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Methods of electromagnetic migration imaging of geologic formation

  • US 8,624,969 B2
  • Filed: 07/15/2011
  • Issued: 01/07/2014
  • Est. Priority Date: 08/02/2010
  • Status: Active Grant
First Claim
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1. A method of imaging-while-drilling and look-ahead imaging of a geological formation using borehole devices measuring multi-component vector and/or tensor induction logging data, said method comprising the steps of:

  • a. operating one or more transmitters of a device representing an electromagnetic logging instrument formed by one or more induction and/or galvanic transmitters and one or more electric and/or magnetic field receivers to generate an electromagnetic field comprising a harmonic (frequency domain) and/or pulse (time domain) field, whereby said generated electromagnetic field propagates through geological formations penetrated by the borehole and ahead of the device in a wellbore;

    b. measuring at least one component of electric and/or magnetic field data with said one or more receivers;

    c. conceptually replacing the one or more receivers with an array of electric and/or magnetic dipole transmitters respectively, the electric and/or magnetic moment of each conceptual dipole transmitter replicating the actually measured electric and/or magnetic field in the corresponding one or more receivers;

    d. obtaining a migration electromagnetic field {Em, Hm} equivalent to that produced by the conceptual transmitters replacing the actual receivers and obtaining a reference field {Er, Hr} representative of a background medium consisting of said examined geological formation without the presence of an anomalous target;

    e. obtaining an integrated sensitivity of the electromagnetic logging device by estimating a least square norm of the values of perturbation of at least one component of measured electromagnetic electromagnetic logging instrument tensor data at said plurality of locations due to conductivity perturbation at a specific local area of the examined geologic formation;

    f. producing a migration image of said anomalous target by calculating a cross power spectra of said reference and said migration fields or cross correlation functions between said reference and said migration fields in the area around the borehole and/or ahead of the device and spatially weighting said cross power spectra or cross correlation functions with said integrated sensitivity;

    g. determining the location, shape and electrical conductivity and/or resistivity of said anomalous target within the geologic formation around a borehole and/or ahead of the device in a wellbore from the said migration image.

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