引言以碳酸盐岩为主岩的浸染状卡林金矿床地质学、矿物学、流体包裹体、地球化学和稳定同位素的综合研究表明,矿化作用(可能还有后来的大量氧化作用)同浅层雨水热液系统的活动有关,热液系统的驱动力可能是下伏的第三纪火成活动。科特兹矿床早期的研究指出,尽管在年龄、构造背景和地球化学的细节上有差异,但其矿化作用基本上与卡林矿床相同。这两个矿床广泛的地球化学相似性表明,内华达州以碳酸盐岩为主岩的浸染状金矿床可能是在各种场合下反复进行的一系列作用的结果。对卡林和科特兹矿床的深入研究能作为建立概念模式的基础。本文还介绍了内华达州其 INTRODUCTION A comprehensive study of geology, mineralogy, fluid inclusions, geochemistry and stable isotopes of carbonate rock-dominated disseminated Carlin gold deposits shows that mineralization (and possibly subsequent massive oxidation) Hydrothermal system of shallow rain hydrothermal activities related to hydrothermal system may be the driving force of the next Tertiary Commission into the activities. Earlier studies of the Cotz Deposit indicate that although mineralization differs in age, tectonic setting and geochemistry, the mineralization is essentially the same as the Carlin deposit. The extensive geochemical similarity between these two deposits suggests that disseminated gold deposits characterized by carbonate rocks in Nevada may be the result of a series of repeated actions on a variety of occasions. An in-depth study of Carlin and Cotz deposits can serve as a basis for establishing conceptual models. This article also describes it in Nevada