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本文简要介绍该领域研究的理论基础和获得的代表性成果，以及如何运用Sr－Nd同位素演化示踪技术探讨：区域基底和合矿层的供矿能力；水-岩交换性质和沉积环境；阐明成岩、成矿时水体介入和基岩参与程度；水源、岩源特征以及同位素交换平衡条件。为研究成矿环境和溶浸条件提供依据。
In this paper, we briefly introduce the theoretical basis and the representative results obtained in this field, and how to use the Sr-Nd isotope evolution tracing techniques to explore: the supply capacity of regional basement and ore-hosting; water-rock exchange and sedimentary environment; The degree of water body involvement and bedrock involvement during mineralization; the characteristics of water source and source rocks and the isotope exchange equilibrium conditions. It provides the basis for studying the metallogenic environment and leaching conditions.