对蒙大拿州Powder River和Carter县的美国地质调查局地震反射剖面和垂直地震剖面进行处理和解释

A. Balch, John J. Miller, M. Lee, R. Ryder
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引用次数: 1

摘要

1977年8月3日至5日,美国地质调查局麦迪逊石灰石测试井2号井进行了垂直地震剖面(VSP)测试。地震能量源为单个60英寸。/sup 3/螺栓LSS-3/sup 4/陆地气枪,操作压力2000psi。记录间距为25英尺,从7900英尺到3800英尺;40英尺从3800英尺到1500英尺;从1500英尺到地面50英尺。VSP数据经过数字记录、编辑、合成、小波整形、速度滤波、时移和垂直求和。采用带通滤波器匹配表面记录频带。地表反射数据记录于1978年10月15日至19日。能源由四个Pelco振动器提供,振动器间距为73英尺,在440英尺的线段上进行16次扫描。检波器的模式是36个探测器排成一条220英尺长的线,每个震源点有48个通道,在震源上有5个站的间隙。地面数据上的主要反射事件在剖面上显示为连续线,与USGS麦迪逊石灰石测试井2号井的垂直地震剖面相关联。为了准确识别,在VSPmore»上垂直追踪这些事件,直到它们在地球上的起源点,并在该点与图表下部所示的岩性测井曲线联系起来。同时还显示了与岩性测井相对应的地层名称。下图上的粗线一般对应主要的地质构造边界。较浅的线条表示较小反射器的一般排列。这些数据有助于石油和天然气的调查。(DP)«更少
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Processed and interpreted U.S. Geological Survey seismic reflection profile and vertical seismic profile, Powder River and Carter Counties, Montana
A US Geological Survey Vertical Seismic Profile (VSP) at the USGS Madison Limestone Test Well No. 2 was run on August 3-5, 1977. The seismic energy source was a single 60 in./sup 3/ Bolt LSS-3/sup 4/ land air gun, operated at 2000 psi. The recording interval was 25 feet from 7900 ft to 3800 ft; 40 ft from 3800 ft to 1500 ft; and 50 ft from 1500 ft to the surface. VSP data were digitally recorded, edited, composited, wavelet shaped, velocity filtered, time shifted, and vertically summed. A band pass filter was applied to match the surface recording frequency band. The surface reflection data were recorded October 15-19, 1978. The energy source was supplied by four Pelco vibrators spaced at 73 ft, with 16 sweeps over a 440 ft line segment. The geophone pattern was 36 detectors in a line 220 ft. long, 48 channels per source point with a five station gap across the source. Major reflecting events on the surface data, shown as continuous lines on the profile, were tied to the summed vertical seismic profile at the USGS Madison Limestone Test Well No. 2. For positive identification, these events were then tracked vertically on the VSPmore » to their point of origin in the earth, and tied at that point to the lithologic log shown in the lower portion of this chart. Formation names corresponding to the lithologic log are also shown. Heavy lines on the lower figure generally correspond to principal geologic formation boundaries. The lighter lines show the general arrangement of lesser reflectors. This data aids petroleum and natural gas investigatons. (DP)« less
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