"Exploring the interrelationships between subvolcanic and volcanic architecture, magmatism, tectonics and VMS deposit genesis"

“探索地下火山和火山结构、岩浆作用、构造和 VMS 沉积成因之间的相互关系”

• 批准号: 105663-2012
• 负责人: Gibson, Harold
• 金额: $ 2.77万
• 依托单位: Laurentian University of Sudbury
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2012
• 资助国家: 加拿大
• 起止时间: 2012-01-01 至 2013-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=507817
• 关键词: Exploring; interrelationships; between; subvolcanic; volcanic

Volcanogenic massive sulphide (VMS) ore bodies are rare and incredibly valuable accumulations of sulphide minerals from which important industrial and precious metals such as zinc, copper, silver and gold are produced. They form during submarine volcanism where hot (>300 C), evolved, metal- and sulphur-bearing seawater, perhaps with a component derived from magmas (magmatic fluid), is discharged onto the seafloor within ancient and modern volcanoes and, due to rapid cooling, deposited sulphide minerals at, and immediately below the seafloor.

火山块状硫化物 (VMS) 矿体是稀有且极具价值的硫化物矿物堆积物，可生产锌、铜、银和金等重要工业金属和贵金属。它们是在海底火山活动期间形成的，其中热（> 300 C）、演化的、含金属和硫的海水，可能含有源自岩浆（岩浆液）的成分，被排放到古代和现代火山内的海底，并且由于快速冷却后，硫化物矿物沉积在海底及其正下方。