Provenance analysis of the Middle Jurassic Wanbao Formation on western edge of Longjiang Basin: Constraints from detrital Zircon ages and geochemistry characteristics
Zhang Yu-Jin, Zhang Chao, Wu Xin-Wei, Tan Hong-Yan, Ma Yong-Fei, Li Wei, Wang Yan
Shenyang Center of Geological Survey,China Geological Survey,Shenyang 110034,China
Abstract Longjiang Basin is one of the newly established Meso-Cenozoic basins in the periphery area of the Songliao Basin. Analysis on clastic components of sandstones,heavy mineral combination,rock geochemistry and zircon U-Pb ages,and related comprehensive research of clastic rocks from the Middle Jurassic Wanbao Formation in Longjiang Basin,were carried out in this paper. The combination of sandstone clastic components and heavy minerals reflects that the mother rocks of the Wanbao Formation are mainly middle acid magmatic rocks and low grade metamorphic rocks,followed by a small number of medium basic magmatic rocks. Geochemical characteristics of sediment materials from the Wanbao Formation show that they are enriched in LREEs and depletion in HREEs,with a right-dipping signature. Meanwhile,they are enriched with(HFSE)Cs,Th,U,depletion of Nb,P,and Ti,which have similar geochemical characteristics of the Upper Crust. Detrital zircon shows four age peaks,the main peak is 167.5 Ma,the secondary peak ages are 236.4 Ma,309.1 Ma and 309.1 Ma,which reflect the multi-source characteristics of sediments in the Wanbao Formation. These sediments are mainly from the Middle Jurassic volcanic rocks,followed by products from the Late Devonian-Triassic magmatic activities. The comprehensive analysis shows that the sediments of the Wanbao Formation in the Longjiang basin have the characteristics of acid and neutral volcanic sources,most of which come from the upper crust. The primary rocks of the Wanbao Formation are formed in continental island arc environment under the background of active continental margin background. The Middle Jurassic of the Longjiang Basin may be affected by the dual effects of the subduction of the paleo-Pacific plate and the evolution of the Mongolian-Okhotsk suture zone.
Fund:[Co-funded by the Young Scientists Foundation of National Natural Science Foundation of China(No.41702032) and the projects of China Geological Survey(Nos. DD20160048-04,DD20190039,DD20190042,DD20190360)]
About author: Zhang Yu-Jin,born in 1984,is a senior engineer in Shenyang Center of Geological Survey. He is mainly engaged in stratigraphy and sedimentary environment. E-mail: syzhangyujin@163.com.
Cite this article:
Zhang Yu-Jin,Zhang Chao,Wu Xin-Wei et al. Provenance analysis of the Middle Jurassic Wanbao Formation on western edge of Longjiang Basin: Constraints from detrital Zircon ages and geochemistry characteristics[J]. JOPC, 2019, 21(3): 490-504.
Zhang Yu-Jin,Zhang Chao,Wu Xin-Wei et al. Provenance analysis of the Middle Jurassic Wanbao Formation on western edge of Longjiang Basin: Constraints from detrital Zircon ages and geochemistry characteristics[J]. JOPC, 2019, 21(3): 490-504.
[1] 陈全红,李文厚,刘昊伟,李克永,庞军刚,郭艳琴,袁珍. 2009. 鄂尔多斯盆地上石炭统—中二叠统砂岩物源分析. 古地理学报, 11(6): 629-640. [Chen Q H,Li W H,Liu H W,Li K Y,Pang J G,Guo Y Q,Yuan Z.2009. Provenance analysis of sandstone of the Upper Carboniferous to Middle Permian in Ordos Basin. Journal of Palaeogeography(Chinese Edition), 11(6): 629-640] [2] 陈树旺,丁秋红,郑月娟,李永飞,张健,王杰,方慧,钟清. 2013. 松辽盆地外围新区、新层系: 油气基础地质调查进展与认识. 地质通报, 32(8): 1147-1158. [Chen S W,Ding Q H,Zhang Y J,Li Y F,Zhang J,Wang J,Fang H,Zhong Q.2013. New areas and series of strata on the periphery of Songliao Basin: The progress and recognition based on foundational geological survey for oil and gas resources. Geological Bulletin of China, 32(8): 1147-1158] [3] 陈小双,吕奥,宋贺民,刘磊,杨宝忠,侯红星. 2018. 新疆阿合奇地区志留系砂岩地球化学特征及大地构造背景. 古地理学报, 20(2): 271-284. [Chen X S,Lü A,Song H M,Liu L,Yang B Z,Hou H X.2018. Geochemical characteristics and tectonic history of the Silurian sandstones in Akeqi area,Xinjiang. Journal of Palaeogeography(Chinese Edition), 20(2): 271-284] [4] 陈志广,张连昌,周新华,万博,英基丰,王非. 2006. 满洲里新右旗火山岩剖面年代学和地球化学特征. 岩石学报, 22(12): 2971-2986. [Chen Z G,Zhang L C,Zhou X H,Wan B,Ying J F,Wang F.2006. Geochronology and geochemical characteristics of volcanic rocks section in Manzhouli Xinyouqi,Inner-Mongolia. Acta Petrologica Sinica, 22(12): 2971-2986] [5] 丁秋红,陈树旺,张立君,郑月娟,王杰,张健. 2013. 松辽盆地外围油气新区中生代地层研究新进展. 地质通报, 32(8): 1159-1176. [Ding Q H,Chen S W,Zhang L J,Zheng Y J,Wang J,Zhang J.2013. New research progress of the Mesozoic strata in new areas on the periphery of Songliao Basin. Geological Bulletin of China, 32(8): 1159-1176] [6] 董树文,张岳桥,陈宣华,龙长兴,王涛,杨振宇,胡健民. 2008. 晚侏罗世东亚多向汇聚构造体系的形成与变形特征. 地球学报, 29(3): 306-317. [Dong S W,Zhang Y Q,Chen X H,Long C X,Wang T,Yang Z Y,Hu J M.2008. The formation and deformational characteristics of East Asia multi-direction convergent tectonic system in Late Jurassic. Acta Geoscientica Sinica, 29(3): 306-317] [7] 葛文春,吴福元,周长勇,张吉衡. 2005. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义. 岩石学报, 21(3): 749-762. [Ge W C,Wu F Y,Zhou C Y,Zhang J H.2005. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region,central Da Hinggan Mountain. Acta Petrologica Sinica, 21(3): 749-762] [8] 何付兵,魏波,徐吉祥,孙永华,李瑞杰. 2017. 内蒙古巴彦敖包地区宝力高庙组火山岩地球化学特征、锆石U-Pb年龄及地质意义. 中国地质, 44(6): 1159-1174. [He F B,Wei B,Xu J X,Sun Y H,Li R J.2017. Ages,origin and geological implications of the volcanic rocks in the Baoligaomiao Formation of East Ujimqin Banner,Inner Mongolia. Geology in China, 44(6): 1159-1174] [9] 李双应,杨栋栋,王松,万秋,王道轩. 2014. 南天山中段上石炭统碎屑岩岩石学、地球化学、重矿物和锆石年代学特征及其对物源区、构造演化的约束. 地质学报, 88(2): 167-184. [Li S Y,Yang D D,Wang S,Wan Q,Wang D X.2014. Characteristics of petrology,geochemistry,heavy minerals and isotope chronology of Upper Carboniferous detrital rocks in the middle segment of South Tianshan and constraints to the provenance and tectonic evolution. Acta Geologica Sinica, 88(2): 167-184] [10] 李永飞,郜晓勇,卞雄飞,陈树旺,丁秋红. 2013. 大兴安岭北段龙江盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义. 地质通报, 32(8): 1195-1211. [Li Y F,Gao X Y,Bian X F,Chen S W,Ding Q H.2013. LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Mesozoic volcanic rocks from Longjiang Basin in northern Da Hinggan Mountains and their geological implications. Geological Bulletin of China, 32(8): 1195-1211] [11] 李宇,丁磊磊,许文良,王枫,唐杰,赵硕,王子进. 2015. 孙吴地区中侏罗世白云母花岗岩的年代学与地球化学: 对蒙古—鄂霍茨克洋闭合时间的限定. 岩石学报, 31(1): 56-66. [Li Y,Ding L L,Xu W L,Wang F,Tang J,Zhao S,Wang Z J.2015. Geochronology and geochemistry of muscovite granite in Sunwu area,NE China: Implications for the timing of closure of the Mongol-Okhotsk Ocean. Acta Petrologica Sinica, 31(1): 56-66] [12] 刘建峰,迟效国,张兴洲,马志红,赵芝,王铁夫,胡兆初,赵秀羽. 2009. 内蒙古西乌旗南部石炭纪石英闪长岩地球化学特征及其构造意义. 地质学报, 83(3): 365-376. [Liu J F,Chi X G,Zhang X Z,Ma Z H,Zhao Z,Wang T F,Hu Z C,Zhao X Y.2009. Geochemical characteristic of Carboniferous quartz diorite in the southern Xiwuqi area,Inner Mongolia and its tectonic significance. Acta Geologica Sinica, 83(3): 365-376] [13] 刘建峰,迟效国,赵芝,胡兆初,陈军强. 2013. 内蒙古巴林右旗建设屯埃达克岩锆石U-Pb年龄及成因讨论. 岩石学报, 29(3): 827-839. [Liu J F,Chi X G,Zhao Z,Hu Z C,Chen J Q.2013. Zircon U-Pb age and petrogenetic discussion on Jianshetun adakite in Balinyouqi,Inner Mongolia. Acta Petrologica Sinica, 29(3): 827-839] [14] 孟恩,许文良,杨德彬,邱昆峰,李长华,祝洪涛. 2011. 满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义. 岩石学报, 27(4): 1209-1226. [Meng E,Xu W L,Yang D B,Qiu K F,Li C H,Zhu H T.2011. Zircon U-Pb chronology,geochemistry of Mesozoic volcanic rocks from the Lingquan Basin in Manzhouli area,and its tectonic implications. Acta Petrologica Sinica, 27(4): 1209-1226] [15] 苗来成,范蔚茗,张福勤,刘敦一,简平,施光海,陶华,石玉若. 2003. 小兴安岭西北部新开岭—科洛杂岩锆石SHRIMP年代学研究及其意义. 科学通报, 48(22): 2315-2323. [Miao L C,Fan W M,Zhang F Q,Liu D Y,Jian P,Shi G H,Tao H,Shi Y R.2003. SHRIMP zircon geochronology from Xinkailing-Kele complex in northwestern Xiao Hinggan Mts and its significance. Chinese Science Bulletin, 48(22): 2315-2323] [16] 隋振民,葛文春,吴福元,张吉衡,徐学纯,程瑞玉. 2007. 大兴安岭东北部侏罗纪花岗质岩石的锆石 U-Pb 年龄、地球化学特征及成因. 岩石学报, 23(2): 461-480. [Sui Z M,Ge W C,Wu F Y,Zhang J H,Xu X C,Cheng R Y.2007. Zircon U-Pb ages,geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts. Acta Petrologica Sinica, 23(2): 461-480] [17] 田景春,张翔. 2016. 沉积地球化学. 北京: 地质出版社,1-203. [Tian J C,Zhang X.2016. Sedimentary Geochemistry. Beijing: Geological Publishing House,1-203] [18] 王杰,陈树旺,丁秋红. 2013. 内蒙古突泉盆地中侏罗统万宝组碎屑岩LA-ICP-MS锆石U-Pb测年、地球化学特征及对源区的制约. 地质通报, 32(8): 1224-1235. [Wang J,Chen S W,Ding Q H.2013. Zircon U-Pb dating and geochemical characteristics of detrital rocks and their constraints on the provenance of Middle Jurassic Wanbao Formation in Tuquan Basin. Geological Bulletin of China, 32(8): 1224-1235] [19] 辛后田,滕学建,程银行. 2011. 内蒙古东乌旗宝力高庙组地层划分及其同位素年代学研究. 地质调查与研究, 34(1): 1-9. [Xin H T,Teng X J,Cheng Y H.2011. Stratigraphic subdivision and Baoligaomiao Formation in the isotope geochronology study on the east Ujimqin County,Inner Mongolia. Geological Survey and Research, 34(1): 1-9] [20] 许文良,孙德有,尹秀英. 1999. 大兴安岭海西期造山带的演化: 来自花岗质岩石的证据. 长春科技大学学报, 29(4): 319-323. [Xu W L,Sun D Y,Yin X Y.1999. Evolution of hercynian orogenic belt in Daxing'anling MT: Evidence from granitic rocks. Journal of Changchun University of Science and Technology, 29(4): 319-323] [21] 许文良,王枫,裴福萍,孟恩,唐杰,徐美君,王伟. 2013. 中国东北中生代构造体制与区域成矿背景: 来自中生代火山岩组合时空变化的制约. 岩石学报, 29(2): 339-353. [Xu W L,Wang F,Pei F P,Meng E,Tang J,Xu M J,Wang W.2013. Mesozoic tectonic regimes and regional ore-forming background in NE China: Constraints from spatial and temporal variations of Mesozoic volcanic rock associations. Acta Petrologica Sinica, 29(2): 339-353] [22] 闫臻,边千韬,Korchagin O A,李继亮,王宗起,Pospelov I I.2008. 东昆仑南缘早三叠世洪水川组的源区特征: 来自碎屑组成、重矿物和岩石地球化学的证据. 岩石学报, 24(5): 1068-1078. [Yan Z,Bian Q T,Korchagin O A,Li J L,Wang Z Q,Pospelov I I.2008. Provenance of Early Triassic Hongshuichuan Formation in the southern margin of the East Kunlun Mountains: Constrains from detrital framework heavy mineral analysis and geochemistry. Acta Petrologica Sinica, 24(5): 1068-1078] [23] 杨梅,洪天求,徐锦龙,李秀财,罗雷. 2018. 皖南志留系唐家坞组物源分析: 来自碎屑锆石年代学和岩石地球化学的制约. 沉积学报, 36(1): 42-56. [Yang M,Hong T Q,Xu J L,Li X C,Luo L.2018. Provenance analysis for the clastic rocks in Tangjiawu Formation,South Anhui: Constraints from detrital zircon ages and geochemistry characteristics. Acta Sedimentologica Sinica, 36(1): 42-56] [24] 杨仁超,李进步,樊爱萍,宗敏,张涛. 2013. 陆源沉积岩物源分析研究进展与发展趋势. 沉积学报, 31(1): 99-107. [Yang R C,Li J B,Fan A P,Zong M,Zhang T.2013. Research progress and development tendency of provenance analysis on terrigenous sedimentary rocks. Acta Sedimentologica Sinica, 31(1): 99-107] [25] 杨雅军,张立东,张立君,周国民,庞雪娇. 2012. 大兴安岭地区三叠系划分与对比. 地质与资源, 21(1): 67-73. [Yang Y J,Zhang L D,Zhang L J,Zhou G M,Pang X J.2012. Division and correlation of the Triassic strata in Daxinganling region. Geology and Resources, 21(1): 67-73] [26] 张宏,王明新,柳小明. 2008. LA-ICP-MS 测年对辽西—冀北地区髫髻山组火山岩上限年龄的限定. 科学通报, 53(15): 1815-1824. [Zhang H,Wang M X,Liu X M.2008. Constraints on the upper boundary age of the Tiaojishan Formation volcanic rocks in West Liaoning-North Hebei by LA-ICP-MS dating. Chinese Science Bulletin, 53(15): 1815-1824] [27] 张渝金,吴新伟,江斌,郭威,杨雅军,刘世伟,崔天日,李伟,李林川,司秋亮,张超. 2015. 大兴安岭扎兰屯地区格根敖包组碎屑锆石U-Pb年代学、地球化学特征及其地质意义. 吉林大学学报(地球科学版), 45(2): 404-416. [Zhang Y J,Wu X W,Jiang B,Guo W,Yang Y J,Liu S W,Cui T R,Li W,Li L C,Si Q L,Zhang C.2015. U-Pb geochronology of detrital zircon and the constraint of geochemistry the from the Gegen'aobao Formation in Middle of Zalantun area of Da Hinggan Mountains and its tectonic significance. Jilin University(Earth Science Edition), 45(2): 404-416] [28] 张渝金,张超,吴新伟,崔天日,杨雅军,陈会军,江斌,郭威,马永非. 2016. 大兴安岭北段扎兰屯地区晚古生代海相火山岩年代学和地球化学特征及其构造意义. 地质学报, 90(10): 2706-2720. [Zhang Y J,Zhang C,Wu X W,Cui T R,Yang Y J,Chen H J,Jiang B,Guo W,Ma Y F.2016. Geochronology and geochemistry of Late Paleozoic marine volcanic from the Zhalantun area in northern Da Hinggan Mountains and its geological significance. Acta Geologica Sinica, 90(10): 2706-2720] [29] 张渝金,吴新伟,张超,郭威,杨雅军,孙革. 2018. 黑龙江龙江盆地中侏罗统万宝组时代确定新证据及其地质意义. 地学前缘, 25(1): 182-196. [Zhang Y J,Wu X W,Zhang C,Guo W,Yang Y J,Sun G.2018. New evidences for dating of the Middle Jurassic Wanbao Formation in the Longjiang Basin,western margin of Heilongjiang Province. Earth Science Frontiers, 25(1): 182-196] [30] 张志萍,林春明,李艳丽,岳信东,张霞,徐深谋,漆滨汶. 2008. 内蒙古二连盆地白音查干凹陷达尔其地区下白垩统腾格尔组物源分析及沉积特征. 古地理学报, 10(6): 599-612. [Zhang Z P,Lin C M,Li Y L,Yue X D,Zhang X,Xu S M,Qi B W.2008. Sedimentary characteristics and provenance analysis of the Lower Cretaceous Tenggeer Formation in Daerqi area of Baiyinchagan sag,Erlian Basin,Inner Mongolia. Journal of Palaeogeography(Chinese Edition), 10(6): 599-612] [31] 赵红格,刘池洋. 2003. 物源分析方法及研究进展. 沉积学报, 21(3): 409-415. [Zhao H G,Liu C Y.2003. Approaches and prospects of provenance analysis. Acta Sedimentologica Sinica, 21(3): 409-415] [32] 赵越,徐刚,张拴宏,杨振宇,张岳桥,胡健民. 2004. 燕山运动与东亚构造体制的转变. 地学前缘, 11(3): 319-328. [Zhao Y,Xu G,Zhang S H,Yang Z Y,Zhang Y Q,Hu J M.2004. Yanshanian movement and conversion of tectonic regimes in East Asia. Earth Science Frontiers, 11(3): 319-328] [33] 郑勇,孔屏. 2013. 四川盆地西缘晚新生代大邑砾岩的物源及其成因: 来自重矿物和孢粉的证据. 岩石学报, 29(8): 2949-2958. [Zheng Y,Kong P.2013. Provenance and origin of the Late Cenozoic Dayi conglomerates in the western margin of the Sichuan Basin: New insights from heavy mineral and spore-pollen assemblages. Acta Petrologica Sinica, 29(8): 2949-2958] [34] 朱志军,郭福生. 2017. 云南兰坪盆地古近系碎屑岩重矿物分布规律及其指示意义. 地质通报,36(z1): 199-208. [Zhu Z J,Guo F S.2017. Heavy mineral distribution regularity of Paleogene detrital rocks in Lanping Basin,Yunnan Province. Geological Bulletin of China,36(z1): 199-208] [35] Bhatia M R.1983. Plate tectonics setting of sandstones and geochemical composition of sandstones. Journal of Geology, 91(6): 611-627. [36] Bhatia M R.1985. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks: Province and tectonic control. Sedimentary Geology, 45: 97-113. [37] Bhatia M R,Crook K A W.1986. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contribution to Mineralogy and Petrology, 92(2): 181-193. [38] Damiani D,Giorgetti G.2008. Provenance of glacial-marine sediments under the McMurdo Ross Ice Shelf(Windless Bight,Antarctica): Heavy minerals and geochemical data. Palaeogeography,Palaeoclimatology,Palaeoecology, 260(1-2): 262-283. [39] Dill H G.1998. A review of heavy minerals in clastic sediments with case studies from the alluvial-fan through the nearshore-marine environments. Earth-Science Reviews,45(1/2): 103-132. [40] Giorgetti G,Talarico F,Sandroni S.2009. Provenance of Pleistocene sediments in the ANDRILL AND-1B drillcore: Clay and heavy mineral data. Global and Planetary Change, 69(3): 94-102. [41] Pettijohn F J.1975. Sedimentary Rocks. New York: Harper & Row Pub, 523. [42] Roser B P,Korsch R J.1988. Provenance signatures of sandstone-mudstone suites determinant function analysis of major-element data. Chemical Geology, 67(1-2): 119-139. [43] Wu F Y,Yang J H,Lo C H,Wilde S A,Sun D Y,Jahn B M.2007. The Heilongjiang Group: A Jurassic accretionary complex in the Jiamusi Massif at the western Pacific margin of northeastern China. The Island Arc, 16(1): 156-172.
