摘要
经对发生水热爆炸频率高、强度大的西藏、云南温泉进行研究，发现水热爆炸与温泉中硅浓度高有关。认为硅氢化物从地壳深部，通过深断裂系统，迁移至地壳浅部，被氧化、水解生成硅胶，逐渐将围岩和出口胶结形成一个相对封闭的系统，致使以后迁来的硅氢化物、硼氢化物、其它氢化物及热能逐渐积蓄，当温度、压力、氢化物浓度达一定限度时，冲破封闭层，氢化物迅速被氧化，产生大量热、气，发生水热爆炸。
Upon study of hotspring in Tibet and Yunnan that explodes frequently and strongly it was found that the explosion is related to silicon concentration in hot sprihg．Sillcon hydrate from deep into the crust moves to shallow area and is oxidized and hydrolyzed into silica gel which close the outlet so heat is cumulated to a point when other hydrate break through and is oxidized very quickly and give rise to explosion.
出处
《盐湖研究》
CSCD
2001年第4期1-7,共7页
Journal of Salt Lake Research
