Line integral method of magneto-electric exploration

• US 3,943,436 A
• Filed: 01/21/1974
• Issued: 03/09/1976
• Est. Priority Date: 01/21/1974
• Status: Expired due to Term

• Current Assignee: Jacques E. Pirson, Sylvain J. Pirson
• Original Assignee: Jacques E. Pirson, Sylvain J. Pirson
• Inventors: Pirson, Sylvain J., Pirson, Jacques E.
• Primary Examiner(s): Strecker, Gerard R.
• Application Number:
  US05/435,120
• Time in Patent Office: 778 Days
• Field of Search: 324/1, 324/4, 324/6, 324/8
• US Class Current: 324/345
• CPC Class Codes: G01V 3/082 operating with fields produced by spontaneous potentials, e.g. electrochemical or produced by telluric currents G01V3/26 takes precedence

Abstract

A method of exploration for deposits of oil, gas and of other minerals in the earth including geothermal energy, which is based on the existence of electrotelluric currents that are generated spontaneously by such deposits because of the geochemical modifications caused by their presence within rocks in the proximity of such deposits, which method consists in measuring the magnetic perturbations created by said electrotelluric currents in the normaly existing earth magnetic field.

When such electrotelluric currents exist, closed line-integrals of the earth magnetic field performed at or near the earth'"'"'s surface so not vanish and the residual values of such integrals are a direct function of the magnitude and of the polarity of the electrotelluric current flux densities generated by the underground mineral deposits sought.

Claims

1. A method of locating oil, gas, minerals, or geothermal energy deposits comprising the steps of:

a. measuring the total earth magnetic field intensity H_t at a plurality of stations numbered from 1 to n and forming a closed traverse around an area to be investigated

b. evaluating the line-integral LI defined by ##EQU5## along said traverse, wherein ds is an elementary length of the traverse, α

is the angle between H_t and ds and ##EQU6## denotes the algebraic summation of n terms of the form H_t. ds. cosine α

evaluated in the series of intervals 1-2, 2-3, . . . . (n-1)-n, n-1,

c. correlating the value of LI to the presence or absence of the deposits sought on the basis of its magnitude and its sign, positive values of LI evaluated along the closed traverses in a clockwise direction are indicative of mineral deposits giving rise to downward electro-telluric current flow such as are generated by hydrocarbon accumulations, whereas negative values of LI are indicative of the presence of mineral deposits giving rise to upward electro-telluric currents such as are generated by geothermal energy, the aforesaid relationship between the polarity of LI and the electrotelluric current flow direction being reversed when the line integration is performed counterclockwise.

2. The method of claim 1, in which:

a. the horizontal component of the earth magnetic field is measured and a line integration of said component is performed around a closed traverse.

3. A method of locating oil, gas, minerals, or geothermal energy deposits comprising the steps of:

a. selecting a plurality of adjacent or over-lapping closed traverses enclosing areas to be investigated, preferably all substantially of the same area-magnitude

b. measuring the total earth magnetic field intensity H_t at a plurality of stations numbered from 1 to n along each closed traverse

c. evaluating the line integral LI defined by ##EQU7## around each of the closed traverse, wherein ds is an elementary length of the profile, α

is the angle between H_t and ds, and ##EQU8## denotes the algebraic summation of n terms of the form H_t.ds;

cosine α

evaluated in the series of intervals 1-2, 2-3, . . . . . (n-1)-n, n-1,

d. plotting the values of LI so obtained at the center of each of the areas surveyed for the purpose of evaluating the presence and the areal extent of the deposits sought, positive values of LI evaluated along the closed traverses in a clockwise direction are indicative of mineral deposits giving rise to upward electrotelluric currents such as are generated by geothermal energy, the aforesaid relationship between the polarity of LI and the electrotelluric current flow direction being reversed when the line integration is performed counterclockwise.

4. The method of claim 3, in which:

a. the horizontal component of the earth magnetic field is measured along a plurality of adjacent or overlapping closed traverses.

5. A method of locating oil, gas, minerals, or geothermal energy deposits comprising the steps of:

a. selecting a plurality of long and substantially parallel traverses all oriented in the same direction and another plurality of such traverses intersecting the first set of traverses substantially at right angle and covering an area under investigation

b. recording continuously along such traverses the total intensity H_t of the earth magnetic field

c. evaluating the line integral segment

space="preserve" listing-type="equation">LI = ∫

H.sub.t .sup.. ds .sup.. cosine α

along each intercept between the two groups of traverses, wherein ds is an elementary length of the traverse, α

is the angle between H_t and ds and ds and ##EQU9## denotes the algebraic summation of n terms of the form H_t .ds.cosine α

evaluated in series of intervals 1-2, 2-3, . . . . (n-1)-n, n-1

d. evaluating the closed line integrals LI_c around each mesh grid formed by the two groups of traverses by adding algebraically the four LI'"'"'s values around each grid

e. plotting the values of LI_c so obtained at the centers of each of the mesh grid for the purpose of evaluating the presence and the areal extent of the deposits sought, positive values of LI evaluated along the closed traverses in a clockwise direction are indicative of mineral deposits giving rise to downward flow of electrotelluric currents such as are generated by hydrocarbon accumulations, whereas negative values of LI are upward electrotelluric currents such as are generated by geothermal energy, the aforesaid relationship between the polarity of LI and the electrotelluric current flow direction being reversed when the line integration is performed counterclockwise.

6. The method of claim 5, in which:

a. the horizontal component of the earth magnetic field is measured.

11. The method of claim 5, in which:

a. a single plurality of long and substantially parallel traverses are selected all in the magnetic North-South direction

b. the line integral of the total earth magnetic field intensity is evaluated along equal segments on two adjacent sides of mesh grids along the said traverses.

12. The method of claim 11, in which:

a. the horizontal component of the earth magnetic field is measured.

7. A method of locating oil, gas, minerals, or geothermal energy deposits by intepreting maps of the total earth magnetic field intensity comprising the steps of:

a. gridding the area of interest on such maps and reading the magnetic field values A at each grid apex

b. transferring said values to computer cards or to magnetic tape for computer processing

c. evaluating the line integrals LI (I, J) around each four mesh grid by

space="preserve" listing-type="equation">LI (I, J) = A (I, J+1) + A (I, J+2) + A (I, J+3) + A (I, J+4) + A (I+2,2,

     4) + A (I+3, J+4) - A (I+4, J+3) - A (I+4, J+2) - A (I+4, J+1) - A (I+3, J) - A (I+2, J) - A (I+1, J) - 3.0 * [ A (I, J+4) - A (I+4, J)]

wherein A is the total earth magnetic field intensity at points of row number values I to I + 4 and of column number values J to J + 4.

d. plotting the values of LI so obtained at the center of each of the mesh grid for the purpose of evaluating the presence and the areal extent of the deposits sought.

8. The method of claim 7, in which:

a. the horizontal component of the earth magnetic field is measured.

9. The method of claim 7, in which the line integral LI around each four mesh grid is evaluated by

a. computing the curvature D (I, J) of the readings A by:

space="preserve" listing-type="equation">D (I, J) = 2.0*A (I+1, J+1) - [A (I, J) + A (I, J+1) + A (I, J+2) + A (I+1, J) + A (I+2, J) + A (I+2, J+1) + A (I+2, J+2)+ A (I+1, J+2) + A (I+1, J+1)] 1 3.0

b. computing the line integrals LI (I+1, J+1) around each four mesh grid by;

space="preserve" listing-type="equation">LI (I+1, J+1) = D (1, J+1) + D (I+1, J+2) +D (I+2, J+1) +D (I+1, J) - D (I, J) - D (I, J+2) - D (I+2, J+2) - D (I+2, J)

wherein A is the total earth magnetic field intensity and D is the curvature of a surface defined by the A values, the numerical values of A and D being represented at points of coordinates of row number values I to I + 2 and of column number values J to J + 2.

10. The method of claim 9, in which:

a. the horizontal component of the earth magnetic field is measured.

13. The method of locating oil, gas, minerals and geothermal energy deposits comprising the steps of:

a. measuring the total earth magnetic field intensity at a plurality of stations numbered from 1 to n along a first closed traverse in an area to be investigated and at another plurality of stations numbered from 1 to m along a second closed traverse in the same area and enclosing the said first traverse, totally or partially

b. evaluating the line integrals ##EQU10## and ##EQU11## along each of said traverse, wherein LI₁ is the line integral evaluated along the first closed traverse comprising stations numbered 1 to n, ##EQU12## denoting the algebraic sum of terms H_t.ds.cosine α

, H_t being the total earth magnetic field intensity measured at stations 1 to n, ds, is an elementary length of this traverse and α

, is the angle between H_t and ds, whereas LI₂ is the line integral along the second closed traverse comprising stations numbered 1 to m and performed in the same manner and in the same direction as LI₁

c. evaluating the difference LI₁ - LI₂ in intensity and in polarity in order to determine the differential change in the electro-telluric currents within the depth interval bracketed by the depths of investigation of each closed profile.

14. The method of claim 13, in which

a. the horizontal component of the earth magnetic field is measured.