川西高原水热活动分布特征与成因分析
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摘要
川西高原甘孜-理塘-巴塘地区发现的200余处温泉,其中11处泉口温度超过当地沸点。温泉大多出露于断裂附近或河谷地区,呈条带状分布。对区内构造特征、岩体热物性、断裂活动性质、重力和磁异常以及地震资料解释、水文地球化学等资料进行了综合分析,得出以下初步认识:一是区内温泉分布具有东西分带的特点,受断裂控制,可分为巴塘、理塘、康定三个地热带;二是区内莫霍面深度平均约为58 km,居里面平均深度22 km,构造上隆区与温泉分布有较好对应关系;三是理塘中、下地壳S波速较低,15km之下发育高导层,可能与局部高温熔融区有关;四是认识到区内温泉形成热源主要与放射性成因热、下地壳熔体增热、活动断裂摩擦热有关,但在不同地热带其贡献比例与主要成因有所不同。川西高原地热带是喜马拉雅地热带的重要组成部分。
引文
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