ZIRCON U-Pb CHRONOLOGY OF THE HEILONGJIANG COMPLEX IN MUDANJIANG AREA: Geological Implication
ZHAO Liang-liang1, XU Fu-zhong1, ZHANG Yan1, NI Bin1, MA Xiao-hui2
1. Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 100025, China; 2. Geophysical Exploration Academy, China Metallurgical Geology Bureau, Baoding 071051, Hebei Province, China
Abstract:The Heilongjiang complex, mainly occurred in the western margin of Jiamusi massif along Mudanjiang fault, is a tectonic melange formed during the suturing of Jiamusi massif and Songnen massif. The complex is dominated by strongly deformed felsic mylonite, which contains a large number of ultrabasic rocks, metabasic lava (blueschist), meta-silicalite and marble blocks or slices with the nature of oceanic crust. The zircon LA-ICP-MS U-Pb dating of felsic mylonites in Mudanjiang area yields two groups of 206Pb/238U age data, with the weighted mean ages of 509.4±7.1 Ma (n=9, MSWD=1.3) and 269±1.9 Ma (n=22, MSWD=0.93). The zircons with the oldest ages of 2 420 and 2 459 Ma indicate that the complex contains ancient Paleoproterozoic materials. The age about 509 Ma is for advanced metamorphism and granitic magmatism of Mashan Group in Jiamusi massif. The age about 269 Ma suggests the deformed matrix of Heilongjiang complex be formed after Late Permian, which may be related to the closure of Paleo-Asian Ocean in Late Paleozoic.
董申保. 中国蓝闪石片岩带的一般特征及其分布[J]. 地质学报, 1989, 63(3):273-275. Dong S B. The general features and distributions of the glaucophane schist belts of China[J]. Acta Geologica Sinica, 1989, 63(3):273-275.
[2]
Yan Z Y, Tang K D, Bai J W, et al. High pressure metamorphic rocks and their tectonic environment in northeastern China[J]. Journal of Southeast Asian Earth Sciences, 1989, 3(1/4):303-313.
[3]
Liou J G, Maruyama S, Wang X, et al. Precambrian blueschist terranes of the world[J]. Tectonophysics, 1990, 181(1/4):97-111.
[4]
刘静兰. 佳木斯中间地块绿岩带特征及其大地构造环境浅析[J]. 黑龙江地质, 1991, 2(1):33-48. Liu J L. Analysis of characteristics of greenstone belt of Jiamusi medianmassif and its geotectonic setting[J]. Heilongjiang Geology, 1991, 2(1):33-48.
[5]
曹熹, 党增欣, 张兴洲, 等. 佳木斯复合地体[M]. 长春:吉林科学技术出版社, 1992:1-137. Cao X, Dang Z X, Zhang X Z, et al. The Jiamusi complex terrane[M]. Changchun:Jilin Science and Technology Publishing House, 1992:1-137. (in Chinese)
[6]
党廷松, 李德荣. 关于佳木斯地块前寒武纪同位素地质年代学问题的讨论[J]. 长春地质学院学报, 1993, 23(3):312-318. Dang T S, Li D R. Discussion on isotopic geochronology of Precambrian Jiamusi Block[J]. Journal of Changchun University of Earth Science, 1993, 23(3):312-318.
[7]
黑龙江省地质矿产局. 黑龙江省区域地质志[M]. 北京:地质出版社, 1993. Heilongjiang Bureau of Geology and Mineral Resources. Regional geology of Heilongjiang Province[M]. Beijing:Geological Publishing House, 1993. (in Chinese)
[8]
张兴洲. 黑龙江岩系——古佳木斯地块加里东缝合带的证据[J]. 长春地质学院学报, 1992, 22(S1):94-101. Zhang X Z. Heilogjiang mélange:The evidence of Caledonian suture zone of the Jiamusi massif[J]. Journal of Changchun University of Earth Science, 1992, 22(S1):94-101. (in Chinese)
[9]
张兴洲, 张元厚. 蓝片岩与绿片岩共存:龙江岩系构造演化的新证据[J]. 长春地质学院学报, 1991, 21(3):277-282, 348. Zhang X Z, Zhang Y H. Coexistence of blueschist and greenschist:New evidence for tectonic evolution of the Longjiang Suites[J]. Journal of Changchun University of Earth Science, 1991, 21(3):277-282,348.
[10]
张兴洲. 佳木斯地体的早期碰撞史——黑龙江岩系的构造-岩石学证据[D]:长春:长春地质学院, 1992. Zhang X Z. Early collision history of Jiamusi terrain:The tectonic-petrologic evidences of Heilogjiang Mélange[D]. Changchun:Changchun University of Earth Science, 1992. (in Chinese)
[11]
李锦轶, 牛宝贵, 宋彪, 等. 长白山北段地壳的形成与演化[M]. 北京:地质出版社, 1999:1-136. Li J Y, Niu B G, Song B, et al. Crustal formation and evolution of northern Changbai Mountains[M]. Beijing:Geological Publishing House, 1999:1-136. (in Chinese)
[12]
Li J Y. Permian geodynamic setting of Northeast China and adjacent regions:Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26(3/4):207-224.
[13]
唐克东, 王莹, 何国琦, 等. 中国东北及邻区大陆边缘构造[J]. 地质学报, 1995, 69(1):16-30. Tang K D, Wang Y, He G Q, et al. Continental-margin structure of Northeast China and its adjacent areas[J]. Acta Geologica Sinica, 1995, 69(1):16-30.
[14]
Wilde S A. Zhang X Z, Wu F Y. Extension of a newly identified 500 Ma metamorphic terrane in Northeast China:Further U-Pb SHRIMP dating of the Mashan complex, Heilongjiang Province, China[J]. Tectonophysics, 2000, 328(1/2):115-130.
[15]
Wilde S A, 吴福元, 张兴洲. 中国东北麻山杂岩晚泛非期变质的锆石SHRIMP年龄证据及全球大陆再造意义[J]. 地球化学, 2001, 30(1):35-50. Wilde S A, Wu F Y, Zhang X Z. The Mashan complex:SHRIMP U-Pb zircon evidence for a Late Pan-African metamorphic event in NE China and its implication for global continental reconstructions[J]. Geochimica, 2001, 30(1):35-50.
[16]
Wilde S A, Wu F Y, Zhang X Z. Late Pan-African magmatism in Northeastern China:SHRIMP U-Pb zircon evidence from granitoids in the Jiamusi massif[J]. Precambrian Research, 2003, 122(1/4):311-327.
[17]
Wu F Y, Yang J H, Lo C H, et al. Jiamusi massif in China:A Jurassic accrationary terrane in the western Pacific[J]. The Island Arc, 2007, 16:156-172.
[18]
周建波, 张兴洲, Wilde S A, 等. 黑龙江杂岩的碎屑锆石年代学及其大地构造意义[J]. 岩石学报, 2009, 25(8):1924-1936. Zhou J B, Zhang X Z, Wilde S A, et al. Detrital zircon U-Pb dating of Heilongjiang complex and its tectonic implications[J]. Acta Petrologica Sinica, 2009, 25(8):1924-1936.
[19]
Zhou J B, Wilde S A, Zhang X Z, et al. The onset of Pacific margin accretion in NE China:Evidence from the Heilongjiang high-pressure metamorphic belt[J]. Tectonophysics, 2009, 478(3/4):230-246.
[20]
李旭平, 焦丽香, 郑庆道, 等. 黑龙江桦南地区黑龙江杂岩锆石U-Pb定年[J]. 岩石学报, 2009, 25(8):1909-16. Li X P, Jiao L X, Zheng Q D, et al. U-Pb zircon dating of the Heilongjiang complex at Huanan, Heilongjiang Province[J]. Acta Petrologica Sinica, 2009, 25(8)1909-16.
[21]
李旭平, 孔凡梅, 郑庆道, 等. 黑龙江萝北地区黑龙江杂岩年代学研究[J]. 岩石学报, 2010, 26(7):2015-2024. Li X P, Kong F M, Zheng Q D, et al. Geochronological study on the Heilongjiang complex at Luobei area, Heilongjiang Province[J]. Acta Petrologica Sinica, 2010, 26(7):2015-2024.
[22]
姜继圣. 麻山群孔兹岩系主期区域变质作用及演化[J]. 岩石矿物学杂志, 1992, 11(2):97-110. Jiang J S. Regional metamorphism and evolution of Mashan khondalite series[J]. Acta Petrologicaet Mineralogica, 1992, 11(2):97-110.
[23]
卢良兆, 徐学纯, 刘福来. 中国北方早前寒武纪孔兹岩系[M]. 长春:长春出版社, 1996:126-194. Lu L Z, Xu X C, Liu F L. The early Cambrian khounds series in northern China[M]. Changchun:Changchun Publishing House, 1996:126-194. (in Chinese)
[24]
Wilde S A, Dorsett-Bain H L, Liu J L. The identification of a Late Pan-African granulite facies event in northeastern China:SHRIMP U-Pb zircon dating of the Mashan Group at Liumao, Heilongjiang Province, China[C]. Proceedings of the 30th IGC:Precambrian Geol Metamorphic Petrol, Amsterdam:VSP International Science Publishers, 1997, 17:59-74.
[25]
Wilde S A, Dorsett-Bain H L, Lennon R G. Geological setting and controls on the development of graphite, sillimanite and phosphate mineralization within the Jiamusi massif:An exotic fragment of Gondwanaland located in North-Eastern China?[J]. Gondwana Research, 1999, 2(1):21-46.
[26]
吴福元, Wilde S A, 孙德有. 佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄[J]. 岩石学报, 2001, 17(3):443-452. Wu F Y, Wilde S A, Sun D Y. Zircon SHRIMP U-Pb ages of gneissic granites in Jiamusi massif, northeastern China[J]. Acta Petrologica Sinica, 2001, 17(3):443-452.
[27]
周建波, 韩杰, 张兴洲, 等. 牡丹江地区蓝片岩的地球化学特征及其大地构造意义[J]. 吉林大学学报(地球科学版), 2010, 40(1):93-103. Zhou J B, Han J, Zhang X Z, et al. Geochemical Characteristics of the Mudanjiang blueschists in the NE China and its tectonic implications[J]. Journal of Jilin University (Earth Science Edition), 2010, 40(1):93-103.
[28]
Black L P, Kamo S L, Allen C M, et al. TEMORA 1:A new zircon standard for Phanerozoic U-Pb geochronology[J]. Chemical Geology, 2003, 200(1/2):155-170.
[29]
Liu X M, Gao S, Diwu C R, et al. Simultaneous in-situ determination of U-Pb age and trace elements in zircon by LA-ICP-MS in 20μm spot size[J]. Chinese Science Bulletin, 2007, 52(9):1257-1264.
[30]
Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
[31]
Ludwig K R. User's manual for IsoPlot 3.0:A geochronological toolkit for Microsoft Excel[M]. Berkeley, USA:Berkeley Geochronology Center, 2003:71.
[32]
吕长禄, 肖庆辉, 冯俊岭, 等. 黑龙江依兰地区变玄武岩及变堆晶辉长岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报, 2016, 35(7):1081-1094. Lv C L, Xiao Q H, Feng J L, et al. LA-ICP-MS U-Pb ages of zircons from metamorphic basalt and metamorphic accumulated gabbro in Yilan area, Heilongjiang Province, and their geological implications[J]. Geological Bulletin of China, 2016, 35(7):1081-1094.
[33]
Wu F Y, Jahn B M, Wilde S A, et al. Phanerozoic crustal growth:U-Pb and Sr-Nd isotopic evidence from the granites in northeastern China[J]. Tectonophysics, 2000, 328(1/2):89-113.
[34]
Wu F Y, Sun D Y, Li H M, et al. The nature of basement beneath the Songliao Basin in NE China:Geochemical and isotopic constraints[J]. Physics and Chemistry of the Earth, Part A:Solid Earth and Geodesy, 2001, 26(9/10):793-803.
[35]
孙德有, 吴福元, 张艳斌, 等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版), 2004, 34(2):174-181. Sun D Y, Wu F Y, Zhang Y B, et al. The final closing time of the West Lamulun River-Changchun-Yanji plate suture zone:Evidence from the Dayushan granitic pluton, Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2004, 34(2):174-181.