松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

王璞珺; 任延广; 王东坡

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松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

王璞珺, 任延广, 王东坡

文章导航 > 沉积学报 > 1995 > 13(S1): 53-62

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

引用本文:

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

Wang Pujun, Ren Yanguang, Wang Dongpo. Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 53-62.

Citation:

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

引用本文:

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

Citation:

松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

1 长春地质学院长春 130026;
2 大庆石油管理局研究院大庆 163712

详细信息

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学

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文章访问数: 418
HTML全文浏览量: 14
PDF下载量: 424
被引次数: 0

Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

Geoenergy Department, Changchun University of Earth Sciences Jilin 130026

摘要

摘要: 通过对松辽盆地三肇凹陷Ｓ１１３井泉头组蒸发盐岩沉积层序的详细沉积学、矿物学、元素地球化学和同位素地球化学的系统研究，认为该蒸发盐系属海水与淡水混合成因，其形成与周期性的海水入侵有关。
- 松辽盆地白垩系 /
- 蒸发盐岩 /
- 近海内陆盆地 /
- 周期性海水入侵
Abstract: The studied well of S113 is situated on the Sanzhao downwarp of the Songliao Basin. About 500m core sequences containing evaporite of Quantou formation (Albian) in the well were systematicly researched and described in their sedimentary sequences,structural and fabric features, mineral associations, as well as elemental geochemical and isotopic characteristics.According to the above studies,the authors concluded as following:1. The evaporites which are mainly anhydrite,barite as well as celestine and gypsum have two kinds of mineral associations and the cementation order of the minerals ought to be ba rite →calcite→celestine and calcite →gypsum (anhydrite) respectively, which agree with their solubilities.2. The palaeoenvironmental conditions were PH=9, Eh=0. 1, SO₄^2-= 3084mg/L and CO₃^2-= 102mg/L,which were the contents in between playa-lake and marine water.3. There were two sources for forming evaporites-episodical marine water input and continental sources which were mainly composed of meteoric water and oxidation of pyrite from C-P shales and Yanshanian igneous rocks.The ratio of volume of marine input to volume of continental input lay between 0: 12. 6: 1. 4. The marine water input became significant approximatly during the period of 102Ma,106Ma and 107Ma, which agree with the Mid-late Albian eustasy.5. Formed in the arid playa mud flat or salina, the evaporites deposited near water table. And the eolian effect could occasionally become significant.
- Songliao Cretaceous /
- evaporite /
- marine water input /
- palaeoenvironment condition

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参考文献(1)

[1]

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11.Andreason, M. W.，1992, Coastal siliciclastic sabkhas and related evaporative environments of the Permian Yates for-oration. North Ward一Estes field, Ward County, Texas. AAPG Bull. 76:1735一1739.

12.B. A.格里年科和L. H.格里年科，1980,硫同位素地球化学(赵瑞译)，北京:科学出版社.

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17.Purser, B. H.，Soliman, M. and M'Rabet, A.，1987, Carbonate, Evaporate, Siliciclastic stransitions in quaternary rift sediments of the northwest red sea.Sedim. Geol.，53:247一267.

18.Richardson, M. S. and M. Y. Harry.1989, Geochemistry, Prentice一Hall, Inc.，New Jersey.

19.Warren, J. K. and Kendall, C.1985, Comparison of sequences formed in marine sabkha (subaerial) and saliva (sabaqreous) settings一modern ancient. Bull. AAPG Hull.，69,1013一1023.

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松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

1 长春地质学院长春 130026;

2 大庆石油管理局研究院大庆 163712

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学

刊出日期: 1995-12-10

关键词:

摘要: 通过对松辽盆地三肇凹陷Ｓ１１３井泉头组蒸发盐岩沉积层序的详细沉积学、矿物学、元素地球化学和同位素地球化学的系统研究，认为该蒸发盐系属海水与淡水混合成因，其形成与周期性的海水入侵有关。

English Abstract

Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

Geoenergy Department, Changchun University of Earth Sciences Jilin 130026

Publish Date: 1995-12-10

Keywords:

Abstract: The studied well of S113 is situated on the Sanzhao downwarp of the Songliao Basin. About 500m core sequences containing evaporite of Quantou formation (Albian) in the well were systematicly researched and described in their sedimentary sequences,structural and fabric features, mineral associations, as well as elemental geochemical and isotopic characteristics.According to the above studies,the authors concluded as following:1. The evaporites which are mainly anhydrite,barite as well as celestine and gypsum have two kinds of mineral associations and the cementation order of the minerals ought to be ba rite →calcite→celestine and calcite →gypsum (anhydrite) respectively, which agree with their solubilities.2. The palaeoenvironmental conditions were PH=9, Eh=0. 1, SO₄^2-= 3084mg/L and CO₃^2-= 102mg/L,which were the contents in between playa-lake and marine water.3. There were two sources for forming evaporites-episodical marine water input and continental sources which were mainly composed of meteoric water and oxidation of pyrite from C-P shales and Yanshanian igneous rocks.The ratio of volume of marine input to volume of continental input lay between 0: 12. 6: 1. 4. The marine water input became significant approximatly during the period of 102Ma,106Ma and 107Ma, which agree with the Mid-late Albian eustasy.5. Formed in the arid playa mud flat or salina, the evaporites deposited near water table. And the eolian effect could occasionally become significant.

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

引用本文:

王璞珺, 任延广, 王东坡. 松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究[J]. 沉积学报, 1995, 13(S1): 53-62.

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松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学

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Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

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目录

松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

1 长春地质学院长春 130026;

2 大庆石油管理局研究院大庆 163712

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学

English Abstract

Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

Geoenergy Department, Changchun University of Earth Sciences Jilin 130026

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松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

作者简介: 王璞珺,男,37岁,博士、副教授,沉积学与地球化学

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Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

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出版历程

目录

松辽盆地白垩系泉头组蒸发盐岩的成因及其古环境意义研究

1 长春地质学院 长春 130026; 2 大庆石油管理局研究院 大庆 163712

作者简介: 王璞珺,男,37岁,博士、副教授,沉积学与地球化学

English Abstract

Evaporite Origin and Its Palaeoenvironmental Significance of Quantou Formation,Songliao Cretaceous Nearshore Continental Basin (NE China)

Geoenergy Department, Changchun University of Earth Sciences Jilin 130026

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学

1 长春地质学院长春 130026;

2 大庆石油管理局研究院大庆 163712

作者简介:
王璞珺,男,37岁,博士、副教授,沉积学与地球化学