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锆铪在岩浆作用中的地球化学行为
引用本文:让昊,等.锆铪在岩浆作用中的地球化学行为[J].价值工程,2014(8):319-321.
作者姓名:让昊
作者单位:[1]昆明理工大学国土资源工程学院,昆明650093 [2]长安大学地球科学与资源学院,西安710054 [3]云南大学人文学院,昆明650091
摘    要:锆铪是一对地球化学性质比较相似的元素,锆能形成独立矿物,而铪主要以类质同象形式存在,他们在地质作用中的分离携带着丰富的地质信息,本文着重讨论在岩浆作用中锆铪的地球化学行为与大地构造位置、时代、岩性、成矿阶段之间的关系,及物理化学条件对锆铪元素地球化学行为的影响。

关 键 词:锆铪  地球化学行为  岩浆作用

The Geochemical Behavior of Zirconium and Hafnium in Magmatism
RANG Hao,LIU Kai,WU Dan.The Geochemical Behavior of Zirconium and Hafnium in Magmatism[J].Value Engineering,2014(8):319-321.
Authors:RANG Hao  LIU Kai  WU Dan
Institution:1Faculty of Land and Resources Engineering, Kunming University of Science and TechnolOgy, Kunming 650093, China 2The School of Earth Science and Resources, Chang,an University,Xi'an 710054, China; 3School of Humanities, Yunnan University, Kunming 650091, China )
Abstract:Zirconium and hafnium is a pair of elements with similar geochemical properties. Zirconium can form an independent mineral, and hafnium mainly exists in the form of isomorphism. Their separation in the geological process carries abundant geologic information. This article focuses on the relationship between the geochemical behavior of zirconium and hafnium with tectonic location, age, lithology, mineralization stages in magmatism, and the influence of physical and chemical conditions on the geochemical behavior of zirconium and hafnium elements.
Keywords:zirconium and hafnium  geochemical behavior  magmatism
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