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

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

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

计量

文章访问数: 501
HTML全文浏览量: 8
PDF下载量: 304
被引次数: 0

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

HTML全文

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.

[1]	马瑞丰, 张威, 刘亮. 大连西海岸低地沉积环境特征及其对气候环境指示意义 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.051
[2]	时蕴琳, 谢远云, 康春国, 迟云平, 魏振宇, 吴鹏, 孙磊, 汪烨辉. 呼伦贝尔巴彦塔拉砂砾石剖面沉积物组成和锆石U⁃Pb年龄 . 沉积学报, 2024, 42(2): 502-520. doi: 10.14027/j.issn.1000-0550.2023.009
[3]	李泉泉, 鲍志东, 肖毓祥, 陈建阳, 李忠诚, 王振军, 刘敏昭, 李卓伦, 许西挺, 操凡. 混合沉积研究进展与展望 . 沉积学报, 2021, 39(1): 153-167. doi: 10.14027/j.issn.1000-0550.2020.140
[4]	唐玄, 刘树根, 宋金民, 李智武, 余永强, 龙翼, 昝博文, 赵聪. 四川盆地东北缘灯影组核形石特征及环境意义 . 沉积学报, 2018, 36(2): 232-242. doi: 10.14027/j.issn.1000-0550.2018.090
[5]	张旻旻, 张梅生, 李晓波, 王旖旎, 杨明, 姚路, 王成龙, 张乾. 辽西兴城地区上古生界沉积环境识别 . 沉积学报, 2015, 33(6): 1159-1169. doi: 10.14027/j.cnki.cjxb.2015.06.009
[6]	梁俊红. 辽西义县盆地义县组底部沉积相与沉积环境分析 . 沉积学报, 2007, 25(4): 545-553.
[7]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[8]	谢小平, 佟再三, 沈焕庭. 甘肃景泰红水堡晚石炭世沉积环境与沉积相分析 . 沉积学报, 2003, 21(3): 381-390.
[9]	邓寅生, 张鸿升, 许建国, 葛云. 利用灰色聚类判定沉积环境 . 沉积学报, 1998, 16(3): 156-160.
[10]	王新民, 宋春晖, 师永民, 晁吉俊, 武安斌. 青海湖现代沉积环境与沉积相特征 . 沉积学报, 1997, 15(S1): 157-162.
[11]	岳文浙, 业治铮, 姜月华. 江苏晚白垩世赤山组沉积环境 . 沉积学报, 1997, 15(S1): 1-7.
[12]	何海清. 浙江省栖霞组沉积微相、旋回、沉积环境及其演化规律 . 沉积学报, 1996, 14(S1): 75-83.
[13]	游仲华, 唐锦龙. 台湾海峡西部沉积物中粘土矿物的初步研究 . 沉积学报, 1992, 10(4): 129-136.
[14]	雒昆利, 邓宝. 陕南志留系五峡河组地层的沉积环境与笔石生活和保存的关系 . 沉积学报, 1992, 10(2): 79-87.
[15]	朱莲芳, 马宝林. 塔里木盆地阿克苏—柯坪地区寒武系—奥陶系的沉积环境 . 沉积学报, 1991, 9(2): 55-62.
[16]	王建华. 克列斯特盆地布尔季加尔阶海相磨拉石沉积作用研究 . 沉积学报, 1990, 8(2): 87-96.
[17]	王云飞, 王苏民, 冯敏. 泌阳凹陷下第三系核桃园组湖相隐藻层纹石岩的发现及其环境意义 . 沉积学报, 1990, 8(4): 49-58.
[18]	郑庆年. 再论凡口矿区中上泥盆统叠层石及其地层沉积环境意义 . 沉积学报, 1990, 8(3): 103-109.
[19]	罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系 . 沉积学报, 1989, 7(4): 77-84.
[20]	刘光华. 粘土矿物特征与沉积环境关系的初步探讨 . 沉积学报, 1987, 5(1): 48-57.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 501
HTML全文浏览量: 8
PDF下载量: 304
被引次数: 0

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.

Citation:

全文HTML

参考文献 (1)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

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

计量

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

计量

出版历程

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

计量

出版历程

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

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