您好,欢迎访问中国地质大学(武汉)机构知识库!
Image search

   Paste the image URL
黔中开阳震旦纪陡山沱组磷块岩沉积地质特征与多阶段成矿作用
张亚冠; 杜远生; 陈国勇; 刘建中; 王泽鹏
2018-09
Source Publication第十五届全国古地理学及沉积学学术会议摘要集
Pages57-58
Abstract黔中震旦纪陡山沱组磷矿层是在新元古代全球性成磷事件背景下发育的厚度大、品位高的磷块岩沉积组合。位于开阳-息烽境内的开阳磷矿以量大质优闻名,矿区勘查程度高,与湖北襄阳磷矿、云南昆阳磷矿并称"三阳开泰",磷矿石P2O5含量常常大于30%,最高可达40%,为国内外平均含磷品位最高的磷矿产区。
Keyword磷块岩 磷矿层 成矿作用 沉积地质 震旦纪陡山沱组
Language中文
URL查看原文
Conference Name第十五届全国古地理学及沉积学学术会议
Conference Place中国四川成都
Document Type会议论文
Identifierhttp://ir.cug.edu.cn/handle/2XU834YA/104481
Collection教学院系_资源学院
教学院系_地球科学学院
Affiliation1.中国地质大学(武汉)
2.贵州省地矿局
Recommended Citation
GB/T 7714
张亚冠,杜远生,陈国勇,等. 黔中开阳震旦纪陡山沱组磷块岩沉积地质特征与多阶段成矿作用[C],2018:57-58.
Files in This Item: Download All
File Name/Size DocType Version Access License
黔中开阳震旦纪陡山沱组磷块岩沉积地质特征(817KB)期刊论文出版稿开放获取CC BY-NC-SAView Download
Related Services
Usage statistics
Google Scholar
Similar articles in Google Scholar
[张亚冠]'s Articles
[杜远生]'s Articles
[陈国勇]'s Articles
Baidu academic
Similar articles in Baidu academic
[张亚冠]'s Articles
[杜远生]'s Articles
[陈国勇]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[张亚冠]'s Articles
[杜远生]'s Articles
[陈国勇]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 黔中开阳震旦纪陡山沱组磷块岩沉积地质特征与多阶段成矿作用.caj
Format: Unknown
This file does not support browsing at this time
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.