华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2020.01.002

古地理学报 ›› 2020, Vol. 22 ›› Issue (1): 39-55. doi: 10.7605/gdlxb.2020.01.002

• 构造古地理学及古构造 • 上一篇下一篇

华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义^*

王淼¹, 周洪瑞¹, 张恒²

1 中国地质大学(北京)地球科学与资源学院,北京 100083;
2 中国地质科学院地质研究所,北京 100037

收稿日期:2019-05-02 出版日期:2020-02-01 发布日期:2020-03-04
通讯作者: 周洪瑞,男,1958年生,教授,博士生导师,主要从事沉积学和地层学的教学与研究工作。E-mail: zhouhr@cugb.edu.cn。
作者简介:王淼,男,1993年生,硕士生,矿物学、岩石学、矿床学专业,主要从事岩石学与沉积学研究。E-mail: 1623385801@qq.com。
基金资助:
*中国地质调查局项目(编号:DD20190370)和科技部基金项目(批准号:2015FY310100)联合资助

Detrital zircon geochronology and tectonic implications of the Mesoproterozoic Gaoshanhe Group in south margin of North China Craton

Wang Miao¹, Zhou Hong-Rui¹, Zhang Heng²

1 School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China;
2 Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China

Received:2019-05-02 Online:2020-02-01 Published:2020-03-04
Contact: Zhou Hong-Rui, born in 1958, is a professor and Ph.D. supervisor. He is mainly engaged in teaching and researches of sedimentology and stratigraphy. E-mail: Zhouhr@cugb.edu.cn.
About author:Wang Miao,born in 1993,is a master student. He is mainly engaged in petrology and sedimentology research. E-mail: 1623385801@qq.com.

摘要/Abstract

摘要： 为了探讨华北板块南缘中元古代沉积地层的时代归属和物质来源、区域古地理格局和大地构造特征,对豫西灵宝福地地区的高山河群进行碎屑锆石U-Pb年代学和锆石微量元素特征研究。获得的高山河群年龄最小(年轻)的单颗碎屑锆石 ²⁰⁷Pb/²⁰⁶Pb 年龄值为1685±39 Ma,从而限制了高山河群最早沉积年龄不早于1700 Ma。结合上覆的龙家园组年代学标定(1594±12 Ma),将高山河群的形成年代限定为1700—1600 Ma,即中元古代长城纪的中晚期,属国际地质年表的“固结纪”。高山河群中碎屑锆石 ²⁰⁷Pb/²⁰⁶Pb 年龄范围为1685—2751 Ma,呈现1850 Ma、2150 Ma、2300 Ma和2500 Ma共4个年龄峰值,对应于华北克拉通古元古代重要的地质事件,并且高山河群以1850 Ma和2500 Ma峰值年龄段的地质体为主要的物源区。根据高山河群与云梦山组碎屑锆石年龄频率对比,推测在豫西地区西侧存在以往报道较少的年龄为2500 Ma的地质体。根据熊耳群火山岩及其对应锆石的地球化学特征和熊耳期盆地动力学性质,并结合高山河群沉积相特征和沉积盆地构造属性,认为熊耳群形成于与“岛弧”共生的拉张性质的弧后盆地地区,而其上覆的高山河群为弧后盆地靠近大陆一侧的具有被动大陆边缘性质的滨浅海沉积。

关键词: 华北克拉通, 高山河群, 碎屑锆石U-Pb年代学, 物源分析, 大地构造

Abstract: In order to investigate the age attribution of the Mesoproterozoic sedimentary strata,regional paleogeographic pattern and tectonic evolution in the southern margin of the North China Craton(NCC),this study reports U-Pb geochronology and characteristics of trace elements of detrital zircons from the Gaoshanhe Group in the Lingbao-Fudi area of the western Henan Province. The ²⁰⁷Pb/²⁰⁶Pb age of the youngest zircon of the Gaoshanhe Group is 1685±39 Ma,which limited the earliest sedimentary age of the Gaoshanhe Group is no earlier than 1700 Ma. Combined with the chronological calibration of the Longjiayuan Formation(1594±12 Ma)overlying the Gaoshanhe Group,the age of the Gaoshanhe Group was limited to 1700-1600 Ma,which is the middle and late period of the Mesoproterozoic Changcheng period,corresponding to the international Statherian Period. The ²⁰⁷Pb/²⁰⁶Pb ages of the detrital zircons from the Gaoshanhe Group range from 1685 Ma to 2751 Ma,presenting four age peaks of 1850 Ma,2150 Ma,2300 Ma and 2500 Ma,corresponding to the Paleoproterozoic geological events of the North China Craton. The provenance of the Gaoshanhe Group is dominated by geological body of the 1850 Ma peak age and the 2500 Ma peak age. According to thecomparison of age frequency of detrital zircons in the Gaoshanhe Group and Yunmengshan Formations,it is speculated that there are 2500 Ma geological bodies reported less frequently in the west of the western Henan area. According to the geochemical characteristics of the Xionger Group volcanic rocks and their corresponding zircons,the basin dynamic property during the deposition of the Xionger Group,and the sedimentary properties of the Gaoshanhe Group and tectonic property of the sedimentary basin,the Xionger Group was most likely formed in the post-arc basin symbiotic with “island arcs” and the Gaoshanhe Group overlying the Xionger Group was deposited near the shore and shallow sea of passive continental marginal and close to the continental side of the back-arc basin.

Key words: North China Craton, Ganshanhe Group, detrital zircon U-Pb geochronology, provenance analysis, tectonic

中图分类号:

王淼, 周洪瑞, 张恒. 华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义^*[J]. 古地理学报, 2020, 22(1): 39-55.

Wang Miao, Zhou Hong-Rui, Zhang Heng. Detrital zircon geochronology and tectonic implications of the Mesoproterozoic Gaoshanhe Group in south margin of North China Craton[J]. JOPC, 2020, 22(1): 39-55.

http://www.gdlxb.cn/CN/Y2020/V22/I1/39

参考文献

[1] 陈晋镳. 1999. 中国地层典·中元古界. 北京: 地质出版社,16-28.
[Chen J B. 1999. Chinese Stratigraphic Code: Mesoproterozoic. Beijing: Geological Publishing House, 16-28]
[2] 第五春荣,孙勇,袁洪林,王洪亮,钟兴平,柳小明. 2008. 河南登封地区嵩山石英岩碎屑锆石U-Pb年代学、Hf同位素组成及其地质意义. 科学通报, 53(16): 1923-1934.
[Diwu C R,Sun Y,Yuan H L,Wang H L,Zhong X P,Liu X M.2008. Detrital zircon U-Pb chronology,Hf isotopic compositions and geological significance of Songshan quartzites from Dengfeng,Henan. Chinese Science Bulletin, 53(16): 1923-1934]
[3] 高林志,张传恒,史晓颖,宋彪,王自强,刘耀明. 2008a. 华北古陆下马岭组归属中元古界的锆石 SHRIMP 年龄新证据. 科学通报, 53(21): 2617-2623.
[Gao L Z,Zhang C H,Shi X Y,Song B,Wang Z Q,Liu Y M.2008a. Mesoproterozoic age for Xiamaling Formation in North China Plate indicated by zircon SHRIMP dating. Chinese Science Bulletin, 53(21): 2617-2623]
[4] 高林志,张传恒,尹崇玉,史晓颖,王自强,刘耀明,刘鹏举,唐烽,宋彪. 2008b. 华北古陆中、新元古代年代地层框架 SHRIMP 锆石年龄新依据. 地球学报, 29(3): 366-376.
[Gao L Z,Zhang C H,Yin C Y,Shi X Y,Wang Z Q,Liu Y M,Liu P J,Tang F,Song B.2008b. SHRIMP zircon ages: Basis for refining the chronostratigraphic classification of the Meso- and Neoproterozoic strata in North China old land. Acta Geoscientica Sinica, 29(3): 366-376]
[5] 高林志,张传恒,刘鹏举,丁孝忠,王自强,张彦杰. 2009. 华北—江南地区中、新元古代地层格架的再认识. 地球学报, 30(4): 433-446.
[Gao L Z,Zhang C H,Liu P J,Ding X Z,Wang Z Q,Zhang Y J.2009. Recognition of Meso- and Neoproterozoic stratigraphic framework in North and South China. Acta Geoscientica Sinica, 30(4): 433-446]
[6] 河南省地质矿产局. 1997. 河南省岩石地层. 武汉: 中国地质大学出版社: 1-299.
[Henan Bureau of Geology and Mineral Resources. 1997. Stratigraphy of Henan Province. Wuhan: China University of Geosciences Press,1-299]
[7] 呼延钰莹,路玉. 2016. 小秦岭熊耳群火山岩锆石U-Pb年龄及其地球化学特征. 地质科技情报, 35(5): 1-8.
[Huyan Y Y,Lu Y.2016. Zircon U-Pb age and geochemical characteristics of Xiong'er Group volcanic rocks from Xiaoqinling area. Geological Science and Technology Information, 35(5): 1-8]
[8] 胡波,翟明国,彭澎,刘富,第五春荣,王浩铮,张海东. 2013. 华北克拉通古元古代末—新元古代地质事件: 来自北京西山地区寒武系和侏罗系碎屑锆石LA-ICP-MS U-Pb年代学的证据. 岩石学报, 29(7): 2508-2536.
[Hu B,Zhai M G,Peng P,Liu F,Diwu C R,Wang H Z,Zhang H D.2013. Late Paleoproterozoic to Neoproterozoic geological events of the North China Craton: Evidences from LA-ICP-MS U-Pb geochronology of detrital zircons from the Cambrian and Jurassic sedimentary rocks in Western Hills of Beijing. Acta Petrologica Sinica, 29(7): 2508-2536]
[9] 胡国辉,周艳艳,赵太平. 2012. 河南嵩山地区元古宙五佛山群沉积岩的地球化学特征及其对物源区和构造环境的制约. 岩石学报, 28(11): 3692-3704.
[Hu G H,Zhou Y Y,Zhao T P.2012. Geochemistry of Proterozoic Wufoshan Group sedimentary rocks in the Songshan area,Henan Province: Implications for provenance and tectonic setting. Acta Petrologica Sinica, 28(11): 3692-3704]
[10] 胡云绪,付嘉媛. 1982. 陕西洛南上前寒武系高山河组的微古植物群及其地层意义. 中国地质科学院西安地质矿产研究所文集: 100-114.
[Hu Y X,Fu J Y.1982. Micropalaeoflora from the Gaoshanhe Formation of Late Precambrian of Luonan,Shaanxi and its stratigraphic significance. Bulletin of the Xi'an Institute of Geology and Mineral Resources,Chinese Academy of Geological Science: 100-114]
[11] 华洪,胡云绪,翦万筹. 1995. 犁沟迹: 一类中元古代节肢动物爬迹. 西北大学学报(自然科学版), 25(5): 494-496.
[Hua H,Hu Y X,Jian W C.1995. Alocichnus: A Middle Proterozoic arthropod track. Journal of Northwest University(Natural Science Edition), 25(5): 494-496]
[12] 李承东,赵利刚,常青松,许雅雯,王世炎,许腾. 2017. 豫西洛峪口组凝灰岩锆石LA-MC-ICPMS U-Pb年龄及地层归属讨论. 中国地质, 44(3): 511-525.
[Li C D,Zhao L G,Chang Q S,Xu Y W,Wang S Y,Xu T.2017. Zircon U-Pb dating of tuff bed from Luoyukou Formation in western Henan Province on the southern margin of the North China Craton and its stratigraphic attribution discussion. Geology in China, 44(3): 511-525]
[13] 李怀坤,朱士兴,相振群,苏文博,陆松年,周红英,杨锋杰. 2010. 北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束. 岩石学报, 26(7): 2131-2140.
[Li H K,Zhu S X,Xiang Z Q,Su W B,Lu S N,Zhou H Y,Yang F J.2010. Zircon U-Pb dating on tuff bed from Gaoyuzhuang Formationin in Yanqing,Beijing: Further constraints on the new subdivision of the Mesoproterozoic stratigraphy in the northern North China. Acta Petrologica Sinica, 26(7): 2131-2140]
[14] 李怀坤,苏文博,周红英,耿建珍,相振群,崔玉荣,刘文灿,陆松年. 2011. 华北克拉通北部长城系底界年龄小于1670 Ma: 来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束. 地学前缘, 18(3): 108-120.
[Li H K,Su W B,Zhou H Y,Geng J Z,Xiang Z Q,Cui Y R,Liu W C,Lu S N.2011. The base age of the Changchengian System at the northern North China Craton should be younger than 1670 Ma: Constraints from zircon U-Pb LA-MC-ICPMS dating of a graniteporphyry dike in Miyun County,Beijing. Earth Science Frontiers, 18(3): 108-120]
[15] 李怀坤,苏文博,周红英,相振群,田辉,杨立公,Ettensohn F R.2014. 中—新元古界标准剖面蓟县系首获高精度年龄制约: 蓟县剖面雾迷山组和铁岭组斑脱岩锆石SHRIMP U-Pb同位素定年研究. 岩石学报, 30(10): 2999-3012.
[Li H K,Su W B,Zhou H Y,Xiang Z Q,Tian H,Yang L G,Ettensohn F R.2014. The first precise age constraints on the Jixian System of the Meso-Neoproterozoic standard section of China: SHRIMP zircon U-Pb dating of bentonites from the Wumishan and Tieling Formations in the Jixian section,North China Craton. Acta Petrologica Sinica, 30(10): 2999-3012]
[16] 李猛,王超,王钊飞. 2013. 华北克拉通西南缘汝阳群沉积时代及其地质意义: 来自碎屑锆石U-Pb年龄的证据. 地质科学, 48(4): 1115-1139.
[Li M,Wang C,Wang Z F.2013. Depositional age and geological implications of the Ruyang Group in the southwestern margin of the North China Craton: Evidence from detrital zircon U-Pb ages. Chinese Journal of Geology, 48(4): 1115-1139]
[17] 李钦仲,杨应章,贾金昌. 1985. 华北地台南缘(陕西部分)晚前寒武纪地层研究. 陕西: 西安交通大学出版社.
[Li Q Z,Yang Y Z,Jia J C. 1985. Late Cambrian Stratigraphy in the Southern Margin of the North China Platform(Shaanxi). Shaanxi: Xi'an Jiaotong University Press]
[18] 李文厚. 1987. 陕西洛南长城系一种可能的蠕形动物的发现. 西北大学学报, 17(8): 64-67+125.
[Li W H.1987. The discovery of a possible worm from Changcheng Syetem in Luonan County, Shaanxi Province. Journal of Northwest University, 17(8): 64-67+125]
[19] 柳晓艳,蔡剑辉,阎国翰. 2011. 华北克拉通南缘熊耳群眼窑寨组次火山岩岩石地球化学与年代学研究及其意义. 地质学报, 85(7): 1134-1145.
[Liu X Y,Cai J H,Yan G H.2011. Lithogeochemistry and geochronology of Xiong'er Group Yanyaozhai subvolcanics in the southern margin of the North China Craton and their geological significance. Acta Geologica Sinica, 85(7): 1134-1145]
[20] 彭楠,旷红伟,柳永清,耿元生,夏晓旭,王玉冲,陈骁帅,郑行海. 2018. 华北克拉通南缘汝阳群大型具刺疑源类时代再厘定及早期真核生物群演化意义. 古地理学报, 20(4): 595-608.
[Peng N,Kuang H W,Liu Y Q,Geng Y S,Xia X X,Wang Y C,Chen X S,Zheng H H.2018. Recognition of geological age for acanthomorphic acritarchs from the Ruyang Group,southern margin of North China Craton and its implication for evolution of early eukaryotes. Journal of Palaeogeography(Chinese Edition), 20(4): 595-608]
[21] 苏文博,李怀坤,Huff W D,Ettensohn F R,张世红,周红英,万渝生. 2010. 铁岭组钾质斑脱岩锆石 SHRIMP U-Pb年代学研究及其地质意义. 科学通报, 55(22): 2197-2206.
[Su W B,Li H K,Huff W D,Ettensohn F R,Zhang S H,Zhou H Y,Wan Y S.2010. SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation,North China. Chinese Science Bulletin, 55(22): 2197-2206]
[22] 苏文博,李怀坤,徐莉,贾松海,耿建珍,周红英,王志宏,蒲含勇. 2012. 华北克拉通南缘洛峪群—汝阳群属于中元古界长城系: 河南汝州洛峪口组层凝灰岩锆石LA-MC-ICPMS U-Pb年龄的直接约束. 地质调查与研究, 35(2): 96-108.
[Su W B,Li H K,Xu L,Jia S H,Geng J Z,Zhou H Y,Wang Z H,Pu H Y.2012. Luoyu and Ruyang group at the south margin of the North China Craton should belong in the Mesoproterozoic Changchengian System: Direct constraints from the LA-MC-ICPMS U-Pb age of the tuffite in the Luoyukou Formation,Ruzhou,He'nan,China. Geological Survey and Research, 35(2): 96-108]
[23] 苏文博. 2014.2012年全球前寒武纪新年表与中国中元古代年代地层学研究. 地学前缘, 21(2): 119-138.
[Su W B.2014. A review of the revised Precambrian Time Scale(GTS2012)and the research of the Mesoproterozoic chronostratigraphy of China. Earth Science Frontiers, 21(2): 119-138]
[24] 谭聪,卢远征,宋昊南,吕奇奇,邓胜徽,王华建,苏玲. 2019. 华北克拉通西南缘高山河组凝灰岩锆石U-Pb年龄及其地质意义. 地质学报, 93(5): 1113-1124.
[Tan C,Lu Y Z,Song H N,Lü Q Q,Deng S H,Wang H J,Su L.2019. Zircon U-Pb dating of the Gaoshanhe Formation tuff in the southwestern margin of the North China Craton and its geological singificance. Acta Geologica Sinica, 93(5): 1113-1124]
[25] 阎国翰,马芳,蔡剑辉,任康绪,刘楚雄,柳晓艳,牟保磊,杨斌,李凤棠,黄宝玲. 2010. 华北克拉通南缘栾川群大洪口组碱性粗面岩锆石SHRIMP U-Pb年龄及其意义. 北京: 2010年全国岩石学与地球动力学研讨会,289-290.
[Yan G H,Ma F,Cai J H,Ren K C,Liu C X,Liu X Y,Mou B L,Yang B,Li F T,Huang B L.2010. SHRIMP U-Pb zircon ages of the trachyte in the Dahongkou Formation,Luanchuan Group,southern margin of the North China Craton. Beijing: National Symposium on Petrologyand Geodynamics,289-290]
[26] 汪校锋. 2015. 华北南缘中—新元古代地层年代学研究及其地质意义. 中国地质大学(武汉)博士学位论文: 1-120.
[Wang X F.2015. The geochronology of the Meso-Neoproterozoic strata in the southern margin of North China and its geological significance. Doctoral Dissertation of China University of Geosciences(Wuhan): 1-120]
[27] 王淼,周洪瑞,张恒. 2020. 华北南缘中元古代地层归属及大地构造演化:来自碎屑锆石U-Pb年代学和锆石微量元素的证据.地质学报, doi:10.19762/j.cnki.dizhixuebao.2019000.
[Wang M, Zhou H R, Zhang H.2020. Mesoproterozoic stratigraphic attribution and tectonic evolution in south margin of the North China Craton: Evidences from the detrital zircon U-Pb geochronology and zircon trace elements. Acta Geologica Sinica, doi:10.19762/j.cnki.dizhixuebao.2019000]
[28] 项礼文,朱兆玲,李善姬,周志强. 1999. 中国地层典·寒武系. 北京: 地质出版社.
[Xiang L W,Zhu Z L,Li S J,Zhou Z Q.1999. Chinese Stratigraphy Code: Cambrian System. Beijing: Geological Publishing House]
[29] 谢良鲜,司荣军,王世炎,马瑞申. 2014. 嵩山地区熊耳群火山岩岩石学、地球化学及成因探讨. 地质找矿论丛, 29(3): 408-416.
[Xie L X,Si R J,Wang S Y,Ma R S.2014. Petrology,geochemistry and genesis for volcanics of Xiong'er Group in Songshan area. Contributions to Geology and Mineral Resources Research, 29(3): 408-416]
[30] 邢裕盛. 1996. 中国地层典·新元古界. 北京: 地质出版社,17-29.
[Xing Y S. 1996. Chinese Stratigraphic Code: Neoproterozoic. Beijing: Geological Publishing House,17-29]
[31] 翟明国,孟庆任,刘建明,侯泉林,胡圣标,李忠,张宏福,刘伟,邵济安,朱日祥. 2004. 华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨. 地学前缘, 11(3): 285-297.
[Zhai M G,Meng Q R,Liu J M,Hou Q L,Hu S B,Li Z,Zhang H F,Liu W,Shao J A,Zhu R X.2004. Geological features of Mesozoic tectonic regime in version in Eastern North China and implication for geodynamics. Earth Science Frontier, 11(3): 285-297]
[32] 翟明国,彭澎. 2007. 华北克拉通古元古代构造事件. 岩石学报, 23(11): 2665-2682.
[Zhai M G,Peng P.2007. Paleoproterozoic events in the North China Craton. Acta Petrologica Sinica, 23(11): 2665-2682]
[33] 翟明国. 2010. 华北克拉通的形成演化与成矿作用. 矿床地质, 29(1): 24-36.
[Zhai M G.2010. Tectonic evolution and metallogenesis of North China Craton. Mineral Deposits, 29(1): 24-36]
[34] 张航川,徐亚军,杜远生,王国庆,杨坤光. 2018. 北京周口店太平山南坡晚古生代碎屑锆石U-Pb年代学及其大地构造意义. 地球科学, 43(6): 2100-2115.
[Zhang H C,Xu Y J,Du Y S,Wang G Q,Yang K G.2018. Detrital zircon geochronology of Late Paleozoic strata from southern hill side of Taiping Hill in Zhoukoudian area,Beijing and their tectonic implications. Earth Science, 43(6): 2100-2115]
[35] 张拴宏,赵越,叶浩,胡健民,吴飞. 2013. 燕辽地区长城系串岭沟组及团山子组沉积时代的新制约. 岩石学报, 29(7): 2481-2490.
[Zhang S H,Zhao Y,Ye H,Hu J M,Wu F.2013. New constraints on ages of the Chuanlinggou and Tuanshanzi Formations of the Changcheng System in the Yan-Liao area in the northern North China Craton. Acta Petrologica Sinica, 29(7): 2481-2490]
[36] 张恒,高林志,周洪瑞,宋彪,丁孝忠,张传恒,刘昊岗,龚成强. 2019. 华北克拉通南缘官道口群和洛峪群的年代学研究新进展: 来自凝灰岩 SHRIMP 锆石U-Pb年龄的新证据. 岩石学报, 35(8): 2470-2486.
[Zhang H,Gao L Z,Zhou H R,Song B,Ding X Z,Zhang C,Liu H G,Gong C Q.2019. Guandaokou and Luoyu groups in the southern margin of North China Craton: Constraints on zircon U-Pb dating of tuff by means of the SHRIMP. Acta Petrologica Sinica, 35(8): 2470-2486]
[37] 赵太平,翟明国,夏斌,李惠民,张毅星,万渝生. 2004. 熊耳群火山岩锆石SHRIMP年代学研究: 对华北克拉通盖层发育初始时间的制约. 科学通报, 49(22): 2342-2349.
[Zhao T P,Zhai M G,Xia B,Li H M,Zhang Y X,Wan Y S.2004. Zircon U-Pb SHRIMP dating for the volcanic rocks of the Xiong'er Group: Constraints on the initial formation age of the cover of the North China Craton. Chinese Science Bulletin, 49(22): 2342-2349]
[38] 赵太平,徐勇航,翟明国. 2007. 华北陆块南部元古宙熊耳群火山岩的成因与构造环境: 事实与争议. 高校地质学报, 13(2): 191-206.
[Zhao T P,Xu Y H,Zhai M G.2007. Petrogenesis and tectonic setting of the Paleoproterozoic Xiong'er Group in the southern part of the North China Craton: A review. Geological Journal of China Universities, 13(2): 191-206]
[39] 周洪瑞,王自强,崔新省,雷振宇,董文明. 1998. 豫西地区中、新元古代地层沉积特征及层序地层学研究. 现代地质, 12(1): 18-25.
[Zhou H R,Wang Z Q,Cui X S,Lei Z Y,Dong W M.1998. Study on sedimentology and sequence stratigraphy of the Mesoproterozoic and Neoproterozoic in the west of Henan Province. Geoscience, 12(1): 18-25]
[40] Andersen T.2002. Correction of common lead in U-Pb analyses that do not report ²⁰⁴Pb. Chemical Geology, 192(1-2): 59-79.
[41] Belousova E,Griffin W,O'Reilly Y S,Fisher N.2002. Igneous zircon: Trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology, 143(5): 602-622.
[42] Carley T L,Miller C F,Wooden J L,Padilla A J,Schmitt A K,Economos R C,Bindeman I N, Jordan B T.2014. Iceland is not a magmatic analog for the Hadean: Evidence from the zircon record. Earth and Planetary Science Letters, 405: 85-97.
[43] Cawood P,Nemchin A.2001. Paleogeographic development of the East Laurentian margin: Constraints from U-Pb dating of detrital zircons in the Newfoundland Appalachians. Geological Society of America Bulletin, 113(9): 1234-1246.
[44] Cherniak D J,Hanchar J M,Watson E B.1997. Diffusion of tetravalent cations in zircon. Contributions to Mineralogy and Petrology, 127(4): 383-390.
[45] Cherniak D J,Watson E B.2001. Pb diffusion in zircon. Chemical Geology, 172(1-2): 5-24.
[46] Liu Y S,Hu Z C,Zong K Q,Gao C G,Gao S,Xu J,Chen H H.2010. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15): 1535-1546.
[47] Pei Q M,Zhang S T,Santosh M,Cao H W,Zhang W,Hu X K,Wang L.2017. Geochronology,geochemistry,fluid inclusion and C,O and Hf isotope compositions of the Shuitou fluorite deposit,Inner Mongolia,China. Ore Geology Reviews, 83: 174-190.
[48] Peng P,Zhai M G,Zhang H F,Guo J H.2005. Geochronological constraints on the Paleoproterozoic evolution of the North China Craton: SHRIMP zircon ages of different types of mafic dikes. International Geology Review, 47(5): 492-508.
[49] Roser B P,Korsch R J.1986. Determination of tectonic setting of sandstone-mudstone suites using SiO₂ content and K₂O/Na₂O ratio. The Journal of Geology, 94(5): 635-650.
[50] Sircombe K,Freeman M.1999. Provenance of detrital zircons on the Western Australia coastline: Implications for the geological history of the Perth Basin and denudation of the Yilgarn Craton. Geology, 27(10): 879.
[51] Wilde S A.2001. Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago. Nature, 409(6817): 175-178.
[52] Wilde S A,Zhao G C.2005. Archean to Paleoproterozoic evolution of the North China Craton. Journal of Asian Earth Sciences, 24(5): 519-522.
[53] Wu F Y,Zhao G C,Wilde S A,Sun D Y.2005. Nd isotopic constraints on crustal formation in the North China Craton. Journal of Asian Earth Sciences, 24(5): 523-545.
[54] Yang J H,Cawood P A,Du Y S,Huang H,Huang H W,Tao P.2012. Large igneous province and magmatic arc sourced Permian-Triassic volcanogenic sediments in China. Sedimentary Geology, 261-262: 120-131.
[55] Zhai M G,Li T,Peng P,Hu B,Liu F,Zhang Y.2010. Precambrian key tectonic events and evolution of the North China Craton. Geological Society, 338(1): 235-262.
[56] Zhai M G.2011. Cratonization and the ancient north China continent: A summary and review. Science China: Earth Sciences, 54(8): 1110-1120.

选择文件类型/文献管理软件名称

选择包含的内容

华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义^*

Detrital zircon geochronology and tectonic implications of the Mesoproterozoic Gaoshanhe Group in south margin of North China Craton

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张连昌, 佟小雪, 张新, 董志国, 王长乐, 朱明田, 高炳宇, 李文君. 华北克拉通沉积矿产与地球环境演变的关系^*[J]. 古地理学报, 2025, 27(2): 271-285.
[2]	杨文涛, 付强, 方特. 华北板块南缘洛南地区二叠系石盒子组沉积物源特征及其隆升过程^*[J]. 古地理学报, 2024, 26(3): 655-670.
[3]	宋双双, 索艳慧, 李三忠, 丁雪松, 韩续, 田子晗, 付新建. 华北早白垩世古地貌动态演变及热河生物群东迁^*[J]. 古地理学报, 2024, 26(1): 172-191.
[4]	翟明国. 太古宙的洋-陆与古地理问题^*[J]. 古地理学报, 2022, 24(5): 825-847.
[5]	任纪舜, 赵磊. 古地理与大地构造研究——简评目前的学术乱象^*[J]. 古地理学报, 2022, 24(5): 848-851.
[6]	何发岐, 王杰, 赵永强, 安川, 王付斌, 陶成, 倪春华, 贾会冲. 鄂尔多斯盆地东胜富氦气田成藏特征及其大地构造背景^*[J]. 古地理学报, 2022, 24(5): 937-950.
[7]	张青林, 张向涛, 许长海, 郑金云, 贾兆扬. 裂变径迹热年代学在珠江口盆地渐新统珠海组物源分析中的应用^*[J]. 古地理学报, 2022, 24(1): 129-138.
[8]	何佳伟, 谢渊, 侯明才, 刘建清, 何利, 芦云飞. 川西南盐津地区志留系龙马溪组页岩地球化学特征及地质意义^*[J]. 古地理学报, 2021, 23(6): 1174-1191.
[9]	罗立源, 李双应. 安徽宿松志留系—泥盆系碎屑锆石物源分析及其大地构造意义^*[J]. 古地理学报, 2021, 23(5): 999-1009.
[10]	和源, 文龙, 罗冰, 周刚, 王启宇, 李堃宇, 贾敏, 陈友莲, 白晓亮. 四川盆地开江地区WT1井震旦系陡山沱组物源分析及构造背景判断^*[J]. 古地理学报, 2021, 23(4): 683-702.
[11]	张连昌, 兰彩云, 王长乐, 彭自栋, 佟小雪, 李文君, 董志国. 古元古代大氧化事件(GOE)前后海洋环境的变化: 来自华北条带状铁建造(BIF)岩相学和地球化学的证据^*[J]. 古地理学报, 2020, 22(5): 827-840.
[12]	刘学飞, 王庆飞, 马遥, 李中明, 赵利华, 周智慧, 刘百顺, 马欣莉. 华北克拉通南缘石炭系本溪组铁-铝黏土矿物质来源: 以河南三门峡大安铝黏土矿床为例^*[J]. 古地理学报, 2020, 22(5): 965-976.
[13]	李磊, 向芳, 刘一鸣, 台梓含. 岷江演化讨论: 来自四川宜宾地区第四纪河流沉积物的重矿物证据^*[J]. 古地理学报, 2020, 22(4): 761-774.
[14]	刘朱睿鸷, 何幼斌, 李华, 黄伟. 鄂尔多斯盆地西南缘上奥陶统平凉组砂岩微量元素特征及构造背景: 以陇县段家峡剖面为例^*[J]. 古地理学报, 2020, 22(2): 333-348.
[15]	刘帅, 阮壮, 杨志辉, 吴雨轩, 李怡佳, 韩淑筠. 鄂尔多斯盆地南缘中晚三叠世物源演变及其地质意义^*[J]. 古地理学报, 2019, 21(6): 939-958.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义*

Detrital zircon geochronology and tectonic implications of the Mesoproterozoic Gaoshanhe Group in south margin of North China Craton

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

华北南缘中元古界高山河群碎屑锆石U-Pb年代学及其地质意义^*