渤海东北部辽东凸起锦州27构造沙河街组碎屑锆石物源示踪

耿名扬, 刘志峰, 雷杭山. 渤海东北部辽东凸起锦州27构造沙河街组碎屑锆石物源示踪[J]. 海洋地质前沿, 2025, 41(7): 54-65. doi: 10.16028/j.1009-2722.2024.067
引用本文: 耿名扬, 刘志峰, 雷杭山. 渤海东北部辽东凸起锦州27构造沙河街组碎屑锆石物源示踪[J]. 海洋地质前沿, 2025, 41(7): 54-65. doi: 10.16028/j.1009-2722.2024.067
GENG Mingyang, LIU Zhifeng, LEI Hangshan. Source tracing of detrital zircons from Shahejie Formation of the Jinzhou 27 Structure in Liaodong Uplift, northeastern Bohai Sea[J]. Marine Geology Frontiers, 2025, 41(7): 54-65. doi: 10.16028/j.1009-2722.2024.067
Citation: GENG Mingyang, LIU Zhifeng, LEI Hangshan. Source tracing of detrital zircons from Shahejie Formation of the Jinzhou 27 Structure in Liaodong Uplift, northeastern Bohai Sea[J]. Marine Geology Frontiers, 2025, 41(7): 54-65. doi: 10.16028/j.1009-2722.2024.067

渤海东北部辽东凸起锦州27构造沙河街组碎屑锆石物源示踪

  • 基金项目: 国家重点研发计划“板块俯冲驱动下的流体循环机制及其效应”(2022YFF0800403)
详细信息
    作者简介: 耿名扬(1990—),男,硕士,工程师,主要从事石油天然气地质方面的研究工作. E-mail:gengmy@cnooc.com.cn
  • 中图分类号: P736

Source tracing of detrital zircons from Shahejie Formation of the Jinzhou 27 Structure in Liaodong Uplift, northeastern Bohai Sea

  • 渤海东北部辽东凸起锦州27构造沙河街组砂体发育情况横向变化快,开展物源示踪对于明确砂体分布具有重要意义。通过对研究区砂岩的锆石U-Pb年龄、锆石形态和岩屑成分分析,明确研究区沙河街组母岩时代、类型及主要物源区。结果表明:①沙河街组主要发育峰值年龄为120 Ma的白垩纪锆石和峰值年龄为1 800、2 500 Ma的古元古代锆石。白垩纪锆石多呈柱状,发育棱角,具有生长环带,古元古代锆石多呈浑圆状,棱角不明显,生长环带多发生破坏。②沙四段沉积时期,砂岩中古元古代锆石占比为55%,白垩纪锆石占比为25%,岩屑类型以变质岩为主。沙三段—沙一二段沉积时期,砂岩中古元古代锆石占比为44%,白垩纪锆石占比为33%,岩屑类型以火山岩、变质岩为主。③沙河街组母岩以胶辽隆起复州北部地区新元古界沉积岩为主,同时受辽东凸起不断隆升影响,盆地内白垩系火山岩物源的影响逐渐增加。

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  • 图 1  研究区位置和构造背景

    Figure 1. 

    图 2  辽东湾坳陷构造演化剖面

    Figure 2. 

    图 3  辽东凸起JZ27-6S-A、JZ27-6-A、JZ27-2-A井沙河街组岩性剖面

    Figure 3. 

    图 4  辽东凸起JZ27-2-A 沙一二段砂岩碎屑锆石U-Pb年龄协和图

    Figure 4. 

    图 5  辽东凸起JZ27-6S-A、JZ27-6-A、JZ27-2-A沙河街组砂岩碎屑锆石Th/U比值

    Figure 5. 

    图 6  辽东凸起JZ27-2-A、JZ27-6-A井沙河街组碎屑锆石U-Pb年龄谱图

    Figure 6. 

    图 7  辽东凸起JZ27-2-A井沙四段碎屑锆石CL图像

    Figure 7. 

    图 8  辽东凸起JZ27-2-A井沙一二段碎屑锆石CL图像

    Figure 8. 

    图 9  辽东凸起JZ27-6-A井沙河街组母岩岩屑类型

    Figure 9. 

    图 10  辽东凸起JZ27-6S-A、JZ27-6-A井沙河街组薄片

    Figure 10. 

    图 11  辽东湾坳陷及胶辽隆起前古近系岩性分布

    Figure 11. 

    图 12  辽东凸起JZ33-1-A和JZ28-1-A井基底岩性柱状图

    Figure 12. 

  • [1]

    徐长贵. 陆相断陷盆地源-汇时空耦合控砂原理:基本思想、概念体系及控砂模式[J]. 中国海上油气,2013,25(4):1-11,21.

    XU C G. Controlling sand principle of source-sink coupling in time and space in continental rift basins:basic idea,conceptual systems and controlling sand models[J]. China Offshore Oil and Gas,2013,25(4):1-11,21.

    [2]

    聂银兰,朱筱敏,董艳蕾,等. 陆相断陷盆地源-汇系统要素表征及研究展望[J]. 地质论评,2022,68(5):1881-1896.

    NIE Y L,ZHU X M,DONG Y L,et al. Characterization and research prospect of source-to-sink system elements in continental rift basin[J]. Geological Review,2022,68(5):1881-1896.

    [3]

    朱红涛,徐长贵,朱筱敏,等. 陆相盆地源-汇系统要素耦合研究进展[J]. 地球科学. 2017,42(11):1851-1870.

    ZHU H T,XU C G,ZHU X M,et al. Advances of the source-to-sink units and coupling model research in continental basin[J]. Earth Science,2017,42(11):1851-1870.

    [4]

    赵红格,刘池洋. 物源分析方法及研究进展[J]. 沉积学报,2003,21(3):409-415. doi: 10.3969/j.issn.1000-0550.2003.03.007

    ZHAO H G,LIU C Y. Approaches and prospects of provenance analysis[J]. Acta Sedimentologica Sinica,2003,21(3):409-415. doi: 10.3969/j.issn.1000-0550.2003.03.007

    [5]

    徐杰,姜在兴. 碎屑岩物源研究进展与展望[J]. 古地理学报,2019,21(3):379-396.

    XU J,JIANG Z X. Provenance analysis of clastic rocks:current research status and prospect[J]. Journal of Palaeogeography,2019,21(3):379-396.

    [6]

    赵梦,杜晓峰,王清斌,等. 渤海东部旅大29-1构造沙二段砂砾岩锆石定年及物源示踪[J]. 沉积学报,2019,37(1):62-71.

    ZHAO M,DU X F,WANG Q B,et al. Detrital zircon U-Pb geochronology of the Es2 sandstones of Lvda 29-1 structure in the eastern Bohai Sea,and its implication for provenance[J]. Acta Sedimentologica Sinica,2019,37(1):62-71.

    [7]

    赵梦,徐长贵,杜晓峰,等. 石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪[J]. 地球科学,2017,42(11):1984-1993.

    ZHAO M,XU C G,DU X F,et al. Detrital zircon U-Pb geochronology and provenance tracing of the fan deltas along the southwestern slope of the Shijiutuo Uplift[J]. Earth Science,2017,42(11):1984-1993.

    [8]

    刘强虎,朱筱敏,李顺利,等. 沙垒田凸起前古近系基岩分布及源-汇过程[J]. 地球科学,2016,41(11):1935-1949.

    LIU Q H,ZHU X M,LI S L,et al. Pre-Palaeogene bedrock distribution and source-to-sink system analysis in the Shaleitian Uplift[J]. Earth Science,2016,41(11):1935-1949.

    [9]

    李欢,杨香华,朱红涛,等. 渤中西环古近系东营组物源转换与沉积充填响应[J]. 沉积学报,2015,33(1):36-48.

    LI H,YANG X H,ZHU H T,et al. The provenance transformation and sedimentary filling response of Paleogene Dongying Formation in western slope of Bozhong Sag[J]. Acta Sedimentologica Sinica,2015,33(1):36-48.

    [10]

    余宏忠. 渤中凹陷西斜坡碎屑锆石特征及物源定量示踪[J]. 特种油气藏,2014,21(6):42-46. doi: 10.3969/j.issn.1006-6535.2014.06.010

    YU H Z. Clastic zircon characteristics and quantitative tracing of provenances in western slope of Bozhong Sag[J]. Special Oil and Gas Reservoirs,2014,21(6):42-46. doi: 10.3969/j.issn.1006-6535.2014.06.010

    [11]

    杨克基,漆家福,余一欣,等. 辽东湾地区潜山差异演化及成藏条件分析[J]. 天然气地球科学,2016,27(6):1014-1024. doi: 10.11764/j.issn.1672-1926.2016.06.1014

    YANG K J,QI J F,YU Y X,et al. The differential evolution of buried hills in Liaodong Bay area and analysis on their reservoir forming conditions[J]. Natural Gas Geoscience,2016,27(6):1014-1024. doi: 10.11764/j.issn.1672-1926.2016.06.1014

    [12]

    贾楠,刘池阳,周立宏,等. 辽东湾坳陷新生代断裂特征及其对油气的控制作用[J]. 西北大学学报(自然科学版),2018,48(6):839-849.

    JIA N,LIU C Y,ZHOU L H,et al. Characteristics of fault structure and its control on hydrocarbons in the Liaodong Bay Depression[J]. Journal of Northwest University (Natural Science Edition),2018,48(6):48-94.

    [13]

    贾楠,刘池洋,张功成,等. 辽东湾坳陷新生代差异抬升事件的确定及其地质意义[J]. 地学前缘,2015,22(3):77-87.

    JIA N,LIU C Y,ZHANG G C,et al. The Cenozoic distinct uplift events in the Liaodong Bay Depression and their geological significance[J]. Earth Science Frontiers,2015,22(3):77-87.

    [14]

    刘新新. 辽东凸起北段的形成与演化[D]. 青岛:中国石油大学(华东),2019.

    LIU X X. The formation and evolution of northern Liaodong Dome[D]. Qingdao:China University of Petroleum (East China),2019.

    [15]

    张婧,吴智平,李伟,等. 辽东湾坳陷新生代构造特征及演化[J]. 海洋地质前沿,2017,33(11):9-17.

    ZHANG J,WU Z P,LI W,et al. Cenozoic tectonic characteristics and evolution of Liaodong Bay Depression[J]. Marine Geology Frontiers,2017,33(11):9-17.

    [16]

    黄雷,周心怀,刘池洋,等. 渤海海域新生代盆地演化的重要转折期证据及区域动力学分析[J]. 中国科学(地球科学),2012,42(6):893-904.

    HUANG L,ZHOU X H,LIU C Y,et al. The important turning points during evolution of Cenozoic basin offshore the Bohai Sea:evidence and regional dynamics analysis[J]. Science China Earth Science,2012,42(6):893-904.

    [17]

    彭靖淞,徐长贵,吴奎,等. 郯庐断裂带辽东凸起的形成与古辽中洼陷的瓦解[J]. 石油学报,2015,36(3):274-285. doi: 10.7623/syxb201503003

    PENG J S,XU C G,WU K,et al. Formation of Liaodong Uplift and collapse of the ancient Liaozhong Sag in Tan-Lu Fault Zone[J]. Acta Petrolei Sinica,2015,36(3):274-285. doi: 10.7623/syxb201503003

    [18]

    徐长贵,张功成,黄胜兵,等. 渤海湾盆地海域白垩系大中型火山岩油气藏形成条件[J]. 石油勘探与开发,2024,51(3):467-477. doi: 10.11698/PED.20230288

    XU C G,ZHANG G C,HUANG S B,et al. Formation of large-and medium-sized Cretaceous volcanic reservoirs in the offshore Bohai Bay Basin,East China[J]. Petroleum Exploration and Development,2024,51(3):467-477. doi: 10.11698/PED.20230288

    [19]

    杨东升,刘志峰,吴斌,等. 渤海海域辽东凸起南段潜山构造演化及其对油气成藏的控制[J]. 中国石油勘探,2022,27(3):78-87. doi: 10.3969/j.issn.1672-7703.2022.03.007

    YANG D S,LIU Z F,WU B,et al. Tectonic evolution and its control on hydrocarbon accumulation of buried hill in the south section of Liaodong Bulge,Bohai Sea[J]. China Petroleum Exploration,2022,27(3):78-87. doi: 10.3969/j.issn.1672-7703.2022.03.007

    [20]

    牛绍武,辛后田. 辽东半岛南部中新元古界地层的重新厘定[J]. 地质调查与研究,2012,35(1):1-15.

    NIU S W,XIN H T. Collation on the subdivision and correlation of Meso-Neoproterozoic strata in southern Liaodong Peninsula,Liaoning Province,China[J]. Geological Survey and Research,2012,35(1):1-15.

    [21]

    于泓超. 胶-辽-吉造山带吉南地区古元古代沉积-岩浆作用及构造意义[D]. 长春:吉林大学,2023.

    YU H C. Paleoproterozoic sedimentary-magmatism and its tectonic significance in the southern Jilin Province of Jiao-Liao-Ji Orogenic Belt[D]. Changchun:Jilin University,2023.

    [22]

    高林志,张传恒,陈寿铭,等. 辽东半岛细河群沉积岩碎屑锆石SHRIMP U-Pb年龄及其地质意义[J]. 地质通报,2010,29(8):1113-1122. doi: 10.3969/j.issn.1671-2552.2010.08.002

    GAO L Z,ZHANG C H,CHEN S M,et al. Detrital zircon SHRIMP U-Pb age from the Diaoyutai Formation,Xihe Group in Liaodong Peninsula,China and its geological significance[J]. Geological Bulletin of China,2010,29(8):1113-1122. doi: 10.3969/j.issn.1671-2552.2010.08.002

    [23]

    ZHANG W,LIU F L,LIU C H,et al. Provenance transition from the North China Craton to the Grenvillian orogeny-related source:evidence from Late Mesoproterozoic-Early Neoproterozoic strata in the Liao-Ji area[J]. Precambrian Research,2021,362:1-17.

    [24]

    王伟,杨红,冀磊. 辽南地块新太古代2.52~2.46 Ga构造-热事件的识别及地质意义[J]. 岩石学报,2017,33(9):2775-2784.

    WANG W,YANG H,JI L. The identification of the Neoarchean 2.52~2.46 Ga tectono-thermal events from the Liaonan terrain and its geological significance[J]. Acta Petrologica Sinica,2017,33(9):2775-2784.

    [25]

    吴福元,杨进辉,柳小明,等. 辽东半岛中生代花岗质岩浆作用的年代学格架[J]. 高校地质学报,2005,11(3):305-317. doi: 10.3969/j.issn.1006-7493.2005.03.003

    WU F Y,YANG J H,LIU X M et al. Geochronological framework of the Mesozoic granitic magmatism in the Liaodong Peninsula,Northeast China[J]. Geological Journal of China Universities,2005,11(3):305-317. doi: 10.3969/j.issn.1006-7493.2005.03.003

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收稿日期:  2024-03-22
刊出日期:  2025-07-28

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