必须声明标量变量 "@Script_ID"。 鄂尔多斯盆地子长地区延长组深水砂岩露头精细解剖-《地球科学与环境学报》
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[1]江涧,赵俊峰*,李嫄.鄂尔多斯盆地子长地区延长组深水砂岩露头精细解剖[J].地球科学与环境学报,2019,41(04):491-504.
 JIANG Jian,ZHAO Jun-feng*,LI Yuan.Finely Outcrop Analysis of Deep Water Sandstones from Yanchang Formation in Zichang Area of Ordos Basin, China[J].Journal of Earth Sciences and Environment,2019,41(04):491-504.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第04期
页码:
491-504
栏目:
基础地质与矿产地质
出版日期:
2019-07-15

文章信息/Info

Title:
Finely Outcrop Analysis of Deep Water Sandstones from Yanchang Formation in Zichang Area of Ordos Basin, China
文章编号:
1672-6561(2019)04-0491-14
作者:
江涧123赵俊峰12*李嫄14
(1. 西北大学 地质学系,陕西 西安 710069; 2. 西北大学 大陆动力学国家重点实验室,陕西 西安 710069; 3. 合肥工业大学 资源与环境工程学院,安徽 合肥 230009; 4. 中国石油长庆油田分公司第一采气厂,陕西 靖边 718500)
Author(s):
JIANG Jian123 ZHAO Jun-feng12* LI Yuan14
(1. Department of Geology, Northwest University, Xi’an 710069, Shaanxi, China; 2. State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, Shaanxi, China; 3. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China; 4. No.1 Natural Gas Plant, Changqing Oilfield Company, PetroChina, Jingbian 718500, Shaanxi, China)
关键词:
深水沉积 浊积砂岩 露头 岩相 等级界面 构型单元 延长组 鄂尔多斯盆地
Keywords:
deep-water deposition turbidite sandstone outcrop lithofacies bounding surface hierarchy architectural element Yanchang Formation Ordos Basin
分类号:
P586
DOI:
-
文献标志码:
A
摘要:
鄂尔多斯盆地子长地区广泛出露延长组长1油层组深湖相浊积砂岩,在露头观测的基础上对其进行了构型单元分析。研究区长1油层组内可见7种岩相类型,分别为块状砂岩相(Sm)、具撕裂屑块状砂岩相(Smt)、平行层理砂岩相(Sh)、沙纹交错层理粉砂岩相(Fr)、同生变形构造粉砂岩相(Fd)、水平层理粉砂岩相(Fl)与块状泥岩相(Fm); 识别出水道(CH)、堤岸(LV)和朵体(LB)3种不同类型的构型单元。根据水道构型单元垂向上的岩相组合和空间分布特点,将水道分为4类,对应于浊积扇体的不同部位:在上扇区域,主要发育Ⅰ类水道(Smt-Fm-Sm),砂体横向延伸有限; 在中扇区域,主要发育Ⅱ类水道(Sm-Sh-Fr-Fl-Fm)与Ⅲ类水道(Sm-Fr-Fl-Fm),这两类砂体延伸性较好,是子长地区长1油层组深水砂体的主要组成部分; 在下扇区域,发育Ⅳ类水道(Sm-Fl-Fm)。根据水道类型的差别探索提出子长地区长1油层组深水砂体沉积模式。
Abstract:
The deep lacustrine turbidite sandstone widely develops in Chang-1 interval of Triassic Yanchang Formation, and well exposes in Zichang area of the central Ordos Basin. Based on outcrop observation, the deep lacustrine turbidite sandstone was finely analyzed to study the sedimentary architectural elements of the lacustrine turbidite sandstone. 7 different types of lithofacies, including massive sandstone facies(Sm), massive sandstone facies with teared intraclasts(Smt), parallel bedding sandstone facies(Sh), ripple cross bedding siltstone facies(Fr), contemporaneous deformed structural siltstone facies(Fd), horizontal lamination siltstone facies(Fl)and mudstone facies(Fm), were summarized in Chang-1 interval of Zichang area; and 3 kinds of architectural elements, including channel(CH), levee(LV)and lobe(LB), were recognized. The channel architectural elements can be further divided into 4 types according to their vertical association of lithofacies and spatial distribution characteristics, which correspond to different parts of turbidite fan. In the upper fan area, channel Ⅰ(Smt-Fm-Sm)is developed, and the lateral extensibility of sand body is limited. The middle fan area is mainly composed of channel Ⅱ(Sm-Sh-Fr-Fl-Fm)and channel Ⅲ(Sm-Fr-Fl-Fm); the two types of sandbodies have very large extensibility and are the main components of deep-water sandbodies of Chang-1 interval in Zichang area. In the lower fan area, channel Ⅳ(Sm-Fl-Fm)with poor lateral extensibility is developed. According to the distinction of different types of channels, the depositional model for deep water sandstones of Chang-1 interval in Zichang area was preliminarily proposed.

参考文献/References:

[1] BOUMA A H.Sedimentology of Some Flysch Deposits:A Graphic Approach to Facies Interpretation[M].Amsterdam:Elsevier,1962.
[2] SHANMUGAN G.Ten Turbidite Myths[J].Earth Science Reviews,2002,58(3):311-341.
[3] 李相博,卫平生,刘化清,等.浅谈沉积物重力流分类与深水沉积模式[J].地质论评,2013,59(4):607-614.
LI Xiang-bo,WEI Ping-sheng,LIU Hua-qing,et al.Discussion on the Classification of Sediment Gravity Flow and the Deep-water Sedimentary Model[J].Geo-logical Review,2013,59(4):607-614.
[4] MUTTI E,LUCCHI F R.Turbidites of the Northern Apennines:Introduction to Facies Analysis[J].International Geology Review,1978,20(2):125-166.
[5] STOW D A V,MAYALL M.Deep-water Sedimentary Systems:New Models for the 21st Century[J].Marine and Petroleum Geology,2000,17(2):125-135.
[6] CHEN H,XIE X,ROOIJ D V,et al.Depositional Characteristics and Spatial Distribution of Deep-water Sedimentary Systems on the Northwestern Middle-lower Slope of the Northwest Sub-basin,South China Sea[J].Marine Geophysical Research,2013,34(3/4):239-257.
[7] 庞 雄,陈长民,朱 明,等.深水沉积研究前缘问题[J].地质论评,2007,53(1):36-43.
PANG Xiong,CHEN Chang-min,ZHU Ming,et al.Frontier of the Deep-water Deposition Study[J].Geological Review,2007,53(1):36-43.
[8] 胡孝林,刘新颖,刘 琼,等.深水沉积研究进展及前缘问题[J].中国海上油气,2015,27(1):10-18.
HU Xiao-lin,LIU Xin-ying,LIU Qiong,et al.Advances in Research on Deep Water Deposition and Their Frontier Problems[J].China Offshore Oil and Gas,2015,27(1):10-18.
[9] 李利阳.浊流沉积研究的新进展:鲍马序列、海底扇的重新审视[J].沉积与特提斯地质,2015,35(4):106-112.
LI Li-yang.Current Advances in the Research of Turbidity Current Deposits:Reinterpretation of the Bouma Sequence and Submarine Fan Deposits[J].Sedimentary Geology and Tethyan Geology,2015,35(4):106-112.
[10] 何起祥,刘招君,王东坡,等.湖泊相浊积岩的主要特征及其地质意义[J].沉积学报,1984,2(4):33-46.
HE Qi-xiang,LIU Zhao-jun,WANG Dong-po,et al.Characteristics of Lacustrine Turbidites and Their Tectonic Significance[J].Acta Sedimentologica Sinica,1984,2(4):33-46.
[11] SHANMUGAM G.High-density Turbidity Currents:Are They Sandy Debris Flows?[J].Journal of Sedimentary Research,1996,66(1):2-10.
[12] SHANMUGAM G,BLOCH R B,MITCHELL S M,et al.Slump and Debris-flow Dominated Basin-floor Fans in the North Sea:An Evaluation of Conceptual Sequence-stratigraphical Models Based on Conventional Core Data[J].Geological Society,London,Special Publications,1996,103:145-176.
[13] SYVITSKI J P M.Supply and Flux of Sediment Along Hydrological Pathways:Research for the 21st Century[J].Global and Planetary Change,2003,39(1/2):1-11.
[14] 潘树新,刘化清,ZAVALA C,等.大型坳陷湖盆异重流成因的水道-湖底扇系统:以松辽盆地白垩系嫩江组一段为例[J].石油勘探与开发,2017,44(6):28-38.
PAN Shu-xin,LIU Hua-qing,ZAVALA C,et al.Sublacustrine Hyperpycnal Channel-fan System in a Large Depression Basin:A Case Study of Nen-1 Member,Cretaceous Nenjiang Formation in the Songliao Basin,NE China[J].Petroleum Exploration and Development,2017,44(6):28-38.
[15] POSTMA G,CARTIGNY M J B.Supercritical and Subcritical Turbidity Currents and Their Deposits:A Synthesis[J].Geology,2014,42(11):987-990.
[16] 尚 婷,陈 刚,李文厚,等.鄂尔多斯盆地富黄探区延长组浊流沉积与油气聚集关系[J].西北大学学报(自然科学版),2013,43(1):81-88.
SHANG Ting,CHEN Gang,LI Wen-hou,et al.Turbidity Current Deposit and Its Relation to the Hydrocarbon Accumulation of Yanchang Formation in Fuhuang Exploration Area,Ordos Basin[J].Journal of Northwest University(Natural Science Edition),2013,43(1):81-88.
[17] 刘池洋,赵红格,桂小军,等.鄂尔多斯盆地演化-改造的时空坐标及其成藏(矿)响应[J].地质学报,2006,80(5):617-638.
LIU Chi-yang,ZHAO Hong-ge,GUI Xiao-jun,et al.Space-time Coordinate of the Evolution and Reformation and Mineralization Response in Ordos Basin[J].Acta Geologica Sinica,2006,80(5):617-638.
[18] ZHAO J F,MOUNTNEY N P,LIU C Y,et al.Outcrop Architecture of a Fluvio-lacustrine Succession:Upper Triassic Yanchang Formation,Ordos Basin,China[J].Marine and Petroleum Geology,2015,68:394-413.
[19] 傅 强,吕苗苗,刘永斗.鄂尔多斯盆地晚三叠世湖盆浊积岩发育特征及地质意义[J].沉积学报,2008,26(2):186-192.
FU Qiang,LU Miao-miao,LIU Yong-dou.Developmental Characteristics of Turbidite and Its Implication on Petroleum Geology in Late-Triassic Ordos Basin[J].Acta Sedimentologica Sinica,2008,26(2):186-192.
[20] 徐勇为.陕北定边—横山地区晚三叠世晚期—早中侏罗世延安组的几种沉积体系和聚煤作用[D].武汉:中国地质大学,1989.
XU Yong-wei.Several Sedimentary Systems and Coal Accumulation of the Late Triassic to Early-Middle Jurassic Yan’an Formation in Dingbian-Hengshan Area,Northen Shaanxi[D].Wuhan:China University of Geoscience,1989.
[21] 李 祯,温显端,周慧堂,等.鄂尔多斯盆地东缘中生代延长组浊流沉积的发现与意义[J].现代地质,1995,9(1):99-107.
LI Zhen,WEN Xian-duan,ZHOU Hui-tang,et al.Discovery of Turbidity Deposit in Yanchang Group Along Eastern Margin of Ordos Basin and Its Significance[J].Geoscience,1995,9(1):99-107.
[22] 罗静兰,张成立,阎世可,等.盆地埋藏史及其对砂岩储层物性演化的影响:以陕北延长油区砂岩储层为例[J].石油与天然气地质,2001,22(2):123-127.
LUO Jing-lan,ZHANG Cheng-li,YAN Shi-ke,et al.Effect of Burial History on Physical Property of Sandstone Reservoirs:Take Yanchang Oil Region in North Shaanxi as an Example[J].Oil and Gas Geology,2001,22(2):123-127.
[23] 王起琮,李文厚,赵 虹,等.鄂尔多斯盆地东南部三叠系延长组一段湖相浊积岩特征及意义[J].地质科学,2015,41(1):54-63.
WANG Qi-cong,LI Wen-hou,ZHAO Hong,et al.Characteristics and Significance of Lacustrine Turbidites in the Member 1 of Yanchang Formation,Upper Triassic in the Southeastern Ordos Basin[J].Chinese Journal of Geology,2015,41(1):54-63.
[24] 张 惠,孟祥振,蒲仁海,等.子长—蟠龙地区长1半深—深湖相沉积及其生油意义[J].西北大学学报(自然科学版),2012,42(1):82-87.
ZHANG Hui,MENG Xiang-zhen,PU Ren-hai,et al.Chang-1 Lacustrine Sediments and Oil-source-rock Conditions in Zichang-Panlong Area[J].Journal of Northwest University(Natural Science Edition),2012,42(1):82-87.
[25] 王起琮,李文厚,赵靖舟,等.鄂尔多斯盆地延长组长1段烃源岩有机地球化学特征[J].煤田地质与勘探,2006,34(1):26-30.
WANG Qi-cong,LI Wen-hou,ZHAO Jing-zhou,et al.Organic Geochemistry Characteristics of Hydrocarbon Source Rocks in the Member 1 of Upper Triassic Yanchang Formation in Ordos Basin[J].Coal Geology and Exploration,2006,34(1):26-30.
[26] 赵俊峰,屈红军,林晋炎,等.湖泊三角洲沉积露头精细解剖:以鄂尔多斯盆地裴庄剖面为例[J].沉积学报,2014,32(6):1026-1034.
ZHAO Jun-feng,QU Hong-jun,LIN Jin-yan,et al.Outcrop-based Anatomy of a Lacustrine Delta Succession:A Case Study from Peizhuang Section,Ordos Basin[J].Acta Sedimentologica Sinica,2014,32(6):1026-1034.
[27] 廖纪佳,朱筱敏,邓秀芹,等.鄂尔多斯盆地陇东地区延长组重力流沉积特征及其模式[J].地学前缘,2013,20(2):29-39.
LIAO Ji-jia,ZHU Xiao-min,DENG Xiu-qin,et al.Sedimentary Characteristics and Modle of Gravity Flow in Triassic Yanchang Formation of Longdong Area in Ordos Basin[J].Earth Science Frontiers,2013,20(2):29-39.
[28] 李文厚,魏红红,邵 磊,等.西北地区湖相浊流沉积[J].西北大学学报(自然科学版),2001,31(1):57-62.
LI Wen-hou,WEI Hong-hong,SHAO Lei,et al.Turbidity Current Deposits of Lake Facies in Northwestern China[J].Journal of Northwest University(Natural Science Edition),2001,31(1):57-62.
[29] SESTINI G.Flysch Facies and Turbidite Sedimento-logy[J].Sedimentary Geology,1970,4(3):559-597.
[30] 吕奇奇,罗顺社,付金华,等.湖泊深水重力流沉积露头精细解剖:以鄂尔多斯盆地瑶曲剖面长7油层组为例[J].地质学报,2017,91(3):617-628.
LU Qi-qi,LUO Shun-she,FU Jin-hua,et al.Outcrop-based Analysis of a Deep-water Gravity Flow Sediments in Lake:A Case Study from the Chang-7 of Yaoqu Section,Ordos Basin[J].Acta Geologica Sinica,2017,91(3):617-628.
[31] MIALL A D.Architectural Elements and Bounding Surfaces in Channlized Clastic Deposits:Notes on Comparison Between Fluvial and Turbidite Systems[M]∥TAIRA A,MASUDA F.Sedimentary Facies in the Active Plate Margin.Tokyo:Terra Scientific Publishing Company,1989:3-15.
[32] MIALL A D.Architectural Elements and Bounding Surfaces in Fluvial Deposits:Anatomy of the Kayenta Formation(Lower Jurassic),Southwest Colorado[J].Sedimentary Geology,1988,55(3/4):233-262.
[33] MIALL A D.Architectural-element Analysis:A New Method of Facies Analysis Applied to Fluvial Deposits[J].Earth-science Reviews,1985,22(4):261-308.
[34] 王 振,张元福,张 娜,等.鄂尔多斯盆地南部地区延长组深水沉积构造特征及地质意义[J].现代地质,2018,32(1):121-132.
WANG Zhen,ZHANG Yuan-fu,ZHANG Na,et al.Deep-water Sedimentary Structures of Yanchang Formation in Southern Ordos Basin and the Geological Significance[J].Geoscience,2018,32(1):121-132.
[35] 陈全红,李文厚,郭艳琴,等.鄂尔多斯盆地南部延长组浊积岩体系及油气勘探意义[J].地质学报,2006,80(5):656-663.
CHEN Quan-hong,LI Wen-hou,GUO Yan-qin,et al.Turbidite Systems and the Significance of Petroleum Exploration of Yanchang Formation in the Southern Ordos Basin[J].Acta Geologica Sinica,2006,80(5):656-663.
[36] 兰朝利,吴 峻,张为民,等.冲积沉积构型单元分析法:原理及其适用性[J].地质科技情报,2001,20(2):37-40.
LAN Chao-li,WU Jun,ZHANG Wei-min,et al.Architectural Element Analysis for Alluvial Deposits:Principle and Applicability[J].Geological Science and Technology Information,2001,20(2):37-40.
[37] MIALL A D.Reservoir Heterogeneities in Fluvial Sandstones:Lessons from Outcrop Studies[J].AAPG Bulletin,1988,72(6):682-697.
[38] ALLEN J R L.Studies in Fluviatile Sedimentation:An Exploratory Quantitative Model for the Architecture of Avulsion-controlled Alluvial Suites[J].Sedimentary Geology,1978,21(2):129-147.
[39] 蒋 平,赵应成,李顺明,等.不同沉积体系储集层构型研究与展望[J].新疆石油地质,2013,34(1):111-115.
JIANG Ping,ZHAO Ying-cheng,LI Shun-ming,et al.Reservoir Configuration Research and Prospect of Different Deposit Systems[J].Xinjiang Petroleum Geology,2013,34(1):111-115.
[40] 王志章,张国印,周 旭,等.储集层构型分析及其在油田开发中的意义[J].新疆石油地质,2012,33(1):61-64.
WANG Zhi-zhang,ZHANG Guo-yin,ZHOU Xu,et al.Reservoir Configuration Analysis and Its Significance in Oilfield Development[J].Xinjiang Petroleum Geology,2012,33(1):61-64.
[41] POSAMENTIER H W,KOLLA V.Seismic Geomorphology and Stratigraphy of Depositional Elements in Deep-water Settings[J].Journal of Sedimentary Research,2003,73(3):367-388.
[42] 林 煜,吴胜和,王 星,等.深水浊积水道体系构型模式研究:以西非尼日尔三角洲盆地某深水研究区为例[J].地质论评,2013,59(3):510-520.
LIN Yu,WU Sheng-he,WANG Xing,et al.Research on Architecture Model of Deepwater Turbidity Channel System:A Case Study of a Deepwater Research Area in Niger Delta Basin,West Africa[J].Geological Review,2013,59(3):510-520.
[43] KANE I A,HODGSON D M.Sedimentological Criteria to Differentiate Submarine Channel Levee Subenvironments:Exhumed Examples from the Rosario Fm.(Upper Cretaceous)of Baja California,Mexico,and the Fort Brown Fm.(Permian),Karoo Basin,South Africa[J].Marine and Petroleum Geology,2011,28(3):807-823.
[44] 李志鹏,杨 勇,侯加根,等.渤南五区浊积水道砂体储层构型研究[J].中国石油大学学报(自然科学版),2015,39(5):36-42.
LI Zhi-peng,YANG Yong,HOU Jia-gen,et al.Reservoir Architecture of Turbidity Channels in the 5th Area of Bonan Oilfield[J].Journal of China University of Petroleum(Natural Science Edition),2015,39(5):36-42.
[45] PICKERING K T,HISCOTT R N,KENYON N H,et al.Architectural Element Analysis of Turbidite Systems,and Selected Topical Problems for Sand-prone Deep-water Systems[M]∥PICKERING K T,HISCOTT R N,KENYON N H,et al.Atlas of Deep Water Environments:Architectural Style in Turbidite Systems.Berlin:Springer,1995:1-10.
[46] ZELT F B,ROSSEN C.Geometry and Continuity of Deep-water Sandstones and Siltstones,Brushy Canyon Formation(Permian)Delaware Mountains,Texas[M]∥PICKERING K T,HISCOTT R N,KENYON N H,et al.Atlas of Deep Water Environments:Architectural Style in Turbidite Systems.Berlin:Springer,1995:167-183.
[47] 李 华,何幼斌,王振奇.深水高弯度水道-堤岸沉积体系形态及特征[J].古地理学报,2011,13(2):139-149.
LI Hua,HE You-bin,WANG Zhen-qi.Morphology and Characteristics of Deep Water High Sinuous Channel-levee System[J].Journal of Palaeogeography,2011,13(2):139-149.
[48] 李 华,何幼斌,冯 斌,等.鄂尔多斯盆地西缘奥陶系拉什仲组深水水道沉积类型及演化[J].地球科学,2018,43(6):2149-2159.
LI Hua,HE You-bin,FENG Bin,et al.Type and Evolution of Deep-water Channel Deposits of Ordovician Lashizhong Formation in Western Margin of Ordos Basin[J].Earth Science,2018,43(6):2149-2159.
[49] 万琼华,陈 亮,林 煜,等.基于深水浊积水道构型的流动单元分布规律[J].石油与天然气地质,2015,36(2):306-313.
WAN Qiong-hua,CHEN Liang,LIN Yu,et al.Analysis of Flow Unit Distribution Based on Architecture of Deep-water Turbidite Channel Systems[J].Oil and Gas Geology,2015,36(2):306-313.
[50] 刘 芬,朱筱敏,李 洋,等.鄂尔多斯盆地西南部延长组重力流沉积特征及相模式[J].石油勘探与开发,2015,42(5):577-588.
LIU Fen,ZHU Xiao-min,LI Yang,et al.Sedimentary Characteristics and Facies Modle of Gravity Flow Deposits of Late Triassic Yanchang Formation in Southwestern Ordos Basin,NW China[J].Petroleum Exploration and Development,2015,42(5):577-588.
[51] 邹才能,赵政璋,杨 华,等.陆相湖盆深水砂质碎屑流成因机制与分布特征:以鄂尔多斯盆地为例[J].沉积学报,2009,27(6):1065-1075.
ZOU Cai-neng,ZHAO Zheng-zhang,YANG Hua,et al.Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin[J].Acta Sedimentologica Sinica,2009,27(6):1065-1075.
[52] MUTTI E.Turbidite Systems and Their Relations to Depositional Sequences[M]∥ZUFFA G G.Provenance of Arenites.Dordrecht:Springer,1985:65-93.
[53] ZOU C N,WANG L,LI Y,et al.Deep-lacustrine Transformation of Sandy Debrites into Turbidites,Upper Triassic,Central China[J].Sedimentary Geology,2012,265/266:143-155
[54] HANSEN L A S,CALLOW R H T,KANE I A,et al.Genesis and Character of Thin-bedded Turbidites Associated with Submarine Channels[J].Marine and Petroleum Geology,2015,67:852-879.
[55] XIAN B Z,WANG J H,GONG C L,et al.Classification and Sedimentary Characteristics of Lacustrine Hyperpycnal Channels:Triassic Outcrops in the South Ordos Basin,Central China[J].Sedimentary Geology,2018,368:68-82.

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备注/Memo

备注/Memo:
收稿日期:2019-04-13; 修回日期:2019-05-20投稿网址:http://jese.chd.edu.cn/
基金项目:国家基础科学人才培养基金地质学科学研究培训项目(XDCX2015-18); 国家重点研发计划项目(2017YFC0603106)
作者简介:江涧(1995-),男,江西上饶人,合肥工业大学理学硕士研究生,E-mail:2734365251@qq.com。
*通讯作者:赵俊峰(1975-),男,山西晋中人,副教授,博士研究生导师,工学博士,E-mail:zjf@nwu.edu.cn。
更新日期/Last Update: 2019-07-11