Comprehensive system for evaluation of velocities of acoustical energy of sedimentary rocks

Claim 2

In an environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining functional relationships between a plurality of said post deposition physical processes and the velocity distribution depicted in said maps and said plots, by classifying the characteristics of said processes against the response of each of said sequences thereto; generating a sequence velocity correction surface for each said process showing said relationship; and removing said sequence velocity correction surface from said maps and said plots.

Claim 3

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a short wave inversion, such as a salt diapir or swell, and the velocity distribution depicted in said maps and said plots, by calculating from the area and volume of said salt in said basin the average thickness and at any location therein a plurality of local thicknesses derived from seismic mapping; identifying locations and amounts of salt uplift by subtracting said average thickness from said plurality of local thicknesses, said locations of said salt uplift corresponding to positive differences thereof; spatially storing the product of compaction factor and the proportion of salt movement since sequence midpoint deposition; generating a sequence velocity correction surface covering said plurality of locations; subtracting said sequence velocity correction surface from said maps and said plot to obtain normalized velocity maps unaffected by said short wave inversions; and adding said sequence velocity correction surface to said normalized velocity maps to obtain a depth conversion unaffected by said short wave inversions.

Claim 4

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a short wave inversion, such as a salt diapir or swell, and the velocity distribution depicted in said maps and said plots, by calculating from the area and volume of said salt in said basin the average thickness and at any location therein a plurality of local thicknesses derived from seismic mapping; identifying locations and amounts of salt uplift by subtracting said average thickness from said plurality of local thicknesses, said locations of said salt uplift corresponding to positive differences thereof; spatially storing the product of compaction factor and the proportion of salt movement since sequence midpoint deposition; generating a sequence velocity correction surface covering said plurality of locations; subtracting said sequence velocity correction surface from said maps and said plot to obtain normalized velocity maps unaffected by said short wave inversions; and adding said sequence velocity correction surface to said normalized velocity maps to obtain a depth conversion unaffected by said short wave inversions.

Claim 5

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a long wave inversion, such as basin inversion, and the velocity distribution depicted in said maps and said plots; defining the areas of said basin the sequence thickens in association with an anticlinal trend; estimating inversion at a plurality of locations by using the relief of said anticlines; spatially storing the product of compaction factor and the said amount of long wave inversion since sequence midpoint deposition; generating a sequence velocity correction surface covering said plurality of locations; subtracting said sequence velocity correction surface from said maps and said plot to obtain normalized velocity maps unaffected by said long wave inversions; and adding said sequence velocity correction surface to said normalized velocity maps to obtain a depth conversion unaffected by said long wave inversions.

Claim 6

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a long wave inversion, such as basin inversion, and the velocity distribution depicted in said maps and said plots; defining the areas of said basin the sequence thickens in association with an anticlinal trend; estimating inversion at a plurality of locations by using the relief of said anticlines; spatially storing the product of compaction factor and the said amount of long wave inversion since sequence midpoint deposition; generating a sequence velocity correction surface covering said plurality of locations; subtracting said sequence velocity correction surface from said maps and said plot to obtain normalized velocity maps unaffected by said long wave inversions; and adding said sequence velocity correction surface to said normalized velocity maps to obtain a depth conversion unaffected by said long wave inversions.

Claim 7

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes of all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a tectonic episode involving compression or extension, and the velocity distribution depicted in said maps and said plots; defining the areas of said basin where sequences show estimable shortening or extension using seismic horizon data; generating maps of said compression and said extension by calculating a plurality of ratios of straight line distances between a plurality of corresponding pairs of points to unfaulted horizon length; estimating stress directions and strain amounts; generating a sequence velocity correction surface for each said tectonic episode showing said relationship; and removing said sequence velocity correction surface from said maps and said plots.

Claim 8

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes of all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a tectonic episode involving compression or extension, and the velocity distribution depicted in said maps and said plots; defining the areas of said basin where sequences show estimable shortening or extension using seismic horizon data; generating maps of said compression and said extension by calculating a plurality of ratios of straight line distances between a plurality of corresponding pairs of points to unfaulted horizon length; estimating stress directions and strain amounts; generating a sequence velocity correction surface for each said tectonic episode showing said relationship; and removing said sequence velocity correction surface from said maps and said plots.

Claim 9

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a post depositional episode involving changes in pore pressure, and the velocity distribution depicted in said maps and said plots; defining a first plurality of areas where sequences show an overpressuring effect using normalized velocities; further defining a second plurality of areas where seismic interpretations show an apparent overpressuring effect; generating a sequence velocity correction surface for each said post depositional episode showing said relationship; and removing said sequence velocity correction surface from said maps and said plots.

Claim 10

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a post depositional episode involving changes in pore pressure, and the velocity distribution depicted in said maps and said plots; defining a first plurality of areas where sequences show an overpressuring effect using normalized velocities; further defining a second plurality of areas where seismic interpretations show an apparent overpressuring effect; generating a sequence velocity correction surface for each said post depositional episode showing said relationship; and removing said sequence velocity correction surface from said maps and said plots.

Claim 11

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a tectonic process involving faulting, and the velocity distribution depicted in said maps and said plots; defining mapped sequence fault area polygons having hanging and foot wall positions and throws with added contours related spatially from said polygons at distances which are multiples of said fault throws; coordinating said tectonic process map with said maps and said plots depicting velocity distribution to develop a sequence velocity correction surface; and removing said sequence velocity correction surface from said maps and said plots.

Claim 12

In a basin environment encompassing sedimentary rocks disposed insitu in subsurface sequences, from which conventional well log data, including sonic data, has been obtained downhole, and from which seismic time sections and velocity spectra at discrete locations have been conventionally obtained, a method of evaluating velocity distributions and interpreting the depositional and post depositional causes therefor, comprising: selecting lithological units from said seismic sequences and well log data to provide interval velocities therefor; inverting said sonic well log data to obtain velocities therefor; plotting velocity versus depth for said well sonic data; determining compaction factor by calculating the mean slope of all individual sonic data segments; determining preliminary normalized interval velocity with constant average compaction factor by calculating an average of the slopes for all of said segments for each well segment penetrating each said sequence; mapping compaction variation per sequence to determine the affect of lateral compaction variation upon velocity distribution; ascertaining a functional relationship between a tectonic process involving faulting, and the velocity distribution depicted in said maps and said plots; defining mapped sequence fault area polygons having hanging and foot wall positions and throws with added contours related spatially from said polygons at distances which are multiples of said fault throws; coordinating said tectonic process map with said maps and said plots depicting velocity distribution to develop a sequence velocity correction surface; and removing said sequence velocity correction surface from said maps and said plots.

Claim 15

Each and every novel method for geophysical prospecting or exploration to locate oil rich shale deposits as hereinbefore described or defined specifically or generally.

Claim 16

Each and every novel method for geophysical prospecting or exploration to locate oil rich shale deposits as hereinbefore described or defined specifically or generally.

Claim 17

Apparatus embodying means to put into effect a method according to any one of claims 1 to 9.

Claim 18

Apparatus according to claim 10, which apparatus comprises a computer set up to operate according to one or more programs which put into effect said method of any one or more of claims 1 to 9.

Claim 19

A technical process making use of a method according to any one of claims 1 to 9 in the solution of one or more technical problems associated with geophysical prospecting or exploration based on the determination of velocities of accoustic energy of sedimentary rocks to locate oil rich shale deposits.

Claim 20

A technical process according to claim 12, which process is carried out under the control of a computer program which puts into effect a method according to any one of claims 1 to 9.