|
|||||
|
|
| 湖北宜昌白果园陡山沱组磷块岩地球化学特征研究 | |
| 引用本文： | 密文天.湖北宜昌白果园陡山沱组磷块岩地球化学特征研究[J].地质与勘探,2011,47(6):982-993. |
| 作者姓名： | 密文天 |
| 作者单位： | 1. 成都理工大学博士后科研流动站,四川成都,610059 2. 重庆地质矿产研究院,重庆,400042 3. 中国石油化工股份有限公司西北油田分公司,新疆乌鲁木齐,830011 |
| 基金项目： | 教育部高等学校博士点基金“寒武系牛蹄塘组热水沉积中的微生物群的研究冶(编号:20095122110013)资助 |
| 摘 要： | 湖北宜昌地区白果园含磷岩系位于黄陵背斜西北部，属于宜昌磷矿的一部分；磷块岩形成于震旦纪陡山沱期大海侵时期，其富磷层位于陡山沱组樟村坪段。对白果园剖面进行地球化学方面研究，得出以下认识：（1）白果园磷块岩富集层主要为以P3O5与CaO构成的磷酸盐矿物、以CaO、CO2为特征的碳酸盐矿物和A12O3与SiO，构成的粘土矿物... |
| 关 键 词： | 震旦系 陡山沱组磷块岩成因 地球化学特征湖北宜昌 |
| 收稿时间： | 3/8/2011 12:00:00 AM |
| 修稿时间： | 2011/7/25 0:00:00 |
Geochemical Characteristics of Phosphorites in the Doushantuo Formation at Baiguoyuan, Yichang, Hubei Province |
|
| MI Wen-tian.Geochemical Characteristics of Phosphorites in the Doushantuo Formation at Baiguoyuan, Yichang, Hubei Province[J].Geology and Prospecting,2011,47(6):982-993. | |
| Authors: | MI Wen-tian |
| Institution: | Chengdu University of Technology, Chengdu ,Sichuan |
| Abstract: | Phosphatic series of Baiguoyuan in Yichang is located in the northwest of the Huangling anticline, which is a part of Yichang phosphate. The phosphorite was formed in the transgression of the Sinian Doushantuo period. The enrichment phosphorus lies in the Zhang cun-ping layer of Doushantuo Formation. From geochemical study on the profile of Baiguoyuan, we obtained the following conclusions:(1).The rich layer of phosphorite in Baiguoyuan is mainly composed of phosphate mineral, which is constituted by P2O5 a... |
| Keywords: | Sinian Doushantuo Formation genesis of phosphorite geochemical characteristics Yichang Hubei |
| 本文献已被 CNKI 万方数据 等数据库收录！ | |
| 点击此处可从《地质与勘探》浏览原始摘要信息 | |
| 点击此处可从《地质与勘探》下载免费的PDF全文 | |