东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

王慧中; 盛蔚; 舒小辛; 刘青春; 司志华; 李云新

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东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新

文章导航 > 沉积学报 > 1996 > 14(1): 47-58

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

引用本文:

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

Wang Huizhong, Sheng Wei, Su Xiaoxin, Liu Qingchun, Si Zhihua, Li Yunxin. Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield[J]. Acta Sedimentologica Sinica, 1996, 14(1): 47-58.

Citation:

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

引用本文:

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

Citation:

东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

1 同济大学海洋地质开放实验室上海 200092;
2 胜利油田钻井地质公司东营 257000

详细信息

作者简介:
王慧中,男,57岁,副教授,沉积学

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Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

1 Department of Marine Geology, Tongji Universiyt, Shanghai 200092;
2 Geological Drilling Company,Shengli Petroleum Administration,Dongying 257000

摘要

摘要: 通过环境磁学、沉积学、遗迹化石学与地球化学对牛３８井厘米级红灰韵律层的综合研究发现红层中具明显的胶体凝聚现象，其磁化率值、总铁与游离铁含量较高，层内生物扰动作用相对较强，表明气候变化引起的化学沉积是控制韵律旋回的主因，底栖生物的潜穴活动促进了沉积界面处微化学环境的变化。经频谱分析等时序分析法的估算可知该红灰韵律层是受十年级与百年级主周期的控制，可能与太阳黑子或太阳磁场活动等天文周期有关。虽然此类天文周期对地球气候变化的影响能力也许不强，但由于化学沉积对气候变化反应灵敏，而且可能当时湖水化学环境正处于胶体沉积的临界值附近，因而水体化学性质稍有偏离即可导致韵律层的形成。
- 韵律沉积 /
- 气候旋回 /
- 絮凝作用 /
- 频谱分析 /
- 气候响应 /
- 沉积临界值
Abstract: Based on multidisciplinary analyses of sedimentology,environmental magnetism,ichnology, mineralogy and geochemistry, it is found that,in the reddish- grey lamination in rhythmic deposits,there are various features about flocculent deposits with high susceptibility , high contents of total Fe and free Fe, and higher grades of bioturbation,showing that changes with chemical sedimentation caused by climatic cycles are the main controlling factor on the rhythmic beddings, and bioturbation could accelerate changes in micro-chemical environment on surface between water and sediments.Results from spectral analysis on time sequences show that the reddish-grey rhythmic deposits were controlled by decade-or century-level climatic periods which might be related to several astronomic cycles,such as sunspot or solar magnetic field. The influence of these astronomic factors on climatic changes is not likely very strong, but this kind of rhythmic bedding could be visible,probably resulting from the sensitive response of chemical sedimentation to climatic cycles ,and or the lacustrine chemical environment was nearby the sedimentary threshold for flocculation during the period in the upper and middle member of Shahejie Formation.
- rhythmic deposit /
- climatic cycles /
- flocculation /
- bioturbation /
- spectral Analysis /
- response to climate

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参考文献(1)

[1]

1.舒小辛，刘志伟，王慧中等，磁化率在牛38井早第三纪古湖泊沉积物研究中的初步应用，复式油气田，1993, (3):10-18。

2.王慧中，江浙一带现代海滩的生物扰动构造及其指相意义，地质科学，1985,(1):53-58。

3.刘宝王君，沉积岩石学，北京:地质出版社，1980, 8-26,48-54。

4.Anderson,R. Y&Dean, W. E.，Lacustrine verve formation through time，PalaeocGmatol.，Palaeoecol.1988 , 62 : 215-23.

5.Weedon, G. P.，The detection and iVustration of regular sedimentary cycles using Walsh Power Spectra and filtering,with examples from the Lias of Switzerland. Journal of the Geological Society, London, 1989,146: 133-144.

6.程乾生，信号数字处理数学原理，北京:石油工业出版社，1978。

7.Negi, J.G. and Tiwari, K. G.，Periodicities of geomagnetic intensity and paleornagnetic variations; a Walsh spectral approactf,Eartlr Plant. Sci. Lett.，1984 , 70: 139-147.

8. Anderson, R.Y、The varve fnicroc}m: propagator of cyclic 6eddin云.Paleoceanography, 1986,-1(4):273-282.

9.徐道一，杨正宗，张勤文，孙亦因，天文地质学概论，北京:地质出版社，1983 ,1-284。

10.Glenn， C. R. and Kelts, K.，Seditnentaty rhythms in lake deposit. in "Cycles and Events in Stratigraphy" Einsele.，et aL. (eds.)，1931, 88-Z21.

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东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

1 同济大学海洋地质开放实验室上海 200092;

2 胜利油田钻井地质公司东营 257000

作者简介:
王慧中,男,57岁,副教授,沉积学

收稿日期: 1994-12-02
刊出日期: 1996-03-10

关键词:

摘要: 通过环境磁学、沉积学、遗迹化石学与地球化学对牛３８井厘米级红灰韵律层的综合研究发现红层中具明显的胶体凝聚现象，其磁化率值、总铁与游离铁含量较高，层内生物扰动作用相对较强，表明气候变化引起的化学沉积是控制韵律旋回的主因，底栖生物的潜穴活动促进了沉积界面处微化学环境的变化。经频谱分析等时序分析法的估算可知该红灰韵律层是受十年级与百年级主周期的控制，可能与太阳黑子或太阳磁场活动等天文周期有关。虽然此类天文周期对地球气候变化的影响能力也许不强，但由于化学沉积对气候变化反应灵敏，而且可能当时湖水化学环境正处于胶体沉积的临界值附近，因而水体化学性质稍有偏离即可导致韵律层的形成。

English Abstract

Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

1 Department of Marine Geology, Tongji Universiyt, Shanghai 200092;

2 Geological Drilling Company,Shengli Petroleum Administration,Dongying 257000

Received Date: 1994-12-02
Publish Date: 1996-03-10

Keywords:

Abstract: Based on multidisciplinary analyses of sedimentology,environmental magnetism,ichnology, mineralogy and geochemistry, it is found that,in the reddish- grey lamination in rhythmic deposits,there are various features about flocculent deposits with high susceptibility , high contents of total Fe and free Fe, and higher grades of bioturbation,showing that changes with chemical sedimentation caused by climatic cycles are the main controlling factor on the rhythmic beddings, and bioturbation could accelerate changes in micro-chemical environment on surface between water and sediments.Results from spectral analysis on time sequences show that the reddish-grey rhythmic deposits were controlled by decade-or century-level climatic periods which might be related to several astronomic cycles,such as sunspot or solar magnetic field. The influence of these astronomic factors on climatic changes is not likely very strong, but this kind of rhythmic bedding could be visible,probably resulting from the sensitive response of chemical sedimentation to climatic cycles ,and or the lacustrine chemical environment was nearby the sedimentary threshold for flocculation during the period in the upper and middle member of Shahejie Formation.

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

引用本文:

王慧中, 盛蔚, 舒小辛, 刘青春, 司志华, 李云新. 东营凹陷牛38井沙三中上段红灰韵律层中的环境信息[J]. 沉积学报, 1996, 14(1): 47-58.

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东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

作者简介:
王慧中,男,57岁,副教授,沉积学

计量

Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

计量

目录

东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

1 同济大学海洋地质开放实验室上海 200092;

2 胜利油田钻井地质公司东营 257000

作者简介:
王慧中,男,57岁,副教授,沉积学

English Abstract

Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

1 Department of Marine Geology, Tongji Universiyt, Shanghai 200092;

2 Geological Drilling Company,Shengli Petroleum Administration,Dongying 257000

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东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

作者简介: 王慧中,男,57岁,副教授,沉积学

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Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

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出版历程

目录

东营凹陷牛38井沙三中上段红灰韵律层中的环境信息

1 同济大学海洋地质开放实验室 上海 200092; 2 胜利油田钻井地质公司 东营 257000

作者简介: 王慧中,男,57岁,副教授,沉积学

English Abstract

Environmental Information in Reddish-Grey Lacustrine Rhythmic Deposits of the Core Niu-38 in the Upper and Middle Members of Shahejie Formation,in Dongying Depression,Shengli Oilfield

1 Department of Marine Geology, Tongji Universiyt, Shanghai 200092; 2 Geological Drilling Company,Shengli Petroleum Administration,Dongying 257000

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王慧中,男,57岁,副教授,沉积学

1 同济大学海洋地质开放实验室上海 200092;

2 胜利油田钻井地质公司东营 257000

作者简介:
王慧中,男,57岁,副教授,沉积学

1 Department of Marine Geology, Tongji Universiyt, Shanghai 200092;

2 Geological Drilling Company,Shengli Petroleum Administration,Dongying 257000