陆相高分辨率层序界面识别的地球化学方法

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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

文章导航 > 沉积学报 > 2004 > 22(1): 79-86

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[J]. 沉积学报, 2004, 22(1): 79-86.

引用本文:

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[J]. 沉积学报, 2004, 22(1): 79-86.

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

Citation:

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

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[J]. 沉积学报, 2004, 22(1): 79-86.

引用本文:

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[J]. 沉积学报, 2004, 22(1): 79-86.

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

Citation:

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

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

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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文章访问数: 678
HTML全文浏览量: 11
PDF下载量: 705
被引次数: 0

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: 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

参考文献(17)

[1]	1] 赵永胜.云南星云湖断陷湖盆中粘土矿物组合特征与沉积环境的初步探讨.海洋与湖沼, 1993, 24(5):447～455[Zhao Yongsheng. A preliminary study on the relationship between the characteristics of clay mineral assemblage and sedimentary environments in down-faulted lake basin of Xingyun lake,Yunan province. Oceanologia et Limnologia Sinica, 1993, 24(5): 447～455]
[2]	Blaise B. Clay.Minerals assemblages from late Quaternary depositson Vancouver Island, Southwestern British Columbia,Canada. Quaternary Research, 1989, 31: 41～56
[3]	Singer A. The paleoclimatic interpretation of clay minerals in soils and weathering profiles. Earth Science Reviews, 1980, 15: 303～326
[4]	顿铁军,高约友,张丽虹.粘土矿物与油层保护.西安:西北大学出版社, 1994. 27～31[Dun Tiejun, Gao Yueyou, Zhang Lihong. Clay mineral and reservoir protection. Xi'an: Northwest University Press, 1994. 27～31]
[5]	胡受权,张永贵,颜其彬.泌阳断陷下第三系核三段上段陆相层序个体系域岩石地球化学旋回性特征.地质地球化学, 1998, 26(2): 45～52[Hu Shouquan, Zhang Yonggui,Yan Qibin Lithologic-geochemical cyclicity in every system track of terrigenous sequence in the upper member of Eh3of Biyang fault depression. Geology Geochemistry, 1998, 26(2):45～52]
[6]	胡受权, 颜其彬,张永贵.陆相层序界面的岩石地球化学标志探讨.石油学报, 1999,20(1):24～29[Hu Shouquan, Yan Qibin, ZhangYonggui. Discussion on lithologic-geochemical of features of boundary identification in terrigenous sequence. Acta Petrolei Sinica, 1999, 20(1): 24～29]
[7]	纪友亮,张世奇.层序地层序原理及层序成因机制模式.北京:地质出版社,1998.24～38[Ji Youliang, Zhang Shiqi. The theory of sequence stratigraphy and genesis mechnism mode of sequence. Beijing:Geological Publishing House, 1998. 24～38]
[8]	王随继,黄杏珍,妥进才,等.泌阳凹陷核桃园组微量元素演化特征及其古气候意义.沉积学报,1997,15(1):65～70[Wang Suiji, Huang Xiangzhen, Tuo Jincai, et al. Evolution characteristics and their paleoclimate siginificanceof trace elements in the Hetaoyuan formation,Biyang depression. Acta Sedimentologica Sinica, 1997, 15(1):65～70]
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计量

文章访问数: 678
HTML全文浏览量: 11
PDF下载量: 705
被引次数: 0

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

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

收稿日期: 2003-02-10
修回日期: 2003-04-15
刊出日期: 2004-03-10

中图分类号: P593

关键词:

高分辨率层序地层 /

胜北断层下降盘 /

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。

English Abstract

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[J]. 沉积学报, 2004, 22(1): 79-86.

引用本文:

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[J]. 沉积学报, 2004, 22(1): 79-86.

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

Citation:

ZHAO Jun qing, JI You liang, ZHANG Shi qi, XIA Bin. Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence[J]. Acta Sedimentologica Sinica, 2004, 22(1): 79-86.

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参考文献 (17)

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