|本期目录/Table of Contents|

[1]王华,姜华,林正良,等.南堡凹陷东营组同沉积构造活动性与沉积格局的配置关系研究[J].地球科学与环境学报,2011,33(01):70-77.
 WANG Hua,JIANG Hua,LIN Zheng-liang,et al.Relations Between Synsedimentary Tectonic Activity and Sedimentary Framework of Dongying Formation in Nanpu Sag[J].Journal of Earth Sciences and Environment,2011,33(01):70-77.
点击复制

南堡凹陷东营组同沉积构造活动性与沉积格局的配置关系研究(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第33卷
期数:
2011年第01期
页码:
70-77
栏目:
基础地质与矿产地质
出版日期:
2011-03-15

文章信息/Info

Title:
Relations Between Synsedimentary Tectonic Activity and Sedimentary Framework of Dongying Formation in Nanpu Sag
文章编号:
1672-6561(2011)01-0070-08
作者:
王华1姜华2林正良1赵淑娥1
1.中国地质大学 资源学院,湖北 武汉 430074; 2.中国石油勘探开发研究院 地质研究所,北京 100083
Author(s):
WANG Hua1JIANG Hua2LIN Zheng-liang1ZHAO Shu-e1
1. School of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China; 2. Institute of Geological Research, Research Institute of Petroleum Exploration and Development PetroChina, Beijing 100083, China
关键词:
南堡凹陷东营组断坡带高柳断层构造活动性
Keywords:
Nanpu Sag Dongying Formation faulted slope zone Gaoliu Fault intensive tectonic activity
分类号:
P618.130.2;TE122.3+21
DOI:
-
文献标志码:
A
摘要:
应用构造-层序地层分析的思维,通过构造格架与地层格架的关联分析,对南堡凹陷东营组沉积充填样式与过程、控制要素进行了综合研究。通过沉降史分析,并结合区域构造演化特征,古近纪可划分为4个次级构造幕。凹陷内断裂发育,同沉积断裂及其时空配置关系对凹陷内结构和沉积体系类型及其展布起着重要的控制作用。控凹断裂直接控制了局部构造带的可容纳空间变化和古地貌形态,从而形成不同的沉积展布特征。高柳断层是南堡凹陷内最为重要的二级断裂,其活动始于Es1沉积时期,在东营组沉积时期活动最为强烈。在东营组沉积时期,高柳断层将凹陷分为南、北两个独立的沉积系统,尤其在Ed3沉积期其强烈的翘倾作用使高柳地区成为一个孤立的湖盆,直接影响到了高柳地区的沉积充填。根据东营组沉积时期同沉积断裂组合样式划分出4种断裂坡折带:断崖型、断坡型、同向断阶型和反向断阶型,为研究南堡凹陷东营组同沉积断裂对沉积格局的控制作用提供了有利的指导,具有重要的石油地质意义。
Abstract:
Under the guidance of tectono-sequence stratigraphy and the association analysis of tectonic and sequence framework, the sedimentary filling patterns, process, and controlling factors of Dongying Formation in Nanpu Sag are comprehensively studied. Through the analysis on subsidence history and regional tectonic evolution characteristics, the Paleogene can be divided into four secondary tectonic episodes. Faults are very developed within Nanpu Sag. It is found that the synsedimentary faults and their temporal and spatial configuration have significant control on the intra-sag structures, types and distribution of sedimentary system. The boundary faults control the variation of accommodation space and paleogeomorphology of some local tectonic zones, which result in forming different sediments distribution features. Gaoliu Fault is the most important secondary fault in Nanpu Sag. It starts during the Es1 depositional period, and its activity gradually reaches the strongest in Dongying Formation. During the deposition period of Dongying Formation, Gaoliu Fault divides sag into two parts, the southern and northern parts. After its development, the Gaoliu Area becomes an isolated lacustrine basin for the intensive tilting process of the fault during the sedimentary period of Ed3, which directly influences the sedimentation in Gaoliu Area. Based on the faults combination styles of Dongying Formation in Nanpu Sag, four types of tectonic slope break are identified, which are faulted scarp type, faulted slope type, concordant and antithetic faulted terrace types. These tectonic slope breaks provide a favorable guidance to the study on the controlling of synsedimentary faults on sedimentary framework in Dongying Formation, Nanpu Sag.

参考文献/References:

[1] Lin C S,Li S T,Wan Y X,et al.Depositional Systems,Sequence Stratigraphy and Basin Filling Evolution of Erlian Fault Lacustrine Basin,Northeast China[C]∥Liu B J,Li S T.Basin Analysis,Global Sedimentary Geology and Sedimentology:Proceedings of the 30th International Geological Congress.Utrecht:Brill Academic Publisher,1997:163-175.
[2] 林畅松,刘景彦,张燕梅,等.库车坳陷第三系构造层序的构成特征及其对前陆构造作用的响应[J].中国科学:D辑,2002,32(3):177-183.
[3] 林畅松.沉积盆地的构造地层分析[J].现代地质,2006,20(2):185-194.
[4] 林畅松,郑和荣,任建业,等.渤海湾盆地东营、沾化凹陷早第三纪同沉积断裂作用对沉积充填的控制[J].中国科学:D辑,2003,33(11):1025-1036.
[5] 李思田,潘元林,陆永潮,等.断陷湖盆隐蔽油藏预测及勘探的关键技术[J].地球科学——中国地质大学学报,2002,27(5):592-598.
[6] 王家豪,王 华,赵忠新,等.层序地层学应用于古地貌分析:以塔河油田为例[J].地球科学——中国地质大学学报,2003,28(4):425-429.
[7] 田景春,彭 军,陈高武,等.塔里木盆地东河塘组层序地层学研究[J].地球科学与环境学报,2007,29(2):130-136.
[8] 邓宏文,郭建宇,王瑞菊,等.陆相断陷盆地的构造层序地层分析[J].地学前缘,2008,15(2):1-7.
[9] 严德天,王 华,王清晨.中国东部第三系典型断陷盆地幕式构造旋回及层序地层特征[J].石油学报,2008,29(2):185-190.
[10] 解习农,程守田,陆永潮.陆相盆地幕式构造旋回与层序构成[J].地球科学——中国地质大学学报,1996,21(1):27-33.
[11] 徐安娜,郑红菊,董月霞,等.南堡凹陷东营组层序地层格架及沉积相预测[J].石油勘探与开发,2006,33(4):437-443.
[12] 刘延莉,邱春光,邓宏文,等.冀东南堡凹陷古近系东营组构造对扇三角洲的控制作用[J].石油与天然气地质,2008,29(1):95-101.
[13] 王 华.南堡凹陷构造古地貌、沉积体系、热动力学研究及有利勘探方向预测[R].唐山:中国石油天然气集团公司冀东油田分公司,2009.
[14] 任建业,陆永潮,张青林.断陷盆地构造坡折带形成机制及其对层序发育样式的控制[J].地球科学——中国地质大学学报,2004,29(5):596-602.
[15] 林畅松,潘元林,肖建新,等.构造坡折带——断陷盆地层序分析和油气预测的重要概念[J].地球科学——中国地质大学学报,2000,25(3):260-266.
[16] 王家豪,王 华,肖敦清,等.伸展构造体系中传递带的控砂作用[J].石油与天然气地质,2008,29(1):19-25.
[17] 操应长.断陷湖盆中强制湖退沉积作用及其成因机制[J].沉积学报,2005,23(1):84-90.
[18] 管 红,朱筱敏.南堡凹陷东营组层序地层格架与沉积体系[J].沉积学报,2008,26(5):730-736.

相似文献/References:

[1]陈清华,王晶,石艳红,等.济阳坳陷沾化凹陷桩南断裂带储层精细划分对比方法研究[J].地球科学与环境学报,2013,35(02):75.
 CHEN Qing-hua,WANG Jing,SHI Yan-hong,et al.Study on the Method of Stratigraphic Accurate Correlation and Subdivision in Zhuangnan Fault Zone of Zhanhua Sag,Jiyang Depression[J].Journal of Earth Sciences and Environment,2013,35(01):75.
[2]付广,葛思.静止期未成岩断裂侧向封闭能力评价方法及其应用[J].地球科学与环境学报,2018,40(03):301.
 FU Guang,GE Si.Evaluation Method and Application of Fault Lateral Sealing Ability in Quiescent Undiagenetic Period[J].Journal of Earth Sciences and Environment,2018,40(01):301.
[3]欧阳黎明,杨少春,张博明,等.南堡凹陷3号构造区古近系东营组/沙河街组不整合结构特征[J].地球科学与环境学报,2018,40(03):322.
 OUYANG Li-ming,YANG Shao-chun,ZHANG Bo-ming,et al.Characteristics of Unconformity Structure Between Palaeogene Dongying Formation and Shahejie Formation in No.3 Tectonic Region of Nanpu Sag[J].Journal of Earth Sciences and Environment,2018,40(01):322.

备注/Memo

备注/Memo:
收稿日期:2010-07-26
基金项目: 中国地质大学构造与油气资源教育部重点实验室基金项目(TPR-2009-19; TPR-2010-08)
作者简介: 王 华(1964-),男,黑龙江甘南人,教授,博士研究生导师,从事应用沉积学、应用层序地层学研究。E-mail:wanghua@cug.edu.cn

更新日期/Last Update: 2011-03-20