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织金新华磷矿碎屑磷灰石的矿物成分研究
刘世荣; 胡瑞忠; 周国富; 龚国洪; 金志升; 郑文勤
2008
Source Publication矿物学报
Volume28Issue:3Pages:244-250
metadata_24其它
Abstract织金新华磷矿是我国扬子地台西南缘早寒武世重要的海相沉积磷矿床。长期以来,织金磷块岩磷酸盐矿物成分被认为是碳氟磷灰石或低碳氟磷灰石,有学者认为,产于沉积岩中的磷灰石基本上都属于碳氟磷灰石。本文利用电子探针的微区成分定量分析技术和X射线衍射分析技术,确认织金磷矿碎屑磷灰石为氟磷灰石。
Keyword新华磷矿
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Indexed ByCSCD
Language中文
CSCD IDCSCD:3384789
Citation statistics
Cited Times:13[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/508
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
矿床地球化学国家重点实验室
Recommended Citation
GB/T 7714
刘世荣,胡瑞忠,周国富,等. 织金新华磷矿碎屑磷灰石的矿物成分研究[J]. 矿物学报,2008,28(3):244-250.
APA 刘世荣,胡瑞忠,周国富,龚国洪,金志升,&郑文勤.(2008).织金新华磷矿碎屑磷灰石的矿物成分研究.矿物学报,28(3),244-250.
MLA 刘世荣,et al."织金新华磷矿碎屑磷灰石的矿物成分研究".矿物学报 28.3(2008):244-250.
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