Abstract In marine seismic exploration, a long array of sources efficiently transfers energy along the reflection path. Multiple reflection rejection is achieved by normal move-out discrimination at selected trace distances for each reflection. The length of the source array is changed in accordance with the geological characteristics of the sub-surface formations being explored and the reflection time of reflections from formations of interest. A split source array allows one section of the array to be moved with respect to the other to change the overall length of the array without changing the number of sources which are fired. Primary to multiple reflection enhancement is obtained by selecting only traces having source to detector offset distances with a primary to multiple amplitude response ratio greater than one.
An array of seismic sources for marine seismic exploration comprising: first and second towing cables, marine seismic sources attached to approximately equally spaced intervals to said towing cables, and means for extending and retracting one cable with respect to the other so that the total length of the array formed by both towing cables can be changed.
Claim 2
Dependent Claim
57 words
An array of seismic sources for marine seismic exploration comprising: first and second towing cables, marine seismic sources attached to approximately equally spaced intervals to said towing cables, and means for extending and retracting one cable with respect to the other so that the total length of the array formed by both towing cables can be changed.
Claim 3
Dependent Claim
80 words
The array of seismic sources recited in claim 1 wherein said total length is given by: L.sub.max = Kτ/δt.sub.p where δt p is given by: ##EQU3## where X is the maximum usable offset distance from the source to any detector array, T is the reflection time, T 0 is the zero offset reflection time, V is the acoustic velocity characteristic of the earth, α is the dip of the subsurface formations, and τ is the period of the seismic energy.