GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
个旧锰结核矿床地质地球化学与成因初步研究
张宝贵; 张忠; 胡静; 符亚洲; 刘世荣
Corresponding Author张宝贵
2007
Source Publication矿物学报
ISSN1000-4734
Volume27Issue:4Pages:366-371
metadata_24其它
Abstract个旧锰结核矿床产在锡石-多金属硫化物矿田顶部的第四系砂锡矿之中.从矿床地质产状、化学组成、微量元素、稀土元素、矿物组合等方面进行了讨论,认为个旧锰结核属于异地海相成因,后经搬运沉积在第四系砂锡矿之中;与中太平洋海山CAD19锰结核的物质组成和微量元素进行对比,表明个旧和CAD19锰结核有相类似的稀土模式,相对富集轻稀土,并出现明显的Eu负异常和Ce的正异常.
metadata_83矿床地球化学国家重点实验室
Keyword锰结核矿床
Subject Area主题分类subject.discipline
Funding Organization国家自然科学基金项目(批准号:40372047)
Indexed ByCSCD
Language中文
CSCD IDCSCD:3057098
Citation statistics
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/689
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Corresponding Author张宝贵
Recommended Citation
GB/T 7714
张宝贵,张忠,胡静,等. 个旧锰结核矿床地质地球化学与成因初步研究[J]. 矿物学报,2007,27(4):366-371.
APA 张宝贵,张忠,胡静,符亚洲,&刘世荣.(2007).个旧锰结核矿床地质地球化学与成因初步研究.矿物学报,27(4),366-371.
MLA 张宝贵,et al."个旧锰结核矿床地质地球化学与成因初步研究".矿物学报 27.4(2007):366-371.
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