Definition: A cross section is a profile showing geological features in a vertical plane through the earth There are two categories of cross sections: structural and stratigraphic.. •
Trang 1Chapter 07
SUBSURFACE MAPPING
AND CROSS SECTION
UA-2011
Trang 2– MECHANICAL & INTERPRETIVE CONTOURING
• STRUCTURAL CONTOUR MAP
• ISOPACH AND OTHER SUBSURFACE MAPS
Trang 3– STRUCTURAL CROSS SECTIONS
– STRATIGRAPHIC CROSS SECTIONS
– CORRELATION AND GEOLOGICAL INTERPRETATION
– COMPLETING THE CROSS SECTION
• CROSS-SECTION DIAGRAMS IN 3 DIMENSIONS
– FENCE DIAGRAMS
– BLOCK DIAGRAMS
• COMPUTER-DRAWN CROSS SECTION s
Trang 4– MECHANICAL & INTERPRETIVE CONTOURING
• STRUCTURAL CONTOUR MAP
• ISOPACH AND OTHER SUBSURFACE MAPS
Trang 5LATERAL CORRELATION OF LOGGED DATA
• Using Data Points to Define Surfaces
Trang 6Fig 01-Sharp vertical stratigraphic changes are excellent regional markers
Trang 7Fig : 02
Trang 8Fig : 03
……
Trang 9• Using Surfaces to Delimit Units
• Contour Mapping
• Mechanical & Interpretive Contouring
Trang 10Fig : 04
Trang 11Fig : 05
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Trang 14– STRUCTURAL CROSS SECTIONS
– STRATIGRAPHIC CROSS SECTIONS
– CORRELATION AND GEOLOGICAL INTERPRETATION
– COMPLETING THE CROSS SECTION
• CROSS-SECTION DIAGRAMS IN 3 DIMENSIONS
– FENCE DIAGRAMS
– BLOCK DIAGRAMS
• COMPUTER-DRAWN CROSS SECTION s
Trang 15Definition: A cross section is a profile showing
geological features in a vertical plane through the
earth
There are two categories of cross sections:
structural and stratigraphic
Structural cross sections illustrate
present-day structural features such as dips, folds, and faults
Stratigraphic cross sections show
characteristics such as formation thicknesses,
lithologic sequences, stratigraphic correlations, facies changes, unconformities, fossil zones, and ages
Trang 16Cross sections are also useful for
display purposes Diagrammatic cross sections show broad relationships
and serve to orient the audience to
the general geology of a region (Fig: 06)
Trang 17Fig : 06
Trang 18– STRUCTURAL CROSS SECTIONS
– STRATIGRAPHIC CROSS SECTIONS
– CORRELATION AND GEOLOGICAL INTERPRETATION
– COMPLETING THE CROSS SECTION
• CROSS-SECTION DIAGRAMS IN 3 DIMENSIONS
– FENCE DIAGRAMS
– BLOCK DIAGRAMS
• COMPUTER-DRAWN CROSS SECTION s
Trang 19• Input Data
Different types of data can be used in developing a cross section The diagram may be based on outcrop information, or on subsurface data derived from wells and geophysical surveys, or it may use both outcrop and subsurface data
Trang 20• Outcrop information are particularly
useful in frontier areas of petroleum
exploration, where subsurface
information is often sparse or
unavailable
• Many geological cross sections made for
petroleum exploration rely on subsurface data.
• The geologist should recorrelate all logs
to ensure accuracy and consistency.
Trang 21Distortion of true thickness (t) and true dip (d) measurements
due to borehole deviation; tA= apparent thickness and dA=
apparent dip.
Fig : 07
Trang 22Segments of the borehole which do not lie in the plane of section are dashed onto the cross sections Due to foreshortening, the dashed segments show only apparent deviation This can be
seen by comparison with the inset plan view
Fig : 08
Trang 23• Line of Section
After gathering available data, the next
in cross section development step is
to choose the line of section, i.e., the line along which the cross section
would intersect the surface of the
earth (Fig 08)
Cross sections may trend perpendicular
to strike, oblique (uốn theo) to strike,
or parallel to strike (Fig 09)
Trang 26– STRUCTURAL CROSS SECTIONS
– STRATIGRAPHIC CROSS SECTIONS
– CORRELATION AND GEOLOGICAL INTERPRETATION
– COMPLETING THE CROSS SECTION
• CROSS-SECTION DIAGRAMS IN 3 DIMENTIONS
– FENCE DIAGRAMS
– BLOCK DIAGRAMS
• COMPUTER-DRAWN CROSS SECTION s
Trang 27The most common type of diagram showing geological relationships in three dimensions
is a fence diagram (Figure 1) Fence diagrams consist of a three-dimensional network of geological cross sections drawn
in two dimensions The diagram is built on a map base which is seen in plan view.
Trang 28Figure 01
Trang 29Fence Diagrams
In constructing a fence diagram, the plane
of the map base corresponds to the chosen datum plane, and the well location on the
map is taken to be the point where the well intersects the datum plane The wells are
hung on the datum and then individual
cross section panels are filled in, beginning
at the front of the diagram
In fence diagrams, one must consider the overall orientation of the figure, bearing in mind that panels oriented parallel to the viewing direction will appear only as straight lines Such panels are usually omitted from the diagram If important panels are not displayed to the best advantage, the viewing direction can be changed so that the features of interest are presented in the most effective way
Trang 30Fence Diagrams
Front panels sometimes obscure parts of rear
panels in fence diagrams Where two panels
overlap, the correlations on the front panel are drawn in with solid lines and highlighted with
colors, while the correlations on the overlapped part of the rear panel are simply dashed in
When the vertical scale is too large or the spacing of sections is too close, very large parts
of the rear panels may be obscured (Figure 2)
Trang 31Figure 02
Trang 32Fence Diagrams
Usually, this problem can be minimized if the vertical scale and the panel spacing
are carefully chosen However, it is not
always possible to change the scale or
spacing without losing important details illustrated by the diagram In such a case, one can construct an isometric projection
of the fence diagram ( Figure 4 , only lines
parallel to the North-South and East-West axes are undistorted)
The map base in an isometric projection is shown as if it was turned at an angle and tilted toward the viewer The conversion
is actually a transformation from
orthogonal to nonorthogonal axes A
rectangular map base will become a
parallelogram in an isometric projection
( Figure 3 and Figure 4)
Trang 33• All lines that were parallel to the original
horizontal and vertical axes remain
parallel to the corresponding new axes, and the scale along these lines also
remains unchanged However, lines
which were not parallel to the original
axes will be distorted Points along such lines must be transferred onto the
projection by coordinates relative to the new axes A grid system is helpful in this process
Trang 34Figure 03
Trang 36Block Diagrams
• Along with the fence diagram, another
dimensional geological relationships is a block diagram (Figure 5)
• This type of figure is a two-dimensional
representation of a rectangular block Two intersecting cross sections often form the sides of the block; the top of the block
shows either a mapped surface or relief on the uppermost geological boundary shown
in the cross sections The block may be
rotated to achieve the most effective
viewing angle, and it may be drawn with or without the use of perspective
Trang 37Figure 05
Trang 38Block Diagrams
• Isometric block diagrams do not employ
perspective opposite sides of the block
remain parallel, making the distant end of the diagram appear to be larger (Figure
6 , Figure 7, and Figure 8)
The top of this type of block diagram may
be given any degree of tilt toward the
viewer
Trang 39Figure 06
Trang 41Figure 08
Trang 42• A large amount of tilt emphasizes features
on the top surface of the block; a smaller degree of tilt brings out details on the
sides of the block Scales along the x, y,
and z axes need not be equal
• The scale along the sides of the figure (y)
is sometimes chosen to be smaller than
the scale across the front and back edges (x), thus creating an illusion of
perspective
• Perspective can be used in constructing
block diagrams (Figure 9)
Trang 43Figure 09
Trang 44In perspective blocks, all parallel lines with
a component in the y direction converge to a vanishing point on the horizon
Sets of parallel lines with different orientations converge to different vanishing points
The cross section on the front face of the
perspective It is possible both to rotate the block about the z axis or to display it at different elevations relative to the horizon Again, the choice of block orientation is made to emphasize the important features
of the diagram
Trang 45Computer-Drawn Cross Sections