松辽盆地长岭断陷火山岩锆石U-Pb测年及其地质意义

doi:10.11743/ogg20150504

石油与天然气地质 ›› 2015, Vol. 36 ›› Issue (5): 736-744.doi: 10.11743/ogg20150504

松辽盆地长岭断陷火山岩锆石U-Pb测年及其地质意义

李瑞磊^1,2, 朱建峰², 刘玮³, 刘曼丽², 陆建林⁴, 王保华⁴, 陈光宇²

1. 中国地质大学(北京) 能源学院, 北京 100083;
2. 中国石化东北分公司, 吉林长春 130062;
3. 吉林大学地球科学学院, 吉林长春 130062;
4. 中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126

收稿日期:2014-12-24 修回日期:2015-03-05 出版日期:2015-10-28 发布日期:2015-10-23
第一作者简介:李瑞磊(1970—),男,博士、高级工程师,油气地质勘查。E-mail:liruilei99@163.com。
基金项目:
国家基础研究发展计划(973计划)项目(2012CB82000);国家自然科学基金项目(41472304,41202072);中国石化科技项目(P14020)。

Zircon U-Pb dating of volcanic rocks of Changling Fault Depression in the southern Songliao Basin and its geological significance

Li Ruilei^1,2, Zhu Jianfeng², Liu Wei³, Liu Manli², Lu Jianlin⁴, Wang Baohua⁴, Chen Guangyu²

1. College of Energy Resources, China University of Geosciences, Beijing 100083, China;
2. Research Institute of Exploration and Development, Northeast Branch Corporation, SINOPEC, Changchun, Jilin 130062, China;
3. College of Earth Sciences, Jilin University, Changchun, Jilin 130061, China;
4. Wuxi Institute of Petroleum Geology, Exploration and Production Research Institute, SINOPEC, Wuxi, Jiangsu 214126, China

Received:2014-12-24 Revised:2015-03-05 Online:2015-10-28 Published:2015-10-23

摘要/Abstract

摘要： 火山岩是松辽盆地断陷期盆地充填的主体，其年龄的精确标定是认识盆地裂陷启动时间和地层划分对比的基础。系统采集了长岭断陷20件火山岩样品，进行了LA-ICP-MS锆石U-Pb同位素分析。锆石U-Pb测年结果显示，原定火石岭组的火山岩形成于110～119 Ma，应划归为营城组一段；原定营城组的火山岩形成于100～109 Ma，应划归为营城组三段。所选火山岩样品鉴定为安山岩、粗面岩、流纹质凝灰岩和流纹岩；在TAS图解中落入流纹岩、粗面岩以及粗面英安岩区域。两个年龄区间的火山岩具有相似的地球化学特征，如铕负异常和稀土配分曲线都为轻稀土富集的右倾斜型，进一步暗示了二者的亲缘性。作为松辽盆地南部最大的深层构造单元，长岭断陷的火山岩地层序列需要重新厘定；松南地区火山-裂谷作用起始于早白垩世晚期而非晚侏罗世，相应的盆地构造-沉积史和油气形成演化史也需要进一步认识。

关键词: 锆石U-Pb年龄, 地层划分, 裂陷启动期, 火山岩, 长岭断陷

Abstract: Volcanic rocks are the main basin fillings during the formation of fault depression in the Songliao Basin,and their accurate dating is the basis of the rifting timing and layer subdivision.Twenty volcanic rocks samples were collected from the Changling Fault Depression and dated with LA-ICP-MS zircon U-Pb ages.Zircon U-Pb dating shows that the previous recognized Huoshiling Fm volcanic rocks formed between 110～119 Ma and should be grouped into the 1^st Member of the Yingcheng Fm.While the previously recognized Yingcheng Fm volcanic rocks formed between 100～109 Ma and should be grouped into the 3^rd Member of the Yingcheng Fm.Petrologically,the volcanic rocks are composed dominantly of andesite,trachyte,rhyolitic tuff and rhyolite,which are displayed in TAS diagram.Geochemical data show that the volcanic rocks have similar features such as light rare earth elements enrichment and negative Eu anomalies,indicating their affinity.As the deepest structure unit in the southern Songliao Basin,new layer subdivision and correlation strategy need to be proposed.And the results also indicate that the syn-rift stage of the southern Songliao Basin started at the Early Cretaceous rather than the previously believed Late Jurassic,which means the corresponding structure-sedimentary and hydrocarbon formation history need to be further recognized.

Key words: zircon U-Pb dating, layer subdivision, initiation of fault depression, volcanic rock, Changling Fault Depression

中图分类号:

TE135

李瑞磊,朱建峰,刘玮,等. 松辽盆地长岭断陷火山岩锆石U-Pb测年及其地质意义[J]. 石油与天然气地质, 2015, 36(5): 736-744. doi: 10.11743/ogg20150504 Li Ruilei,Zhu Jianfeng,Liu Wei,et al. Zircon U-Pb dating of volcanic rocks of Changling Fault Depression in the southern Songliao Basin and its geological significance[J]. Oil & Gas Geology, 2015, 36(5): 736-744. doi: 10.11743/ogg20150504

参考文献

[1] Wang Pujun,Chen Shumin.Cretaceous volcanic reservoirs and their exploration in the Songliao Basin Northeast China[J].AAPG Bulletin,2015,98,(In Press).
[2] 张玮,李洪革,李明杰.松辽盆地南部长岭断陷区深层构造特征与天然气聚集[J].石油与天然气地质,2008,29(1):120-127. Zhang Wei,Li Hongge,Li Mingjie.Structural characteristics and gas accumulation in the deep of the Changling Fault Depression,the South Songliao Basin[J].Oil & Gas Geology,2008,29(1):120-127.
[3] 郑曼,李建忠,王立武,等.松辽盆地长岭断陷营城组火山岩储集空间特征及演化集[J].岩石学报,2010,26(1):135-141. Zheng Man,Li Jianzhong,Wang Liwu,et al.Reservoir space characteristics and evolution of the volcanic rocks in Yingcheng Formation of Changling fault depression,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):135-141.
[4] 冯志强.松辽盆地庆深大型气田的勘探前景[J].天然气工业,2006,26(6):1-5. Feng Zhiqiang.Exploration potential of large Qingshen Gas Field in the Songliao Basin[J].Natural Gas Industry,2006,26(6):1-5.
[5] 侯启军.南北辉映气贯松辽——吉林油田公司长岭断陷长深1井发现纪略[J].中国石油企业,2006,(3):45-46. Hou Qijun.Gas through out the Songliao Basin:Discovery of well CSI in Changling Fault Depression of Jinlin Oilfeild Company[J].China Petroleum Enterprise,2006,(3):45-46.
[6] Wang Pujun,Xie Xiao'an,Mattern Frank,et al.The Cretaceous Songliao Basin:Volcanogenic succession,sedimentary sequence and tectonic evolution,NE China[J].Acta Geologica Sinica,2007,81(6):1002-1011.
[7] 贾军涛,王璞珺,邵锐,等.松辽盆地东南缘营城组地层序列的划分与区域对比[J].吉林大学学报(地球科学版),2007,37(6):1110-1123. Jia Juntao,Wang Pujun,Shao Rui,et al.Stratigraphical sequence and regional correlation of Yingcheng Formation in the Southern of Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2007,37(6):1110-1123.
[8] 陈孔全,陆建林,张玺,等.松辽盆地南部长岭断陷火山岩储层的特征与勘探潜力[J].地质通报,2011,30(2/3):228-234. Chen Kongquan,Lu Jianlin,Zhang Xi,et al.Volcanic reservoir features and exploration potential of Changling fault depression in the southern Songliao Basin[J].Geological Bulletin of China,2011,30(2/3):228-234.
[9] 孙凯,宋立斌,李本才,等.松辽盆地南部深层地层划分与对比[J].地层学杂志,2013,37(4):472-478. Sun Kai,Song Libin,Li Bencai,et al.The deep sequence characteristics of the southern Songliao Basin[J].Journal of Stratigratigraphy,2013,37(4):472-478.
[10] 王力圆,唐华风,王璞珺,等.松辽盆地长岭断陷火山岩相地震特征及其响应关系[J].地球物理学进展,2012,27(1):271-278. Wang Liyuan,Tang Huafeng,Wang Pujun,et al.The seismic reflection characteristics and response relationship of volcanic rocks lithofacies in Changling fault depression,Songliao Basin[J].Progress in Geophysics(in Chinese),2012,27(1):271-278.
[11] 瞿雪姣,王璞珺,姚瑞士,等.松辽盆地南部火石岭组地层序列划分与区域对比[J].中南大学学报(自然科学版),2014,45(8):2716-2727. Qu Xuejiao,Wang Pujun,Yao Ruishi,et al.Stratigraphical sequence and regional correlation of Huoshiling Formation in the southern of Songliao Basin[J].Journal of Central South University(Science and Technology),2014,45(8):2716-2727.
[12] 瞿雪姣,王璞珺,高有峰,等.松辽盆地断陷期火石岭组时代归属探讨[J].地学前缘,2014,21(2):234-250. Qu Xuejiao,Wang Pujun,Gao Youfeng,et al.Chronostratigraphy of the Huoshilin Formation in the Songliao Basin,NE China:An Overview[J].Earth Science Frontiers,2014,21(2):234-250.
[13] 裴福萍,许文良,杨德彬,等.松辽盆地南部中生代火山岩:锆石U-Pb年代学及其对基底性质的制约[J].地球科学—中国地质大学学报,2008,33(5):603-617. Pei Fuping,Xu Wenliang,Yang Debin,et al.Mesozoic volcanic rocks in the southern Songliao Basin:zircon U-Pb ages and their constraints on the nature of basin basement[J].Earth Science-Journal of China University of Geosciences,2008,33(5):603-617.
[14] 高妍.松辽盆地东南缘中生代火山岩的年代学和地球化学特征[D].长春:吉林大学,2008. Gao Yan.Chronology and geochemistry of Mesozoic volcanic rocks in southeastern Songliao Basin[D].Changchun:Jilin University,2008.
[15] 陈井胜.松辽盆地南部营城组火山岩成因[D].长春:吉林大学,2009. Chen Jingsheng.The genesis of volcanic rocks of Yingcheng Formation in southern Songliao Basin[D].Changchun:Jilin University,2009.
[16] 章凤奇,程晓敢,陈汉林,等.松辽盆地东南缘晚中生代火山事件的锆石年代学与地球化学制约[J].岩石学报,2009,25(1):39-54. Zhang Fengqi,Cheng Xiaogan,Chen Hanlin,et al.Ziron chronological and geochemical constraints on the late Mesozoic volcanic events in the southeastern margin of the Songliao Basin,NE China[J].Acta Petrologica Sinica,2009,25(1):39-54.
[17] 王璞珺,陈树民,李伍志,等.松辽盆地白垩纪火山期后热液活动的岩石地球化学和年代学及其地质意义[J].岩石学报,2010,26(1):33-46. Wang Pujun,Chen Shumin,Li Wuzhi,et al.Chronology,petrology and geochemistry of the Cretaceous crypto-explosive breccia-bearing volcanic rocks:Implication for volcanic reservoir and tectonic of the Songliao Basin,NE China[J].Acta Petrologica Sinica,2010,26(1):33-46.
[18] 吴群,蒲仁海,韩敏强,等.长岭凹陷白垩系火山岩的锆石LA-ICP-MSU-Pb定年及其地质意义[J].矿物岩石,2010,30(2):111-119. Wu Qun,Pu Renhai,Han Minqiang,et al.Ziron LA-ICP-MS U-Pb dating for the volcanic rocks in Changling Depression,and its geological implication[J].Mineral Petrol,2010,30(2):11-119.
[19] 刘玮,孙德有,李瑞磊,等.松辽盆地长岭断陷营城组火山岩的时代与岩石成因[J].世界地质,2013,32(3):522-530. Liu Wei,Sun Deyou,Li Ruilei,et al.Chronology and petrogenesis of volcanic rocks in Yingcheng Formation from Changling Depression in Songliao Basin[J].Global Geology,2013,32(3):522-530.
[20] 刘玮.松辽盆地长岭断陷营城组酸性火山岩的时代、地球化学特征及岩石成因[D].长春:吉林大学,2014. Liu Wei.Age,geochemistry and petrogenesis of the Yingcheng Formation from Changling Depression in the Songliao Basin[D].Changchun:Jilin University,2014.
[21] 温升福,刘曼丽,刘玮,等.松辽盆地长岭断陷中基性火山岩的时代与其成因[J].吉大学报(地球科学版),2013,43(6);1762-1771. Wen Shengfu,Liu Manli,Liu wei,et al.Geochronology and petrogenesis of intermediate-basic volcanic rocks from Changling Depression in the Songliao Basin[J].Journal of Jilin University(Earth Science Edition),2013,43(6);1762-1771.
[22] 胡纯心.长岭断陷构造特征及白垩纪以来的构造演化[J].石油与天然气地质,2013,34(2):229-235. Hu Chunxin.Structural characteristics and post-Cretaceous tectonic evolution of the Changling Rift[J].Oil & Gas Geology,2013,34(2):229-235.
[23] Boynton W V.Cosmochemistry of the rare earth elements:Meteorite studies[C]//Henderson P.Rare Earth Element Geochemistry.Amsterdam:Elsevier,1984:63-114.
[24] Wang Pujun,Liu Wanzhu,Wang Shuxue,et al.⁴⁰Ar/³⁹Ar and K/Ar dating on the volcanic rocks in the Songliao Basin,NE China:constraints on stratigraphy and basin dynamics[J].International Journal of Earth Sciences,2002,91:331-340.
[25] Wang Pujun,Ren Yanguang,Shan Xuanlong,et al.The Cretaceous volcanic succession around the Songliao Basin,NE China:relationship between volcanism and sedimentation[J].Geological Journal,2002b,37:97-115.
[26] 宋立忠,赵泽辉,焦贵浩,等.松辽盆地早白垩世火山岩地球化学特征及其构造意义[J].岩石学报,2010,26(4):1182-1194. Song Lizhong,Zhao Zehui,Jiao Guihao,et al.Geochemical characteristics of Early Cretaceous volcanic rocks from Songliao Basin,Northeast China,and its tectonic implication[J].Acta Petrologica Sinica,2010,26(4):1182-1194.
[27] 王璞珺,赵然磊,蒙启安,等.白垩纪松辽盆地:从火山裂谷到陆内拗陷的动力学环境[J].地学前缘,2015,22(2). Wang Pujun,Zhao Ranlei,Meng Qi'an,et al.The Cretaceous Songliao Basin:Dynamic background from volcanic rift to interior sag basin[J].Earth Science Frontier,2015,22(2).
[28] 谢忱,胡纯心.松辽盆地长岭断陷南部天然气成藏与富集特征[J].石油与天然气地质,2010,31(3):381-385. Xie Chen,Hu Chunxin.Gas accumulations and distribution features in the south of the Changling fault depression in the Songliao Basin[J].Oil & Gas Geology,2010,31(3):381-385.
[29] 王洪江,吴聿元.松辽盆地长岭断陷火山岩天然气藏分布规律与控制因素[J].石油与天然气地质,2011,33(3):360-367. Wang Hongjiang,Wu Yuyuan.Distribution patterns and controlling factors of volcanic gas pools in the Changling fault depression,the Songliao Basin[J].Oil & Gas Geology,2011,33(3):360-367.
[30] 闫鹏伟,李建忠,王立武,等.松辽盆地长岭断陷深层天然气资源潜力分析[J].现代地质,2009,23(5):902-907. Yan Pengwei,Li Jianzhong,Wang Liwu,et al.Prediction of the deep natural gas potential of Changling Fault Depression,Songliao Basin[J].Geoscience,2009,23(5):902-907.
[31] 唐华风,李瑞磊,吴艳辉,等.火山地层结构特征及其对波阻抗反演的约束[J].地球物理学报,2011,54(2):620-627. Tang Huafeng,Li Ruilei,Wu Yanhui,et al.Textural characteristics of volcanic strata and its constraint to impedance inversion[J].Chinese Journal of Geophysics,2011,54(2):620-627.
[32] 王璞珺,张功成,蒙启安,等.地震火山地层学及其在我国火山岩盆地中的应用[J].地球物理学报,2011,54(2): 597-610. Wang Pujun,Zhang Gongchang,Meng Qian,et al.Application of seismic volcanostratigraphy to the volcanic rifted basins of China[J].Chinese Journal of Geophysics,2011,54(2): 597-610.

松辽盆地长岭断陷火山岩锆石U-Pb测年及其地质意义

Zircon U-Pb dating of volcanic rocks of Changling Fault Depression in the southern Songliao Basin and its geological significance

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