鄂尔多斯盆地杭锦旗地区晚古生代盆缘古地貌控砂及油气勘探意义

胡华蕊; 邢凤存; 齐荣; 王超; 刘晓晨; 陈林; 陈孝全

doi:10.11781/sysydz201904491

鄂尔多斯盆地杭锦旗地区晚古生代盆缘古地貌控砂及油气勘探意义

doi: 10.11781/sysydz201904491

胡华蕊^1,2,
邢凤存^1,2, ,,
齐荣³,
王超⁴,
刘晓晨^5,6,
陈林⁷,
陈孝全^1,2

1. 油气藏地质与开发工程国家重点实验室(成都理工大学), 成都 610059;
2. 成都理工大学沉积地质研究院, 成都 610059;
3. 中国石化华北油气分公司勘探开发研究院, 郑州 450006;
4. 中国石化江汉油田分公司勘探开发研究院, 湖北 430223;
5. 中国地质大学(武汉) 构造与油气资源教育部重点实验室, 武汉 430074;
6. 中国地质大学资源学院, 武汉 430074;
7. 武汉地质调查中心, 武汉 430205

基金项目:

国家自然科学基金项目（41672103，41302089）和成都理工大学中青年骨干教师培养计划项目联合资助。

详细信息

作者简介:
胡华蕊(1983-),女,博士研究生,从事沉积学、层序地层学等研究。E-mail:hhr_889@163.com。

通讯作者:
邢凤存(1978-),男,博士,副教授,从事沉积学、油气储层地质学和层序地层学等研究。E-mail:xingfengcun@163.com。

中图分类号: TE121.3
计量
- 文章访问数: 974
- HTML全文浏览量: 131
- PDF下载量: 156
- 被引次数: 0
出版历程
- 收稿日期: 2019-02-21
- 修回日期: 2019-06-28
- 刊出日期: 2019-07-28

Paleogeomorphologic features and their controls on sandbody distribution on basin margin during Late Paleozoic Era and significance for petroleum exploration, Hangjinqi area, Ordos Basin

HU Huarui^1,2,
XING Fengcun^{1,2
, ,},
QI Rong³,
WANG Chao⁴,
LIU Xiaochen^5,6,
CHEN Lin⁷,
CHEN Xiaoquan^1,2

1. State Key Laboratory of Oil and Gas Reservoir Geology(Chengdu University of Technology), Chengdu, Sichuan 610059, China;
2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
3. Research Institute of Exploration and Development, SINOPEC Huabei Oilfield Company, Zhengzhou, Henan 450006, China;
4. Research Institute of Exploration and Development, SINOPEC Jianghan Oilfield, Wuhan, Hubei 430223, China;
5. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China;
6. Faculty of Earth Resource, China University of Geosciences, Wuhan, Hubei 430074, China;
7. Wuhan Center of China Geological Survey, Wuhan, Hubei 430205, China

摘要

摘要: 使用井震资料，在高精度层序地层格架建立的基础上，对鄂尔多斯盆地杭锦旗地区晚古生代古地貌进行了恢复，探讨了古地貌演化及其沉积和砂体响应。该区上石炭统太原组-中二叠统下石盒子组盒1段沉积期，古地貌具有东西向两隆三洼格局，垂向上划分出太原组-山1段沟谷超覆充填、山2段-盒1段隆洼继承性填平、盒2段-盒3段均一平整等3个古地貌演化阶段。不同地貌演化阶段控制了砂体结构演化，沟谷超覆充填阶段，太原组仅分布在泊尓江海子断裂南部，反映了该断裂的控制性，北部沟谷输砂、南部低洼区聚砂明显，砂体以垂向加积样式分布于隆起分隔的沟谷及低洼区域；隆洼继承性填平阶段，地貌逐渐平整化，断裂控制不明显，砂体连片且具有一定的侧向摆动，3个继承性低洼区为主砂体区；均一平整阶段，物源北退，地貌平整，形成了"泥包砂"且横向摆动的孤立砂体分布结构。
- 古地貌恢复 /
- 致密砂岩 /
- 晚古生代 /
- 杭锦旗地区 /
- 鄂尔多斯盆地
Abstract: The paleogeomorphology in the Hangjinqi area of the Ordos Basin during the Late Paleozoic was restored by establishing a high-resolution sequence stratigraphy framework based on seismic data. The paleogeomorphologic features and their controls on sandbody distribution were discussed. When the Carboniferous Taiyuan Formation to the first member of Permain Shihezi Formation deposited, the study area featured by two distinct uplifts and three depressions from east to west. Vertically, three evolution periods were identified. In the first period, incised valleys developed and were overlapped and filled from the Taiyuan Formation to the first member of Shanxi Formation. In the second period, uplifts and depressions were inherited and gradually filled from the second member of Shanxi Formation to the first member of Shihezi Formation. In the last period, paleogeo-morphology was gentle and flat from the second to the third member of Shihezi Formation. Different periods of geomorphological evolution controlled the sandbody structure evolution. At the first period, the Taiyuan Formation distributed in the southern of Boerjianghaizi fault, which indicates the influence of the fault. Sand transported from the incised valleys in the north to deposit in the depressions in the south. Aggradational sandbodies deposited in the incised valleys and depressions. In the second period, the paleogeomorphology gradually became more and more flat, and faults showed weak controls on sandbody distribution. Sandbodies were contiguous with a certain degree of lateral oscillation. The inherited three depressions were the main distribution area of sandbodies. In the final period, sources retreated northward, and the paleogeomorphology was flat which formed the structure of mudstone-enclosed isolated sandbodies characterized by lateral isolation.
- paleogeomorphology reconstruction /
- tight sandstone /
- Late Paleozoic Era /
- Hangjinqi area /
- Ordos Basin

HTML全文

参考文献(21)

[1]	郑文波,胡向阳,陈舒薇,等.鄂尔多斯盆地大牛地气田上古生界沉积演化特征[J].沉积学报,2015,33(2):306-313. ZHENG Wenbo,HU Xiangyang,CHEN Shuwei,et al.Characte-ristics of sedimentary evolution in the Upper Paleozoic,Daniudi Gasfield,Ordos Basin[J].Acta Sedimentologica Sinica,2015,33(2):306-313.
[2]	孙晓,李良,丁超.鄂尔多斯盆地杭锦旗地区不整合结构类型及运移特征[J].石油与天然气地质,2016,37(2):165-172. SUN Xiao,LI Liang,DING Chao.Unconformity structure types and hydrocarbon migration characteristics in Hangjinqi area of Ordos Basin[J].Oil & Gas Geology,2016,37(2):165-172.
[3]	郝蜀民,李良,张威,等.鄂尔多斯盆地北缘石炭系-二叠系大型气田形成条件[J].石油与天然气地质,2016,37(2):149-154. HAO Shumin,LI Liang,ZHANG Wei,et al.Forming conditions of large-scale gas fields in Permo-Carboniferous in the northern Ordos Basin[J].Oil & Gas Geology,2016,37(2):149-154.
[4]	朱宗良,李文厚,李克永,等.杭锦旗地区上古生界层序及沉积体系发育特征[J].西北大学学报(自然科学版),2010,40(6):1050-1054. ZHU Zongliang,LI Wenhou,LI Keyong,et al.The characteristic of sequence stratigraphy and sedimentary systems of Taiyuan-Xiashihezi formation in Hangjinqi area[J].Journal of Northwest University (Natural Science Edition),2010,40(6):1050-1054.
[5]	陈洪德,李洁,张成弓,等.鄂尔多斯盆地山西组沉积环境讨论及其地质启示[J].岩石学报,2011,27(8):2213-2229. CHEN Hongde,LI Jie,ZHANG Chenggong,et al.Discussion of sedimentary environment and its geological enlightenment of Shanxi Formation in Ordos Basin[J].Acta Petrologica Sinica,2011,27(8):2213-2229.
[6]	李婕,赵俊兴,孔祥超,等.鄂北杭锦旗地区下石盒子组沉积相演化及控制因素[J].山东科技大学学报(自然科学版),2013,32(2):34-42. LI Jie,ZHAO Junxing,KONG Xiangchao,et al.Sedimentary facies evolution and controlling factors of Lower Shihezi Formation in Hangjinqi area,north Ordos Basin[J].Journal of Shandong University of Science and Technology(Natural Science),2013,32(2):34-42.
[7]	邱隆伟,朱士波,高青松,等.杭锦旗地区山西组辫状河三角洲的判定及其沉积演化[J].河南理工大学学报(自然科学版),2015,34(5):626-633. QIU Longwei,ZHU Shibo,GAO Qingsong,et al.Judgement and sedimentary evolution of braided river delta of Shanxi Formation in Hangjinqi area[J].Journal of Henan Polytechnic University (Natural Science),2015,34(5):626-633.
[8]	倪春华,刘光祥,朱建辉,等.鄂尔多斯盆地杭锦旗地区上古生界天然气成因及来源[J].石油实验地质,2018,40(2):193-199. NI Chunhua,LIU Guangxiang,ZHU Jianhui,et al.Origin and source of natural gas in the Upper Paleozoic in Hangjinqi area,Ordos Basin[J].Petroleum Geology and Experiment,2018,40(2):193-199.
[9]	齐荣,李良.鄂尔多斯盆地杭锦旗地区泊尔江海子断裂以北有效圈闭的识别[J].石油实验地质,2018,40(6):793-799. QI Rong,LI Liang.Identification of effective traps north of Boerjianghaizi Fault,Hangjinqi area,Ordos Basin[J].Petroleum Geology and Experiment,2018,40(6):793-799.
[10]	XIA Lu,LIU Zhen,LI Weilian,et al.Initial porosity and compaction of consolidated sandstone in Hangjin Qi,North Ordos Basin[J].Journal of Petroleum Science and Engineering,2018,166:324-336.
[11]	赵振宇,郭彦如,王艳,等.鄂尔多斯盆地构造演化及古地理特征研究进展[J].特种油气藏,2012,19(5):15-20. ZHAO Zhenyu,GUO Yanru,WANG Yan,et al.Study progress in tectonic evolution and paleogeography of Ordos Basin[J].Special Oil & Gas Reservoirs,2012,19(5):15-20.
[12]	王双明.鄂尔多斯盆地叠合演化及构造对成煤作用的控制[J].地学前缘,2017,24(2):54-63. WANG Shuangming.Ordos Basin superposed evolution and structural controls of coal forming activities[J].Earth Science Frontiers,2017,24(2):54-63.
[13]	陈洪德,侯中健,田景春,等.鄂尔多斯地区晚古生代沉积层序地层学与盆地构造演化研究[J].矿物岩石,2001,21(3):16-22. CHEN Hongde,HOU Zhongjian,TIAN Jingchun,et al.Study on sequence stratigraphy of deposits and tectono-sedimentary evolution in Ordos Basin during Late Palaeozoic[J].Journal of Mineralogy and Petrology,2001,21(3):16-22.
[14]	付锁堂,石小虎,南珺祥.鄂尔多斯盆地东北部上古生界太原组及下石盒子组碎屑岩储集层特征[J].古地理学报,2010,12(5):609-617. FU Suotang,SHI Xiaohu,NAN Junxiang.Characteristics of clastic reservoir of the Upper Paleozoic Taiyuan and Xiashihezi formations in northeastern Ordos Basin[J].Journal of Palaeogeography,2010,12(5):609-617.
[15]	窦伟坦,侯明才,董桂玉.鄂尔多斯盆地北部山西组-下石盒子组物源分析[J].天然气工业,2009,29(3):25-28. DOU Weitan,HOU Mingcai,DONG Guiyu.Provenance analysis of the Upper Paleozoic Shanxi to Lower Shihezi formations in north Ordos basin[J].Natural Gas Industry,2009,29(3):25-28.
[16]	ZHU Hongtao,CHEN Kaiyuan,LIU Keyu,et al.A sequence stratigraphic model for reservoir sand-body distribution in the Lower Permian Shanxi Formation in the Ordos Basin,northern China[J].Marine and Petroleum Geology,2008,25(8):731-743.
[17]	郭顺,闫继福,郭兰,等.鄂北杭锦旗地区太原组沉积微相分析[J].西北大学学报(自然科学版),2009,39(2):283-287. GUO Shun,YAN Jifu,GUO Lan,et al.The sedimentary microfacies of Taiyuan Formation in the Hangjinqi area,the north of Ordos Basin[J].Journal of Northwest University(Natural Science Edition),2009,39(2):283-287.
[18]	李潍莲,纪文明,刘震,等.鄂尔多斯盆地北部泊尔江海子断裂对上古生界天然气成藏的控制[J].现代地质,2015,29(3):584-590. LI Weilian,JI Wenming,LIU Zhen,et al.Control of Boerjianghaizi Fault on gas accumulation of Upper Paleozoic in northern Ordos Basin[J].Geoscience,2015,29(3):584-590.
[19]	肖冬生,付强.鄂尔多斯盆地北部杭锦旗区块下石盒子组自生石英形成机制[J].岩石矿物学杂志,2011,30(1):113-120. XIAO Dongsheng,FU Qiang.The genetic mechanism of authigenic quartz in Lower Shihezi Formation of Hanggin Banner,northern Ordos Basin[J].Acta Petrologica et Mineralogica,2011,30(1):113-120.
[20]	王付斌,马超,安川.鄂北杭锦旗地区三维地震勘探难点与对策[J].石油化工应用,2016,35(6):109-113. WANG Fubin,MA Chao,AN Chuan.The difficulties and countermeasures of 3-D seismic exploration in Hangjinqi area[J].Petrochemical Industry Application,2016,35(6):109-113.
[21]	邢凤存,陆永潮,刘传虎,等.车排子地区构造-古地貌特征及其控砂机制[J].石油与天然气地质,2008,29(1):78-83. XING Fengcun,LU Yongchao,LIU Chuanhu,et al.Structural-paleogeomorphologic features of Chepaizi area and mechanism of their control on sandbodies[J].Oil & Gas Geology,2008,29(1):78-83.