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根据怀特岛过去的地表勘测、特别是对喷出气体的调查,制作了火山、地热系模型。根据该模型,怀特岛600m地下存在岩浆房,岩浆房的周围是自岩浆分离出来的蒸汽及蒸汽吹入热水中形成的高温盐水。因此,决定钻探至该高温蒸汽层,以证实蒸汽及热水的存在,同时还要探明其物理、化学特征。井位预选在康格列斯火山口以东600n处。预定在100m、300m、600m三个孔段进行各种测井,并采取水样。从资源开发观点看,这种调查相当于火山型
According to the Isle of Wight’s past surface survey, in particular, to investigate the discharge of gas, produced a volcano, geothermal model. According to the model, a magma chamber exists on the Isle of Wight 600m underground. The magma chamber is surrounded by the steam separated from the magma and the high-temperature brine formed by the steam blown into the hot water. Therefore, it is decided to drill to the high temperature steam layer to confirm the presence of steam and hot water, while also ascertaining its physical and chemical characteristics. The pit pre-selection is 600n east of the Congleles crater. Scheduled at 100m, 300m, 600m three holes for a variety of well logging and water samples taken. From a resource development point of view, this survey is equivalent to a volcano