地热能作为一种清洁可再生能源已被广泛应用于发电、供暖等领域，放射性产热是地球内热的主要来源。目前，关于放射性产热的研究主要集中于高放射性花岗岩在干热岩资源探测和潜力评价中的应用，而同样作为放射性产热源的热液型铀矿与地热研究不足，二者的成因联系尚缺乏深入研究。白马峪温泉与白马洞铀矿床相毗邻，均位于贵州省息烽地热田内，受同一构造体系控制，具有一定的时空关系，是研究地热与热液型铀矿成因联系的理想对象。本项目拟以白马峪温泉和白马洞铀矿床为研究对象，综合运用水文地球化学、稳定同位素地球化学（如C、H、O）和流体包裹体地球化学等关键技术手段，旨在查明白马峪温泉热水水文地球化学特征与古地热流体来源、特征及其演化等，同时对比白马洞铀矿床成矿流体的特征，进而揭示温泉（地热）和热液型铀矿间的成因联系。此外，本项目将为地热与热液型铀矿成因联系研究提供新思路和新方法，并为“热矿共采”提供一定的理论依据。

As a type of clean and renewable resource, geothermal energy has been widely utilized in power generation and heating. Radiogenic heat is a primary source for geothermal energy in earth. The research on radiogenic geothermal energy has been focused on its application in detecting and evaluating potential for dry hot rock. However, as vital radioactive source, the research about the genetic relationship between hydrothermal uranium deposits and geothermal energy is poor. The Baimayu hot spring adjoins with the Baimadong uranium deposit, which all located in the Xifeng geothermal field and controlled by the same tectonic regim. They have close temporal-spatial relationship and could be applied to investigate the genetic relationship between geothermal energy and hydrothermal uranium deposits. This project focus on hot spring water and hydrothermal calcite from the Baimayu hot spring, utilizing hydrogeochemistry, stable isotope (C, H, O) and fluid inclusion to illuminate the characteristics of hot spring water, as well as source, feature and evoluation of paleo-geothermal fluid. Comparing the feature of paleo-geothermal fluid from the Baimayu hot spring and ore-forming fluid from the Baimadong uranium deposit is a key point to reveal the genetic relationship between hot spring (geothermal energy) and hydrothermal uranium deposits. Based on this study, a new thought and method can be provided for studying the genetic relationship of geothermal energy and hydrothermal uranium deposits and certain theoretical basis could be supplied for “jointly exploring of geothermal energy and ore”.