Muting the noise cone in near-surface reflection data: An example from southeastern Kansas

被引:23
作者
Baker, GS [1 ]
Steeples, DW
Drake, M
机构
[1] Univ Kansas, Dept Geol, Lawrence, KS 66044 USA
[2] Kansas State Univ, Dept Geol, Manhattan, KS 66506 USA
关键词
D O I
10.1190/1.1444434
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A 300-m near-surface seismic reflection profile was collected in southeastern Kansas to locate a fault(s) associated with a recognized stratigraphic offset on either side of a region of unexposed bedrock. A substantial increase in the S/N ratio of the final stacked section was achieved by muting all data arriving in time after the airwave. Methods of applying traditional seismic data processing techniques to near-surface data (200 ms of data or less) often differ notably from hydrocarbon exploration-scale processing (3-4 s of data or more). The example of noise cone muting used is contrary to normal exploration-scale seismic data processing philosophy, which is to include all data containing signal. The noise cone mute applied to the data removed more than one-third of the total data volume, some of which contains signal. In this case, however, the severe muting resulted in a higher S/N ratio in the final stacked section, even though some signal could be identified within the muted data. This example supports the suggestion that nontraditional techniques sometimes need to be considered when processing near-surface seismic data.
引用
收藏
页码:1332 / 1338
页数:7
相关论文
共 12 条
[1]   MIGRATION OF SHALLOW SEISMIC-REFLECTION DATA [J].
BLACK, RA ;
STEEPLES, DW ;
MILLER, RD .
GEOPHYSICS, 1994, 59 (03) :402-410
[2]   SHALLOW SEISMIC-REFLECTION MAPPING OF THE OVERBURDEN-BEDROCK INTERFACE WITH THE ENGINEERING SEISMOGRAPH - SOME SIMPLE TECHNIQUES [J].
HUNTER, JA ;
PULLAN, SE ;
BURNS, RA ;
GAGNE, RM ;
GOOD, RL .
GEOPHYSICS, 1984, 49 (08) :1381-1385
[3]   OBSERVATIONS OF THE AIR-COUPLED WAVE AS A FUNCTION OF DEPTH [J].
KNAPP, RW .
GEOPHYSICS, 1986, 51 (09) :1853-1857
[4]   VERTICAL RESOLUTION OF A SEISMIC SURVEY IN STRATIGRAPHIC SEQUENCES LESS-THAN 100 M DEEP IN SOUTHEASTERN KANSAS [J].
MILLER, RD ;
ANDERSON, NL ;
FELDMAN, HR ;
FRANSEEN, EK .
GEOPHYSICS, 1995, 60 (02) :423-430
[5]   NORMAL MOVEOUT STRETCH MUTE ON SHALLOW-REFLECTION DATA [J].
MILLER, RD .
GEOPHYSICS, 1992, 57 (11) :1502-1507
[6]  
MILLER RD, 1990, GEOL SOC AM BULL, V102, P18, DOI 10.1130/0016-7606(1990)102<0018:SSRSAT>2.3.CO
[7]  
2
[8]  
Mooney H. M., 1962, GEOPHYS PROSPECT, V10, P84, DOI [DOI 10.1111/J.1365-2478.1962.TB01999.X, 10.1111/j.1365-2478.1962.tb01999.x.]
[9]  
ROBINSON EA, 1990, GEOPHYSICAL SIGNAL A
[10]  
Waters K.H., 1987, REFLECTION SEISMOLOG, VThird