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MAPPING NON‐REFLECTING VELOCITY INTERFACES BY NORMAL MOVEOUT VELOCITIES OF UNDERLYING HORIZONS *
Author(s) -
KREY TH.
Publication year - 1980
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1980.tb01231.x
Subject(s) - base (topology) , geology , differential (mechanical device) , differential equation , layer (electronics) , geometry , regional geology , mathematical analysis , chemistry , mathematics , hydrogeology , physics , metamorphic petrology , thermodynamics , geotechnical engineering , organic chemistry
A bstract The normal moveout velocity of a reflecting bed is a function of the dips and curvatures of all overlying velocity interfaces. Now let the ( N – 1)th velocity interface be a non‐ (or badly) reflecting bed, whereas the other interfaces, including the base of the N th layer, reflect satisfactorily, and let the velocities U N – 1 and U N of the ( N – 1)th and N th layer, respectively, be known. Then the normal moveout velocity for the base of the N th layer, if known in one direction at a certain part of the surface of the earth, provides a second order differential equation in the horizontal coordinates x and y for the depth Z N – 1 ( x, y ) of the unknown interface. The mathematics becomes rather simple in the case of two‐dimensional geological structures. For this case and N = 2 the differential equation mentioned can be solved by stepwise integration or by iteration. One of the many possible applications of the new concept is the determination of the structure of the base of an overthrusting sheet.