Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (1): 61-80.doi: 10.13278/j.cnki.jjuese.201501106

Previous Articles     Next Articles

Provenance-Sedimentary System and Tectonic Setting of First Member of Nantun Formation in Wuerxun Depression of Hailar Basin

Zhao Xiaoqing1,2, Cheng Rihui2, Yu Zhenfeng2,3, Sun Fengxian1, Wang Peng1, Gao Huijun1   

  1. 1. Well Logging Company, Daqing Drilling and Exploration Engineering Corporation, Daqing 163412, Heilongjiang, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Key Laboratory of National Energy Coal and Coal Bed Methane Joint Mining Technology, Shanxi Jincheng Anthracite Mining Group Company Limited, Jincheng 048012, Shanxi, China
  • Received:2014-05-06 Published:2015-01-26

PDF (PC)

482

Abstract:

Fracture and volcanism were intensive in First Member of Nantun Formation of Wunan depression in Hailar basin, due to the diversity of detritus. The composition of clastic were metamorphic clastic, pyroclastic and general erosion detrital. The diversity of detritus makes lithology and division have the distinct characteristics. The study of mineral association, cathode luminescence and heavy mineral assemblage shows that the study area can be divided into four single lithology areas and two mixed areas among them. Four single lithology areas are sedimentary rocks area with metamorphic rocks clastics, pyroclastic sedimentary rocks area, welded pyroclastic rocks area and pyroclastic rocks area. According to the contents and components of clastics in rocks, mixed area can be divided into two mixed areas:the area with normal sedimentary clastic was dominant and the area with pyroclastic was dominant. Each single lithology area corresponds with each tectonic unit. The sedimentary rocks area with metamorphic rocks clastics corresponds to Wuxi fault terrace belt, the pyroclastic rocks area correspond to Bayantala structural belt, and pyroclastic sedimentary rocks area is part of Wudong arc structural belt. Geochemical data reveal that magma of source rocks is granitoid magma of crust source, meanwhile be contaminated by magma of mantle-derived, and heavy rare earth elements are enrichment. In Wuxi fault terrace belt, total content of rare earth elements is high and negative anomaly of Eu is not obvious, so the crust-mantle contamination of source rocks magma is heavy. In Bayantala structural belt, total content of rare earth elements is low and negative anomaly of Eu is obvious, so the crust-mantle contamination of source rocks magma is medium. In Wudong arc structural belt, total content of rare earth elements is high and negative anomaly of Eu is obvious, so the crust-mantle contamination of source rocks magma is low. Dickinson graphics of sandstone composition reveal that source regions of Wudong arc structural belt has not deeply cut, and source region of Bayantala structural belt has deeply cut. Noral-slip of Derbgan fault led tectonic gneiss of Chaigang to be developed and Chaigang to uplift relatively, which become erosion area and provided Wuxi fault terrace belt with metamorphic sediments, shaped the sedimentary system of fan delta with metamorphic clastic, meanwhile the fracture provided a channel for the mantle-derived magma rising. Extension slip of Bayantala fault made the rise of mantle-derived magma and volcanic eruption, developed a set of rocks between fusion sintering pyroclastic rock and pyroclastic sedimentary rock, and shaped the sedimentary system of fan delta with pyroclastic. The crust-mantle contamination degree of Bayanshan uplift was low, but underplateing of mantle-derived magma made strong crystallization differentiation, volcanic activity and surface uplift, developed pyroclastic rocks and shaped sedimentary system of delta in Wudong arc structural belt.

Key words: Hailar basin, Wunan depression, First Member of Nantun Formation, provenance, sedimentary system, tectonic setting

CLC Number: 

  • P588.14

[1] 吴河勇, 李子顺, 冯子辉, 等.海拉尔盆地乌尔逊贝尔凹陷构造特征与油气成藏过程分析[J].石油学报, 2006, 27(增刊):1-6. Wu Heyong, Li Zishun, Feng Zihui, et al. Analysis on Structural Features and Reservoir-Forming Process of Wuerxun and Beier Sags in Hailaer Basin[J]. Acta Petrolei Sinica, 2006, 27(Sup.):1-6.

[2] 张成, 李春柏, 楚美娟, 等.乌尔逊凹陷下白垩统高频层序特征及其控制因素分析[J].沉积学报, 2005, 23(4):657-663. Zhang Cheng, Li Chunbai, Chu Meijuan, et al. Analsis on Characteristics and Controls of High-Frequency Sequences of Lower Cretaceous Series in Wuerxun Depression[J]. Acta Sedimentolgica Sinica, 2005, 23(4):657-663.

[3] 刘新颖, 邓宏文, 邸永香, 等.海拉尔盆地乌尔逊凹陷南屯组优质烃源岩发育特征[J].石油实验地质, 2009, 31(1):68-73. Liu Xinying, Deng Hongwen, Di Yongxiang, et al. High Quality Source Rocks of Nantun Formation in Wuerxun Depression, the Hailaer Basin[J]. Petroleum Geology & Experiment, 2009, 31(1):68-73.

[4] 尤丽, 李春柏, 刘立, 等.铜钵庙南屯组砂岩成岩作用与相对高孔隙度的关系:以海拉尔盆地乌尔逊凹陷南部为例[J].吉林大学学报:地球科学版, 2009, 39(5):781-788. You Li, Li Chunbai, Liu Li, et al. Relationship of Sandstone Diagenesis and Relatively High Porosity Areas in Nantun and Tongbomiao Formation:A Case from the Southern of Wuerxun Depression in Hailaer Basin[J]. Journal of Jilin University:Earrh Science Edition, 2009, 39(5):781-788.

[5] 侯启军, 冯子辉, 霍秋立.海拉尔盆地乌尔逊凹陷石油运移模式与成藏期[J].地球科学:中国地质大学学报, 2004, 29(4):397-403. Hou Qijun, Feng Zihui, Huo Qiuli. Oil Migration Model and Entrapment Epoch of North Wuerxun Depression in Hailaer Basin[J]. Earth Science:Journal of China University of Geosciences, 2004, 29(4):397-403.

[6] 李静逸, 刘志峰, 赵东娜, 等.海拉尔盆地乌尔逊凹陷南部南一段沉积相研究[J].内蒙古石油化工, 2009(3):116-119. Li Jingyi, Liu Zhifeng, Zhao Dongna, et al. Sedimentary Facies Reserach of Member K1n1 in South Wuerxun Deperxun of Hailaer Basin[J]. Inner Mongolia Petrochemical Industry, 2009(3):116-119.

[7] 姜茵华.海拉尔盆地乌尔逊凹陷南屯组沉积相分析[J].大庆石油学院学报, 2011, 35(4):12-16. Jiang Yinhua. Analysis of Sedimentary Facies of Nantun Formation in Wuerxun Depression, Hailar Basin[J]. Journal of Daqing Petroleum Institute, 2011, 35(4):12-116.

[8] 王桂芳.乌尔逊凹陷乌南地区南一段沉积微相研究.大庆:大庆石油学院, 2010. Wang Guifang. Study of Sedimentary Microfacies in One Setion of Nantun Group in Wuerxun Hollow. Daqing:Daqing Petroleum Institute, 2010.

[9] 张晓东, 刘光鼎, 王家林.海拉尔盆地的构造特征及其演化[J].石油实验地质, 1994, 16(2):119-127. Zhang Xiaodong, Liu Guangding, Wang Jialin. Structural Characters of the Hailar Basin and Its Geological Evolution[J]. Experimental Petroleum Geology, 1994, 16(2):119-127.

[10] 孙晓猛, 鲁宝亮, 张梅生, 等.海拉尔盆地及盆缘露头区典型构造样式及变形序列[J].吉林大学学报:地球科学版, 2011, 41(增刊):1-8. Sun Xiaomeng, Lu Baoliang, Zhang Meisheng, et al. Typical Structural Styles and Deformation Sequence in Outcrop Area of Hailaer Basin and Its Margin[J]. Journal of Jilin University:Earth Science Edition, 2012, 41(Sup.):1-8.

[11] 程日辉, 沈艳杰, 颜景波, 等.海拉尔盆地火山碎屑岩的成岩作用[J].岩石学报, 2010, 26(1):47-54. Cheng Rihui, Shen Yanjie, Yan Jingbo, et al. Diagenesis of Volcaniclastic Rocks in Hailaer Basin[J]. Acta Petrologica Sinica, 2010, 26(1):47-54.

[12] 陶宏根, 程日辉, 赵小青, 等.海拉尔盆地火山碎屑岩的测井响应与应用[J].地球物理学报, 2011, 54(2):534-544. Tao Honggen, Cheng Rihui, Zhao Xiaoqing, et al. Well Logging Response to the Volcaniclastic Rocks of Hailaer Basin and Application[J]. Chinese Journal of Geophysics, 2011, 54(2):534-544.

[13] 徐惠芬, 崔京钢, 邱小平.阴极发光技术在岩石学和矿床学中的应用[M].北京:地质出版社, 2006:42-63. Xu Huifen, Cui Jinggang, Qiu Xiaoping. The Application of Cathodoluminescence Technology in Petrology and Ore Mineralogy[M]. Beijing:Geological Publishing House, 2006:42-63.

[14] 王衍琦, 张绍平, 应凤祥.阴极发光显微镜在储层研究中的应用[M].北京:地质出版社, 1992:11-29. Wang Yanqi, Zhang Shaoping, Ying Fengxiang. The Application of Cathodoluminescence Microscope in Studying Oil and Gas Reservoirs[M]. Beijing:Geological Publishing House, 1992:11-29.

[15] 牟保磊.元素地球化学[M].北京:北京大学出版社, 1999:41-46. Mou Baolei. Element Geochemistry[M]. Beijing:Peking University Press, 1999:41-46.

[16] 王曰才, 王冠贵.地层倾角测井[M]. 北京:石油工业出版社, 1987:132-144. Wang Yuecai, Wang Guangui. Dip Logging[M]. Beijing:Petroleum Industry Press, 1987:132-144.

[17] Dickinson W R, Suczek C A. Plate Tectonics and Sandstone Compositions[J]. AAPG Bulletin, 1979, 63(2):2164-2182.

[18] Taylor S R, Mclennan S E. The Continential Crust:Its Composition and Evolution[M]. Oxford:Blackwell, 1985:1-312.

[19] Roser B P, Korsem R J. Detemrination of Tectonic Setting of Sandstone Mudstone Suites Using SiO2 Content and K2O/Na2O Ratio[J]. The Jounral of Geol, 1986, 94(5):635.

[20] Bhatia M R, Crook K A W. Trace Element Characteristics of Graywackes and Tectonic Setting Discri-mination of Sedimentary Basins[J]. Contributions to Mineralogy and Petrology, 1986, 92:181-193.

[21] Bhatia M R. Rare Earth Elements Geochemistry of Australian Paleozoic Graywackes and Mudstones:Provenance and Tectonic Control[J]. Sedimentary Geology, 1985, 45:97-113.

[22] 许中杰, 程日辉, 李飞, 等.粤西高明地区晚三叠世小坪组元素地球化学特征[J].吉林大学学报:地球科学版, 2010, 40(2):305-313. Xu Zhongjie, Cheng Rihui, Li Fei, et al. Elemental Geochemical Characteristics of the Xiaoping Formation in Late Triassic Epoch in Gaoming Area of the Western Guangdong Province[J]. Journal of Jilin University:Earth Science Edition, 2010, 40(2):305-313.

[23] 王中刚, 于学元, 赵振华.稀土元素地球化学[M].北京:科学出版社, 1989:212-278. Wang Zhonggang, Yu Xueyuan, Zhao Zhenhua. Rare Earth Elements Geochemistry[M]. Beijing:Science Press, 1989:212-278.

[24] Brijraj K D, Al-Mikhlafi A S, Kaur P. Geochemistry of Mansar Lake Sediments, Jammu, India:Implication for Source-Area Weathering, Provenance, and Tectonic Setting[J]. Journal of Asian Earth Sciences, 2006, 26:649-668.

[25] She Zhenbing, Ma Changqian, Mason R. Provenance of the Triassic Songpan-Ganzi Flysch, West China[J]. Chemical Geology, 2006, 231:159-175.

[26] 吕志成, 段国正, 郝立波, 等.满洲里额尔古纳地区岩浆作用及其大地构造意义[J].矿物岩石, 2001, 21(1):77-85. Lü Zhicheng, Duan Guozheng, Hao Libo, et al. Magmatism and Its Tectonic Significance in the Manzhouli-E'ergona Region[J]. Journal of Minera-logy and Petrology, 2001, 21(1):77-85.

[27] 李锦轶, 莫申国, 和政军, 等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘, 2004, 11(3):157-168. Li Jinyi, Mo Shenguo, He Zhengjun, et al. The Timing of Crustal Sinistral Strike-Slip Movement in the Northern Great Khing'an Ranges and Its Constraint on Reconstruction of the Crustal Tectonic Evolution of NE China and Adjacent Areas Since the Mesozoic[J]. Earth Science Frontiers, 2004, 11(3):157-168.

[28] 张旗, 金惟俊, 李承东, 等.中国东部燕山期大规模岩浆活动与岩石圈减薄:与大火山岩省的关系[J].地学前缘, 2009, 16(2):21-51. Zhang Qi, Jin Weijun, Li Chengdong, et al.Yan-shanian Large-Scale Magmatism and Lithosphere Thinning in Eastern China:Relation to Large Igneous Province[J]. Earth Science Frontiers, 2009, 16(2):21-51.

[29] 董树文, 张岳桥, 陈宣华, 等.晚侏罗世东亚多向汇聚构造体系的形成与变形特征[J].地球学报, 2008, 29(3):306-317. Dong Shuwen, Zhang Yueqiao, Chen Xuanhua, et al. The Formation and Deformational Characteristics of East Asia Multi-Dirention Convergent Tectonic System in Late Jurassic[J]. Acta Geoscientica Sinica, 2008, 29(3):306-317.

[30] 孙晓猛, 刘财, 朱德丰, 等.大兴安岭西坡德尔布干断裂地球物理特征与构造属性[J].地球物理学报, 2011, 54(2):433-440. Sun Xiaomeng, Liu Cai, Zhu Defeng, et al. Geophysical Features and Tectonic Attribute of the Derbugan Fault in the Western Slope of Da Hinggan Ling Mountains[J]. Chinese Journal of Geophysics, 2011, 54(2):433-440.

[31] 郑常青, 周建波, 金巍, 等.大兴安岭地区德尔布干断裂带北段构造年代学研究[J].岩石学报, 2009, 25(8):1989-2000. Zheng Changqing, Zhou Jianbo, Jin Wei, et al. Geochronology in the North Segment of the Derbugan Fault Zone, Great Xing'An Range, NE China[J]. Acta Petrologica Sinica, 2009, 25(8):1989-2000.

[32] 杨勉, 付广, 张云峰, 等.构造变换带沉积充填特征与油气分布规律[J].大庆石油地质与开发, 2008, 27(3):15-17. Yang Mian, Fu Guang, Zhang Yunfeng, et al. Sedimentary Filling Features Hydrocarbon Distribution Rules in Structural Transfer Zone[J]. Petroleum Geology & Oilfield Development in Daqing, 2008, 27(3):15-17.

[33] 洪大卫, 王式光, 谢锡林, 等.兴蒙造山带正ε(Nd, t)值花岗岩的成因和大陆地壳生长[J].地学前缘, 2000, 7(2):441-456. Hong Dawei, Wang Shiguang, Xie Xilin, et al.Genesis of Positive ε(Nd, t) Granitoids in the Da Hinggan Mts-Mongolia Orogenic Belt and Growth Continental Crust[J]. Earth Science Frontiers, 2000, 7(2):441-456.

[34] Richards M A. Prospecting for Jurassic Slabs[J]. Nature, 1999, 397(21):203-204.

[35] 邵济安, 张履桥, 肖庆辉, 等.中生代大兴安岭的隆起:一种可能的陆内造山机制[J].岩石学报, 2005, 21(3):789-794. Shao Ji'an, Zhang Lüqiao, Xiao Qinghui, et al.Rising of Da Hinggan Mts in Mesozoic:A Possible Mechanism of Intracontinental Orogeny[J]. Acta Petrologica Sinica, 2005, 21(3):789-794.
[1] Qiao Jian, Luan Jinpeng, Xu Wenliang, Wang Zhiwei, Zhao Shuo, Guo Peng. Age and Provenance of Early Paleozoic Sedimentary Formation in Northern Jiamusi Massif: Evidence from U-Pb Ages and Hf Isotope Compositions of Detrital and Magmatic Zircons [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(1): 118-131.
[2] Meng En, Wang Chaoyang, Liu Chaohui, Shi Jianrong, Li Yanguang. Geochronology, Petrogenesis and Constraints on Regional Tectonic Evolution of the Meta-Volcanic Rocks in Southeastern Liaodong Peninsula [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1589-1619.
[3] Sun Zhenjun, Sun Guosheng, Yu Henan, Xiang Zhu, Tian Yi, Liu Tong, Chen Xu, Li Yang. Chronology and Geochemical Characteristics of Zhuanshanzi Granite in Chifeng and Its Diagenetic Dynamics Background [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1740-1753.
[4] Li Fulai, Xiao Fei, Meng Fanchao, Ren Zeying. Geochemical Characteristics and Implication for Provenance of Upper Permian Linxi Formation Clastic Rocks in Solonker Area, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1769-1780.
[5] Wang Xi, Duan Mingxin, Ren Yunsheng, Hou Zhaoshuo, Sun Deyou, Hao Yujie. Characteristics of Fluid Inclusions and Mineralization Age of Badaguan Cu-Mo Deposit in Erguna Area, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(5): 1354-1367.
[6] Xu Chao, Xiao Yuanfu, Shen Lijun, Chang Jing, Li Hongxiao, Zhao Yanan, Yang Kairui. Geochemical Characteristics and Tectonic Setting of Gejiumu Lithosome in Nanjian County, Yunnan [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(2): 461-468.
[7] Gao Fuhong, Wang Lei, Xu WenLiang, Wang Feng. Age and Provenance of the Late Paleozoic Strata in Lesser Xing'an Range: Evidence from Field Geology and Detrital Zircon U-Pb Ages [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(2): 469-481.
[8] Tian Zhixian, Li Yongjun, Tian Meng, Yang Gaoxue, Xiang Kunpeng, Tong Lili. Zircon U-Pb Geochronology, Geochemical Characteristics and Geological Significance of Volcanic Rocks of Haerjiawu Formation in Qiada, West Junggar [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 135-145.
[9] Zheng Xiangwei, Wu Jian, He Shenglin, Hu Xiangyang, Liang Yunan. Fine Evaluation of Permeability of Conglomerate Reservoir Based on Flow Unit [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 286-294.
[10] Zhang Yukun, Hu Xiaoqing, Niu Tao, Zhang Xianwen, Gao Yufei, Wang Hui, Fan Ting'en, Bu Fanqing. Controlling of Paleogeomorphology to Paleogene Sedimentary System of Shijiutuo Uplift in Bohai Basin [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(6): 1589-1596.
[11] Zhang Yujin, Wu Xinwei, Jiang Bin, Guo Wei, Yang Yajun, Liu Shiwei, Cui Tianri, Li Wei, Li Linchuan, Si Qiuliang, Zhang Chao. U-Pb Geochronology of Detrital Zircon and the Constraint of Geochemistry from the Gegen'aobao Formation in Middle of Zalantun Area of Da Hinggan Mountains and Its Tectonic Significance [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(2): 404-416.
[12] Liu Dong, Li Zhongdong, Chen Wei, Zhan Wei, Chen Shanshan. Provenance Analysis of the Paleogene Strata in Block D and Peripheral in Irrawaddy Basin [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(1): 81-94.
[13] Zhang Yufen，Li Chang’an，Zhou Chou，Kang Chunguo，Xiong Deqiang，Jiang Huajun. Magnetism and Provenance Analysis of High Position Gravel Layer in the Middle Reaches of Yangtze River [J]. Journal of Jilin University(Earth Science Edition), 2014, 44(5): 1669-1677.
[14] Zhang Yinguo, Liang Jie. Sedimentary System Characteristics and Their Sedimentary Evolution from the Permian to Triassic in the Southern Yellow Sea Basin [J]. Journal of Jilin University(Earth Science Edition), 2014, 44(5): 1406-1418.
[15] Xu Wenli，Zheng Rongcai，Yan Xue，Wen Huaguo，Cui Cui. Trace and Rare Earthelement Geochemistry of the Early Paleozoic Black Shales in the Lower Yangtze Area and Its Geological Significances [J]. Journal of Jilin University(Earth Science Edition), 2014, 44(4): 1108-1122.
Viewed
Full text
322
HTML PDF
Just accepted Online first Issue Just accepted Online first Issue
0 0 0 0 0 322

  From Others local
  Times 116 206
  Rate 36% 64%

Abstract
481
Just accepted Online first Issue
0 0 481
  From Others local
  Times 408 73
  Rate 85% 15%

Cited
Web of Science  Crossref   ScienceDirect  Search for Citations in Google Scholar >>
 
This page requires you have already subscribed to WoS.
  Shared   
  Discussed   
No Suggested Reading articles found!
Copyright © Journal of Jilin University(Earth Science Edition), All Rights Reserved.
Tel: +86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
Powered by Beijing Magtech Co. Ltd