
Distance (Km)
Tables
Table 1
REV026C004_p175-206.pdf
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GOOOr L_
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Table 1
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Table 6. Calculated pressures based on reactions (1) and (5)
Table 7. Compilation of published pressure estimates (in kbar) of contact
Figure 55. Number of occurrences of facies series types in contact and regional settings, based on the data in
Tables
Table 1
Table 2
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Appendix 1. Contact aureoles containing meta pelitic assemblages
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Kiglapait
Orijarvi
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Tables
Table 1
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Tables
Table 1
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e
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Tables
Table 1
Table 2
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Table 1
Table 2
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Tables
Table 1
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I f -Q IRT(t)
Tables
Table 1
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k
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