必须声明标量变量 "@Script_ID"。 浅水三角洲分流河道沉积模式分类-《地球科学与环境学报》
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[1]王夏斌,姜在兴,胡光义,等.浅水三角洲分流河道沉积模式分类[J].地球科学与环境学报,2020,42(05):654-667.[doi:10.19814/j.jese.2020.04053]
 WANG Xia-bin,JIANG Zai-xing,HU Guang-yi,et al.Classification of Sedimentary Models of Distributary Channels in Shallow-water Deltas[J].Journal of Earth Sciences and Environment,2020,42(05):654-667.[doi:10.19814/j.jese.2020.04053]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第05期
页码:
654-667
栏目:
基础地质与矿产地质
出版日期:
2020-09-15

文章信息/Info

Title:
Classification of Sedimentary Models of Distributary Channels in Shallow-water Deltas
文章编号:
1672-6561(2020)05-0654-14
作者:
王夏斌1姜在兴2胡光义1范廷恩1范洪军1何明薇1陈 飞1
1. 中海油研究总院有限责任公司,北京 100028; 2. 中国地质大学(北京)能源学院,北京 100083
Author(s):
WANG Xia-bin1 JIANG Zai-xing2 HU Guang-yi1 FAN Ting-en1 FAN Hong-jun1 HE Ming-wei1 CHEN Fei1
1.CNOOC Research Institute Co. Ltd., Beijing 100028, China; 2. School of Energy Resources, China University of Geosciences, Beijing 100083, China
关键词:
浅水三角洲 分流河道 探地雷达 卫星影像 隔夹层 青海湖 鄱阳湖 渤海湾盆地
Keywords:
shallow-water delta distributary channel ground-penetrating radar satellite imagery interlayer Qinghai Lake Poyang Lake Bohai Bay Basin
分类号:
P618.13; TE122
DOI:
10.19814/j.jese.2020.04053
文献标志码:
A
摘要:
通过浅水三角洲现代沉积考察分析,结合探地雷达(GPR)资料,对浅水三角洲分类方案和对应的沉积模式进行探讨。结果表明:根据分流河道弯曲指数和分叉参数,将浅水三角洲分为分叉平直河三角洲、分叉曲流河三角洲、分汇曲流河三角洲和分汇辫状河三角洲4种类型,并建立了各类型的沉积模式; 浅水三角洲沉积模式的控制因素是分流河道下蚀作用和侧蚀作用的强度。将该沉积模式应用于渤海南部海域BZ25-1油田新近系明化镇组下段砂体内部构型的研究认为:明化镇组下段4油层组2小层(NmⅣ2)时期是低位体系域早期,发育分汇曲流河三角洲,河道间为侧积隔夹层; 明化镇组下段4油层组1小层(NmⅣ1)时期湖平面上升,发育分汇辫状河三角洲,河道间为垂积隔夹层。这为下一步的开发方案设计提供了指导。
Abstract:
Through the analysis of modern shallow-water delta sediments, combined with the ground-penetrating radar(GPR)data, the classification and sedimentary models of shallow-water delta were discussed. The results show that according to flexural indices and bifurcation parameters of distributary channel, shallow-water delta can be divided into four types, including distributary straight river delta, distributary meandering river delta, barrier meandering river delta and barrier braided river delta, and the corresponding sedimentary models are built; the controlling factors of shallow-water delta sedimentary models are the strength of distributary channel incision and lateral erosion. The sedimentary models can be applied to the research on sand body architecture of Lower Neogene Minghuazhen Formation in BZ25-1 oilfield of South Bohai. The period of single layer 2 of oil layer group 4 in Minghuazhen Formation(NmⅣ2)is the early low system tract, distributary meandering river delta is developed, and the lateral accretion interbeds are developed; the lake level rises in the period of single layer 1 of oil layer group 4 in Minghuazhen Formation(NmⅣ1), barrier braided river delta is developed, and the vertical accretion interbeds are developed. The above research provides guidance for the next development project design.

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备注/Memo

备注/Memo:
收稿日期:2020-04-23; 修回日期:2020-06-24; 网络首发日期:2020-08-31投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家科技重大专项项目(2011ZX05024-001)
作者简介:王夏斌(1988-),男,江苏扬州人,工程师,工学博士,E-mail:wangxb35@cnooc.com.cn。
更新日期/Last Update: 2020-09-20