Rock-Fabric/Petrophysical
Relationships
Petrophysics
of Interparticle
Pore Space
Limestone
Rock Fabrics
Examples of
nonvuggy limestone
petrophysical rock
fabrics are illustrated in Fig. 7. In grainstone
fabrics, the pore-size distribution is controlled by grain size;
in mud-dominated
fabrics, the size of the micrite particles controls the pore-size
distribution. In grain-dominated
packstones, however, the pore size distribution is controlled
by grain size and by the size of micrite particles between grains.
Figure 8 illustrates all the data for limestones compared with the
permeability
fields. Grainstone and mud-dominated fabrics are reasonably well-constrained
permeability fields. Although grain-dominated packstone fabrics
plot at an intermediate location between grainstones and mud-dominated
limestones, they show more variability because of the large grain
size difference. Grain size of grain-dominated packstone ranges
from 400 microns for oncoid fabrics to 80-150
for fine peloid fabrics.
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Class
1 ooid grainstone
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Class
1 ooid grainstone
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Class
2 peloid grain-dominated packstone
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Class
2 oncoid grain-dominated packstone
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Class
3 fossil mud-dominated packstone
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Class
3 rudist floatstone
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Class
3 Orbitolind wackestone |
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Figure7.
Examples of nonvuggy limestone rock fabrics.
(click
on each image to see a larger version)
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Despite the
considerable scatter in the data, grainstone,
grain-dominated
packstone, and mud-dominated
fabrics are reasonably well constrained to the three permeability
fields. Whereas grain size and sorting define the permeability fields,
the interparticle porosity defines pore-size distribution and thus
the permeability within the field. Systematic changes in intergrain
porosity by cementation, compaction, and dissolution processes will
produce systematic changes in pore-size distribution and result
in systematic changes in permeability. Therefore, permeability in
nonvuggy limestones
is a function of interparticle porosity, grain size, and sorting.
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Figure
8. Porosity-air permeability cross plot for nonvuggy limestone
fabrics compared with the three permeability fields.
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Dolostone
Rock Fabrics
Examples of
nonvuggy dolostone
petrophysical rock
fabrics are illustrated in figure 9. Dolomitization
can change the rock fabric significantly. In limestones,
fabrics can usually be distinguished with little difficulty. If
the rock has been dolomitized, however, the overprint of dolomite
crystals often obscures the limestone fabric precursor. Precursor
fabrics in fine-crystalline dolostones are easily recognizable.
However, as the crystal size increases, the precursor fabrics become
progressively more difficult to determine.
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Class
1 peloid med xl dolograinstone
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Class
1 ooid med xl dolograinstone
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Class
2 peloid med xl g.d. dolopackstone
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Class
2 peloid med xl g.d. dolopackstone
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Class
3 f. xl dolowackestone
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Class
2 med xl dolowackestone
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Class
1 lg xl dolowackestone
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Class
1 lg xl dolograinstone
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Figure
9. Examples of nonvuggy dolostone rock fabrics.
(click
on each image to see a larger version)
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Dolomite crystals
(defined as particles in this classification) commonly range in
size from several m to >200 .
Lime mud particles are usually <20
in size. Thus, dolomitization
of a mud-dominated carbonate fabric can result in an increase in
particle size from <20
to >200
(Fig. 9). The plot of interparticle porosity
against permeability (Fig. 10a) illustrates
the principle that, in mud-dominated
fabrics, permeability increases as dolomite crystal size increases.
Finely crystalline (average 15 m) mud-dominated dolostones
plot within the class 3 permeability
field. Medium crystalline (average 50 )
mud-dominated dolostones
plot within the class 2 permeability field. Large crystalline (average
150 )
plot in the class 1 permeability field.
Grainstones
are usually composed of grains much larger than the dolomite crystal
size (Fig. 9) so that dolomitization
does not have a significant effect on the pore size distribution.
This principle is illustrated in Fig. 10b
where interparticle porosity
is plotted against permeability
measurements from dolograinstones.
The grain size of the dolograinstones is 200 .
Fine crystalline dolograinstone, medium crystalline dolograinstone
and large crystalline dolograinstone all plot within the class 1
permeability field. The large crystalline mud-dominated dolostones
also plot in this permeability field, indicating that they are petrophysically
similar to grainstones (Fig. 10a).
A cross plot
of interparticle porosity and permeability measurements from fine
to medium crystalline grain-dominated
dolopackstones is presented in Fig. 10c.
The average grain size is 200 .
The data plot in the class 2 permeability field. The medium crystalline
mud-dominated dolostones also plot in this field (Fig.
10a).
Figure 11 illustrates
all dolomite data compared with permeability
fields. Dolograinstones
and large crystal dolostones
constitute the class 1 permeability
field. Grains are very difficult to recognize in dolostones with
a > 100
crystal size. However, because all large crystalline dolostones
and all dolograinstones are petrophysically similar, whether the
crystal size or the grain size is described makes little difference
petrophysically. Fine and medium crystalline grain-dominated
dolopackstones and medium crystalline mud-dominated dolostones
constitute the class 2 permeability field. Fine crystalline mud-dominated
dolostones constitute the class 3 field.
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Figure
11. Composite porosity-air permeability cross plot for nonvuggy
dolostone fabrics compared with the three permeability fields. |
The dolomite
permeability
fields are defined by dolomite crystal size as well as grain size
and sorting of the precursor limestone. Within the field, permeability
is defined by interparticle porosity. Systematic changes in intergrain
and intercrystal porosity by predolomite calcite cementation, dolomite
cementation, and compaction will systematically change the pore-size
distribution, resulting in a systematic change in permeability.
Therefore, dolomite crystal size, grain size, and sorting define
the permeability field, and interparticle porosity defines the permeability.
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Figure
12. Composite porosity-air permeability cross plot for nonvuggy
limestones and dolostones showing transforms for each class.
See text for equations. |
Limestone
and Dolostone Combined
Data from limestone
and dolostone
rock fabrics
are combined into one interparticle-porosity permeability
cross plot in figure 12. The fabrics that make up the class 1 field
are (1) limestone and dolomitized
grainstones and (2) large crystalline grain-dominated
dolopackstones and mud-dominated dolostones. An upper particle
size limit of 500
is imposed but not well defined. The upper limit is imposed because
as the grain size increases the slope of the porosity-permeability
transform approaches infinity and permeability becomes independent
of porosity.
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Figure
13. Petrophysical/rock-fabric classes based on similar capillary
properties and interparticle-porosity/permeability transforms. |
Fabrics that make up the class 2 field are (1) grain-dominated
packstones, (2) fine to medium crystalline grain-dominated
dolopackstones, and (3) medium crystalline mud-dominated dolostones.
The class 3 field is characterized by mud-dominated
fabrics (mud-dominated
packstone, wackestone,
and mudstone)
and fine crystalline mud-dominated dolostones. This arrangement
of petrophysically similar rock
fabrics is illustrated in figure 13.
Transforms are
presented below for each combined permeability
field (Fig. 12).

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