乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

张成; 李春柏; 楚美娟; 史淑玲

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乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

张成, 李春柏, 楚美娟, 史淑玲

文章导航 > 沉积学报 > 2005 > 23(4): 657-663

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

引用本文:

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

ZHANG Cheng, LI Chun-bai, CHU Mei-juan, SHI Shu-ling. Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression[J]. Acta Sedimentologica Sinica, 2005, 23(4): 657-663.

Citation:

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

引用本文:

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

Citation:

乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

1.
中国地质大学资源学院盆地所,武汉 430074;
2.
大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712;
3.
中国地质大学能源学院,北京 100083

详细信息

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

中图分类号: P539.2

计量

文章访问数: 617
HTML全文浏览量: 4
PDF下载量: 706
被引次数: 0

Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

1.
China University of Geosciences, Wuhan 430074;
2.
Institute of Exploration and Development of Daqing Oilfield Company Ltd. Daqing Heilongjiang 163712;
3.
China University of Geosciences, Beijing 100083

摘要

摘要: 利用地质、地球物理等资料对乌尔逊凹陷下白垩统高频层序特征及其控制因素进行了分析。高频层序赋存于三级复合层序CSq7和CSq8内部,沿凹陷走向分布,总体以前积形态下超于复合密集段之上。层序边界属Ⅰ型性质,但不整合规模较小;层序内部包含3个体系域,准层序组总体呈加积—前积—退积—前积的叠加样式。研究区共识别出16个高频层序,平均周期为0.22~0.28Ma,沉积速率为0.57~0.76m/kyr。研究表明,低构造沉降速率和温暖潮湿气候条件下的高沉积物供给速率是控制高频层序发育的主要因素,三级基准面旋回高位稳定—缓慢下降阶段是高频层序发育的有利时期,盆缘地貌对高频层序几何学特征也有较大影响。
- 高频层序 /
- 复合层序 /
- 沉积特征 /
- 乌尔逊凹陷 /
- 下白垩统
Abstract: Based on the geological and geophysical data, this paper analyses characteristics and controls of high-frequency sequences of Lower Cretaceous Series in Wuerxun Depression. High-frequency sequences occur along the strike direction of the depression in third-order composite sequence 7 and 8, and show downlap of reflections onto the composite condensed section. Most of high-frequency sequences belong in type I, but the scopes of unconformities are very limited. There are three system tracts and parasequences stacking patterns from aggradation-progradation-retrogra-dation-progradation in high-frequency sequences. Sixteen high-frequency sequences are identified in this area. The average period and the sediment velocity of which is about 0.22～0.28 Ma and 0.57～0.76 m /kyr, respectively.This study suggests that high-frequency sequences have the greatest chance of forming under the conditions of low tectonic subsidence and high sediment supp ly during third-order base-level relative stabilizing and descending periods,and that the marginalmorphology of basin controls the geometry of high-frequency sequences
- high-frequency sequence /
- composite sequence /
- depositional feature /
- Wuerxun Depression /
- Lower Cretaceous Series

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参考文献(1)

[1]

1 Vail P R,Audemard F,Bowman SA, et al. The stratigraphic signatures of tectonics, eustasy and sedimentology - an view. In: Seilacher A and Eisner G, eds. Cycles and events in stratigraphy. New York: Springer-Verlag, 1991. 611～659

2 Goldhammer P K,Dunn P A,Haidie L A. Depositional cycles,composite sea level changes,cycle stacking patterns,and the hierarchy of stratigraphic forcing: examples from the Alpine platform carbonates[J].Geological Society of America Bulletin,1990.535-562.

3 Mitchum R M,Van Wagoner J C. High-frequency sequences and their stacking patterns: sequence stratigraphic evidence of high-frequency eustatic cycles[J].Sedimentary Geology,1991.131-160.

4 Meckel Ⅲ L D,Galloway W E. Formation of high-frequency sequences and their bounding surfaces: case study of the Eocene Yegua Formation,Texas Gulf Coast,USA[J].Sedimentary Geology,1996.155-186.

5 Henriksen S,Weimer P. High-frequency depositional sequences and stratal stacking patterns in lower Pliocene coastal deltas,mid-Norwe-gian continental shelf[J].AAPG Bulletin,1996,(12):1867-1895.

6 Sorensen J C,Gregersen U,Breiner M. High-frequency sequence stratigraphy of Upper Cenozoic deposits in the central and southeastern North Sea areas[J].Marine and Petroleum Geology,1997,(02):99-123.

7 陈代钊. 河流沉积占优势地层中高频层序地层--以贵州盘县西部龙潭组为例[J].地质科学,1997,(04):432-444.

8 Somoza L,Barnolas A,Arasa A. Architectural stacking patterns of the Ebro delta controlled by Holocene high-frequency eustatic fluctuations,delta-lobe switching and subsidence processes[J].Sedimentary Geology,1998.11-32.

9 陈国俊,薛莲花,王琪. 塔里木盆地巴楚地区石炭系高频旋回层序分析[J].沉积学报,1998,(04):37-41.

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11 Prokoph A,Thurow J. Diachronous pattern of Milankovitch cyclicity in late Albian pelagic marlstones of the North German Basin[J].Sedimentary Geology,2000.287-303.

12 武法东,苏新,周平. 东海陆架盆地下第三系高频层序分析[J].地质论评,2001,(01):47-52.

13 Hillgartner H,Strasser A. Quantification of high-frequency sea-level fluctuations in shallow-water carbonates: an example from the Berriasian-Valanginian ( French Jura)[J].Palaeogeography Palaeoclimatology Palaeoecology,2003,(1/4):43-63.

14 Castelltort S,Van Den Driessche J. How plausible are high-frequency sediment supply-drive cycles in the stratigraphic record[J].Sedimentary Geology,2003.3-13.

15 Helle S K. Sequence stratigraphy in a marine moraine at the head of Hardangerfjorden,western Norway: evidence for a high-frequency relative sea-lavel cycle[J].Sedimentary Geology,2004.155-186.

16 赵俊青,纪友亮,张世奇. 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,(01):79-86.

17 张晓东,刘光鼎,王家林. 海拉尔盆地构造特征及其演化[J].石油实验地质,1994,(02):119-127.

18 李志安,丁文龙,张凤莲. 海拉尔地洼型盆地演化历程及地热特征[J].大地构造与成矿学,1996,(04):329-332.

19 王鸿祯,史晓颖. 沉积层序及海平面旋回的分类级别-旋回周期的成因讨论[J].现代地质,1998,(01):1-16.

20 于秀英,杨懋新,王革. 乌尔逊断陷构造演化与含油气系统[J].大庆石油地质与开发,2004,(03):14-16.

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乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

1. 中国地质大学资源学院盆地所,武汉 430074;

2. 大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712;

3. 中国地质大学能源学院,北京 100083

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

收稿日期: 2004-12-14
修回日期: 2005-04-13
刊出日期: 2005-12-10

中图分类号: P539.2

关键词:

摘要: 利用地质、地球物理等资料对乌尔逊凹陷下白垩统高频层序特征及其控制因素进行了分析。高频层序赋存于三级复合层序CSq7和CSq8内部,沿凹陷走向分布,总体以前积形态下超于复合密集段之上。层序边界属Ⅰ型性质,但不整合规模较小;层序内部包含3个体系域,准层序组总体呈加积—前积—退积—前积的叠加样式。研究区共识别出16个高频层序,平均周期为0.22~0.28Ma,沉积速率为0.57~0.76m/kyr。研究表明,低构造沉降速率和温暖潮湿气候条件下的高沉积物供给速率是控制高频层序发育的主要因素,三级基准面旋回高位稳定—缓慢下降阶段是高频层序发育的有利时期,盆缘地貌对高频层序几何学特征也有较大影响。

English Abstract

Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

1. China University of Geosciences, Wuhan 430074;

2. Institute of Exploration and Development of Daqing Oilfield Company Ltd. Daqing Heilongjiang 163712;

3. China University of Geosciences, Beijing 100083

Received Date: 2004-12-14
Rev Recd Date: 2005-04-13
Publish Date: 2005-12-10

Keywords:

Abstract: Based on the geological and geophysical data, this paper analyses characteristics and controls of high-frequency sequences of Lower Cretaceous Series in Wuerxun Depression. High-frequency sequences occur along the strike direction of the depression in third-order composite sequence 7 and 8, and show downlap of reflections onto the composite condensed section. Most of high-frequency sequences belong in type I, but the scopes of unconformities are very limited. There are three system tracts and parasequences stacking patterns from aggradation-progradation-retrogra-dation-progradation in high-frequency sequences. Sixteen high-frequency sequences are identified in this area. The average period and the sediment velocity of which is about 0.22～0.28 Ma and 0.57～0.76 m /kyr, respectively.This study suggests that high-frequency sequences have the greatest chance of forming under the conditions of low tectonic subsidence and high sediment supp ly during third-order base-level relative stabilizing and descending periods,and that the marginalmorphology of basin controls the geometry of high-frequency sequences

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

引用本文:

张成, 李春柏, 楚美娟, 史淑玲. 乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J]. 沉积学报, 2005, 23(4): 657-663.

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乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

计量

Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

计量

目录

乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

1. 中国地质大学资源学院盆地所,武汉 430074;

2. 大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712;

3. 中国地质大学能源学院,北京 100083

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

English Abstract

Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

1. China University of Geosciences, Wuhan 430074;

2. Institute of Exploration and Development of Daqing Oilfield Company Ltd. Daqing Heilongjiang 163712;

3. China University of Geosciences, Beijing 100083

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乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

作者简介: 张成，男，1977年出生，博士研究生，层序地层学与沉积学。

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Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

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出版历程

目录

乌尔逊凹陷下白垩统高频层序特征及其控制因素分析

1. 中国地质大学资源学院盆地所,武汉 430074; 2. 大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712; 3. 中国地质大学能源学院,北京 100083

作者简介: 张成，男，1977年出生，博士研究生，层序地层学与沉积学。

English Abstract

Analysis on Character istics and Controls of High-Frequency Sequences of Lower Cretaceous Ser ies in Wuerxun Depression

1. China University of Geosciences, Wuhan 430074; 2. Institute of Exploration and Development of Daqing Oilfield Company Ltd. Daqing Heilongjiang 163712; 3. China University of Geosciences, Beijing 100083

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期刊在线

联系我们

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

1. 中国地质大学资源学院盆地所,武汉 430074;

2. 大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712;

3. 中国地质大学能源学院,北京 100083

作者简介:
张成，男，1977年出生，博士研究生，层序地层学与沉积学。

1. China University of Geosciences, Wuhan 430074;

2. Institute of Exploration and Development of Daqing Oilfield Company Ltd. Daqing Heilongjiang 163712;

3. China University of Geosciences, Beijing 100083