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地质科学  1995, Vol. Issue (4): 401-413    DOI:
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碳酸盐岩成岩研究的新方法:成岩综合柱状图
张秀莲
北京大学 北京 100871
A NEW METHOD IN THE STUDY OF CARBONATITE DIAGENESIS-COMPOSITE COLUMN OF DIAGENESIS
Zhang Xiulian
Peking University, Bening 100871
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摘要 主要介绍了成岩段、成岩环境综合柱状图的提出背景、完善过程及其重要的理论实践意义。成岩段的提出解决了成岩柱的绘制问题,从而成岩环境综合柱状图得以产生,亦从而使因该种基础图件无法绘出而使成岩研究裹足不前的状况得以改观。
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张秀莲
关键词成岩环境   成岩相   成岩标志   成岩段   成岩环境综合柱状图     
Abstract: The main aim of this article is to discuss the diagenetic environment, diageneticTactes, diagenetic mark, diagenetic sections and the concept of the diagelletic columns.And the advanced background of diagenetic section, composite column of diageneticenvironment, the process of perfection and its important theoretical and practicalsignificance are also introduced.The different diagenetic assemblages can be born in the same diagenetic environment because of the different original carbonatite. But in particular rock-stratigraphicunit, they may share the basically same diagenetic characteristics, and these stratigraphic units are called diagenetic sections.Practically, the diagenetic sections can be divided into two kinds:the singlediagenetic section (the compaction diagenetic section,dissolution diagenetic section,for example), and the double diagenetic section (recrystallization-pressure solutiondiagenetic section, recrystallization-dolomitizatio diagenetic section, for example),and then, we can further specify them according to the diagenetic marks.The advancement of the diagenetic section, division of diagenetic section anddesign of diagenetic legend make it possible to chart the diagenetic columna whichare analogous to the Lithologic columns. So, the abstract diagenesis can now be easilytransformed into practice diagenetic columns through the bridge of diagenetic sections.The advance of the diagenetic section and the use of the diagenetic columnswill bring a new method for study of diagenesis.
Key wordsDiagenetic environment   Diagenetic factes   Diageuetic mark   Diagenetic section   Composite columll of diagenetic environment   
收稿日期: 1993-12-20;
引用本文:   
张秀莲. 1995, 碳酸盐岩成岩研究的新方法:成岩综合柱状图. 地质科学, (4): 401-413.
Zhang Xiulian. A NEW METHOD IN THE STUDY OF CARBONATITE DIAGENESIS-COMPOSITE COLUMN OF DIAGENESIS[J]. Chinese Journal of Geology, 1995, (4): 401-413.
 
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[1] 刘江斌 任战利 李文厚 胡桂林 . 鄂尔多斯盆地旬邑地区三叠系延长组长9储层成岩作用及成岩相[J]. 地质科学, 2017, 52(2): 440-452.
[2] 李渭, 白薷, 马瑶, 李兆雨. 鄂尔多斯盆地陕北地区长7砂岩储层成岩相特征研究[J]. 地质科学, 2015, 50(3): 955-969.
[3] 张善文, 袁静, 隋风贵, 陈鑫. 东营凹陷北部沙河街组四段深部储层多重成岩环境及演化模式[J]. 地质科学, 2008, (3): 576-587,602.
[4] 张云峰, 王清晨. 济阳坳陷奥陶系碳酸盐岩及缝洞充填方解石C、O同位素特征及其意义[J]. 地质科学, 2007, (3): 570-578.
[5] 赵玉琛. 宁芜地区中生代火山岩地层划分及其特征[J]. 地质科学, 1990, (3): 243-258.
 
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