Exploration system for discovering deposits of ore, marker rock and/or economic minerals

Claim 2

Method of accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation: (a) generating a seismic wave at a first sourcepoint location adjacent said series of detectors; (b) after said wave undergoes refraction, detecting arrival of a refracted wave at said series of detectors at said inline offset positions, to obtain a first set of traces associated with said offset positions X 1 , X 2 , . . . X n ; (c) repeating steps (a) and (b) by generating a second wave at a second sourcepoint adjacent to inline position X n of said detector positions, and detecting said refracted wave to obtain a second set of traces; (d) advancing said series of detectors a selected number of inline positions or fractions thereof and repeating steps (a), (b) and (c) above to obtain additional sets of traces, but in which said additional sets of traces are associated with more than two inline positions overlapping common inline positions of said first and second sets of traces; (e) distinguishing arrival times of shear waves from compressional waves; and (f) analyzing arrival times of at least one segment of (i) shear waves and (ii) compressional waves as a function of inline position whereby shape of said earth formation as well as elastic parameters indicative of likelihood of said formation being an ore, marker rock, economic mineral, and the like, are provided.

Claim 3

Method of accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation: (a) generating a seismic wave at a first sourcepoint location adjacent said series of detectors; (b) after said wave undergoes refraction, detecting arrival of a refracted wave at said series of detectors at said inline offset positions, to obtain a first set of traces associated with said offset positions X 1 , X 2 , . . . X n in which arrival times of shear waves are distinguished from compressional waves; (c) repeating steps (a) and (b) by generating a second wave at a second sourcepoint adjacent to inline position X n of said detector positions, and detecting said refracted wave to obtain a second set of traces in which arrival times of shear waves are distinguished from compressional waves; (d) advancing said series of detectors a selected number of inline positions or fractions thereof and repeating steps (a), (b) and (c) above to obtain additional sets of traces, but in which said additional sets of traces are associated with more than two inline positions overlapping common inline positions of said first and second sets of traces; and (e) analyzing arrival times of at least one segment of (i) shear waves and (ii) compressional waves as a function of inline position whereby shape of said earth formation as well as elastic parameters indicative of likelihood of said formation being an ore, marker rock, economic mineral, and the like, are provided.

Claim 4

Method of accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation: (a) generating a seismic wave at a first sourcepoint location adjacent said series of detectors; (b) after said wave undergoes refraction, detecting arrival of a refracted wave at said series of detectors at said inline offset positions, to obtain a first set of traces associated with said offset positions X 1 , X 2 , . . . X n in which arrival times of shear waves are distinguished from compressional waves; (c) repeating steps (a) and (b) by generating a second wave at a second sourcepoint adjacent to inline position X n of said detector positions, and detecting said refracted wave to obtain a second set of traces in which arrival times of shear waves are distinguished from compressional waves; (d) advancing said series of detectors a selected number of inline positions or fractions thereof and repeating steps (a), (b) and (c) above to obtain additional sets of traces, but in which said additional sets of traces are associated with more than two inline positions overlapping common inline positions of said first and second sets of traces; and (e) analyzing arrival times of at least one segment of (i) shear waves and (ii) compressional waves as a function of inline position whereby shape of said earth formation as well as elastic parameters indicative of likelihood of said formation being an ore, marker rock, economic mineral, and the like, are provided.

Claim 5

Method of claim 1 with the additional sub-step of determining shape of said earth formation by (i) classifying bedding shape as horizontal or vertical based on displaying refraction travel time values as a function of horizontal offset coordinate and sourcepoint offset location, (ii) normalizing said sourcepoint locations to a common direction; (iii) comparing slopes of at least a common line through breakpoints of said travel time value whereby shape of said earth formation is determined.

Claim 6

Method of claim 2 with the additional sub-step of determining shape of said earth formation by (i) classifying bedding shape as horizontal or vertical based on displaying refraction travel time values as a function of horizontal offset coordinate and sourcepoint offset location, (ii) normalizing said sourcepoint locations to a common direction; (iii) comparing slopes of at least a common line through breakpoints of said travel time values whereby shape of said earth formation is determined.

Claim 7

In accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation, means for plotting a series of refracted travel time values versus horizontal offset coordinate annotated by sourcepoint-profile number and refraction arrival direction indicated by sourcepoint offset positions at one of a forward and trailing inline position X 1 and X n of said detectors, slope of said travel time values versus offset being indicative to apparent P-wave and/or S-wave velocities, said sourcepoint offset positions being alignable along an imaginary line of ascertainable slope.

Claim 8

In accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation, means for plotting a series of refracted travel time values versus horizontal offset coordinate annotated by sourcepoint-profile number and refraction arrival direction indicated by sourcepoint offset positions at one of a forward and trailing inline position X 1 and X n of said detectors, slope of said travel time values versus offset being indicative to apparent P-wave and/or S-wave velocities, said sourcepoint offset positions being alignable along an imaginary line of ascertainable slope.

Claim 9

Means for plotting claim 5 including means for selecting refraction events from field data provided by said refraction field system, and means for plotting said events to indicate refraction travel time as a function of horizontal offset.

Claim 10

Means for plotting of claim 6 in which said first-mentioned means is an event selector and said second-mentioned means is a counter having a reset signal for driving an encoding head of a recording means.

Claim 11

Means for plotting of claim 6 in which said first- and second-mentioned means are a properly programmed digital computer.

Claim 12

In accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n , and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation: means for plotting a series of refracted travel time values versus horizontal offset coordinates annotated by sourcepoint number and refraction arrival direction of a forward and reverse direction indicated by reverse direction sourcepoint offset position at one of (i) a trailing inline position and (ii) a forward inline position closest to positions X 1 and X 2 respectively of said detectors, slope of said travel time values versus offset being indicative of apparent P-wave and/or S-wave velocities; said sourcepoint offset positions being changeable along at least first and second imaginary lines of common slope; said first line being common to all sourcepoint offset positions associated with said refraction values arriving in said forward direction, and said second line being common to all sourcepoint offset position associated with said refraction values occurring in said reverse direction.

Claim 13

In accurately determining shape and elastic parameters of an earth formation to identify ore, marker rocks, economic minerals or the like, using a refraction exploration field system including a series of detectors, positioned along a line or survey at inline positions X 1 , X 2 , . . . X n , and at least one seismic source located adjacent to said detectors for producing a seismic wave for travel through said formation: means for plotting a series of refracted travel time values versus horizontal offset coordinates annotated by sourcepoint number and refraction arrival direction of a forward and reverse direction indicated by reverse direction sourcepoint offset position at one of (i) a trailing inline position and (ii) a forward inline position closest to positions X 1 and X 2 respectively of said detectors, slope of said travel time values versus offset being indicative of apparent P-wave and/or S-wave velocities; said sourcepoint offset positions being changeable along at least first and second imaginary lines of common slope; said first line being common to all sourcepoint offset positions associated with said refraction values arriving in said forward direction, and said second line being common to all sourcepoint offset position associated with said refraction values occurring in said reverse direction.

Claim 14

Means for plotting of claim 9 including means for selecting refraction events from field data provided by said refraction field system, and means for plotting said events to indicate refraction travel time as a function of horizontal offset.

Claim 15

Means for plotting of claim 9 in which said first-mentioned means is an event selector and said second-mentioned means is a counter having a reset signal for driving an encoding head of a recording means.

Claim 16

Means for plotting of claim 9 in which said first- and second-mentioned means are a properly programmed digital computer.