Granted Patent B2

US 12,560,740 · App. 17/610,074 · Granted Feb 24, 2026

Inventors: Gérard Massonnat (Pau, FR); Fanny Bastide (Pau, FR)

Assignee: TotalEnergies One Tech

G01V20/00G01V2210/661

Abstract

Claims (61)

1 . A computer-implemented method for modelling the formation of a sedimentary basin using a stratigraphic forward modelling program, wherein the stratigraphic forward modelling program simulates the superposition of successive layers of sediments, each layer of sediments corresponding to a determined period of time, the method comprising:

receiving a facies log corresponding to an initial state of at least one well belonging to the sedimentary basin to be modelled, wherein the facies log comprises a succession of layers of different facies wherein each layer extends from a respective depth with a respective thickness,

determining environmental conditions associated to at least some of the facies of the facies log to infer, for at least one environmental factor, an environmental factor log associated to the facies log,

determining, from the facies log, a number of layers of sediments and a thickness of each layer of sediments to be simulated by the stratigraphic forward modelling program for modelling the facies log, and

determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program such that the superposition of the simulated layers of sediments corresponds to the facies logs,

wherein determining, from the facies log, the number of layers of sediments and the thickness of each layer of sediments to be simulated by the stratigraphic forward modelling program comprises:

determining an average deposition rate of the facies over each facies log, expressed as an average thickness of deposited sedimentary elements during the period of time corresponding to each layer of sedimentary elements,

determining the number of layers of sediments to be simulated in order to model each facies log, from the average deposition rate of the facies, a number of different facies within the facies log, and a thickness of each facies layer,

computing an average thickness of the layers of sediments as the overall thickness of the facies log divided by the number of layers of sedimentary elements to be simulated in order to model the facies log, and

adjusting the thickness of each layer such that a change between two successive facies in the facies log corresponds to an interface between two successive layers of sediments.

2 . The computer-implemented method according to claim 1 , wherein receiving a facies log corresponding to an initial state of at least one well belonging to the sedimentary basin to be modelled comprises receiving a current facies log corresponding to a current state of the at least one well, and processing the current facies log to form the facies log corresponding to the initial state of the at least one well.

3 . The computer-implemented method according to claim 1 , wherein determining environmental conditions associated to at least some of the facies of the facies log to infer, for at least one environmental factor, an environmental factor log associated to the facies log comprises loading a library assigning to each of a plurality of facies an associated production model comprising at least one type of element and at least one environmental factor, and inferring from the library at least one environmental factor value and/or at least one element corresponding to each facies layer of the facies log.

4 . The computer-implemented method according to claim 1 , the at least one environmental factor includes at least one of:

water depth,

salinity,

temperature,

pH level,

slope of a sedimentary surface on which sediments are deposited,

water current velocity,

volcano activity,

spring activity,

river activity, or

variation of water depth between the periods of time corresponding to the deposition of two successive layers of sediments.

5 . The computer-implemented method according to claim 1 , wherein environmental conditions associated to one facies comprise minimum and maximum values of an environmental factor, and the determination of an environmental factor log comprises:

computing an average value of the environmental factor for each facies of the facies log from the respective minimum and maximum values associated to each facies, the succession of average values corresponding to each facies of the log forming an environment factor log, and

smoothing the environment factor log.

6 . The computer-implemented method according to claim 1 , wherein receiving a facies log corresponding to an initial state of at least one well belonging to the sedimentary basin to be modelled comprises the reception of at least two facies logs corresponding to the initial states of two respective wells belonging to the sedimentary basin to be modelled, and

determining environmental conditions associated to at least some of the facies of the facies log further comprises establishing correlations between the facies logs from the environmental factor logs established for each facies log and identifying, from the established correlations, parts of each facies log corresponding to a same time interval.

7 . The computer implemented method according to claim 6 , wherein said determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program comprises inferring, from each facies log, a maximum water current velocity at water bottom associated to each transported facies layer,

the method further comprising running the stratigraphic forward simulation model to model the formation of the sedimentary basin, thereby obtaining a simulated water current velocity at a time and location corresponding to the formation of the transported facies layer of the facies log for which the maximum water current velocity has been inferred, and

said determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program further comprises:

computing an error between the maximum water current velocity and the simulated water current velocity,

extrapolating the computed error over the sedimentary basin, and

computing corrected simulation values of water current velocity from values simulated by the program and the error computed over the sedimentary basin.

8 . The computer-implemented method according to claim 6 , wherein the environmental factor logs comprise, for each facies log, at least an environment factor log corresponding to an environment factor which is, at a given time, homogeneous over the sedimentapry basin, and comprises, for each part of the facies log corresponding to a time interval, a range of values of said homogeneous environmental factor, and

determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program comprises assigning a value of the environmental factor to at least one layer of sediments to be modelled in order to represent facies layers of the part of the facies logs corresponding to the same time interval, said value being comprised in the intersection of the ranges of values of the environmental factor associated to the part of each facies log corresponding to said time interval.

9 . The computer-implemented method according to claim 8 , wherein if there is no intersection of the ranges of values of the environmental factor associated to the facies layer of each facies log corresponding to said time interval, the method comprises defining a reference facies log, and the value assigned to the layer of sediments to be modelled is chosen among the range of values of the environmental factor associated to the facies layer of the reference facies log corresponding to said time interval.

10 . A non-transitory computer readable storage medium, having stored thereon a computer program comprising program instructions, the computer program being loadable into a processor and adapted to cause the processor to carry out, when the computer program is run by the processor, the method according to claim 1 .

11 . A device for modelling the formation of a sedimentary basin, the device comprising a processor configured to implement the method according to claim 1 .

12 . A computer-implemented method for modelling the formation of a sedimentary basin using a stratigraphic forward modelling program, wherein the stratigraphic forward modelling program simulates the superposition of successive layers of sediments, each layer of sediments corresponding to a determined period of time, the method comprising:

receiving a facies log corresponding to an initial state of at least one well belonging to the sedimentary basin to be modelled, wherein the facies log comprises a succession of layers of different facies wherein each layer extends from a respective depth with a respective thickness,

determining environmental conditions associated to at least some of the facies of the facies log to infer, for at least one environmental factor, an environmental factor log associated to the facies log,

determining, from the facies log, a number of layers of sediments and a thickness of each layer of sediments to be simulated by the stratigraphic forward modelling program for modelling the facies log,

determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program such that the superposition of the simulated layers of sediments corresponds to the facies logs,

wherein the environmental factor logs comprise, for each facies log, at least an environment factor log corresponding to an environment factor which is, at a given time, homogeneous over the sedimentary basin, and comprises, for each part of the facies log corresponding to a time interval, a range of values of said homogeneous environmental factor, and

determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program comprises assigning a value of the environmental factor to at least one layer of sediments to be modelled in order to represent facies layers of the part of the facies logs corresponding to the same time interval, said value being comprised in the intersection of the ranges of values of the environmental factor associated to the part of each facies log corresponding to said time interval, and

if there is no intersection of the ranges of values of the environmental factor associated to the facies layer of each facies log corresponding to said time interval, the method comprises defining a reference facies log, and the value assigned to the layer of sediments to be modelled is chosen among the range of values of the environmental factor associated to the facies layer of the reference facies log corresponding to said time interval.

13 . A computer-implemented method for modelling the formation of a sedimentary basin using a stratigraphic forward modelling program, wherein the stratigraphic forward modelling program simulates the superposition of successive layers of sediments, each layer of sediments corresponding to a determined period of time, the method comprising:

receiving a facies log corresponding to an initial state of at least one well belonging to the sedimentary basin to be modelled, wherein the facies log comprises a succession of layers of different facies wherein each layer extends from a respective depth with a respective thickness,

determining environmental conditions associated to at least some of the facies of the facies log to infer, for at least one environmental factor, an environmental factor log associated to the facies log,

determining, from the facies log, a number of layers of sediments and a thickness of each layer of sediments to be simulated by the stratigraphic forward modelling program for modelling the facies log, and

determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program such that the superposition of the simulated layers of sediments corresponds to the facies logs,

wherein receiving the facies log corresponding to the initial state of at least one well belonging to the sedimentary basin to be modelled comprises:

receiving at least two facies logs corresponding to the initial states of two respective wells belonging to the sedimentary basin to be modelled, and

determining environmental conditions associated to at least some of the facies of the facies log further comprises establishing correlations between the facies logs from the environmental factor logs established for each facies log and identifying, from the established correlations, parts of each facies log corresponding to a same time interval, and

wherein said determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program comprises inferring, from each facies log, a maximum water current velocity at water bottom associated to each transported facies layer,

the method further comprising running the stratigraphic forward simulation model to model the formation of the sedimentary basin, thereby obtaining a simulated water current velocity at a time and location corresponding to the formation of the transported facies layer of the facies log for which the maximum water current velocity has been inferred, and

wherein said determining, from the environmental factor log associated to the facies log, environmental parameters associated to the layers of sediments to be simulated by the stratigraphic forward modeling program further comprises:

computing an error between the maximum water current velocity and the simulated water current velocity,

extrapolating the computed error over the sedimentary basin, and

computing corrected simulation values of water current velocity from values simulated by the program and the error computed over the sedimentary basin.

Assignments (7)

Continuity (1)

References Cited (16)