论文部分内容阅读
该矿床是近年来探明的一个大型金矿床。由于埋藏浅,可以露天开采,伴生Ag、Pb、Zn等多种有益元素,具有综合利用价值以及在成矿上颇具特征,因而日益引起人们的关注。本文旨在综合矿床地质特征的基础上,结合硫化物矿物同位素组成的研究,试图对矿床成因进行初步探讨,以便确定找矿方向。众所周知,对矿物中稳定同位素研究在解决矿床一些基本问额上起着极为重要的作用,它不仅可以确定成矿时代,而且还能提供矿质来源及成矿作用的物理化学条件等与矿床成因有关的重要信息。
This deposit is a large gold deposit proved in recent years. Due to the shallow burial, open-pit mining, associated beneficial elements such as Ag, Pb, Zn and so on, with the comprehensive utilization value and the characteristic of mineralization, it has drawn more and more attention. Based on the geological characteristics of the deposit and the study of the isotopic composition of sulfide minerals, this paper tries to discuss the genesis of the deposit in order to determine the prospecting direction. It is well-known that the study of stable isotopes in minerals plays an extremely important role in solving some basic quarry deposits. It not only determines the mineralization age, but also provides the mineralization and the mineralization of the physical and chemical conditions related to the genesis of the deposit Important information.