Please wait a minute...
E-mail Alert Rss
 
物探与化探  1990, Vol. 14 Issue (6): 432-437    
  论文 本期目录 | 过刊浏览 | 高级检索 |
酸性火山成因的粘土岩在自然伽玛测井曲线上的显示及其在事件地层学上的应用
冯宝华
中国地质科学院矿床研究所
THE MANIFESTATION OF CLAY ROCK OF ACIDIC VOLCANIC ORIGIN ON NATURAL GAMMA-RAY LOGGING CURVE AND ITS APPLICATION TO EVENT STRATIGRAPHY
Feng Baohua
Institute of Mineral Deposits, Chinese Academy of Geological Sciences
全文: PDF(503 KB)  
输出: BibTeX | EndNote (RIS)      
摘要 

本文将自然伽玛测井资料试用在火山事件粘土岩层的研究中。根据现代自然伽玛测井技术水平和研究对象中放射性元素含量说明应用的可能性,分析沉积岩的物源与放射性元素含量的关系。非正常沉积岩中以酸性火山碎屑及其水解产物(粘土)含放射性元素较高。例举三种产状的火山成因粘土岩论证用自然伽玛测井资料寻找和研究火山事件粘土岩层的必要和优越性。笔者用此法发现川南筠连地区二叠三叠系地层之间存在界线粘土岩层。最后对自然伽玛测井技术发展远景提出设想。

服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
Abstract

This paper attempts to use natural gamma-ray logging data in the research of clay strata formed by volcanic events. The feasibility of this application is illustrated in the light of present technical level of natural gamma log-ging and contents of radiogenic elements in studied objects; the relations of material sources of sedimentary rocks with contents of radiogenic elements are analysed. Of all the uncommon sedimentary rocks, acidic volcaniolastic material and its hydrolyzates(clay)contain rather abundant radiogenic elements. With three types of volcanogenic clay rocks as examples, the natural gamma logging data are proved to be essential for finding and studying clay strata formed by volcanic events. Using this method, the author has found that there exists in Junlian area of southern Sichuan a layer of clay rocks between Permian and Triassic strata, which serves as the boundary of these two systems. Finally, some opinions are put forward concerning the ?future development of the natural gamma-ray logging technique.

     出版日期: 1990-12-24
引用本文:   
冯宝华. 酸性火山成因的粘土岩在自然伽玛测井曲线上的显示及其在事件地层学上的应用[J]. 物探与化探, 1990, 14(6): 432-437.
Feng Baohua. THE MANIFESTATION OF CLAY ROCK OF ACIDIC VOLCANIC ORIGIN ON NATURAL GAMMA-RAY LOGGING CURVE AND ITS APPLICATION TO EVENT STRATIGRAPHY. Geophysical and Geochemical Exploration, 1990, 14(6): 432-437.
链接本文:  
https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y1990/V14/I6/432

[1] 黄隆垄:放射性测井原理,1985年,石汕工业出版社。
[2] 叶庆生、李崇儒:自然伽玛测井在煤田勘探中的应用与探讨,物探与化探,1980,3。
[3] 谭廷栋:测井识别碎屑岩沉积相,物探与化探,1988,5。
[4] 魏魁生等:自然伽玛测井相研究,测井技术,1988, 5。
[5] 冯宝华:我国北方石炭二叠纪火山灰沉积水解改造而成的高岭岩,沉积学报,1989,1。
[6] 周义平等:中国西南地区二叠世含煤岩系中粘土岩夹砰研究的新进展,云南地质,1988,3。
[7] 佟英梅:利用自然伽玛测井曲线研究煤层结构及其沉积环境,测井技术,1983,4。
[8] 吴瑞棠、杨菊芬:全国事件地层学术讨论会论文摘要集,1988年。
[9] Lei Zhou and Frand T. Kyte, "The Permian Triassic boundary event: a gcochemical study of three Chinese sections"Earth and Pianctarv Science Letters. 90(1988)。

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
京ICP备05055290号-3
版权所有 © 2021《物探与化探》编辑部
通讯地址:北京市学院路29号航遥中心 邮编:100083
电话:010-62060192;62060193 E-mail:whtbjb@sina.com