必须声明标量变量 "@Script_ID"。 辽河西部凹陷欢喜岭地区沙河街组三段层序地层与沉积相研究-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]董洁,陈世悦,李聪.辽河西部凹陷欢喜岭地区沙河街组三段层序地层与沉积相研究[J].地球科学与环境学报,2010,32(03):245.
 DONG Jie,CHEN Shi-yue,LI Cong.Sequence Stratigraphy and Sedimentary Faces in the Third Member of Shahejie Formation of Huanxiling Area in the West Depression, Liaohe Basin[J].Journal of Earth Sciences and Environment,2010,32(03):245.
点击复制

辽河西部凹陷欢喜岭地区沙河街组三段层序地层与沉积相研究(PDF)
分享到:

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

卷:
第32卷
期数:
2010年第03期
页码:
245
栏目:
基础地质与矿产地质
出版日期:
2010-09-20

文章信息/Info

Title:
Sequence Stratigraphy and Sedimentary Faces in the Third Member of Shahejie Formation of Huanxiling Area in the West Depression, Liaohe Basin
文章编号:
1672-6561(2010)03-0245-07
作者:
董洁陈世悦李聪
(中国石油大学 地球资源与信息学院,山东 东营 257061)
Author(s):
DONG Jie CHEN Shi-yue LI Cong
(School of Geo-resources and Information, China University of Petroleum, Dongying 257061, Shandong, China)
关键词:
沉积相湖底扇扇三角洲沙河街组三段欢喜岭地区辽河盆地
Keywords:
sedimentary facies sublacustrine fan fan delta the third member of Shahejie Formation Huanxiling Area Liaohe Basin
分类号:
TE121.3;P539.2
DOI:
-
文献标志码:
A
摘要:
利用高分辨率层序地层学方法,结合岩芯、测井和地震资料,识别辽河西部凹陷欢喜岭地区各级层序界面,建立地层层序格架,探讨地层格架下沉积相类型、演化规律以及平面展布,并就有利沉积相带分布进行了讨论。结果表明:从钻测井资料看出,层序界面识别标志主要为岩性和颜色发生突变,沉积相类型发生突变,电性特征发生明显变化等;将欢喜岭地区沙河街组划分为6个三级层序,12个四级层序;沙河街组三段发育扇三角洲、湖底扇和湖泊相等沉积相类型,其中,上亚段扇三角洲发育,中亚段广泛发育湖底扇相沉积,下亚段以深湖、滨浅湖相为主,斜坡边缘发育扇三角洲沉积;沙河街组三段中亚段湖底扇相和下亚段扇三角洲相的储集物性最好,为有利沉积相带。
Abstract:
With the high resolution sequence stratigraphy and the correlation analysis of cores, logs and seismic data, different orders of stratigraphic sequence interface were identified for the third member of Shahejie Formation of Huanxiling Area in the west depression of Liaohe Basin, the stratigraphic framework was built, the types of sedimentary facies, evolution and distribution of the framework were discussed, and the distribution of favorable sedimentary reservoir was forecasted. The results showed that the recognition marks of stratigraphic sequence interface were the significant changes of lithology, color, type of sedimentary facies and electricity character; Shahejie Formation of Huanxiling Area was divided into 6 three-order strata sequences and 12 four-order strata sequences; fan dalta, sublacustrine fan and lacustrine facies were developed in the third member of Shahejie Formation, fan dalta was developed in the upper subsection, sublacustrine fan was widely developed in the middle subsection, deep, littoral and shallow lacustrine facies was mainly developed in the lower subsection; reservoir physical properties of sublacustrine fan in the middle subsection of the third member of Shahejie Formation and fan dalta in the lower subsection were best, and it was the favorable sedimentary reservoir.

参考文献/References:

[1] Cross T A.Quantitative Dynamic Stratigraphy[M].New Jersey:Prenrice Hall,1990.
[2] Cross T A.Stratigraphic Controls on Reservoir Attributes in Continental Strata [J].Earth Science Frontiers,2000,7(4):322-350.
[3] 邓宏文.美国层序地层研究中的新学派——高分辨率层序地层学[J].石油与天然气地质,1995,16(2):89-97.
[4] 侯维虹,渠永宏,张永庆,等.通过地层沉积过程进行储集层的精细描述[J].石油勘探与开发,2004,31(增刊):106-109.
[5] 田景春,康建威,林小兵,等.台盆沉积体系及层序地层特征研究[J].西南石油大学学报:自然科学版,2007,29(6):39-42.
[6] 范春花,王英民,陈振岩,等.陈家洼陷沙三下亚段层序地层和沉积相分析[J].西南石油大学学报:自然科学版,2009,31(2):31-35.
[7] 李宏伟,朱怡翔,李胜利,等.辽河西部凹陷北部地区隐蔽油气藏预测与成藏机制分析[J].石油勘探与开发,2003,30(1):44-46.
[8] 于福生,吉珍娃,杨 雪,等.辽河盆地西部凹陷北部地区新生代断裂特征与圈闭类型[J].地球科学与环境学报,2007,29(2):149-153.
[9] 张凤奇,庞雄奇,冷济高,等.辽河西部凹陷构造圈闭含油性定量预测模型[J].西南石油大学学报:自然科学版,2009,31(2):27-30.
[10] 陈金龙,张庆龙,于兰兄,等.断层对辽河盆地杜229断块超稠油成藏与生产的影响[J]. 地球科学与环境学报,2006,28(3):48-52.
[11] 许 坤,潘耀丽,彭 峰.辽河盆地下第三系层序分析[J].地层学杂志,1997,21(4):267-274.
[12] 沈守文,彭大钧,颜其彬,等.层序地层学预测隐蔽油气藏的原理和方法[J].地球学报,2000,21(3):300-305.
[13] 徐怀大.层序地层学理论用于我国断陷盆地分析中的问题[J].石油与天然气地质,1991,12(1):52-57.
[14] 郝雪峰.陆相断陷盆地层序地层与成藏单元类比分析——以济阳拗陷为例[J].油气地质与采收率,2007,14(2):16-18.
[15] 邱桂强.陆相断陷盆地高精度层序地层研究现状与思路[J].油气地质与采收率,2005,12(3):1-4.
[16] 樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2):12-17.
[17] 廖兴明,姚继峰,于天庆,等.辽河盆地构造演化与油气[M].北京:石油工业出版社,1996.
[18] 高先志,李敬生,李晓光,等.辽河西部凹陷兴隆台—马圈子地区沙三段层序地层研究[C]∥匡立春,顾家裕,吕焕通,等.油气层序地层学新进展.北京:石油工业出版社,2006:68-69.
[19] 袁 波,陈世悦,袁文芳,等.辽西凹陷欢喜岭地区沙河街组层序格架的建立[J].西南石油大学学报:自然科学版,2008,30(2):27-30.
[20] 李德江,朱筱敏,董艳蕾,等.辽东湾拗陷古近系沙河街组层序地层分析[J].石油勘探与开发,2007,34(6):669-676.
[21] 鞠俊成,张凤莲,喻国凡,等.辽河盆地西部凹陷南部沙三段储层沉积特征及含油气性分析[J].古地理学报,2001,3(1):63-70.
[22] 林会喜,鄢继华,袁文芳,等.渤海湾盆地东营凹陷古近系沙河街组三段沉积相类型及平面分布特征[J].石油实验地质,2005,27(1):55-61.

相似文献/References:

[1]季汉成,门相勇,翁庆萍,等.东北大三江地区早白垩世岩相古地理研究[J].地球科学与环境学报,2013,35(02):81.
 JI Han-cheng,MEN Xiang-yong,WENG Qing-ping,et al.Study on Early Cretaceous Lithofacies Paleogeography in Dasanjiang Area of Northeast China[J].Journal of Earth Sciences and Environment,2013,35(03):81.
[2]张喜林.东海盆地西湖凹陷中—下始新统宝石组沉积特征[J].地球科学与环境学报,2014,36(03):31.
 ZHANG Xi-lin.Sedimentary Characteristics of Baoshi Formation of Lower-Middle Eocene in Xihu Sag of East China Sea Basin[J].Journal of Earth Sciences and Environment,2014,36(03):31.
[3]武春英,韩会平,康锐,等.鄂尔多斯盆地苏里格南部地区盒8段沉积相特征及其意义[J].地球科学与环境学报,2014,36(04):77.
 WU Chun-ying,HAN Hui-ping,KANG Rui,et al.Characteristics and Significance of Sedimentary Facies in He-8Member in the Southern Sulige Area of Ordos Basin[J].Journal of Earth Sciences and Environment,2014,36(03):77.
[4]李骞,田孝茹,胡瀚文,等.天山北缘安集海河组湖相灰岩氧碳同位素变化的古环境意义[J].地球科学与环境学报,2016,38(03):398.
 LI Qian,TIAN Xiao-ru,HU Han-wen,et al.Paleo-environmental Significance of Oxygen and Carbon Isotopic Records in Lacustrine Limestone from Anjihaihe Formation, Northern Tianshan[J].Journal of Earth Sciences and Environment,2016,38(03):398.
[5]时瑞坤,陈世悦,鄢继华,等.辽河西部凹陷欢喜岭地区沙河街组沉积特征及其演化[J].地球科学与环境学报,2011,33(03):275.
 SHI Rui-kun,CHEN Shi-yue,YAN Ji-hua,et al.Sedimentary Characteristics and Evolution of Shahejie Formation of Huanxiling Area in the West Depression, Liaohe Basin[J].Journal of Earth Sciences and Environment,2011,33(03):275.
[6]邵洪伟,马青,邓强,等.轮南地区石炭系砂泥岩段S3层储层特征与评价[J].地球科学与环境学报,2010,32(01):54.
 SHAO Hong-wei,MA Qing,DENG Qiang,et al.Reservoir Characteristics and Evaluation on S3 Sand Layer of Carboniferous Sand and Claystone Member in Lunnan Area[J].Journal of Earth Sciences and Environment,2010,32(03):54.
[7]钟福平,钟建华,由伟丰,等.内蒙古雅布赖盆地红柳沟中侏罗统沉积相及沉积环境研究[J].地球科学与环境学报,2010,32(02):149.
 ZHONG Fu-ping,ZHONG Jian-hua,YOU Wei-feng,et al.Study on Sedimentary Facies and Environment of Middle Jurassic in Hongliugou of Yabulai Basin, Inner Mongolia[J].Journal of Earth Sciences and Environment,2010,32(03):149.
[8]丁海军,孟祥化,葛 铭,等.贺兰拗拉谷北段奥陶系等深流沉积[J].地球科学与环境学报,2009,31(01):58.
 DING Hai-jun,MENG Xiang-hua,GE Ming,et al.Ordovician Contourite of the North Part of Helan Aulacogen[J].Journal of Earth Sciences and Environment,2009,31(03):58.
[9]明海会,金振奎,李清作,等.泌阳凹陷安棚油田深层系沉积相 及对油气分布的控制作用[J].地球科学与环境学报,2005,27(02):48.
 MING Hai-hui,JIN Zhen-kui,LI Qing-zuo,et al.Sedimentary facies of deep sequences of Anpeng Oilfield in Biyang Depression and its control over oil-gas distribution[J].Journal of Earth Sciences and Environment,2005,27(03):48.
[10]钱杰,冯文光,董志林,等.大庆萨尔图中部油田主力油层 单元间夹层发育特征[J].地球科学与环境学报,2005,27(03):23.
 QIAN Jie,FENG Wen-guang,DONG Zhi-lin,et al.Sediment characteristics of interunited interlays of chief zone in central saertu oilfield , Daqing[J].Journal of Earth Sciences and Environment,2005,27(03):23.

备注/Memo

备注/Memo:
收稿日期:2009-10-24
基金项目: 中国石油天然气股份公司项目(07-01C-01-04)
作者简介: 董 洁(1984-),女,山西运城人,理学硕士研究生,从事沉积学及岩相古地理研究。E-mail:dj8418@126.com
更新日期/Last Update: 2010-09-20