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皮尔斯元素比斜率法在研究中国东部新生代火山岩浆演化中的应用
引用本文:张毅刚,鄂莫岚.皮尔斯元素比斜率法在研究中国东部新生代火山岩浆演化中的应用[J].岩石学报,1992,8(3):284-290.
作者姓名:张毅刚  鄂莫岚
作者单位:中国科学院地质研究所,中国科学院地质研究所 北京 100029,北京 100029
基金项目:国家自然科学基金,编号48970099
摘    要:

关 键 词:皮尔斯元素比  火山岩  岩浆  演化

APPLICATION OF PEARCE'S ELEMENT RATIO TO STUDY OF MAGMA DIFFERENTIATION PROCESSES OF SOME CENOZOIC BASALTS IN EASTERN CHINA
Zhang Yigang and E Molan.APPLICATION OF PEARCE''S ELEMENT RATIO TO STUDY OF MAGMA DIFFERENTIATION PROCESSES OF SOME CENOZOIC BASALTS IN EASTERN CHINA[J].Acta Petrologica Sinica,1992,8(3):284-290.
Authors:Zhang Yigang and E Molan
Abstract:Pearce's element ratio is a ratio of variable elements to constant element which didn't participate in the geological process to be studied in petrochemistry. In this paper, the authors discuss the comagmatic properties and differentiation processes of some Cenozoic basalts in Eastern China using the method: the eomagmatic property of potassium-rich basalts in Wudalianchi-Keluo area in Heilongjiang Province, the magma differentiation processes of Cenozoic basalts in Hannuoba and. Changbaishan areas, in Hebei and Jilin Provinces, respectively. The results show that the Pearce's element ratio can be used to study the origins and differentiation processes of basalts, and can be a good supplementary method to other traditional methods and have more replete and efficient use in whole-rock analysis.
Keywords:Cenozoic basalts  Eastern China  Pearce's element ratio
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