Ore Metals In Magma-Volatile Systems

请求继续我的研究在实验，现场， 岩浆热液过程的理论研究。 中心研究了元素Cu、Mo、W与一些 扩展到Zn，Nb，Ta，而不是检查广泛的 以肤浅的方式。 1)审查这一限制 一套深入的元素将使人们有可能模拟 更完整的感兴趣的过程; 2）这些过程的一些子集 元素在大多数岩浆中以异常的浓度存在， 热液矿床; 3）早期数据（Tacker和 Canadian，1987; Canadian，1989 b; Canadian和Bouton，1990， 附录）已证明在回答基本问题方面卓有成效 成矿作用

Request to continue my research in the experimental, field, and theoretical investigations of magmatic-hydrothermal processes. The center research on the elemental Cu, Mo, W with some extensions to Zn, Nb, Ta rather than examine a wide range of elements in a superficial manner. 1) examining this restricted suite of elements in depth will make it possible to model the processes of interest more completely; 2) some subset of these elements is present in anomalous concentrations in most magmatic- hydrothermal mineral deposits; and 3) early data (Tacker and Candela, 1987; Candela 1989b; Candela and Bouton, 1990 and appendix) have proven fruitful in answering fundamental questions in ore genesis