锆铪元素在岩浆作用中的地球化学行为浅析  

GEOCHEMICAL BEHAVIOR OF ZIRCONIUM AND HAFNIUM IN MAGMATISM

作　　者：王小钊[1,2] 杨柳晨 樊双虎[1,3] 陈淑娥[1,3] 

机构地区：[1]长安大学地球科学与资源学院,西安710054 [2]陕西省地质矿产实验研究所,西安710054 [3]西部矿产资源与地质工程教育部重点实验室,西安710054

出　　处：《陕西地质》2016年第1期67-72,共6页Geology of Shaanxi

摘　　要：锆铪是一对地球化学性质相似的元素,锆能形成独立矿物,而铪主要以类质同象形式存在。在岩浆作用过程中Zr、Hf和Zr/Hf值在基性、中性及酸性岩中的变化及变化规律是含量逐渐变大,Zr/Hf值逐渐降低。Zirconium and hafnium is a pair of elements with similar geochemical properties. Zirconium can form an independent mineral and hafnium mainly exists in isomorphism state. Their separation and variation in geological process carries abundant geologic information. Some indicative functions are involved in some changes in zirconium and hafnium contents included in basic, intermediate and acidic rocks and the ratio value of Zr/Hf, showing that when the content of Zr and Hf increases, the Zr/Hf ratio would decrease gradually in general.

关 键 词：锆铪 岩浆作用 地球化学行为 

分 类 号：P588.11[天文地球—岩石学]