CAJ | 학술논문

对唐古拉山北侧温泉盆地多年冻土区冷泉气体样品的化学分析表明，CH4平均含量为370×10-6，是青藏铁路沿线（昆仑山口—安多）多年冻土区冷泉气体中CH4平均含量的近113倍，表现出极高的地球化学异常。与国内外多年冻土区天然气水合物的形成条件相比，温泉盆地地区具有天然气水合物形成的冻土厚度与温压、烃类气体与水源、流体运移与储集的良好条件，预示该区可能具有天然气水合物的存在，是今后值得重视的天然气水合物调查评价区。
대당고랍산북측온천분지다년동토구랭천기체양품적화학분석표명，CH4평균함량위370×10-6，시청장철로연선（곤륜산구—안다）다년동토구랭천기체중CH4평균함량적근113배，표현출겁고적지구화학이상。여국내외다년동토구천연기수합물적형성조건상비，온천분지지구구유천연기수합물형성적동토후도여온압、경류기체여수원、류체운이여저집적량호조건，예시해구가능구유천연기수합물적존재，시금후치득중시적천연기수합물조사평개구。
Geochemical survey of cold spring from frozen earth zone in the Wenquan basin, north of the Tanggula Mountains show the average content of CH4 of 370×10-6 which is about 113 times of that along the Qinghai-Tibet Railway. There are many favorable conditions for the formation of gas hydrate, such as frozen earth thickness, temperature and pressure, hydrocarbon gas and water source, fluid migration and reservoir in the Wenquan basin.