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: 432
HTML全文浏览量: 16
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]

1.王璞王君、王东坡，1992a，松辽盆地白里纪黑色页岩沉积与湖泊缺氧事件，基础地质专辑，吉林省科技出版社，265-269.

2.王璞王君、周燕、王东坡，1994，白垄纪非海相层序同位素年龄的直接测定研究及盆地分析的同位素年代学方法，世界地质，13(3):124-131.

3.王璞王君、杜小弟、王东坡，1995，松辽盆地白蟹纪湖侵沉积层序的地球化学特征与海进/海退事件的地球化学记录，岩相古地理，15(4) :14-20.

4.刘宝王君,1980，沉积岩石学，北京;地质出版社.

5.刘英俊、李兆麟、王鹤年等，1979，地球化学，北京:科学出版社.

6.杜小弟、王璞王君,1992b，冰筏沉积与古气候、古地理，岩相古地理，4期，35-41页.

7.杜小弟、王玻王君,1992。沉积速率的定t计算，长春地质学院学报，22(1),67-71.

8.钟其权、马力、石宝琦,1985，松辽盆地的演化和构造格局对沉积建造的控制，松辽陆相盆地石油地质(杨万里主编)，石油工业出版社，26-34页.

9.赵其渊,1989,海洋地球化学，北京:地质出版社.

10.Anadon, P.，Rossell, L. and Talbot, M. R.，1992, Carbonate replacement of lacustrine gypsum deosits in two Neo-gene continental bsins, eastern Spain. Sedim. Geol.，78:201一216.

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.

13.Hay, R. L.，1978，沉积岩中的沸石及其成因(黄典豪译)，北京:地质出版社.

14.Holser, W. T. and Kaplan, J. R.，1966, Isotope geochemistry of sedimentary sulphates, Chem. Geol.，1:93一135.

15.Mazzullo, J.，Alexander, A.，Tieh. T. and M. L. Ding, 1992, The effects of wind transport on the shapes of guartz silt grains. J. Sedim. Petrol.，62:961一971.

16.Purvis, K.，1992, Lower Permian Rotilegend Sandstones, southern North sea: a case study of sandstone diagenesis in evaporate一associated sequences, Sedim. Geol.，77:155一171.

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.

20.Wolf. K. H.，1980，层控矿床和层状矿床(谢学锦等译)，北京:地质出版社.

21.Faure, G. . and Powell, J. L.，1975,惚同位素地质(中科院贵阳地化所译)，北京:科学出版社.

22.Burke, W. H.，benison, R. E.，Hetherington, E. A.，Koephnik, R. B.，Nelson, H. F.，and Otto, J. B.，1982, Vari-anon of seawater ⁸⁷Sr/⁸⁶Sr throughout Phanerozoic time. Geology. 10:516一519.

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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