# Patent

## Title
Healthcare data acquisition device

## Abstract

This application claims the benefit of U.S. Provisional Application No. 60/100,019, filed Sep. 11, 1998.

## Background
This invention relates generally to beds, or reservoir layers, and in particular to methods for determining the net and gross thickness of a bed. Hydrocarbon reservoirs in general are not perfect blocky beds, but rather have internal structure in the form of embedded layers of non-reservoir or poor reservoir quality material. However, existing methods for determining gross or net reservoir thickness of these reservoirs ignore or do not accurately consider the internal structure. Thus, those methods have neglected to include effects associated with the internal structure of beds, in the determination of the net and gross thickness of beds.

The method of the present invention, for the determination of the net and gross thickness of reservoir beds, solves the difficulties of other existing methods, by providing a method that takes into account the internal structure of reservoir beds.

FIG. 1 is an illustration of the band pass filters, and the outputs generated by those filters, used in the method of the present invention.

FIG. 2 is a cross-sectional illustration of different types of beds which are analyzed using the method of the present invention.

FIG. 3 is an illustration of an amplitude signature of a blocky bed, with an embedded reservoir layer.

FIG. 4 is an illustration of an amplitude signature of the bed of FIG. 3, with another, thinner bed embedded within it.

FIG. 5 is an illustration of the amplitude signatures of the beds of FIGS. 3 and 4, with a curve showing the effect of the embedded bed.

FIG. 6 is an illustration of an amplitude signature of a blocky bed, with embedded non-reservoir layers.

The methods of the present invention, for determining the gross and net thickness of a reservoir bed, or layer, have in common the following steps. First, as shown in FIG. 1, the seismic data is filtered by a series of band pass filters, 10, 12, 14, each of which has a fixed lower frequency f.sub.L but with progressively higher upper frequency f.sub.U. Next, the amplitudes are extracted on a lobe, or sample by sample, basis from filtered seismic traces 16, 18, 20, or from the energy envelope derived from the filtered seismic traces. These amplitude values A.sub.i and the corresponding frequencies f.sub.Ui, which characterize the filter applied, make up the "amplitude signature" which, as described below, is used to determine the gross and net thickness.

Referring now to FIG. 2, a variety of types of information is extracted from the amplitude signatures related to the properties of the beds 30, 32 being imaged. These extracted properties will be referred to as Frequency Dependant Attributes or FDA's. The bed geometry described applies for P-P, P-S and S-S data. These time thicknesses .DELTA.t and .delta.t.sub.i are related to each other and to .DELTA.Z as shown below in equations. For all of the methods described, the relationships between the various thicknesses are defined and related to each other as: thickness in two-way travel time

For the case of a single embedded bed, the net thickness is:

.DELTA.t.sub.net =.DELTA.t-.delta.t=the net reservoir thickness in two-way travel time.

The amplitude signature for a blocky reservoir bed is: ##EQU1##

where ##EQU2##

FIG. 3 illustrates the amplitude signature 34 given by Equation 1, for the case of .DELTA.t=.02 seconds.

The amplitude signature for a blocky reservoir bed with one or more smaller non-reservoir layers embedded in it is approximately: ##EQU3##

where the time reference is the position in the trace where the amplitude is an extrema ("Extrema" means the largest value, regardless of the sign, that is, regardless of whether it is positive or negative), and where ##EQU4##

FIG. 4 illustrates the amplitude signature 36 for the bed 32, given by Equation 2, for the case of .DELTA.t=0.02 seconds and for a single embedded layer .delta.t.sub.i =0.005.

Equation 2 reveals that the effect of one or more non-reservoir beds embedded in a thicker reservoir layer is to produce the expected amplitude response of the gross reservoir (see curve 40 in FIG. 5, the black curve), with the polarity reversed amplitude response curve of the unresolved embedded non-reservoir bed (see curve 42FIG. 5, red curve). The net effect is to produce an amplitude decay with increasing frequency (see curve 44, FIG. 5, green curve). From this amplitude decay with frequency effect, curve 44, the net bed thickness is determined as described below.

For the case of a single embedded layer of thickness .delta.t: ##EQU5##

where the time reference is the position in the trace where the amplitude is an extrema, and where ##EQU6##

There are situations where there can be distinct advantages obtained by approximating Equations 2 and 3 to give Equations 4 and 5, which take advantage of the fact that the thickness of the embedded beds is less than the gross thickness .DELTA.t. Thus, Equations 4 and 5 are used in a variety of ways as shown below to solve for the gross and net thickness of the bed. Specifically, if an estimate is made for .DELTA.t, then either .SIGMA..delta..sub.i.sup.2 is found by a linear fitting process (method 3 and 4), or it can be directly solved for .SIGMA..delta..sub.i.sup.2 and .DELTA.t as described below (methods 8 and 9).

The amplitude signature for a blocky reservoir bed with one or more smaller non-reservoir layers embedded in it is approximately: ##EQU7##

where the time reference is the position in the trace where the amplitude is an extrema, and where ##EQU8##

The amplitude signature for a blocky reservoir bed with a single non-reservoir layer embedded in it, of thickness .delta.t, is approximately: ##EQU9##

where the time reference is the position in the trace where the amplitude is an extrema, and where ##EQU10##

In the case where the accumulated thickness of the embedded layers .SIGMA..delta.t.sub.i approaches the thickness .DELTA.t, then Equation 2 becomes: ##EQU11##

where the time reference is the position in the trace where the amplitude is an extrema, and where ##EQU12##

The amplitude signature for a blocky reservoir bed with a single non-reservoir layer embedded in it, of thickness .delta.t, is approximately given by: ##EQU13##

where the time reference is the position in the trace where the amplitude is an extrema, and where ##EQU14##

FIG. 5 illustrates the accuracy of the approximations (curves 46 and 48) for the case where .DELTA.t=.02 seconds, and there is only a single embedded layer of thickness .delta.t=.005 seconds.

Referring now to FIG. 6, given two measured amplitudes and their corresponding frequencies, Ax, fx and Ah, fh, the gross and net thicknesses are calculated using the following equations: ##EQU15##

where .epsilon.=2.14*.function.x* .SIGMA..delta.t.sub.i.sup.2 for the case of more than one embedded layers or

for the case of a single embedded layer

and ##EQU16##

or

for the case of a single embedded layer ##EQU17##

where

In all of the discussion above concerning bed thickness, whether net or gross, .delta.T.sub.2WAY is the two-way travel time for the bed. These travel times are for P-P, P-S, or S-S data types. The spatial thickness .DELTA.Z of the layer is given, for each of these cases by: ##EQU18##

where:

There are a number of methods for quantitatively determining the gross and net bed thicknesses of a reservoir layer using the above equations. They include: pairs to produce optimal data consistent values for .DELTA.t, .delta.t.sub.i and .DELTA.Zp/Zp. .DELTA.t, .delta.t.sub.i and .DELTA.Zp/Zp are the data derived FDA's for this method. pairs to produce optimal data consistent values for .DELTA.t, .delta.t and .DELTA.Zp/Zp for the case where only a single embedded layer is present .DELTA.t, .delta.t and .DELTA.Zp/Zp are the data derived FDA's for this method. fact that the total thickness of the layers t.sub.i are small compared with .DELTA.. The value for .DELTA.t is initially estimated by finding the frequency for which the amplitude is at its maximum .function.x (see FIG. 6) and then substituting .DELTA.t=1(1.4*.function.x). Next, perform a linear fit, using Equation 4, to amplitude and fu.sub.i pairs to produce optimal data consistent values for (.SIGMA..delta.t.sub.i.sup.2) and .DELTA.Zp/Zp. With this initial estimate of .SIGMA..delta.t.sub.i.sup.2, Equation 8 is used to improve the initial estimate made for the gross thickness .DELTA.t. This improved value for .DELTA.t is substituted into Equation 4, and a new fit performed, resulting in an improved estimate for .SIGMA..delta.t.sub.i.sup.2. FIG. 5 illustrates the accuracy of this approach. The red curve, curve 42, represents the exact response while the approximate form, Equation 4, is the cyan curve, curve 48. .DELTA.t, .delta.t.sub.i and .DELTA.Zp/Zp are the data derived FDA's for this method. of the embedded layer .delta.t is small compared with .DELTA.t for the case where only a single embedded layer is present. This gives Equation 5. The value for .DELTA.t is initially estimated by finding the frequency for which the amplitude is at its maximum .function.x (see FIG. 6) and then substituting .DELTA.t=1/(1.4*.function.x). Then a linear fit to the data is made, using Equation 5, to amplitude and f.sub.Ui pairs to produce optimal data consistent values for (.delta.t.sup.2) and .DELTA.Zp/Zp. With this initial estimate of .delta.t.sup.2, Equation 8 is used to improve the initial estimate made for the gross thickness .DELTA.t. This improved value for .DELTA.t is substituted into Equation 5, and a new fit performed, resulting in an improved estimate for .delta.t.sup.2. .DELTA.t, .delta.t and .DELTA.Zp/Zp are the data derived FDA's for this method. reservoir thickness, then an improved approximation to Equations 4 and 5 are 6 and 7 respectively. These equations result from simplifying Equation 2 by taking advantage of the fact that the total thickness of the layers .delta.t.sub.i are small compared with .DELTA.t. This gives Equation 6. The value for .DELTA.t is initially estimated by finding the frequency for which the amplitude is at a maximum .function.x (see FIG. 6) and then substituting .DELTA.t=1(1.4*.function.x). Perform a non-linear fit, using Equation 6, to amplitude and f.sub.Ui pairs to produce optimal data consistent values for (.SIGMA..delta.t.sub.i.sup.2) and .DELTA.Zp/Zp. With this initial estimate of .SIGMA..delta.t.sub.i.sup.2, Equation 8 is used to improve the initial estimate made for the gross thickness .DELTA.t. This improved value for .DELTA.t is substituted into Equation 4, and a new fit is performed, resulting in an improved estimate for .SIGMA..delta.t.sub.i.sup.2. FIG. 5 illustrates the accuracy of this approach. The red curve (curve 42) represents the exact response, while the approximate form, indicated in Equation 6, is the dark blue curve, curve 46. .DELTA.t, .delta.t.sub.i and .DELTA.Zp/Zp are the data derived FDA's for this method. possible to simplify Equation 6 by taking advantage of the fact that the thickness of the embedded layer .delta.t is somewhat small compared with .DELTA.t. This gives Equation 7. The value for .DELTA.t is initially estimated by finding the frequency for which the amplitude is at a maximum .function.x (see FIG. 6), and then substituting .DELTA.t=1/(1.4*.function.x). Then a non-linear fit to the data is made, using Equation 7, to amplitude and fu pairs to produce optimal data consistent values for (.delta.t.sup.2) and .DELTA.Zp/Zp. With this initial estimate of .delta.t.sup.2, Equation 8 is used to improve the initial estimate made for the gross thickness .DELTA.t. This improved value for .DELTA.t is substituted into Equation 7, and a new fit is performed, resulting in an improved estimate for .delta.t.sup.2. .DELTA.t, .delta.t and .DELTA.Zp/Zp are the data derived FDA's for this method.

The final 2 methods do not require any type of linear or nonlinear curve fitting. than the gross bed thickness. In this case the gross and embedded bed thicknesses are solved for by using Equation 4. The result is Equations 8 and 9. All that is required are two amplitude measurements, Ax and Ah, and their corresponding frequencies, fx and fh, where the first measurement is made where the amplitude is at its maximum (Ax,fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum. These are Ah and fh. This arrangement is shown in FIG. 6. The value for .SIGMA..delta.t.sub.i is given by Equation 9, while the value for the gross thickness is given by Equation 8. .DELTA.t, and .SIGMA..delta.t.sub.i are the data derived FDA's for this method. than the gross bed thickness, and that there is only a single embedded layer present. In this case the gross and embedded bed thicknesses are solved for by using Equation 5. The result is Equations 8 and 9. All that is required are two amplitude measurements, Ax and Ah, and their corresponding frequencies, fx and fh, where the first measurement is made where the amplitude is at its maximum (Ax, fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum. These are Ah and fh. This arrangement is shown in FIG. 6. The value for .delta.t is given by Equation 9, while the value for the gross thickness is given by Equation 8. .DELTA.t, and .delta.t.sub.i are the data derived FDA's for this method.

In summary, the following methods of exploration and evaluation have been shown: the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; the non-reservoir material .SIGMA..delta..sub.1, using the extracted amplitude frequency pairs A.sub.i and the f.sub.Ui,; and ##EQU19## the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; following equation, using nonlinear fitting methods, ##EQU20##

to generate fit parameters .DELTA.t, .EPSILON..delta.t.sub.i, and ##EQU21## the net thickness of the reservoir by using ##EQU22##

and reservoir ##EQU23##

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU24##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, using nonlinear fitting methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU25##

to generate fit parameters .DELTA.t, .delta.t, and ##EQU26## thickness of the reservoir by using .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU27##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.I ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU28##

to generate fit parameters .DELTA.t, .SIGMA..delta..sub.i, and ##EQU29## ##EQU30##

to produce an improved estimate of .DELTA.t; the following equation, using linear fitting methods, and using the improved estimate of .DELTA.t, ##EQU31##

to generate new fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU32## determining the net thickness of the reservoir by ##EQU33##

and reservoir ##EQU34##

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU35##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, determining the frequency fx at which the amplitudes are at their maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU36##

to generate fit parameters .DELTA.t, .delta., and ##EQU37## ##EQU38##

to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs .DELTA..sub.i and f.sub.Ui to the following equation, ##EQU39##

to generate new fit parameters .DELTA.t, .delta.t, and ##EQU40## thickness of the reservoir by .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU41##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU42##

to generate fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU43## ##EQU44##

where .epsilon.=2.14*.function.x*.SIGMA..delta.t.sub.i.sup.2, to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU45##

to generate new fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU46## determining the net thickness of the reservoir by ##EQU47## reservoir ##EQU48##

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU49##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, determining the frequency fx at which the amplitudes are at their maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU50##

to generate fit parameters .DELTA.t, .delta.t, and ##EQU51## ##EQU52##

where

to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU53##

to generate new fit parameters .DELTA.t, .delta.t, and ##EQU54## thickness of the reservoir by .DELTA..sub.tNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.tNET =.DELTA.t-.delta.t,

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU55##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; frequencies fx and fh from the amplitude frequency data where the first measurement is made where the amplitude is at its maximum (Ax, fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum; ##EQU56## ##EQU57##

where the reservoir by using ##EQU58##

and; reservoir ##EQU59##

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU60##

depending on whether the data type is P-P, S-S or P-S respectively. the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, extracting two amplitude measurements fx and fh and their corresponding frequencies fx and fh from the amplitude frequency data where the first measurement is made where the amplitude is at its maximum (Ax, fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum; ##EQU61##

d) determining .DELTA.t, using ##EQU62##

where reservoir by using .DELTA..sub.iNet =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t,

determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU63##

depending on whether the data type is P-P, S-S or P-S respectively.

Although this detailed description has shown and described illustrative embodiments of the invention, this description contemplates a wide range of modifications, changes, and substitutions. In some instances, one may employ some features of the present invention without a corresponding use of the other features. Accordingly, it is appropriate that readers should construe the appended claims broadly, and in a manner consistent with the scope of the invention.

## Claims

1. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; the non-reservoir material .SIGMA..delta..sub.1, using the extracted amplitude frequency pairs A.sub.i and the f.sub.Ui ; and ##EQU64##

2. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; following equation, using nonlinear fitting methods, ##EQU65## to generate fit parameters .DELTA.t, .SIGMA..delta.t.sub.1, and ##EQU66## the net thickness of the reservoir by using ##EQU67## and reservoir ##EQU68## determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU69##

3. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, using nonlinear fitting methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU70## to generate fit parameters .DELTA.t, .delta.t, and ##EQU71## thickness of the reservoir by using .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU72##

4. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.I ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU73## to generate fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU74## ##EQU75## to produce an improved estimate of .DELTA.t; following equation, using linear fitting methods, and using the improved estimate of .DELTA.t, ##EQU76## to generate new fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU77## determining the net thickness of the reservoir by ##EQU78## and reservoir ##EQU79## determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU80##

5. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, determining the frequency fx at which the amplitudes are at their maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU81## to generate fit parameters .DELTA.t, .delta.t, and ##EQU82## ##EQU83## where to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui, to the following equation, ##EQU84## to generate new fit parameters .DELTA.t, .delta.t, ##EQU85## thickness of the reservoir by .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU86##

6. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU87## to generate fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU88## ##EQU89## where .epsilon.=2.14*.function.x*.SIGMA..delta.t.sub.i.sup.2, to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU90## to generate new fit parameters .DELTA.t, .SIGMA..delta.t.sub.i, and ##EQU91## determining the net thickness of the reservoir by ##EQU92## and reservoir ##EQU93## determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU94##

7. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, determining the frequency fx at which the amplitudes are at their maximum value by analyzing the amplitude frequency pairs A.sub.i and f.sub.Ui ; amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU95## to generate fit parameters .DELTA.t, .delta.t, and ##EQU96## ##EQU97## where .epsilon.=2.14*.function.x*.delta.t.sup.2 to produce an improved estimate of .DELTA.t; methods, fitting the amplitude and frequency pairs A.sub.i and f.sub.Ui to the following equation, ##EQU98## to generate new fit parameters .DELTA.t, .delta.t, and ##EQU99## thickness of the reservoir by .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU100##

8. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui, to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; frequencies fx and fh from the amplitude frequency data where the first measurement is made where the amplitude is at its maximum (Ax, fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum; ##EQU101## ##EQU102## where the reservoir by using ##EQU103## and reservoir ##EQU104## determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU105##

9. A method of determining the net thickness of a reservoir bed, comprising the following steps: wherein the set is selected from the group consisting of normal moveout corrected and offset stacked seismic traces, or angle stacked seismic traces, with each filter designed to have a common lower frequency f.sub.L, and progressively increasing upper frequency f.sub.Ui to generate filtered seismic traces; traces or the energy envelope of the filtered seismic traces, using a method selected from the group consisting of either a sample-by-sample method or a lobe method, wherein the extracted amplitudes and their corresponding frequencies are A.sub.i and the f.sub.Ui ; present, extracting two amplitude measurements fx and fh and their corresponding frequencies fx and fh from the amplitude frequency data where the first measurement is made where the amplitude is at its maximum (Ax, fx) and the second is for a frequency at least 10% higher than the frequency where the amplitude is at its maximum; ##EQU106## ##EQU107## where .epsilon.=2.14*.function.x*.delta.t.sup.2 reservoir by using .DELTA..sub.iNET =.DELTA.t-.delta.t; and reservoir .DELTA..sub.iNET =.DELTA.t-.delta.t, determining the spatial thickness .DELTA.Z and .DELTA.Z.sub.NET using an equation from the group consisting of the following three equations: ##EQU108##