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CN112799147B - A method for evaluating lateral sealing of shallow faults - Google Patents

A method for evaluating lateral sealing of shallow faults Download PDF

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CN112799147B
CN112799147B CN202110297426.8A CN202110297426A CN112799147B CN 112799147 B CN112799147 B CN 112799147B CN 202110297426 A CN202110297426 A CN 202110297426A CN 112799147 B CN112799147 B CN 112799147B
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王宇
蒋有录
赵凯
苏圣民
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China University of Petroleum East China
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Abstract

本发明提出一种浅层断层侧向封闭性评价方法，属于油气勘探技术领域，能充分考虑断层上盘、下盘中各泥岩对研究点的泥岩涂抹，以及各泥岩内不同深度的点对研究点涂抹的差异性，提出高等断层泥比率(ASGR)方法表征断层侧向封闭性。该评价方法包括如下步骤：收集断层上盘、下盘岩性数据、油气层深度数据D和断距数据T。以断层中深度D的点为研究点，计算深度段[D,D+T]内断层上盘泥岩对研究点涂抹效果ASGRh。计算深度段[D‑T,D]内断层下盘泥岩对研究点涂抹效果ASGRf。将ASGRh与ASGRf相加得研究点ASGR值。以断层中深度D研究点ASGR最小值为阈值Q。如果非深度D研究点ASGR值大于等于阈值Q，该研究点具有断层侧向封闭性；反之,该研究点不具有断层侧向封闭性。

Figure 202110297426

The invention provides a method for evaluating the lateral sealing property of a shallow fault, which belongs to the technical field of oil and gas exploration, and can fully consider the mudstone smear of each mudstone on the research point in the upper wall and the footwall of the fault, as well as the research on the points at different depths in each mudstone. Based on the difference of point smearing, the advanced fault gouge ratio (ASGR) method is proposed to characterize the lateral sealing of faults. The evaluation method includes the following steps: collecting the lithology data of the hanging wall and the foot wall of the fault, the depth data D of the oil and gas layers and the fault distance data T. Taking the point at the depth D in the fault as the research point, the smearing effect ASGR h of the mudstone on the upper wall of the fault in the depth section [D, D+T] is calculated. Calculate the ASGR f of the smearing effect of mudstone in the footwall of the fault on the study point in the depth section [D‑T,D]. Add ASGR h and ASGR f to obtain the study point ASGR value. The minimum value of ASGR at the depth D research point in the fault is taken as the threshold Q. If the ASGR value of the non-depth D research point is greater than or equal to the threshold Q, the research point has the fault lateral sealing; otherwise, the research point does not have the fault lateral sealing.

Figure 202110297426

Description

Shallow fault lateral sealing evaluation method
Technical Field
The invention belongs to the technical field of oil-gas exploration, and particularly relates to a shallow fault lateral sealing evaluation method.
Background
For a shallow layer (generally more than 1600 m), as most of mudstone is plastic, mudstone smearing has an obvious control effect on the lateral sealing performance of a fault, and therefore, the evaluation of the lateral sealing performance of the shallow layer fault is of great significance. Mudstone smearing is an important mechanism for lateral sealing formation of a fault, and refers to smearing effect of the mudstone on the fault in the fault breaking process of a stratum. For a particular research point, the mudstone smearing effect depends on the sum of the smearing effects of one or more mudstones on the research point within a particular depth range.
Regarding the evaluation of mudstone smearing effect, the prior people usually adopt a fault mud Ratio (SGR) method to calculate, and as the most relevant prior art in the present application, the calculation formula is:
Figure GDA0003466542990000011
wherein T is fault distance, H is the sum of all mudstone thicknesses in the upper disc of the fault layer in the length of the downward fault distance T (i.e. the direction towards the deep part) by taking the research point as a starting point.
However, the inventors have found that the prior art SGR method does not take into account mudstone smearing of research points by mudstones in the fault footwall, and does not take into account differences in the smearing effect of points at different depths within each mudstone. In fact, the fault footwall has mudstone smearing on the research points, and smearing effects of all points in the mudstone on the research points are different. Therefore, it is necessary to take the difference between smearing of mudstone on the study point by each mudstone on the upper fault wall and the lower fault wall and smearing of points at different depths in each mudstone to the study point into consideration as a key parameter for evaluating the lateral sealing performance of the fault.
Disclosure of Invention
Aiming at the defects or shortcomings of the existing fault lateral sealing method, the invention provides a shallow fault lateral sealing evaluation method, which can comprehensively consider the smearing of mudstones to research points in an upper fault tray and a lower fault tray, simultaneously consider the difference of smearing of points at different depths in the mudstones to the research points, and quantitatively characterize the fault lateral sealing.
In order to achieve the purpose, the invention adopts the technical scheme that:
a lateral sealing evaluation method for a shallow fault comprises the following steps:
firstly, collecting lithology data, oil-gas reservoir depth data D and fault distance data T of an upper wall and a lower wall of a fault in a research area;
taking a point with the depth of D in the fault as a research point, taking a depth section [ D, D + T ] as a research range, counting the total number n of mudstones in the disc on the fault, recording the ith mudstone as Hih, wherein i belongs to [1, n ], and counting the thickness delta Hih of each mudstone;
taking points with different depths in the mudstone Hih as independent calculation points, each calculation point has a different distance r from the research point; recording the distance from the research point to the top of the mudstone Hih as rih, and then the value range of r is [ rih, rih + delta Hih ];
ASGR is smeared to the mudstone of the research point by using all the calculation points of single mudstone Hih in the upper disc of the computed tomography of formula (1)HihThe expression of formula (1) is:
Figure GDA0003466542990000021
the depth segment [ D, D + T ] is divided by the formula (2)]All mudstones on the upper disc of the fault are overlaid on mudstone smearing of the research point, so that smearing ASGR of the mudstone on the upper disc of the fault on the research point can be obtainedh：
Figure GDA0003466542990000022
Thirdly, taking a point with the depth of D in the fault as a research point, taking a depth section [ D-T, D ] as a research range, counting the total number m of mudstones in the lower wall of the fault, recording the jth mudstone as Hjf, wherein j belongs to [1, m ], and counting the thickness delta Hjf of each mudstone;
taking points of different depths in the mudstone Hjf as independent calculation points, each calculation point has a different distance z from the study point; recording the distance from the research point to the bottom of the mudstone Hjf as rjf, wherein the value range of z is [ rjf, rjf + delta Hjf ];
ASGR is smeared to the mudstone of the research point by using all the calculation points of the single mudstone Hjf in the lower wall of the computed tomography of the formula (3)HjfThe expression of formula (3) is:
Figure GDA0003466542990000023
the depth segment [ D-T, D ] is divided by the formula (4)]All mudstones in the fault footwall are overlaid on mudstone smearing of the research point, and smearing ASGR of the mudstone of the fault footwall on the research point can be obtainedf：
Figure GDA0003466542990000031
And (IV) obtaining a fault lateral sealing evaluation result ASGR of the research point by using a formula (5), wherein the expression of the formula (5) is as follows:
Figure GDA0003466542990000032
fifthly, recording the minimum value of the ASGR result corresponding to the depth D in the fault as a threshold Q; calculating the corresponding ASGR value by taking other points in the fault, which are not the depth D, as research points; the fault lateral sealing performance of the non-depth D research point can be evaluated according to the relation between the Q value and the ASGR value of the non-depth D research point: if the ASGR value of the non-depth D research point is larger than or equal to Q, the research point has fault lateral sealing performance; otherwise, the study point is considered to have no fault lateral seal.
Preferably, in the step (one), the lithological data of the upper wall and the lower wall of the fault is obtained from rock core and rock debris data. All reservoir depth data D are the peak depths of each reservoir.
Preferably, in the calculation processes of the steps (three) to (five), if a single mudstone is away from the research point by the distance z being 0, the mudstone is considered to have the function of laterally sealing oil and gas, and the ASGR value of the research point does not participate in the formulation of the Q value.
Compared with the prior art, the invention has the advantages and positive effects that:
according to the shallow fault lateral sealing evaluation method provided by the invention, the smearing of each mudstone on the research points by each mudstone in the upper fault wall and the lower fault wall can be fully considered, and the smearing difference of points at different depths in each mudstone on the research points is considered, so that the fault lateral sealing can be comprehensively evaluated.
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FIG. 1 is a flow chart of a fault lateral seal evaluation method provided by an embodiment of the invention;
FIG. 2 is a schematic diagram of smearing of mudstone on a fault upper wall and mudstone on a fault lower wall on the fault mudstone in an embodiment of the invention;
fig. 3 is a schematic diagram of a calculation process of smearing mudstone at a research point D by each mudstone on a fault upper wall and a fault lower wall according to an embodiment of the present invention;
FIG. 4 is a schematic diagram of the relative positions of the Zondon X1 well, the Zondon X2 well and the fault F5 provided in example 1 of the present invention;
fig. 5 is a diagram of a process of calculating mudstone smearing on a hydrocarbon reservoir depth D of 1231m research site in a fault F5 by using mudstones in each of a reclaimed east X1 well and a reclaimed east X2 well within the calculation range provided in example 1 of the present invention;
FIG. 6 is a diagram of the calculation process of smearing of non-hydrocarbon layer depth 1306.5m research site mudstone in fault F5 by each mudstone in the reclaimed east X1 well and the reclaimed east X2 well within the calculation range provided by example 1 of the present invention.
Detailed Description
The technical solutions in the embodiments of the present invention will be clearly and completely described below, and it is obvious that the described embodiments are only a part of the embodiments of the present invention, and not all embodiments. All other embodiments, which can be derived by a person skilled in the art from the embodiments given herein without making any creative effort, shall fall within the protection scope of the present invention.
As shown in fig. 1, an embodiment of the present invention provides a shallow fault lateral seal evaluation method, including the following steps:
firstly, collecting lithology data, oil-gas reservoir depth data D and fault distance data T of an upper wall and a lower wall of a fault in a research area;
taking a point with the depth of D in the fault as a research point, taking a depth section [ D, D + T ] as a research range, counting the total number n of mudstones in the disc on the fault, recording the ith mudstone as Hih, wherein i belongs to [1, n ], and counting the thickness delta Hih of each mudstone;
taking points with different depths in the mudstone Hih as independent calculation points, each calculation point has a different distance r from the research point; recording the distance from the research point to the top of the mudstone Hih as rih, and then the value range of r is [ rih, rih + delta Hih ];
ASGR is smeared to the mudstone of the research point by using all the calculation points of single mudstone Hih in the upper disc of the computed tomography of formula (1)HihThe expression of formula (1) is:
Figure GDA0003466542990000041
the depth segment [ D, D + T ] is divided by the formula (2)]All mudstones on the upper disc of the fault are overlaid on mudstone smearing of the research point, so that smearing ASGR of the mudstone on the upper disc of the fault on the research point can be obtainedh：
Figure GDA0003466542990000042
Thirdly, taking a point with the depth of D in the fault as a research point, taking a depth section [ D-T, D ] as a research range, counting the total number m of mudstones in the lower wall of the fault, recording the jth mudstone as Hjf, wherein j belongs to [1, m ], and counting the thickness delta Hjf of each mudstone;
taking points of different depths in the mudstone Hjf as independent calculation points, each calculation point has a different distance z from the study point; recording the distance from the research point to the bottom of the mudstone Hjf as rjf, wherein the value range of z is [ rjf, rjf + delta Hjf ];
ASGR is smeared to the mudstone of the research point by using all the calculation points of the single mudstone Hjf in the lower wall of the computed tomography of the formula (3)HjfThe expression of formula (3) is:
Figure GDA0003466542990000053
the depth segment [ D-T, D ] is divided by the formula (4)]All mudstones in the fault footwall are overlaid on mudstone smearing of the research point, and smearing ASGR of the mudstone of the fault footwall on the research point can be obtainedf：
Figure GDA0003466542990000051
And (IV) obtaining a fault lateral sealing evaluation result ASGR of the research point by using a formula (5), wherein the expression of the formula (5) is as follows:
Figure GDA0003466542990000052
fifthly, recording the minimum value of the ASGR result corresponding to the depth D in the fault as a threshold Q; calculating the corresponding ASGR value by taking other points in the fault, which are not the depth D, as research points; the fault lateral sealing performance of the non-depth D research point can be evaluated according to the relation between the Q value and the ASGR value of the non-depth D research point: if the ASGR value of the non-depth D research point is larger than or equal to Q, the research point has fault lateral sealing performance; otherwise, the study point is considered to have no fault lateral seal.
In the method for evaluating lateral sealing performance of a shallow fault, it should be noted that, in the step (i), when the lithological data of the upper wall and the lower wall of the fault is acquired, the lithological data is preferably acquired from rock core and rock debris data. When the depth data D of all hydrocarbon reservoirs are obtained, the vertex depth of each hydrocarbon reservoir is selected as D as an optimal selection for calculation. In the calculation processes of the third step (b) and the fifth step (b), if the distance between a single mudstone and a research point is the condition that z is equal to 0, the mudstone is considered to have the function of laterally sealing oil and gas, and the ASGR value of the research point does not participate in the formulation of the Q value.
In order to describe the lateral sealing performance evaluation method of the shallow fault provided by the embodiment of the invention in more detail, the following description is given with reference to specific embodiments.
Example 1
Taking a northeast reclamation area as a research area, taking a fault F5 as a research object, and respectively locating a reclamation east X1 well and a reclamation east X2 well on an upper disc and a lower disc of a fault F5 (figure 5), wherein the reclamation east X1 well is an oil well and the reclamation east X2 well is a non-oil well; the two wells have distinct exploration results, which show that the lateral sealing of the fault is a key factor for controlling the oil and gas distribution of the region. Mudstone smearing is a key factor for forming lateral sealing of a local fault, and the mudstone smearing principle of the mudstone on the fault shows that (figure 2) the mudstone is divided into mudstone on the upper wall of the fault and mudstone on the lower wall of the fault in the fault moving process, the mudstone on the upper wall of the fault is smeared on the fault by the wedge-shaped part below a research point in the fault, the mudstone on the lower wall of the fault is smeared by the wedge-shaped part above the research point in the fault, and the smearing thickness of the mudstone far away from the mudstone is smaller.
The mudstone has a certain thickness, the distances between each point in the mudstone and a research point are different (figure 2), the minimum distance between the mudstone and the research point on the fault is rih, and the maximum distance between the mudstone and the research point is rih + delta Hih; the distance from the mudstone under the fault to the research point is rjf at minimum and rjf + delta Hjf at maximum. Since the inner points far from the research point have a lower smearing effect on mudstone at the research point than the inner points near the research point, it is necessary to evaluate the lateral fault blocking performance by using the points inside the mudstone as independent calculation points.
To clarify the smearing effect of the mudstone at the research site, the smearing process of the mudstone at the research site by a plurality of mudstones needs to be clarified. Specifically, mudstone smearing for a specific study point is the sum of the smearing effects of n mudstones on the fault and m mudstones on the fault on the study point (fig. 3).
A shallow fault lateral sealing evaluation method for a reclamation northeast region comprises the following steps:
first, collecting the core and debris data of the X1 well and the X2 well in the Tandow as the lithology data of the upper disc and the lower disc of the fault (figure 5 and figure 6), and the position relation between the two wells and the fault F5 is shown in figure 4. The collection pitch T was 20 m. Since the reclaimed X1 well is a producer (fig. 4), the depth at which the hydrocarbon top of the well is located is taken as the depth data D, which are 1171, 1231, 1261, 1333, 1355, 1462, 1466.5, 1565.5m, respectively. Because the reservoir research point already has the oil and gas reservoir, the fault has lateral sealing performance, and the method can provide basis for evaluating the lateral sealing performance of the fault of the subsequent non-reservoir depth research point.
(II) taking a point with the depth of D in the fault as a research point, taking D to D +20m as a research range, taking a hydrocarbon reservoir with the depth of 1231m as an example (figure 6), and taking a 1231-1251m research range, the upper wall of the fault is provided with two mudstones (n is 2) which are respectively named as H1H and H2H, the distances rih between the tops of the mudstones and the research point are respectively 4 and 15m, and the thicknesses delta Hih of the mudstones are both 5m, so that the range of r is [4,9 ] for the mudstone H1H](ii) a For mudstone H2H, r ranges from [15, 20%]. Calculation of ASGR using equation (1)H1hAnd ASGRH2hRespectively 0.81 and 0.29 (the calculation principle refers to figure 3, and the parameters of mudstone position, distance and the like are shown in figure 5). The break can be known by the formula (2)Layer-to-layer plate coating value ASGRhThe value was 0.81+ 0.29-1.10. Similarly, ASGR corresponding to other reservoir depths can be obtainedhValues (table 1).
Table 1 computation table for mudstone smearing of wall on fault to depth D research point
Figure GDA0003466542990000071
(III) taking a point with the depth of D in the fault as a research point, taking the depth D to D-20m as a research range, taking an oil-gas layer with the depth of 1231m as an example (figure 5), in the research range of 1211-plus 1231m, the lower part of the fault has five mudstones (m is 5) which are respectively named as H1f, H2f, H3f, H4f and H5f, the depths of the bottoms of the five mudstones are 1213, 1216.5, 1218.5, 1223.5 and 1231m, the thicknesses of the five mudstones are delta Hjf and are respectively 2, 0.5, 1.5, 1 and 1.5m, and the distances z between the five mudstones and the research point are respectively [18,20 m]、[14.5,15]、[12.5,14]、[7.5,8.5]And [0,1.5]The application values ASGR of H1f, H2f, H3f and H4f to the study point can be found by the formula (3)HjfThe values are 0.11, 0.03, 0.11 and 0.13 respectively, and the smearing effect ASGR of H1f, H2f, H3f and H4f on the research point in the fault section can be known by the formula (4)fThe value was 0.38. Wherein the distance between the mudstone H5f and the research point is [0,1.5 ]]In the case of 0, it is assumed that this layer of mudstone can necessarily seal the oil and gas in the lateral direction. Similarly, ASGR corresponding to other reservoir depth study points can be obtainedfValues (table 2).
The results of the upper plates of the faults of the reservoir research points 1420m and 1565.5m (table 1) show that the upper plates of the faults have no mudstone in the calculation range, and no mudstone is smeared on the research points, and under the condition that the lower plates of the faults have the mudstone smearing (table 2), the faults can still gather the oil gas (namely, the faults have the lateral sealing performance), so that the geological factor that the lower plates of the faults are smeared on the mudstone of the research points is necessarily introduced.
Table 2 calculation table for mudstone smearing of depth D research point by fault footwall
Figure GDA0003466542990000081
Figure GDA0003466542990000091
(IV) ASGR is expressed by the formula (5)hAnd ASGRfThe additions gave the ASGR values for mudstone smearing at the study site (table 3).
TABLE 3 mudstone smear Effect ASGR values for depth D study points
Figure GDA0003466542990000092
(v) if z is 0 in the 1231 and 1565.5m reservoirs (table 2), and if the threshold Q value is analyzed, the minimum Q value for ASGR for the 1462m reservoir is 0.72, which means that the minimum mudstone smear value for the reservoir is 0.72. Further, comparing the ASGR of the non-depth D research point in the fault with the threshold value of 0.72, the fault blocking performance of the research point can be known. The judgment standard is as follows: if the ASGR value of the non-depth D research point is greater than or equal to 0.72, the research point has fault lateral sealing; otherwise, the study point is considered to have no fault lateral seal.
Taking 1306.5m research sites as an example (fig. 6), only one mudstone on the upper wall of the fault smears the research sites (n ═ 1), and five mudstones on the lower wall of the fault smear the research sites (m ═ 5). The mudstone smearing of the research site by the upper fault wall and the lower fault wall is calculated by using the formula (1) to the formula (4), and the results are shown in the table 4.
TABLE 4 Upper fault wall, lower fault wall, mudstone smearing calculation table for depth 1306.5m research point
Figure GDA0003466542990000101
Smearing value ASGR of fault upper plate to research point by using formula (5)hAnd the smear value ASGR of the fault lower disc to the research pointfThe result of this addition is 2.59+2.77 to 5.36, which is greater than the threshold Q (0.72), and therefore this point has fault lateral seal.

Claims (3)

1.一种浅层断层侧向封闭性评价方法，其特征在于，包括如下步骤：1. a shallow fault lateral sealing evaluation method, is characterized in that, comprises the steps: (一)收集研究区断层上盘与下盘的岩性数据、油气层深度数据D以及断距数据T；(1) Collect the lithology data, oil and gas layer depth data D and fault distance data T of the fault hanging wall and foot wall in the study area; (二)将断层中深度为D的点作为研究点，以深度段[D,D+T]为研究范围，统计断层上盘中泥岩的总个数n，将第i个泥岩记为Hih，其中i∈[1，n]，统计各泥岩的厚度ΔHih；(2) Take the point of depth D in the fault as the research point, take the depth segment [D, D+T] as the research range, count the total number n of mudstones in the upper wall of the fault, and record the i-th mudstone as Hih, where i∈[1,n], the thickness ΔHih of each mudstone is counted; 将泥岩Hih内不同深度的点都当成是独立的计算点，则每个计算点与研究点具有不同的距离r；将研究点到泥岩Hih顶部的距离记为rih，则r的取值范围为[rih,rih+ΔHih]；The points at different depths in the mudstone Hih are regarded as independent calculation points, and each calculation point has a different distance r from the research point; the distance from the research point to the top of the mudstone Hih is recorded as rih, then the value range of r is [rih,rih+ΔHih]; 利用公式(1)计算断层上盘中单个泥岩Hih所有计算点对研究点的泥岩涂抹ASGRHih，公式(1)的表达式为：Using formula (1) to calculate the single mudstone Hih in the fault hanging wall, the mudstone smear ASGR Hih of all calculation points to the study point, the expression of formula (1) is:
Figure FDA0003466542980000011
Figure FDA0003466542980000011
 利用公式(2)将深度段[D,D+T]断层上盘中所有泥岩对研究点的泥岩涂抹进行叠加，可得断层上盘泥岩对研究点的涂抹ASGRh：Using formula (2) to superimpose the mudstone smearing of all mudstones in the hanging wall of the fault in the depth section [D, D+T] to the study point, the ASGR h of the mudstone smearing of the fault hanging wall to the study point can be obtained:
Figure FDA0003466542980000012
Figure FDA0003466542980000012
 (三)将断层中深度为D的点作为研究点，以深度段[D-T,D]为研究范围，统计断层下盘中泥岩的总个数m，将第j个泥岩记为Hjf，其中j∈[1,m]，统计各泥岩的厚度ΔHjf；(3) Take the point of depth D in the fault as the research point, take the depth segment [D-T, D] as the research range, count the total number m of mudstones in the footwall of the fault, and record the jth mudstone as Hjf, where j ∈[1,m], count the thickness of each mudstone ΔHjf; 将泥岩Hjf内不同深度的点都当成是独立的计算点，则每个计算点与研究点具有不同的距离z；将研究点到泥岩Hjf底部的距离记为rjf，则z的取值范围为[rjf,rjf+ΔHjf]；The points at different depths in the mudstone Hjf are regarded as independent calculation points, then each calculation point has a different distance z from the research point; the distance from the research point to the bottom of the mudstone Hjf is recorded as rjf, then the value range of z is [rjf,rjf+ΔHjf]; 利用公式(3)计算断层下盘中单个泥岩Hjf所有计算点对研究点的泥岩涂抹ASGRHjf，公式(3)的表达式为：Using formula (3) to calculate the single mudstone Hjf in the footwall of the fault, the mudstone smear ASGR Hjf of all calculation points to the study point, the expression of formula (3) is:
Figure FDA0003466542980000013
Figure FDA0003466542980000013
 利用公式(4)将深度段[D-T,D]断层下盘中所有泥岩对研究点的泥岩涂抹进行叠加，可得断层下盘泥岩对研究点的涂抹ASGRf：Using formula (4) to superimpose the mudstone smearing of all mudstones in the footwall of the fault in the depth section [DT, D] to the study point, the ASGR f of the mudstone smearing of the study point in the footwall of the fault can be obtained:
Figure FDA0003466542980000014
Figure FDA0003466542980000014
 (四)利用公式(5)得到研究点的断层侧向封闭性评价结果ASGR,公式(5)表达式为:(4) Using the formula (5) to obtain the ASGR evaluation result of the fault lateral sealing of the study point, the formula (5) is expressed as:
Figure FDA0003466542980000021
Figure FDA0003466542980000021
 (五)将断层中深度为D对应的ASGR结果最小值记为阈值Q；以断层中非深度D的其他点为研究点,计算其对应的ASGR值；根据Q值与非深度D研究点ASGR值的关系即可对非深度D研究点的断层侧向封闭性进行评价：如果非深度D研究点的ASGR值大于等于Q，则该研究点具有断层侧向封闭性；反之，则认为该研究点不具有断层侧向封闭性。(5) Record the minimum value of the ASGR result corresponding to the depth D in the fault as the threshold Q; take other points in the fault that are not at the depth D as the research points, and calculate the corresponding ASGR value; according to the Q value and the non-depth D research point ASGR If the ASGR value of the non-depth D research point is greater than or equal to Q, the research point has the fault lateral sealing; otherwise, it is considered that the study Points do not have fault lateral sealing. 2.根据权利要求1所述的断层侧向封闭性评价方法，其特征在于：步骤(一)中所述的断层上盘与下盘的岩性数据由岩心和岩屑资料获取，所有油气层深度数据D为各油气层的顶点深度。2. fault lateral sealing evaluation method according to claim 1 is characterized in that: the lithological data of the fault upper wall and foot wall described in the step (1) are obtained by core and cuttings data, all oil and gas layers The depth data D is the vertex depth of each oil and gas layer. 3.根据权利要求1所述的断层侧向封闭性评价方法，其特征在于：步骤(三)至(五)计算过程中，如果单个泥岩与研究点距离存在z＝0的情况时，则认为该泥岩必有侧向封闭油气的作用，该研究点的ASGR值也不参与Q值的制定。3. fault lateral sealing evaluation method according to claim 1, is characterized in that: in the calculation process of step (3) to (5), if there is a situation of z=0 in the distance between single mudstone and research point, it is considered that The mudstone must have the effect of laterally sealing oil and gas, and the ASGR value of this research point does not participate in the formulation of the Q value.
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Citations (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN108241181A (en) * 2018-01-30 2018-07-03 中国石油化工股份有限公司 A kind of evaluation method of fault sealing property
CN109239778A (en) * 2018-09-14 2019-01-18 中国石油大学(华东) A kind of Lateral fault sealing quantitative evaluation method

Family Cites Families (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
WO2009094064A1 (en) * 2008-01-22 2009-07-30 Exxonmobil Upstream Research Company Dynamic connectivity analysis
AU2009341850A1 (en) * 2009-03-13 2011-09-29 Exxonmobil Upstream Research Company Method for predicting fluid flow

Patent Citations (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN108241181A (en) * 2018-01-30 2018-07-03 中国石油化工股份有限公司 A kind of evaluation method of fault sealing property
CN109239778A (en) * 2018-09-14 2019-01-18 中国石油大学(华东) A kind of Lateral fault sealing quantitative evaluation method

Non-Patent Citations (2)

* Cited by examiner, † Cited by third party
Title
Three-dimensional structure of experimentally produced clay smears:Implications for fault seal analysis;N. Bozkurt Çiftçi et al.;《AAPG Bulletin》;20130531;第97卷(第5期);第733-757页 *
断层泥比率法评价ZD油田通天断层侧向封闭性;张瀛等;《录井工程》;20141231;第25卷(第4期);第76-80页 *

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