Hybrid image of earth formation based on transient electromagnetc measurements

Patent metadata

Field	Value
Publication number	US-2016178787-A1
Application number	US-201414577663-A
Country	US
Kind code	A1
Filing date	Dec 19, 2014
Priority date	Dec 19, 2014
Publication date	Jun 23, 2016
Grant date	—

Abstract

A method for imaging an earth formation includes estimating an apparent resistivity (AR) value and an apparent distance to a bedding plane (AD2B) value for each of a plurality of samples derived from measurements of a time-dependent transient electromagnetic signal, estimating an inversion-based resistivity value (IB-R) and an inversion-based distance to a bedding plane (IB-D2B) value at a first sample of each consecutive depth interval, wherein each depth interval includes a plurality of consecutive samples, and determining a difference between apparent values and the corresponding inversion-based values. The method further includes generating an image of the earth formation using the AR and AD2B values for the entire interval if the difference is less than a threshold value and generating an image of the earth formation using IB-R and IB-D2B values for the entire interval if the difference is greater than the threshold value.

First claim

What is claimed is:

1 . A method for imaging an earth formation, the method comprising:
conveying a carrier through a borehole penetrating the formation; inducing time-dependent electrical currents in the formation at a plurality of depths using a downhole resistivity tool disposed at the carrier; measuring time-dependent transient electromagnetic (TEM) signals induced by the formation responsive to the electrical currents using the downhole resistivity tool; estimating an apparent resistivity (AR) value and an apparent distance to a bedding plane (AD2B) value for each of a plurality of samples derived from the TEM measurements using a processor, wherein each sample corresponds to a discrete time window of the TEM measurements; estimating an inversion-based resistivity (IB-R) value and an inversion-based distance to a bedding plane (IB-D2B) value at a first sample of each consecutive depth interval using the processor, wherein each depth interval comprises a plurality of consecutive samples; determining a difference between the AR and AD2B values and the corresponding IB-R and IB-D2B values using the processor; generating an image of the earth formation using the AR and AD2B values for the entire interval comprising the first sample using the processor if the difference is less than a threshold value at the first sample; and estimating an IB-R value and an IB-D2B value for each of the samples in the entire interval and generating an image of the earth formation using the IB-R and IB-D2B values for the entire interval comprising the first sample if the difference is greater than the threshold value using the processor.

2 . The method according to claim 1 , wherein the threshold value is between 10% and 50% of corresponding AR and AD2B values.

3 . The method according to claim 1 , further comprising transmitting an output signal via an output interface to a signal receiving device configured to display the image to a user.

4 . The method according to claim 3 , wherein the signal receiving device is a display monitor or a printer.

5 . The method according to claim 1 , further comprising storing digital values representing the generated image in memory or a storage medium thereby transforming the memory or storage medium from a prior state not containing image to a new state containing the image.

6 . The method according to claim 1 , further comprising looking up the IB resistivity value in a look-up table.

7 . The method according to claim 6 , wherein the look-up table comprises (a) a first set of tables based on two-layered formation models where model parameters include the resistivity values of the two layers, a distance to a bedding plane, and a relative dip, (b) a second set of tables based on three-layered formation models, where the tool stays horizontal and is in either the upper or bottom layer, and model parameters include the resistivity values of the three layers, and two distances to two bedding planes, or (c) a third set of tables based on three-layered formation models, where the tool stays horizontal and is in the middle layer, and model parameters include the resistivity values of the three layers, and two distances to two bedding planes.

8 . The method according to claim 6 , further comprising generating a first lookup table based on a step-function excitation current pulse shape.

9 . The method according to claim 8 , further comprising generating a second lookup table as a time-shifted version of the first lookup table for a linear excitation current pulse shape.

10 . The method according to claim 8 , further comprising generating a third lookup table by recalculating the first lookup table using a convolution integral for an excitation current pulse shape other than the step-function excitation current pulse shape and a linear excitation current pulse shape.

11 . The method according to claim 1 , wherein estimating the apparent resistivity value for each of the plurality of samples comprises determining for each sample a simulated homogeneous formation that provides a best fit of resistivity for the sample.

12 . The method according to claim 11 , wherein determining for each sample comprises identifying, from a plurality of simulated homogeneous formations, the simulated homogeneous formation having synthetic responses that provide the best fit for the sample, wherein the synthetic responses are determined using the respective simulated homogeneous formation and know parameters of the downhole resistivity tool.

13 . The method according to claim 11 , further comprising using a least squares minimization technique to provide the best fit.

14 . The method according to claim 1 , wherein inducing time-dependent electrical currents comprises changing a magnetic of a transmitter in the downhole resistivity tool.

15 . The method according to claim 1 , further comprising estimating the apparent resistivity value for each of the plurality of samples derived from the TEM measurement while conducting drilling operations in the borehole.

16 . An apparatus for imaging an earth formation, the apparatus comprising:
a carrier configured to be conveyed through a borehole penetrating the formation; a transmitter disposed on the carrier and configured to induce time-dependent electrical currents in the formation; a receiver disposed on the carrier and configured to provide a time-dependent transient electromagnetic (TEM) signal induced the formation responsive to the electrical currents; a processor and a non-transitory computer-readable medium accessible to the processor with instructions thereon that when executed by the processor cause the processor to: measure time-dependent transient electromagnetic (TEM) signals induced by the formation responsive to the electrical current using the downhole resistivity tool; estimate an apparent resistivity (AR) value and an apparent distance to a bedding plane (AD2B) value for each of a plurality of samples derived from the TEM measurements using a processor, wherein each sample corresponds to a discrete time window of the TEM measurements; estimate an inversion-based resistivity (IB-R) value and an inversion-based distance to a bedding plane (IB-D2B) value at a first sample of each consecutive depth interval, wherein each depth interval comprises a plurality of consecutive samples; determine a difference between the AR and AD2B values and the corresponding IB-R and IB-D2B values using the processor; generate an image of the earth formation using the AR and AD2B values for the entire interval comprising the first sample using the processor if the difference is less than a threshold value at the first sample; and estimate an IB-R value and an IB-D2B value for each of the samples in the entire interval and generate an image of the earth formation using the IB-R and IB-D2B values for the entire interval comprising the first sample if the difference is greater than the threshold value.

17 . A non-transitory computer readable medium comprising computer executable instructions for imaging an earth formation that when executed by a computer implements a method comprising:
estimating an apparent resistivity (AR) value and an apparent distance to a bedding plane (AD2B) value for each of a plurality of samples derived from measurements of time-dependent transient electromagnetic (TEM) signals in a borehole penetrating the formation responsive to a TEM current in the formation, wherein each sample corresponds to a discrete time window of the TEM measurements; estimating an inversion-based resistivity (IB-

Assignees

• Le Fei
• Itskovich Gregory B
• Nikitenko Marina N
• Baker Hughes Inc

Inventors

• Le Fei
• Itskovich Gregory B
• Nikitenko Marina N

Classifications

• G01V3/24

  using AC · CPC title

• G01V3/38 Primary

  Processing data, e.g. for analysis, for interpretation, for correction · CPC title

• G01V3/28

  using induction coils · CPC title