Line integral method of magneto-electric exploration

Claim 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.

Claim 2

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.

Claim 4

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.

Claim 5

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.

Claim 7

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 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.

Claim 8

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 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.

Claim 10

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 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.

Claim 11

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 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.

Claim 17

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 LI 1 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 LI 2 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 LI 1 c. evaluating the difference LI 1 - LI 2 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.

Claim 18

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 LI 1 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 LI 2 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 LI 1 c. evaluating the difference LI 1 - LI 2 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.