Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

ZHAO Jun qing; JI You liang; ZHANG Shi qi; XIA Bin

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Article Navigation > Acta Sedimentologica Sinica > 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.

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

Received Date: 2003-02-10
Rev Recd Date: 2003-04-15
Publish Date: 2004-03-10

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

References

[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]
[9]	胡受权,郭文平,杨凤根,等.试论控制断陷湖盆陆相层序发育的影响因素.沉积学报,2001,19(2):256～262[Hu Shouquan, Guo Wemping, Yang Fenggen, et al. Sdudy on influential facters of terrigenous sequence formation and development in fault-depressed lacustrine basin. Acta Sedimentologica Sinica, 2001,19(2):256～262]
[10]	Harder H. Boron content of sediment as a tool in facies analysis. Sedimentary Geology, 1970, 4(1):153～175
[11]	Couch E L. Calculation of paleosalinities from boron and caly mineral data. AAPG Bulletin, 1971, 5(10): 1829～1837
[12]	Potter P E, Shimp N P, Witters J. Trace element in marine and fresh-water argillaceoussediment. Geochimica et Cosmochimica Acta, 1963, 27: 669～694
[13]	龙天才.关于应用硼判别沉积环境的有效性问题.见:中国地质学会第四纪冰川与第四纪地质专业委员会,江苏省地质学会合编.第四纪冰川与第四纪地质论文集(5).北京:地质出版社, 1988. 233～235[Long Tiancai. Effective problemon sedimentary enviroment distinguishing by applying boron. In: The Committee of QuaternaryGlacial and Quaternary Geology, Geological Society of China, Geological Society of Jiangsu Province. Papers Collection of Quaternary Glacial and Quternary Geology Symposium(5). Beijing: Geological Publishing House, 1988. 233～235]
[14]	周仰康,何锦文,王子玉.硼作为古盐度指标的应用.沉积学和有机地球化学学术会议论文选集.北京:科学出版社, 1984. 55～57[Zhou Yangkang, He Jinwen, Wang Ziyu. Application of boronon paleosalinity indication. Papers Collection of Sedimentary and Organic Geochemistry Symposium. Beijing: Science Press, 1984.55～57]
[15]	Walker C T, Price N B. Departure curves for computingpaleosalinity from boron In-illites and shales. AAPG Bulletin, 1963, 47(5): 833～841
[16]	Adams T D, Haynes J R, Walker C T. Boron in Holocene illites of the dovey estuarywales and its relationship to paleosalinity in cycleothems. Sedimentology, 1965,4: 189～195
[17]	Nelson B. Sedimentary phosphate method for estimating paleosalinites. Science, 1967,158(3803): 917～920

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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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

Received Date: 2003-02-10

Rev Recd Date: 2003-04-15

Publish Date: 2004-03-10

Key words:

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.

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Reference (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]
[9]	胡受权,郭文平,杨凤根,等.试论控制断陷湖盆陆相层序发育的影响因素.沉积学报,2001,19(2):256～262[Hu Shouquan, Guo Wemping, Yang Fenggen, et al. Sdudy on influential facters of terrigenous sequence formation and development in fault-depressed lacustrine basin. Acta Sedimentologica Sinica, 2001,19(2):256～262]
[10]	Harder H. Boron content of sediment as a tool in facies analysis. Sedimentary Geology, 1970, 4(1):153～175
[11]	Couch E L. Calculation of paleosalinities from boron and caly mineral data. AAPG Bulletin, 1971, 5(10): 1829～1837
[12]	Potter P E, Shimp N P, Witters J. Trace element in marine and fresh-water argillaceoussediment. Geochimica et Cosmochimica Acta, 1963, 27: 669～694
[13]	龙天才.关于应用硼判别沉积环境的有效性问题.见:中国地质学会第四纪冰川与第四纪地质专业委员会,江苏省地质学会合编.第四纪冰川与第四纪地质论文集(5).北京:地质出版社, 1988. 233～235[Long Tiancai. Effective problemon sedimentary enviroment distinguishing by applying boron. In: The Committee of QuaternaryGlacial and Quaternary Geology, Geological Society of China, Geological Society of Jiangsu Province. Papers Collection of Quaternary Glacial and Quternary Geology Symposium(5). Beijing: Geological Publishing House, 1988. 233～235]
[14]	周仰康,何锦文,王子玉.硼作为古盐度指标的应用.沉积学和有机地球化学学术会议论文选集.北京:科学出版社, 1984. 55～57[Zhou Yangkang, He Jinwen, Wang Ziyu. Application of boronon paleosalinity indication. Papers Collection of Sedimentary and Organic Geochemistry Symposium. Beijing: Science Press, 1984.55～57]
[15]	Walker C T, Price N B. Departure curves for computingpaleosalinity from boron In-illites and shales. AAPG Bulletin, 1963, 47(5): 833～841
[16]	Adams T D, Haynes J R, Walker C T. Boron in Holocene illites of the dovey estuarywales and its relationship to paleosalinity in cycleothems. Sedimentology, 1965,4: 189～195
[17]	Nelson B. Sedimentary phosphate method for estimating paleosalinites. Science, 1967,158(3803): 917～920

Geochemical Methods of Boundary Identification in Terrigenous High-Resolution Sequence

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