机译:中部斑岩铜矿在东部的Tethyan orenogenic带:使用SR,O同位素和SR / Y比率来预测矿石相关和矿石磁带的来源
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
Geological Survey of Iran;
Department of Geology University of Leicester;
Geological Survey of Iran;
Geological Survey of Iran;
Geological Survey of Iran;
Sr; O isotopes; Sr/Y ratios; Deep crustal hot zone model; Eastern Tethyan belt; Urumieh-Dokhtar magmatic arc;
机译:中部斑岩铜矿在东部的Tethyan orenogenic带:使用SR,O同位素和SR / Y比率来预测矿石相关和矿石磁带的来源
机译:中国东北部中亚造山带东部多宝山铜矿床的成矿作用及与矿石有关的斑岩构造背景
机译:来自隋井牙铜矿床,新疆,新泽西新疆的小井子斑岩铜矿矿床的地球化学和SR-ND-HF同位素:对岩石,构造和矿化的影响
机译:中亚造山带斑岩铜矿床与花岗岩岩浆的氧化条件
机译:利用地球化学和锶同位素比值(87 Sr / 86Sr)确定Picher矿区的水混合和水源。
机译:为什么大型斑岩铜矿床会形成高Sr / Y岩浆?
机译:东秦岭 - 大别造山带沙坪沟斑岩钼矿床含矿正长岩的年代学,地球化学和Hf-sr-Nd同位素