关于湘鄂边境区内所分布的铅锌矿床,以往到过该区的地质工作者都知道是属于低温热液或超低温热液充填和交代型的矿床。近年来,由于国家经济建设大力发展的需要,地质工作者又复陆续地前往该区内,在前人研究的基础上进行系统的地质研究工作。 With regard to the lead-zinc deposits distributed in the border area of ​​Hunan, Hubei and Hubei Provinces, the geologic workers who visited the area in the past knew that they belonged to low-temperature hydrothermal or ultra-low temperature hydrothermal filling and dating deposits. In recent years, due to the needs of the vigorous development of the country’s economic construction, geologists have been going to the area one after another in succession and conducted systematic geological research based on previous studies.