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金牙金矿是桂西北微细粒浸染型金矿床具有代表意义的典型矿床。其赋矿层位为三叠系中统百蓬组的富有机碳的浊积岩系。通过对成矿过程中有机包裹体的激光拉曼分子微探针研究认为：（１）有机质在成矿过程中会发生热降解，其降解产物烃的量可衡量热的程度；（２）无机组分和ＣＯ２／ＣＨ４ 参数可用于研究热液的地球化学环境。
The gold tooth gold deposit is a typical deposit that represents the significance of the fine grained gold deposits in the northwest of Guangxi. The ore-bearing layers are organic carbon-rich turbidites in the Triassic Bantu Formation. Through the study on the laser Raman molecular microprobe of organic inclusions in the process of metallogenesis, it is considered that: (1) the organic matter undergoes thermal degradation in the process of metallogenesis, and the amount of hydrocarbon degradation product can measure the degree of heat; (2) Machine components and CO2 / CH4 parameters can be used to study the hydrothermal geochemical environment.