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1965年以来,塔吉克(Tadjik)科学院地震研究所利用GS—12(N182)重力仪,采取重复重力测量在阿什哈巴德地球动力学试验场开展了区域重力变化的研究。1971年以来,又与苏联科学院大地物理研究所联合进行了重力测量。沿着Gaudan剖面布设了7个观测点,这组观测点从北向南穿过Kopetdag前渊断层带。在这个断层带上,利用了十多种地球物理学方法来研究地震构造对地球物理场、水文地质状态、热流值、水氮释放的影响。
Since 1965, the Institute of Seismology, Tadjik Academy of Sciences has conducted a study of the regional gravity changes using the GS-12 (N182) gravimeter using repeated gravimetric measurements at the Ashgabat Geodynamics Experimental Site. Since 1971, it has also conducted gravimetric measurements jointly with the Institute of Geophysics of the Soviet Academy of Sciences. Seven observation points along the Gaudan section have been laid through the Kopetdag fore-tectonic zone from north to south. In this fault zone, more than ten kinds of geophysical methods are used to study the influence of seismic structure on geophysical field, hydrogeological state, heat flow value and water and nitrogen release.