摘要
地热流体中惰性气体的相对丰度和同位素组成 ,不仅可以揭露热田的热源性质 ,而且还能够揭示深、浅层地热流体的内在联系和演化过程等。在西藏羊八井热田的地热气体中 ,已检测出大量的 4 He组分 ,3He/ 4 He值是大气的 0 .0 87～ 0 .2 5 9倍 ,表明深部地壳物质的局部熔融为热田提供能量。浅层地热流体的 3He/ 4 He值自西北向东南呈降低趋势 ,与热储温度的变化相一致 ,反映出侧向运移时补充了更多的壳源氦。热田北区深层地热流体具有稍高的 3He/ 4 He值 ,是浅层地热流体的母源。气体中氪和氙的相对丰度具有大气降水成因的特征。结合现有的实际资料 。
The relative abundances and isotopic composition of noble gases in selected wells were determined to identify heat source, the relationship between shallow and deep thermal fluids, and fluid migration. The thermal fluids contain large 4He excesses with 3He/ 4He ratios of 0.087~0.259 times the ratio in air. Heat source in the region is inferred to be partial melting of the crust at depth. The dense cold groundwater pulled by gravity moves down through the pediment fault of the Nyainquentanglha Mts. Along the flow path, the water absorbs heat from wallrock and gradually loses its density. Differential densities between the thermal and cold waters drive the thermal water to shallow depths. The deep thermal fluid found only in the northern part of the field has the highest 4He enrichment [F( 4He)~7500] and the highest 3He/ 4He ratio ( 0.259Ra ).When the thermal water approaches the surface, the pressure in the fracture zone decreases so that the thermal water can boil CO 2 and H 2S rich steam escaping from the boiling water along its ascent channel. Production wells ZK354 and ZK357, located in the upwelling zone, have slightly higher 3He/ 4He ratios and F( 4He) values than the others nearby. When the upflow of the deep thermal water is blocked, the pressure drives it laterally toward the southeast where it enters the shallow reservoir after mixing with the cold groundwater. The shallow reservoir consists of Quaternary alluvium and altered granite, opal and calcite precipitate from the thermal water to form a self sealed alluvium cap. As the shallow thermal fluid migrates towards the southeast, helium will escape from the reservoir through a thin and loose alluvium cap while at the same time radiogenic helium produced in the underlying granite, will be added to the migrating fluid. These cause the 3He/ 4He ratios and F( 4He) values decrease from northwest to southeast. The relationship between F( 84 Kr) and F( 132 Xe) values implie
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2001年第3期497-503,共7页
Acta Petrologica Sinica
基金
国家自然科学基金 (4 9972 0 93 )
国际原子能机构 (CPR90 95 )和美国能源部地热和风能技术局 (DE-AC0 3 -76SF0 0 0 98)联合资助
