陆相高分辨率层序界面识别的地球化学方法

赵俊青; 纪友亮; 张世奇; 夏斌

陆相高分辨率层序界面识别的地球化学方法

1.
中国科学院广州地球化学所广州 510640;
2.
同济大学海洋与地球科学学院山东东营 257061;
3.
石油大学地球资源与信息学院上海 200092

基金项目: 国家重点基础研究发展规划项目:渤海湾盆地中生代地层剥蚀量恢复及中、新生代盆地叠合关系探讨(G1999043304)专题资助;国家十五科技攻关项目:济阳坳陷下第三系陷蔽油气藏形成机理研究(2001BA60509)部分成果

详细信息

作者简介:
赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

中图分类号: P593

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Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640;
2.
Institute of Earth and Ocean Science, Tongji University, Shanghai 200092;
3.
Institute of Earth Resource and Information, University of Petroleum China, Dongying, Shandong 257061

摘要

摘要: 粘土矿物、微量元素普遍存在于各种类型的沉积物和沉积岩中,它们对环境的变化敏感,同时它们的沉积分异、组合特征、矿物成分及其含量都从不同的角度记录了形成过程中各种环境因素的变化。这些对恢复古环境,研究陆相湖盆水深变化具有重要的指示意义。通过对东营凹陷胜北断层下降盘沙三段 -沙四上段各层序内部高分辨率层序地层单元中岩石地球化学标型参数的研究发现,在一个高分辨率层序地层单元形成过程中,在古气候驱动下的湖平面变化旋回中,沉积岩中的矿物成分 (主要指粘土矿物和胶结物 )、化学成分 (微量元素 )等皆发生周期性变化。
- 粘土矿物 /
- 微量元素 /
- 胶结物 /
- 古盐度 /
- 高分辨率层序地层 /
- 胜北断层下降盘 /
- 东营凹陷
Abstract: Clay minerals and trace elements are disttibuted in different types of sand deposits and sedimentaryrocks. They are sensitive to environmental changes. The characteristics of clay minerals such as sedimentary differentiation, composition and assemblage, contents has recorded the information of environmental change during the processes of clay mineral formation. These information will help to reconstruct paleoenvironment with huge significance in the research of water depth change.By studing lithologic geochemical parameters of high resolution sequence units in differentsequences of the third memberand the fourth upper member of Shahejie formation in Shengbei fault's downwall side of Dongying depression,it has been found in pace of cyclicity of water depth controlledby paleoclimate during the formation period of high resolution sequence units,mineral composition(clay mienral and cement) of sedimentaryrocks,chemical constituents(trace element) would be cyclically changed.
- clayminerals /
- trace element /
- cement /
- paleosalinity /
- high resolution sequence /
- Shengbei fault's downwall side /
- Dongying depression

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参考文献(17)

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陆相高分辨率层序界面识别的地球化学方法

作者简介:
赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

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Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

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目录

陆相高分辨率层序界面识别的地球化学方法

1. 中国科学院广州地球化学所广州 510640;

2. 同济大学海洋与地球科学学院山东东营 257061;

3. 石油大学地球资源与信息学院上海 200092

作者简介:
赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

English Abstract

Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640;

2. Institute of Earth and Ocean Science, Tongji University, Shanghai 200092;

3. Institute of Earth Resource and Information, University of Petroleum China, Dongying, Shandong 257061

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陆相高分辨率层序界面识别的地球化学方法

作者简介: 赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

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Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

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出版历程

目录

陆相高分辨率层序界面识别的地球化学方法

1. 中国科学院广州地球化学所 广州 510640; 2. 同济大学海洋与地球科学学院 山东东营 257061; 3. 石油大学地球资源与信息学院 上海 200092

作者简介: 赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

English Abstract

Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640; 2. Institute of Earth and Ocean Science, Tongji University, Shanghai 200092; 3. Institute of Earth Resource and Information, University of Petroleum China, Dongying, Shandong 257061

全文HTML

目录

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期刊在线

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作者简介:
赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

1. 中国科学院广州地球化学所广州 510640;

2. 同济大学海洋与地球科学学院山东东营 257061;

3. 石油大学地球资源与信息学院上海 200092

作者简介:
赵俊青,男,1974年出生,博士研究生,层序地层学,沉积学及石油地质学

1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640;

2. Institute of Earth and Ocean Science, Tongji University, Shanghai 200092;

3. Institute of Earth Resource and Information, University of Petroleum China, Dongying, Shandong 257061