川西高原沿金沙江断裂、德格-乡城断裂、甘孜-理塘断裂、鲜水河断裂集中出现几个北西-南东向条带状高温水热活动区，它们共处于青藏高原东构造结东北缘挤压、扭转的地球动力学背景，但却具有不同的热源构成与成因机制。本申请将对川西地热带高温地热资源区的深部热源构成与动力学演化机制开展综合地球物理反演与数值模拟研究：1）针对不同断层活动速率、岩浆活动规模，利用重磁反演，计算岩浆热源与断层摩擦热源的结构特点与分布规律；利用热模拟，分析岩浆热源与摩擦热源不同结构组合条件下的热演化模式与主控因素。2）针对断裂带水热系统、盆地水热系统，利用重磁反演，计算断裂带断层参数、隐伏岩体规模、壳幔结构；利用热模拟，分析活动构造条件下热源温度分布、岩浆热源体熔融深度和持续时间、不同热演化体系的热结构。为川西高原地热区动力学过程和机制、地热活动规律研究，热源构成、高温地热资源的勘探开发利用，提供重要的理论支撑和科学依据。

There are a few high-temperature hydrothermal activity strips which attached to the faults of Jinshajiang, Ganzi-litang, Derg-Xiangcheng and Xianshuihe along the northwest-southeast direction distribution in western Sichuan plateau mountain area. They have a similar geodynamics background with squeezing and twisting by the Tibet plateau tectonic knot, but have different heat source composition and formation mechanism. Based on thermal simulation method and geophysical inversion method，this application will research the deep-heat constitution and dynamic evolution mechanism of western Sichuan high temperature geothermal resource belt. 1) For different rate and magmatic size, the gravity-magnetic method will be used inversion the structure of magma and fault, and the thermal simulation method will compute the thermal evolution pattern and control factors under the condition of different structure combinations. 2) According to the characteristics of fault hydrothermal systems, we will calculate the fault parameters, concealed granite body shape and crust-mantle structure using inversion of gravity and magnetic. And then, we will analyze the distribution of heat source temperature under the condition of active tectonic, the magmatic heat source body melting depth and duration, as well as the thermal structure of different thermal evolution system through thermal simulation method. The goal of this research is that to provide important theoretical support for geothermal evolution mechanism of western Sichuan plateau mountain area, and to establish necessary scientific basis for heat source composition exploration as well exploitation of high temperature geothermal system.