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Applications of Reflection Seismics to Mapping Coal-SEAM Structure and Discontinuities.

机译:反射地震学在煤层结构与不连续性测绘中的应用。

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As a means of demonstrating the effectiveness of reflection seismology in determining continuity of coal seams, three US field projects are reviewed. The three projects involve coals of varied thickness (2 to 14 m) and age (Pennsylvanian to Eocene) from three coal areas of the US (Pennsylvania, Wyoming, and Washington). Each projet also employed its own particular seismic technique, recording system, and seismic energy source although all are considered state-of-the-art, high resolution, digital seismic surveys. Project 1 (thin, Pennsylvania coal) sought detection of sand channels using dynamite and standard in-line (2-D) seismic technique. Project 2 (thick, Wyoming underground coal gasification) involved a gas-explosion (Dinoseis) source with areal (3-D) acquisition methods. Project 3 (thick Washington underground coal gasification) employed a shotgun-type source and standard in-line methods. Data processing was handled by different contractors for each project. Each project was successful in accomplishing its own particular objective; however, data quality and interpretation seem to be more a function of thickness of the target seam, complexity of the overburden, and processing contractor than a seismic source, acquisition scheme (2-D versus 3-D), or recording instrumentation. (ERA citation 06:021546)

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