苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

易发成; 田煦; 李虎杰; 郑自立

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苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

易发成, 田煦, 李虎杰, 郑自立

文章导航 > 沉积学报 > 1996 > 14(4): 141-147

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

引用本文:

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

Yi Facheng, Tian Xu, Li Hujie, Zhen Zili. The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces[J]. Acta Sedimentologica Sinica, 1996, 14(4): 141-147.

Citation:

Yi Facheng, Tian Xu, Li Hujie, Zhen Zili. The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces[J]. Acta Sedimentologica Sinica, 1996, 14(4): 141-147.

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

引用本文:

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

Yi Facheng, Tian Xu, Li Hujie, Zhen Zili. The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces[J]. Acta Sedimentologica Sinica, 1996, 14(4): 141-147.

Citation:

苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

西南工学院非金属矿研究所绵阳 621002

详细信息

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学

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文章访问数: 536
HTML全文浏览量: 15
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The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

Southwest Institute of Technology, Mianyang 621002

摘要

摘要: 本文对苏皖沉积型凹凸棒石粘土矿床形成时的沉积环境特征、水介质的ｐＨ值、氧化还原条件、温度及盐度进行了讨论。研究表明凹凸棒石粘土矿床形成于碱性、还原、低盐度的浅水湖相环境。与火山作用有关的热水溶液参与了成矿作用。
- 凹凸棒石粘土 /
- 沉积环境 /
- 介质条件
Abstract: The Sedimentary attapulgite clay deposit on the boder of Jiangsu and Anhui Provinces is an important producing area of attapulgite clay in China. Ore-bearing Series is a set of sedimentary clastic rocks of shallow lake. The sedimentary medium features are as follows: 1) Various attapulgite clays have different pH values, all of them are formed in an alkalic condition; 2) According to the features and Ceanom calculated values of variant clays, the attapulgite clays are formed in a reducing condition, and part of montmorillonite clay is formed in a weak oxido-condition; 3) On the basis of stable isotopic compositions of opal and dolomite, opal-forming temperature is 71℃ 81℃ and dolomite-forming temperature is 29℃ 74℃.These features with other geochemical characteristics infered that the forming temperature of attapulgite clays is higher than the normal sedimentary temperature; 4) MgO/Al ₂O ₃ Sr/Ba Rb/K ratios of variant attapulgite clays showed that the forming salinity of dolomite attapulgite clay, siliceous attapulgite clay and attapulgite clay is higher than that of montmorillonite clay. To sum up, the study indicated that under the conditions of alkalic, reducing conditions and low salinity of water medium, attapulgite clay deposits could be formed in a shallow lacustrine basin. The hydrothermal solution being related to volcanic action is of certain significance to mineralization of attapulgite clay deposits.
- attapulgite clay /
- sedimentary environment /
- medium condition

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参考文献(1)

[1]

(1) Singer A and Galan E, Eds. Palygorskite- Sepiolite Occurrence. g enesis and uses (Developments in sedimentary37). Elsevier Scientific Publishing Company, 1984.

(2) Weaver C, Clays, M uds, and shales. Elsevier Scientific Publishing Company, 1990.

(3) Millot G. Geolog y of clays. Spring er-verlay, New York, 1970.

(4) 方邺森, 许冀泉, 李立文. 苏皖地区凹凸棒粘土. 南京大学学报 (自然科学版 ), 1990, (1), 15-23.

(5) Yi Facheng, Tian Xu and Yuan Jianqi, et al. The geological characteristics and geneses of attapulgite clay depositson Jiangsu- Anhui bo rder. In :clay Minerals, Their Natural Resources and Uses. Proceedings of workshop WB-1, The 29 th Inter. Geol.Cong ress. Nag oya, Japan, 1992.

(6) 孙永传, 李蕙生. 碎屑沉积相和沉积环境. 地质出版社, 1986.

(7) 刘宝君, 曾永孚. 岩相古地理基础和工作方法. 地质出版社, 1985.

( 8) Church T M and V elde B. Geochemistry and Origin of a deep- sea pacific palygorskite deposit. Chemical Geolog y, 1979, (25): 31-39.

(9) V elde B, Clay minerals. A Physic-chemical explanation of their occurrence (Developments in sedimentary ). Else-vier Scientific Publishing Company ).

(10) 易发成, 李虎杰, 田煦, 郑自立. 苏皖地区凹凸棒石粘土矿床稳定同位素特征及其地质意义. 矿物学报, 1995,15 (2): 242-247.

(11) 张士三, 沉积岩镁铝含量比及其应用. 矿物岩石地球化学通报, 1988, (2): 112-113.

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文章访问数: 536
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苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

西南工学院非金属矿研究所绵阳 621002

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学

收稿日期: 1996-01-01

关键词:

凹凸棒石粘土 /

沉积环境 /

介质条件

摘要: 本文对苏皖沉积型凹凸棒石粘土矿床形成时的沉积环境特征、水介质的ｐＨ值、氧化还原条件、温度及盐度进行了讨论。研究表明凹凸棒石粘土矿床形成于碱性、还原、低盐度的浅水湖相环境。与火山作用有关的热水溶液参与了成矿作用。

English Abstract

The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

Southwest Institute of Technology, Mianyang 621002

Received Date: 1996-01-01

Keywords:

Abstract: The Sedimentary attapulgite clay deposit on the boder of Jiangsu and Anhui Provinces is an important producing area of attapulgite clay in China. Ore-bearing Series is a set of sedimentary clastic rocks of shallow lake. The sedimentary medium features are as follows: 1) Various attapulgite clays have different pH values, all of them are formed in an alkalic condition; 2) According to the features and Ceanom calculated values of variant clays, the attapulgite clays are formed in a reducing condition, and part of montmorillonite clay is formed in a weak oxido-condition; 3) On the basis of stable isotopic compositions of opal and dolomite, opal-forming temperature is 71℃ 81℃ and dolomite-forming temperature is 29℃ 74℃.These features with other geochemical characteristics infered that the forming temperature of attapulgite clays is higher than the normal sedimentary temperature; 4) MgO/Al ₂O ₃ Sr/Ba Rb/K ratios of variant attapulgite clays showed that the forming salinity of dolomite attapulgite clay, siliceous attapulgite clay and attapulgite clay is higher than that of montmorillonite clay. To sum up, the study indicated that under the conditions of alkalic, reducing conditions and low salinity of water medium, attapulgite clay deposits could be formed in a shallow lacustrine basin. The hydrothermal solution being related to volcanic action is of certain significance to mineralization of attapulgite clay deposits.

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

引用本文:

易发成, 田煦, 李虎杰, 郑自立. 苏皖沉积型凹凸棒石粘土矿床沉积环境探讨[J]. 沉积学报, 1996, 14(4): 141-147.

Yi Facheng, Tian Xu, Li Hujie, Zhen Zili. The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces[J]. Acta Sedimentologica Sinica, 1996, 14(4): 141-147.

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苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学

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The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

计量

目录

苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

西南工学院非金属矿研究所绵阳 621002

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学

English Abstract

The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

Southwest Institute of Technology, Mianyang 621002

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苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

作者简介: 易发成,男,36岁,副教授,(博士,),矿床学

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The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

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出版历程

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苏皖沉积型凹凸棒石粘土矿床沉积环境探讨

西南工学院非金属矿研究所 绵阳 621002

作者简介: 易发成,男,36岁,副教授,(博士,),矿床学

English Abstract

The Sedimentary Environment of Attapulgite Clay Deposits on the Border of Jiangsu and Anhui Provinces

Southwest Institute of Technology, Mianyang 621002

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学

西南工学院非金属矿研究所绵阳 621002

作者简介:
易发成,男,36岁,副教授,(博士,),矿床学