• 责任者：Zhang Yunguo (China Geological Survey of Non-Ferrous Metal Resources ; Beijing 100012 ; China) ; Zhou Chaoxian
• 刊名：Advances in Earth Science
• 出版年：2011
• 卷期：26(11)
• 关键词：斑岩铜矿床 ; porphyry copper deposit
• 页码：p.1173-1190
• 图表：5 illus., 157 refs.
• 分类号：1001
• 出版序号：20122450
• issnNo：ISSN1001-8166
• isbnNo：CN62-1091/P

Porphyry copper deposit as the largest source of Cu is one of the most important deposits in the world. Porphyry copper deposit not only occured in Circum-Pacific ore-forming region, but also occured in Tethys ore-forming region and Middle-Asian (Paleo-Asian Oceanic) ore-forming region. The mineralization materials derived from the deep. Porphyry forms through four stages:
“Oceanic Crust-Mantle Lava Flow”, “Original Magma”, “Shallow Ore Magma”, “Crystallization of Magma-Minerali-zation”. The proposed genesis models which are commonly accepted, up to now, include the classical model, the system model and the model of polyphasal overprinting events.