机译:宾厄姆峡谷斑岩铜钼金矿床。三,岩浆蒸汽扩展对铜金矿的分区沉积
ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;
ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;
Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305;
ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;
ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland;
ETH Zurich, Department of Earth Sciences, Clausiusstrasse 25, 8092 Zurich, Switzerland, and Faculty of Mathematics and Natural Sciences, University of Zurich;
机译:宾厄姆峡谷斑岩铜钼金矿床。三,岩浆蒸汽扩展对铜金矿的分区沉积
机译:宾厄姆峡谷斑岩铜钼金矿床。二。压力驱动岩石延伸形成的静脉几何形状和矿石壳形成
机译:宾厄姆峡谷斑岩铜钼金矿床。二。压力驱动岩石延伸形成的静脉几何形状和矿石壳形成
机译:岩浆加热系统中曲线过渡的斑岩过渡:Valea Morii铜金矿床,Apuseni MTS,罗马尼亚
机译:犹他州宾厄姆峡谷的岩浆热液和铜金矿形成。
机译:评估卟啉矿石系统的铊元素系统和同位素比变异:宾厄姆峡谷区的案例研究