Geomagnetic studies at Rubaniv gas field in outer zone of Carpathian Foredeep, Ukraine

V. Maksymchuk, R. Kuderavets, O. Menshov, P. Bodlák, I. Chobotok, Y. Nakalov, N. Pyrizhok
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Abstract

SUMMARY The results of geomagnetic studies at the Rubaniv gas field in the Outer zone of the Carpathian Foredeep are considered. A detailed study of the anomalous magnetic field and the magnetic properties of rocks and soils at the zones of hydrocarbon deposits is a basement for the application of the magnetic prospecting for direct hydrocarbon prospecting. At the present study we investigate the structure of the local anomalous magnetic field in the zones of hydrocarbon fields within the Carpathian Foredeep for the identification of the genetic relation of the magnetic properties of surface rocks and soils with the microseepage of hydrocarbons. The total magnetic field vector T and its components (declination, inclination, horizontal and vertical components) along the 5 transect were measured. The soil magnetic susceptibility in transects and in the profiles (genetic horizons) were studied. The local positive magnetic anomalies with the amplitude from 2 to 8 nT and dispersion of the soil magnetic susceptibility above the Rubaniv gas field were detected. This data indicated the genetic relations between gas deposits, microseepage, and changes of the magnetic field and soil magnetism.
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乌克兰喀尔巴阡前深外带鲁巴尼夫气田地磁研究
总结了喀尔巴阡前深外带鲁巴尼夫气田的地磁研究成果。对含油气带异常磁场和岩石、土壤磁性的详细研究,为磁法勘探在油气直接勘探中的应用奠定了基础。本文研究了喀尔巴阡盆地前深油气带的局部异常磁场结构,以确定地表岩石和土壤的磁性与油气微渗流的成因关系。测量了沿5个样带的总磁场矢量T及其分量(赤纬、倾角、水平和垂直分量)。对样带和剖面(遗传层)土壤磁化率进行了研究。检测了鲁巴尼夫气田上方2 ~ 8 nT的局部正磁异常和土壤磁化率的色散。这些数据揭示了天然气沉积、微渗流、磁场和土壤磁性变化之间的成因关系。
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