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INVERSE VERTICAL SEISMIC PROFILING USING A MEASUREMENT WHILE DRILLING TOOL AS A SEISMIC SOURCE
INVERSE VERTICAL SEISMIC PROFILING USING A MEASUREMENT WHILE DRILLING TOOL AS A SEISMIC SOURCE
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机译:在将钻具作为地震源进行测量的同时进行垂直地震剖面反演
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摘要
A reverse VSP system is provided and uses a frequency-controllable modulator of an MWD tool as a downhole seismic source. The modulator has a rotor and stator arranged to provide substantially sinusoidal outputs, and is controlled to provide a "Vi broseis"-type frequency sweep (preferably from 1 Hz to 50 Hz). With the bit of the MWD tool in conta ct with the bottom of the borehole, the force generated by the frequency-controllable modulator will generate measurable axial compressional (P-) waves. These waves which move through th e formation are detected by an array of geophones on the formation surface, and a reference signal is obtained by a kelly-mounted accelerometer or strain gauge. The reference signal and sign als obtained by the geophones are processed using known signal processing techniques. The disclo sed downhole frequency-controllable seismic source provides many advantages including goo d resolution due to the ability to output a sinusoidal wave at desired frequencies and the fa ct that the location of the source signal is well-defined (at the bit), the ability to image formati ons ahead of the bit, and the ability to conduct reverse VSP processing without adding downhole hardwa re equipment and without requiring trips out of the well.
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机译:提供了反向VSP系统,其使用MWD工具的频率可控调制器作为井下地震源。调制器具有布置为提供基本正弦输出的转子和定子,并被控制为提供“ Vi broseis”型扫频(最好从1 Hz到50 Hz)。当MWD工具的钻头与井孔底部接触时,频率可控调制器产生的力将产生可测量的轴向压缩(P-)波。这些穿过地层的波由地层表面上的一系列地震检波器检测,而参考信号则通过安装在方钻杆上的加速度计或应变仪获得。使用已知的信号处理技术处理地震检波器获得的参考信号和信号。所公开的井下频率可控地震源具有许多优势,包括高分辨率,这是因为它能够以所需频率输出正弦波,并且可以很好地确定源信号的位置(在位),能够在位之前对图像进行格式化,并且能够进行反向VSP处理,而无需添加井下硬件设备,也不需要跳井。
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