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Use of Reflection Seismic and Gravimetry for the Exploration of a Salt Structure

机译:反射地震和重力法在盐构造勘探中的应用

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摘要

In autumn 1999 a high resolution seis- mic survey of totaling 15.13 km and a gravimetric survey of 3.5 x 3.5 km were ac- quired over the salt structure of Rudersdorf. The task of both geophysical survey methods Was to scout the structure of the overburden And the depth of the Mesozoic including the Top Zechstein. The seismic survey could not Produce a definite result for the depth of the Lower Mesozoic and the strike and dip of the WSW-ENE running fault zone in this depth Layer. The gravimetric survey should be a so- Lution to the two aforenamed geological que- Stions.
机译:在1999年秋天,对Rudersdorf的盐结构进行了总计15.13 km的高分辨率地震勘测和3.5 x 3.5 km的重力测量。两种地球物理勘测方法的任务都是探查上覆构造和中生代包括顶切赫施泰因的深度。地震勘测无法得出该深度层中下生界的深度以及WSW-ENE走向断裂带的走向和倾角的确切结果。重量测量应该是两个前述地质问题的解决方案。

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