必须声明标量变量 "@Script_ID"。 鄂尔多斯盆地东北缘府谷剖面中二叠统盒8段沉积相特征-《地球科学与环境学报》
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[1]孙诗,王峰*,陈洪德,等.鄂尔多斯盆地东北缘府谷剖面中二叠统盒8段沉积相特征[J].地球科学与环境学报,2019,41(02):225-240.
 SUN Shi,WANG Feng*,CHEN Hong-de,et al.Sedimentary Facies Characteristics of He-8 Member of Middle Permian in Fugu Section, the Northeastern Margin of Ordos Basin, China[J].Journal of Earth Sciences and Environment,2019,41(02):225-240.
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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02期
页码:
225-240
栏目:
基础地质与矿产地质
出版日期:
2019-03-15

文章信息/Info

Title:
Sedimentary Facies Characteristics of He-8 Member of Middle Permian in Fugu Section, the Northeastern Margin of Ordos Basin, China
文章编号:
1672-6561(2019)02-0225-16
作者:
孙诗12王峰12*陈洪德12魏新善3陈东阳12祝圣贤12
(1.成都理工大学 油气藏地质及开发工程国家重点实验室,四川 成都 610059; 2.成都理工大学 沉积地质研究院,四川 成都 610059; 3.中国石油长庆油田分公司勘探开发研究院,陕西 西安 710018)
Author(s):
SUN Shi12 WANG Feng12* CHEN Hong-de12 WEI Xin-shan3 CHEN Dong-yang12 ZHU Sheng-xian12
(1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 3. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi’an 710018, Shaanxi, China)
关键词:
相标志 盒8段 沉积微相 垂向序列 辫状河 曲流河 鄂尔多斯盆地
Keywords:
facies marker He-8 member sedimentary microfacies vertical sequence braided river meandering river Ordos Basin
分类号:
P624; TE122
DOI:
-
文献标志码:
A
摘要:
鄂尔多斯盆地苏里格东部地区中二叠统盒8段为主力产气层,厘清其沉积相特征对指导该地区的天然气勘探具有重要意义。鄂尔多斯盆地东北缘府谷剖面与苏里格东部地区具有相似的物源体系与沉积环境,通过对府谷剖面进行实测,结合剖面岩石颜色、岩石学特征、微量元素特征、岩相特征等相标志分析,对盒8段沉积相进行准确划分并明确其沉积特征,可以弥补苏里格东部地区盒8段研究大部分局限于钻井、地震等方面,缺乏露头沉积相支撑的不足。结果表明:府谷剖面盒8段以灰绿、黄绿色粗—中粒岩屑砂岩为主,结构成熟度中等—较低; 微量元素V/(V+Ni)值表明盒8段沉积时期为氧化—弱还原过渡环境; 共划分出12种岩相,其中,块状砾岩相(Gm)、槽状交错层理砂岩相(St)、板状交错层理砂岩相(Sp)、平行层理砂岩相(Sh)为河流沉积中的典型岩相,不同岩相组合构成盒8段沉积体两种不同的垂向沉积序列; 盒8段—盒82段为辫状河沉积,盒81段为曲流河沉积; 辫状河的垂向沉积序列由滞留沉积(Gm-Gst-Gsp)→心滩(Gst-Sq-Sp-St-Gm-St)→河道充填(Gm-St-Sh-M)→废弃河道(Sh-Fr-Mh-Sh-Fr-Mh)→越岸沉积(Sh-Fr-Mh-Fr-Mh)→泛滥平原(M-Mh-Mc-Mh-M)等6类微相构成了一个二元结构不明显的正粒序沉积序列; 曲流河的垂向沉积序列由滞留沉积(Gm)→边滩(Sp-St-Sm-Sp-St-Sh)→河漫滩(M-Mh-Mc(Fr)-Mh-M)等3类微相构成了一个典型二元结构沉积序列。
Abstract:
The He-8 member of Middle Permian in the eastern Sulige area of Ordos Basin is the main gas producing bed, and is of great significance to clarify the sedimentary facies characteristics for guiding the natural gas exploration. There are similar provenance systems and sedimentary environments between the eastern Sulige area and Fugu section in the northeastern margin of Ordos Basin. By measuring Fugu section combined with facies markers such as color, petrology, trace elements and lithofacies characteristics, the sedimentary facies of He-8 member was divided accurately, and the sedimentary characteristics were clarified to make up for the lack of outcrop sedimentary facies support in most of the previous study of He-8 member in the eastern Sulige area, which was limited to drilling and earthquake. The results show that the grayish green and yellowish green coarse to medium grained lithic sandstone are the main ones in He-8 member of Fugu section, and the structure maturity is medium to low; the trace element V/(V+Ni)ratio indicates that the depositional period of He-8 member is a transitional environment of oxidation-weak reduction; there are 12 types of lithofacies, among which Gm, St, Sp, Sh are typical lithofacies in fluvial sediments, and two different vertical sedimentary sequences are formed by different lithofacies combinations; He-8 lower member to He-8 upper-2 member is braided river deposit, and He-8 upper-1 member is meandering river deposit; the vertical sedimentary sequence of braided rivers consists of six types of microfacies, including stranded sediment(Gm-Gst-Gsp), braided river bar(Gst-Sq-Sp-St-Gm-St), channel filling(Gm-St-Sh-M), abandoned channel(Sh-Fr-Mh-Sh-Fr-Mh), overbank deposits(Sh-Fr-Mh-Fr-Mh)and flood plain(M-Mh-Mc-Mh-M), and forms a sequence of normal sequence deposits with a binary structure unobviously; the vertical sedimentary sequence of meandering river consists of three types of microfacies, including stranded sediment(Gm), side beaches(Sp-St-Sm-Sp-St-Sh)and flood land(M-Mh-Mc(Fr)-Mh-M), and constitutes a typical binary structure sedimentary sequence.

参考文献/References:

[1] 何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.
HE Zi-xin.Evolution and Oil-gas of Ordos Basin[M].Beijing:Petroleum Industry Press,2003.
[2] 李荣西,段立志,张少妮,等.鄂尔多斯盆地低渗透油气藏形成研究现状与展望[J].地球科学与环境学报,2011,33(4):364-372.
LI Rong-xi,DUAN Li-zhi,ZHANG Shao-ni,et al.Review on Oil/Gas Accumulation with Low Permeability in Ordos Basin[J].Journal of Earth Sciences and Environment,2011,33(4):364-372.
[3] 姚泾利,胡新友,范立勇,等.鄂尔多斯盆地天然气地质条件、资源潜力及勘探方向[J].天然气地球科学,2018,29(10):1465-1474.
YAO Jing-li,HU Xin-you,FAN Li-yong,et al.The Geological Conditions,Resource Potential and Exploration Direction of Natural Gas in Ordos Basin[J].Natural Gas Geoscience,2018,29(10):1465-1474.
[4] 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 Wen-bo,HU Xiang-yang,CHEN Shu-wei,et al.Characteristics of Sedimentary Evolution in the Upper Paleozoic,Daniudi Gasfield,Ordos Basin[J].Acta Se-dimentologica Sinica,2015,33(2):306-313.
[5] 李熙喆,张满郎,谢武仁.鄂尔多斯盆地上古生界岩性气藏形成的主控因素与分布规律[J].石油学报,2009,30(2):168-175.
LI Xi-zhe,ZHANG Man-lang,XIE Wu-ren.Controlling Factors for Lithologic Gas Reservoir and Regularity of Gas Distribution in the Upper Paleozoic of Ordos Basin[J].Acta Petrolei Sinica,2009,30(2):168-175.
[6] 胡朝元,钱 凯,王秀芹,等.鄂尔多斯盆地上古生界多藏大气田形成的关键因素及气藏性质的嬗变[J].石油学报,2010,31(6):879-884.
HU Chao-yuan,QIAN Kai,WANG Xiu-qin,et al.Critical Factors for the Formation of an Upper Paleozoic Giant Gas Field with Multiple Gas Reservoirs in Ordos Basin and the Transmutation of Gas Reservoir Properties[J].Acta Petrolei Sinica,2010,31(6):879-884.
[7] 杨 华,刘新社,孟培龙.苏里格地区天然气勘探新进展[J].天然气工业,2011,31(2):1-8.
YANG Hua,LIU Xin-she,MENG Pei-long.New Development in Natural Gas Exploration of the Sulige Gas Fields[J].Natural Gas Industry,2011,31(2):1-8.
[8] 李贤庆,冯松宝,李 剑,等.鄂尔多斯盆地苏里格大气田天然气成藏地球化学研究[J].岩石学报,2012,28(3):836-846.
LI Xian-qing,FENG Song-bao,LI Jian,et al.Geochemistry of Natural Gas Accumulation in Sulige Large Gas Field in Ordos Basin[J].Acta Petrologica Sinica,2012,28(3):836-846.
[9] 杜 洋,欧阳诚,胡 杨,等.苏里格气田苏5区块储集层特征及有利勘探区域[J].新疆石油地质,2013,34(6):636-639.
DU Yang,OUYANG Cheng,HU Yang,et al.The Reservoir Characteristics and the Favorable Prospecting Target in Su-5 Block in Sulige Gas Field[J].Xinjiang Petroleum Geology,2013,34(6):636-639.
[10] 侯加根,唐 颖,刘钰铭,等.鄂尔多斯盆地苏里格气田东区致密储层分布模式[J].岩性油气藏,2014,26(3):1-6.
HOU Jia-gen,TANG Ying,LIU Yu-ming,et al.Distribution Patterns of Tight Reservoirs in Eastern Sulige Gas Field,Ordos Basin[J].Lithologic Reservoirs,2014,26(3):1-6.
[11] 何自新,付金华,席胜利,等.苏里格大气田成藏地质特征[J].石油学报,2003,24(2):6-12.
HE Zi-xin,FU Jin-hua,XI Sheng-li,et al.Geological Features of Reservoir Formation of Sulige Gas Field[J].Acta Petrolei Sinica,2003,24(2):6-12.
[12] 徐 蒙,王家豪,徐东浩,等.苏里格气田苏120区块盒8段浅水辫状河三角洲砂体演化规律[J].沉积学报,2013,31(2):340-349.
XU Meng,WANG Jia-hao,XU Dong-hao,et al.The Sandbody Evolution of Shallow-water Braided River Deltas in the Eighth Member of Shihezi Formation in Block Su120,Sulige Gas Field[J].Acta Sedimentologica Sinica,2013,31(2):340-349.
[13] 沈玉林,郭英海,李壮福.鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒8段沉积相[J].古地理学报,2006,8(1):53-62.
SHEN Yu-lin,GUO Ying-hai,LI Zhuang-fu.Sedimentary Facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in Suligemiao Area,Ordos Basin[J].Journal of Palaeogeography,2006,8(1):53-62.
[14] 李文厚,魏红红,赵 虹,等.苏里格庙地区二叠系储层特征及有利相带预测[J].西北大学学报(自然科学版),2002,32(4):335-340.
LI Wen-hou,WEI Hong-hong,ZHAO Hong,et al.Prediction of Oil-bearing Facies Belts and Reservoir Characteristics of Permian System in Suligemiao Region[J].Journal of Northwest University(Natural Science Edition),2002,32(4):335-340.
[15] 尹志军,余兴云,鲁国永,等.苏里格气田苏6区块盒8段沉积相研究[J].天然气工业,2006,26(3):26-27.
YIN Zhi-jun,YU Xing-yun,LU Guo-yong,et al.Sedimentary Facies of the 8th Member of Shihezi Formation in Block Su-6 in Sulige Gas Field[J].Natural Gas Industry,2006,26(3):26-27.
[16] 何顺利,兰朝利,门成全.苏里格气田储层的新型辫状河沉积模式[J].石油学报,2005,26(6):25-29.
HE Shun-li,LAN Chao-li,MEN Cheng-quan.New Braided River Model in Sulige Gas Field of Ordos Basin[J].Acta Petrolei Sinica,2005,26(6):25-29.
[17] 单敬福,张 吉,王继平,等.苏里格气田西区盒8下亚段辫状河沉积论证与分析[J].吉林大学学报(地球科学版),2015,45(6):1597-1607.
SHAN Jing-fu,ZHANG Ji,WANG Ji-ping,et al.Demenstration and Analysis of Braided River Deposition in the Lower He-8 Member in Western Sulige Gas Field[J].Journal of Jilin University(Earth Science Edition),2015,45(6):1597-1607.
[18] 文华国,郑荣才,高红灿,等.苏里格气田苏6井区下石盒子组盒8段沉积相特征[J].沉积学报,2007,25(1):90-98.
WEN Hua-guo,ZHENG Rong-cai,GAO Hong-can,et al.Sedmientary Facies of the 8th Member of Lower Shihezi Formation in Su6 Area,Sulige Gas Field[J].Acta Sedimentologica Sinica,2007,25(1):90-98.
[19] 徐艺嘉.鄂尔多斯盆地苏里格气田召30井区盒8段高分辨率层序地层及沉积相特征研究[D].成都:成都理工大学,2016.
XU Yi-jia.Study on High-resolution Sequence Stratigraphy and Sedimentary Facies of He-8 Section in Zhao30 Wellblock,Sulige Gas Field of Ordos Basin[D].Chengdu:Chengdu University of Technology,2016.
[20] 陈玉良.鄂尔多斯盆地盒8期原型盆地沉积体系及岩相古地理研究[D].西安:长安大学,2015.
CHEN Yu-liang.Study on Depositional Systems and Lithofacies Paleogeography of He-8 Period,Erdos Prototype Basin[D].Xi’an:Chang’an University,2015.
[21] 林孝先.陆源碎屑岩盆地综合物源分析[D].成都:成都理工大学,2011.
LIN Xiao-xian.A Synthetic Thought of Provenance Analysis in the Terrigenous Clastic Rock Basin[D].Chengdu:Chengdu University of Technology,2011.
[22] 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 Wei-tan,HOU Ming-cai,DONG Gui-yu.Provenance Analysis of the Upper Paleozoic Shanxi to Lower Shihezi Formations in North Ordos Basin[J].Natural Gas Industry,2009,29(3):25-28.
[23] 陈安清,陈洪德,向 芳,等.鄂尔多斯东北部山西组—上石盒子组砂岩特征及物源分析[J].成都理工大学学报(自然科学版),2007,34(3):305-311.
CHEN An-qing,CHEN Hong-de,XIANG Fang,et al.Sandstone Characteristic and Provenance Analysis of the Permian Shanxi Formation-Shangshihezi For-mation in the Northeast of Ordos Basin,China[J].Journal of Chengdu University of Technology(Science and Technology Edition),2007,34(3):305-311.
[24] 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):233-262.
[25] MIALL A D.Architectural Element Analysis:A New Method of Facies Analysis Applied to Fluvial Depo-sits[J].Earth-science Reviews,1985,22(4):261-308.
[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] 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.
[28] 杨 华,付金华,欧阳征健,等.鄂尔多斯盆地西缘晚三叠世构造-沉积环境分析[J].沉积学报,2011,29(3):427-439.
YANG Hua,FU Jin-hua,OUYANG Zheng-jian,et al.Analysis of Tectonic-sedimentary Setting in Middle and Upper Triassic in the West Margin of the Ordos Basin[J].Acta Sedimentologica Sinica,2011,29(3):427-439.
[29] 杨圣彬,耿新霞,郭庆银,等.鄂尔多斯盆地西缘北段中生代构造演化[J].地质论评,2008,54(3):307-315.
YANG Sheng-bin,GENG Xin-xia,GUO Qing-yin,et al.Mesozoic Tectonic Evolution in North Section of the Western Margin of Ordos Basin[J].Geological Review,2008,54(3):307-315.
[30] 张 进,马宗晋,任文军.鄂尔多斯西缘逆冲褶皱带构造特征及其南北差异的形成机制[J].地质学报,2004,78(5):600-611.
ZHANG Jin,MA Zong-jin,REN Wen-jun.Tectonic Characteristics of the Western Ordos Thrust-fold Belt and the Causes for Its North-south Segmentation[J].Acta Geologica Sinica,2004,78(5):600-611.
[31] 李相博,刘化清,完颜容,等.鄂尔多斯晚三叠世盆地构造属性及后期改造[J].石油实验地质,2012,34(4):376-382.
LI Xiang-bo,LIU Hua-qing,WAN Yan-rong,et al.Tectonic Properties and Post-reformation in Late Triassic,Ordos Basin[J].Petroleum Geology and Experiment,2012,34(4):376-382.
[32] 吉海龙.鄂尔多斯苏里格地区上古生界储层沉积相与砂体分布研究[D].北京:中国地质大学,2007.
JI Hai-long.Research on Sedimentary Facies and Sand Body Distribution of Neopaleozoic Reservoir in Sulige Area of the Ordos Basin[D].Beijing:China University of Geosciences,2007.
[33] 王 越,陈世悦,梁绘媛,等.鄂尔多斯盆地保德地区上古生界沉积相与沉积演化特征[J].沉积学报,2016,34(4):775-784.
WANG Yue,CHEN Shi-yue,LIANG Hui-yuan,et al.Sedimentary Facies and Their Evolution in the Upper Paleozoic of Baode Area,Ordos Basin[J].Acta Sedi-mentologica Sinica,2016,34(4):775-784.
[34] 鲁 静,邵龙义,孙 斌,等.鄂尔多斯盆地东缘石炭—二叠纪煤系层序-古地理与聚煤作用[J].煤炭学报,2012,37(5):747-754.
LU Jing,SHAO Long-yi,SUN Bin,et al.Sequence-paleogeography and Coalaccumulation of Carboniferous-Permian Coal Measures in the Eastern Ordos Basin[J].Journal of China Coal Society,2012,37(5):747-754.
[35] 沈玉林,郭英海,李壮福,等.鄂尔多斯盆地东缘本溪组—太原组层序地层特征[J].地球学报,2009,30(2):187-193.
SHEN Yu-lin,GUO Ying-hai,LI Zhuang-fu,et al.Sequ-ence Stratigraphy of Benxi-Taiyuan Formation in Eastern Ordos Basin[J].Acta Geoscientica Sinica,2009,30(2):187-193.
[36] 樊太亮,郭齐军,吴贤顺.鄂尔多斯盆地北部上古生界层序地层特征与储层发育规律[J].现代地质,1999,13(11):32-36.
FAN Tai-liang,GUO Qi-jun,WU Xian-shun.Features of Sequence Stratigraphy and Distribution Regularities of Reservoir in Upper Paleozoic of North Ordos Basin[J].Geoscience,1999,13(11):32-36.
[37] 杨明慧,刘池洋,兰朝利,等.鄂尔多斯盆地东北缘晚古生代陆表海含煤岩系层序地层研究[J].沉积学报,2008,26(6):1005-1013.
YANG Ming-hui,LIU Chi-yang,LAN Chao-li,et al.Sequence Stratigraphy of Late Paleozoic Coal-bearing Measure in Northeastern Ordos Basin[J].Acta Sedimentologica Sinica,2008,26(6):1005-1013.
[38] 张 驰,于兴河,李顺利,等.准噶尔盆地南缘井井子沟组露头沉积特征及模式[J].新疆石油地质,2017,38(5):544-552.
ZHANG Chi,YU Xing-he,LI Shun-li,et al.Sedimentary Characteristics and Model of Outcrop in Jingjingzigou Formation of Southern Margin,Junggar Basin[J].Xinjiang Petroleum Geology,2017,38(5):544-552.
[39] 邹妞妞,张大权,龙国辉,等.柴达木盆地北缘第三系沉积体系演化模式[J].成都理工大学学报(自然科学版),2015,42(2):149-158.
ZOU Niu-niu,ZHANG Da-quan,LONG Guo-hui,et al.Sedimentary System Evolution of Tertiary Reservoirs in Northern Qaidam Basin,China[J].Journal of Chengdu University of Technology(Science and Technology Edition),2015,42(2):149-158.
[40] 李亚龙,于兴河,单 新,等.鄂尔多斯盆地东南部下石盒子组盒8段物源特征与沉积相[J].东北石油大学学报,2016,40(3):51-58.
LI Ya-long,YU Xing-he,SHAN Xin,et al.Proven-
ance and Sedimentary Facies of He-8 Member of Xia-shihezi Formation in Southeastern Ordos Basin[J].Journal of Northeast Petroleum University,2016,40(3):51-58.
[41] 谭程鹏,于兴河,李胜利,等.准噶尔盆地南缘四棵树剖面八道湾组扇三角洲沉积特征[J].现代地质,2014,28(1):181-189.
TAN Cheng-peng,YU Xing-he,LI Sheng-li,et al.Sedimentary Characteristics of Fan Delta of the Badao-wan Formation,Sikeshu Section,Southern Junggar Basin[J].Geoscience,2014,28(1):181-189.
[42] 李玉辉,郑绵平,赵小庆,等.柴达木盆地达布逊湖北雅丹剖面沉积特征及其环境意义[J].地球科学与环境学报,2017,39(6):787-794.
LI Yu-hui,ZHENG Mian-ping,ZHAO Xiao-qing,et al.Sedimentary Characteristics and Environmental Significance of Yadan Profile in the Northern Dabsun Lake of Qaidam Basin,China[J].Journal of Earth Sciences and Environment,2017,39(6):787-794.
[43] 范玉海,曲红军,王 辉,等.微量元素分析在判别沉积介质环境中的应用:以鄂尔多斯盆地西部中区晚三叠世为例[J].中国地质,2012,39(2):382-389.
FAN Yu-hai,QU Hong-jun,WANG Hui,et al.The Application of Trace Elements Analysis to Identifying Sedimentary Media Environment:A Case Study of Late Triassic Strata in the Middle Part of Western Ordos Basin[J].Geology in China,2012,39(2):382-389.
[44] 毛光周,刘池洋.地球化学在物源及沉积背景分析中的应用[J].地球科学与环境学报,2011,34(4):337-348.
MAO Guang-zhou,LIU Chi-yang.Application of Geochemistry in Provenance and Depositional Setting Analysis[J].Journal of Earth Sciences and Environment,2011,34(4):337-348.
[45] 陈 晶,黄文辉,何明倩.鄂尔多斯盆地东南部本溪组—下石盒子组泥岩元素地球化学特征[J].现代地质,2018,32(2):240-250.
CHEN Jing,HUANG Wen-hui,HE Ming-qian.Elemental Geochemistry Characteristics of Mudstones from Benxi Formation to Lower Shihezi Formation in Southeastern Ordos Basin[J].Geoscience,2018,32(2):240-250.
[46] 雷开宇,刘池洋,张 龙,等.鄂尔多斯盆地北部侏罗系泥岩地球化学特征:物源与古沉积环境恢复[J].沉积学报,2017,35(3):621-636.
LEI Kai-yu,LIU Chi-yang,ZHANG Long,et al.Element Geochemical Characteristics of the Jurassic Mudstones in the Northern Ordos Basin:Implications for Tracing Sediment Sources and Paleo-environment Restoration[J].Acta Sedimentologica Sinica,2017,35(3):621-636.
[47] 王 峰,刘玄春,邓秀芹,等.鄂尔多斯盆地纸坊组微量元素地球化学特征及沉积环境指示意义[J].沉积学报,2017,35(6):1265-1273.
WANG Feng,LIU Xuan-chun,DENG Xiu-qin,et al.Geochemical Characteristics and Environmental Implications of Trace Elements of Zhifang Formation in Ordos Basin[J].Acta Sedimentologica Sinica,2017,35(6):1265-1273.
[48] HATCH J R,LEVENTHAL J S.Relationship Between Inferred REDOX Potential of the Depositional Environment and Geochemistry of the Upper Pennsylvanian Stark Shale Member of the Dennis Limestone[J].Chemical Geology,1992,99(1/2/3):65-82.
[49] RIMMER S M.Geochemical Paleo-REDOX Indicators in Devonian-Mississippian Black Shales,Central Appalachian Basin(USA)[J].Chemical Geology,2004,206(3):373-391.
[50] WIGNALL P B,TWITCHETT R J.Oceanic Anoxia and the End Permian Mass Extinction[J].Science,1996,272:1155-1158.
[51] KIMURA H,WATANABE Y.Ocean Anoxia at Precambrian-Cambrian Boundary[J].Geology,2001,29(11):995-998.
[52] DILL H.Metallogenesis of Early Paleozoic Graptolite Shales from the Graefenthal Horst(Northern Bavaria-Federal Republic of Germany)[J].Economic Geology,1986,81(4):889-903.
[53] 陈彬滔,于兴河,潘树新,等.准噶尔盆地南缘头屯河组曲流河沉积特征与成因砂体对比方法[J].天然气地球科学,2013,24(6):1132-1139.
CHEN Bin-tao,YU Xing-he,PAN Shu-xin,et al.Sedi-mentary Characteristics and Sedimentogenic-based Sandbodies Correlation Methods of Meandering River in Toutunhe Formation,Southern Margin of Junggar Basin[J].Natural Gas Geoscience,2013,24(6):1132-1139.
[54] 李志华,黄文辉. 辫状河三角洲岩相特征及沉积模式:以鄂尔多斯盆地苏南地区盒8段为例[J].岩性油气藏,2017,29(1):43-50.
LI Zhi-hua,HUANG Wen-hui.Lithofacies Characteristic and Sedimentary Model of Braided Delta:A Case Study of He-8 Member in the Southern Sulige,Ordos Basin[J].Lithologic Reservoirs,2017,29(1):43-50.
[55] MIALL A D.The Geology of Fluvial Deposits:Sedimentary Facies,Basin Analysis,and Petroleum Geology[M].Berlin:Springer,1996.
[56] FOLK R L,SIEDLECKA A.The “Schizohaline” Environment:Its Sedimentary and Diagenetic Fabrics as Exemplified by Late Paleozoic Rocks of Bear Island,Svalbard[J].Sedimentary Geology,1974,11(1):1-15.
[57] 廖保方,张为民.辫状河现代沉积研究与相模式:中国永定河剖析[J].沉积学报,1998,16(1):34-39.
LIAO Bao-fang,ZHANG Wei-min.Study on Modern Deposit of a Braided Stream and Facies Model:Taking the Yongding River as an Example[J].Acta Sedimentologica Sinica,1998,16(1):34-39.
[58] 于兴河.辫状河储层地质模式及层次界面分析[M].北京:石油工业出版社,2004.
YU Xing-he.Geological Model and Interface Analysis Braided River Reservoir[M].Beijing:Petroleum Industry Press,2004.

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备注/Memo

备注/Memo:
收稿日期:2018-10-12; 修回日期:2018-11-20 投稿网址:http://jese.chd.edu.cn/
基金项目:国家科技重大专项项目(2016ZX05050-005); 四川省教育厅重点项目(16ZA0103)
作者简介:孙 诗(1992-),男,四川乐山人,理学硕士研究生,E-mail:760853598@qq.com。
 *通讯作者:王 峰(1977-),男,陕西汉中人,副教授,理学博士,E-mail:wangfeng07@cdut.cn。
更新日期/Last Update: 2019-02-28