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摘要: 马家街群分布在黑龙江省东部佳木斯地块桦南隆起的西南缘，主要由一套经历了接触变质作用的富铝、富碳沉积碎屑岩所组成。区域上，这套接触变质岩系具有变质矿物分带特征，由西向东依次出现十字石、红柱石、石榴石和黑云母。红柱石碳质板岩和石榴云母石英片岩2件样品获得的LA-ICP-MS U-Pb碎屑锆石年龄谱均显示有272~310Ma、479~533Ma和>800Ma三组年龄。根据两件样品显示的最小年龄均未小于272Ma，而且二者的最小年龄组（272~310Ma）具有类似的峰值年龄，分别为276Ma和279Ma，这限定了马家街群主体岩石沉积年龄的下限应在中二叠世之前。侵入马家街群的花岗岩的锆石年龄为259Ma，说明其接触变质作用时代为晚二叠世早期，限定了马家街群形成时代的上限。479~533Ma年龄组中，2件样品的峰值年龄分别为499Ma和522Ma，这是佳木斯地块麻山群中最为重要的高级变质和花岗质岩浆作用年龄。>800Ma的年龄组具有多个峰值年龄，说明源区（佳木斯地块）具有前寒武纪-早前寒武纪地壳。上述证据表明，马家街群是晚二叠世早期形成的一套接触变质岩系，而非前寒武纪区域变质岩系。鉴于479~533Ma的麻山群在佳木斯地块中普遍存在，说明以麻山群为代表的早古生代变质结晶岩系既是马家街群沉积的基底，也是重要的物源区；而276~279Ma的早二叠世火山岩在佳木斯地块东缘分布广泛，表明其对马家街群的沉积也具有一定的贡献。Abstract: Majiajie Group, exposed in the southwestern part of the Huanan Uplift in the Jiamusi Massif, in eastern Heilongjiang Province, northeastern China is a suit of contact metamorphic rocks, which is characteristics of metamorphic mineral zonation from staurolite, andalusite, garnet to biotite from the west to the east. The LA-ICP-MS zircon U-Pb dating of the andalusite-bearing carbon slate and garnet quatz schists from Majiajie Group give the three age populations: 272~310Ma, 479~533 and >800Ma. The two rock samples with the minimal age population of 272~310Ma show a similar peak age of 276Ma and 279Ma and the youngest age of 272Ma, suggesting that the deposition time of the Majiajie Group was before the Middle Permian. The zircon age of the granite intruding the Majiajie Group is 259Ma, suggesting that the time of contact metamorphism of the Majiajie Group occurred in the early Late Permian. The age population of 479~533Ma in the two samples gives a similar peak ages of 499Ma and 522Ma, which are the most important age of high-grade metamorphism and granitic intrusion in the Jiamusi Massif. The age population of >800Ma shows several peak ages of 975Ma, 1063Ma, 1284Ma and 1422Ma, which suggest that there were Precambrian crust in the source region for the Majiajie Group. These evidences indicate that the Majiajie Group was a suit of contact metamorphic rocks related to the early Late Permian granitic intrusion, instead of the Precambrian metamorphic rock series. In view of the facts that the zircon ages of 479~533Ma and >800Ma are widespread in the Mashan Group and the Early Permian volcanics with the zircon ages of 276~279Ma are widely distributed in the eastern margin of the Jiamusi Massif, it is concluded that the Mashan Group as the basement and material source made great contributions to the formation of the Majiajie Group, and the Early Permian volcanic rocks made a certain contribution to the deposition also.
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[1] Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192: 59-79
[2] Black LP, Kamo SL, Allen CM et al. 2003. TEMORA 1: A new zircon standard for Phanerozoic U-Pb geochronology. Chemical Geology, 200(1-2): 155-170
[3] Bureau of Geology and Mineral Resources of Heilongjiang Province (BGMRH). 1993. Regional Geology of Heilongjiang Province. Beijing: Geological Publishing House, 1-734 (in Chinese)
[4] Cao RJ, Zhao WJ and Xiao ZY.1982. Stratification and Comparison of Precambrian Strata in China. In: Institute of Nanjing Geology and Paleontology, Chinese Academy of Sciences (ed.). Beijing: Science Press, 1-27 (in Chinese)
[5] Cao X, Dang ZX and Zhang XZ. 1992. The Composite Jiamusi Terrane. Changchun: Jilin Publishing House of Science and Technology, 1-137 (in Chinese)
[6] Gao FH, Wang F, Cao HH, Zheng YH and Liu J. 2010. Zircon U-Pb ages of the basement granite from Suibin depression in Sanjiang basin and its tectonic implications. Journal of Jilin University (Earth Science Edition), 40(4): 955-960 (in Chinese with English abstract)
[7] Group of Strata Writing in Heilongjiang Province. 1979. The Regional Stratigraphic Scale of Northeastern China, Heilongjiang Province. Beijing: Geological Publishing House (in Chinese)
[8] Huang YC, Ren DH, Zhang XZ, Xiong XS, Zhang CY, Wang Y and Zhao LL. 2008. Zircon U-Pb dating of Meizuo granite and geological significance in the Huanan Uplift, East Heilongjiang Province. Journal of Jilin University (Earth Science Edition), 38(4): 631-638 (in Chinese with English abstract)
[9] Huang YC, Zhang XZ, Zhang HB, Xiong XS, Liu CL and Zhao LL. 2009. Geochemical characteristics and sedimentation age of the Majiajie Group in eastern Heilongjiang Province, China. Acta Geologica Sinica, 83(2): 295-303 (in Chinese with English abstract)
[10] Jiang JS. 1992. Regional metamorphism and evolution of Mashan Khondalite Series. Acta Petrologica et Mineralogica, 11(2): 97-109 (in Chinese with English abstract)
[11] Li JY, Niu BG, Song B, Xu WX, Zhang YH and Zhao ZR. 1999. Crustal Formation and Evolution of Northern Changbai Mountains, Northeast China. Beijing: Geological Publishing House, 1-136 (in Chinese)
[12] Li JY. 2006. Permian geodynamic setting of Northeast China and adjacent regions: Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate. J. Asian Earth Sci., 26(3-4), 207-224
[13] Li XP, Jiao LX, Zheng QD, Dong X, Kong FM and Song ZJ. 2009. U-Pb zircon dating of the Heilongjiang complex at Huanan, Heilongjang Province. Acta Petrologica Sinica, 25(8): 1909-1916 (in Chinese with English abstract)
[14] Li XP, Kong FM, Zheng QD, Dong X and Yang ZY. 2010. Geochronological study on the Heilongjiang complex at Luobei area, Heilongjiang Province. Acta Petrologica Sinica, 26(7): 2015-2024 (in Chinese with English abstract)
[15] Liu JL. 1991. Characteristics of greenschist belt and analysis of tectonic environment of Jamusi terrane. Heilongjiang Geology, 2(1): 33-48 (in Chinese)
[16] Liu XM, Gao S, Diwu CR, Yuan HL and Hu ZC. 2007. Simultaneous in-situ determination of U-Pb age and trace elements in zircon by LAICP-MS in 20μm spot size. Chinese Science Bulletin, 52(9): 1257-1264
[17] Lu LZ, Xu XC and Liu FL. 1996. Early Precambrian Khondalitic Series in Northern China. Changchun: Changchun Publishing House, 126-194 (in Chinese)
[18] Ludwig KR. 2003. ISOPLOT 3: A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Centre Special Publication, 4, 74
[19] Meng E, Xu WL, Yang DB, Pei FP, Ji WQ, Yu Y and Zhang XZ. 2008. Permian volcanisms in eastern and southeastern margins of the Jiamusi Massif, northeastern China: Zircon U-Pb chronology, geochemistry and its tectonic implications. Chinese Science Bulletin, 53(8): 956-965 (in Chinese)
[20] Song B, Niu BG, Li JY and Xu XW. 1994. Isotope geochronology of granitoids in Mudanjiang-Jixi area. Acta Petrologica et Mineralogica, 13(3): 204-213 (in Chinese with English abstract)
[21] Song B, Li JY, Niu BG and Xu XW. 1997. Single-grain zircon ages and its implications in biotite-plagioclase gneiss in Mashan Group in the eastern Heilongjiang. Acta Geoscientia Sinica, 18(3): 306-312 (in Chinese with English abstract)
[22] Wang Y. 1992. Discussion on Heilongjiang complex. Heilongjiang Geology, 3(3): 1-8 (in Chinese)
[23] Wen QB, Liu YJ, Li WM, Han GQ and Ding L. 2008. Monazite age and its geological significance of granitoid gneiss in the Jiamusi Massif. Journal of Jilin University (Earth Science Edition), 38(2): 187-193 (in Chinese with English abstract)
[24] Wiedenbeck M, Alle P, Corfu F, Griffin WL, Meier M, Oberli F, Vonquadt A, Roddick JC and Speigel W. 1995. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace-element and REE analyses. Geostandards Newsletter, 19(1): 1-23
[25] Wilde SA, Zhang XZ and Wu FY. 2000. Extension of a newly-identified 500Ma metamorphic terrane in Northeast China: Further U-Pb SHRIMP dating of the Mashan Complex, Heilongjiang Province, China. Tectonophysics, 328(1-2): 115-130
[26] Wilde SA, Wu FY and Zhang XZ. 2001. 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. Geochimica, 30(1): 35-50 (in Chinese with English abstract)
[27] Wilde SA, Wu FY and Zhang XZ. 2003. Late Pan-African magmatism in northeastern China: SHRIMP U-Pb zircon evidence for igneous ages from the Mashan Complex. Precambrian Research, 122(1-4): 311-327
[28] Wu FY, Jahn BM, Wilde SA and Sun DY. 2000. Phanerozoic continental crustal growth: Sr-Nd isotopic evidence from the granites in northeastern China. Tectonophysics, 328: 87-113
[29] Wu FY, Wilde SA and Sun DY. 2001. Zircon SHRIMP U-Pb ages of gneissic granites in Jiamusi massif, northeastern China. Acta Petrologica Sinica, 17(3): 443-452 (in Chinese with English abstract)
[30] Wu FY, Yang JH, Lo CH, Wilde SA, Sun DY and Jahn BM. 2007. Jiamusi Massif in China: A Jurassic accrationary terrane in the western Pacific. The Island Arc, 16(1): 156-172
[31] Xie HQ, Zhang FQ, Miao LC, Chen FK and Liu DY. 2008a. Zircon SHRIMP U-Pb dating of the amphibolite from "Heilongjiang Group" and the granite in Mudanjiang area, NE China, and its geological significance. Acta Petrologica Sinica, 24(6): 1237-1250 (in Chinese with English abstract)
[32] Xie HQ, Miao LC, Chen FK, Zhang FQ and Liu DY. 2008b. Characteristics of the "Mashan Group" and zircon SHRIMP U-Pb dating of granite in Muling area, southeastern Heilongjiang Province, China: Constraint on crustal evolution of the southernmost of Jiamusi Massif. Geological Bulletin of China, 27(12): 2127-2137 (in Chinese with English abstract)
[33] Ye HW, Zhang XZ and Zhou YW. 1994. The 40Ar-39Ar age of the vein crossite in blueschist in Mudanjiang area NE China and its geological implication. Journal of Changchun University of Earth Science, 24(4): 369-372 (in Chinese with English abstract)
[34] Yuan HL, Gao S, Liu XM, et al. 2004. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry. Geostandards and Geoanalytical Research, 28(3): 353-370
[35] Zhang XZ and Zhang YH. 1991. Coexistence of blueschists and greenschists: A new evidence for the tectonic evolution of the Heilongjiang rock series. Journal of Changchun University of Earth Science, 21(3): 277-282 (in Chinese with English abstract)
[36] Zhang XZ. 1992. Heilongjiang melange: The evidence of Caledonian suture zone of the Jiamusi Massif. Journal of Changchun University of Earth Science, 22(Suppl.): 94-101 (in Chinese with English abstract)
[37] Zhang XZ, Ma YX, Chi XG, Zhang FX, Sun YW, Guo Y and Zeng Z. 2012. Discussion on Phanerozoic tectonic evolution in northeastern China. Journal of Jilin University (Earth Science Edition), 42(5): 1269-1285 (in Chinese with English abstract)
[38] Zhao LL and Zhang XZ. 2011. Petrologic and geochronologic evidences of tectonic exhumation of Heilongjiang Complex, in east part of Heilongjiang Province, China. Acta Petrologica Sinica, 27(4): 1227-1234 (in Chinese with English abstract)
[39] Zhou JB, Wilde SA, Zhang XZ, Zhao GC, Zheng CQ, Wang YJ and Zhang XH. 2009. The onset of Pacific margin accretion in NE China: Evidence from the Heilongjiang high-pressure metamorphic belt. Tectonophysics, 478(3-4): 230-246
[40] Zhou JB, Zhang XZ, Wilde SA, Zheng CQ, Jin W, Chen H and Han J. 2009. Detrital zircon U-Pb dating of Heilongjiang complex and its tectonic implications. Acta Petrologica Sinica, 25(8): 1924-1936 (in Chinese with English abstract)
[41] Zhou JB, Wilde SA, Zhao GC, Zhang XZ, Zheng CQ, Wang H and Zeng WS. 2010a. Pan-African metamorphic and magmatic rocks of the Khanka Massif, NE China: Further evidence regarding their affinity. Geological Magazine, 147(5): 737-749
[42] Zhou JB, Wilde SA, Zhao GC, Zhang XZ, Zheng CQ and Wang H. 2010b. New SHRIMP U-Pb zircon ages from the Heilongjiang complex in NE China: Constraints on the Mesozoic evolution of NE China. American Journal of Science, 310(9): 1024-1053
[43] 曹瑞骥, 赵文杰, 肖仲洋. 1982. 中国前寒武系的分层和对比. 见: 中国科学院南京地质古生物研究所编. 北京: 科学出版社, 1-27
[44] 曹熹, 党增欣, 张兴洲. 1992. 佳木斯复合地体. 长春: 吉林科技出版社, 1-137
[45] 高福红, 王枫, 曹花花, 郑宇航, 刘军. 2010. 三江盆地绥滨断陷基底花岗岩的锆石U-Pb年代学及其构造意义. 吉林大学学报(地球科学版), 40(4): 955-960
[46] 黑龙江省地质矿产局. 1993. 黑龙江省区域地质志. 北京: 地质出版社, 1-734
[47] 黑龙江省区域地层编写组. 1979. 东北地区区域地层表, 黑龙江省分册. 北京: 地质出版社
[48] 黄映聪, 任东辉, 张兴洲, 熊小松, 张春艳, 王跃, 赵亮亮. 2008. 黑龙江省东部桦南隆起美作花岗岩的锆石U-Pb定年及其地质意义. 吉林大学学报(地球科学版), 38(4): 631-638
[49] 黄映聪, 张兴洲, 张宏宾, 熊小松, 刘昌林, 赵亮亮. 2009. 黑龙江东部马家街群的岩石地球化学特征及其沉积时代. 地质学报, 83(2): 295-303
[50] 姜继圣. 1992. 麻山群孔兹岩系主期区域变质作用及演化. 岩石矿物学杂志, 11(2): 97-108
[51] 李锦轶, 牛宝贵, 宋彪, 徐文喜, 张雨红, 赵子然. 1999. 长白山北段地壳的形成与演化. 北京: 地质出版社, 1-136
[52] 李旭平, 焦丽香, 郑庆道, 董晓, 孔凡梅, 宋召军. 2009. 黑龙江桦南地区黑龙江杂岩锆石U-Pb定年. 岩石学报, 25(8): 1909-1916
[53] 李旭平, 孔凡梅, 郑庆道, 董晓, 杨振毅. 2010. 黑龙江萝北地区黑龙江杂岩年代学研究. 岩石学报, 26(7): 2015-2024
[54] 刘静兰. 1991. 佳木斯中间地块绿岩带特征及其大地构造环境浅析. 黑龙江地质, 2(1): 33-48
[55] 卢良兆, 徐学纯, 刘福来. 1996. 中国北方早前寒武纪孔兹岩系. 长春: 长春出版社, 126-194
[56] 孟恩, 许文良, 杨德彬, 裴福萍, 纪伟强, 于洋, 张兴洲. 2008. 佳木斯地块东缘及东南缘二叠纪火山作用: 锆石U-Pb年代学、地球化学及其构造意义. 科学通报, 53(8): 956-965
[57] 宋彪, 牛宝贵, 李锦轶, 徐文喜. 1994. 牡丹江-鸡西花岗岩类同位素地质年代学研究. 岩石矿物学杂志, 13(3): 204-213
[58] 宋彪, 李锦轶, 牛宝贵, 徐文喜. 1997. 黑龙江省东部麻山群黑云斜长片麻岩中镐石的年龄 及其地质意义. 地球学报, 18(3): 306-312
[59] 王莹. 1992. 论黑龙江杂岩. 黑龙江地质, 3(3): 1-8
[60] 温泉波, 刘永江, 李伟民, 韩国卿, 丁凌. 2008. 佳木斯地块花岗质片麻岩的独居石年龄及其地质意义黑龙江桦南地区黑龙江杂岩锆石U-Pb 定年. 吉林大学学报(地球科学版), 38(2): 187-193
[61] Wilde SA, 吴福元, 张兴洲. 2001. 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. 地球化学, 30(1): 35-50
[62] 吴福元, Wilde SA, 孙德有. 2001. 佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄. 岩石学报, 17(3): 443-452
[63] 颉颃强, 张福勤, 苗来成, 陈福坤, 刘敦一. 2008a. 东北牡丹江地区"黑龙江群"中斜长角山岩与花岗岩的锆石SHRIMP U-Pb定年及其地质学意义. 岩石学报, 24(6): 1237-1250
[64] 颉颃强, 苗来成, 陈福坤, 张福勤, 刘敦一. 2008b. 黑龙江东南部穆棱地区"麻山群"的特征及花岗岩锆石SHRIMP U-Pb定年——对佳木斯地块最南缘地壳演化的制约. 地质通报, 27(12): 2127-2137
[65] 叶慧文, 张兴洲, 周裕文. 1994. 牡丹江地区蓝片岩中脉状青铝闪石40Ar-39Ar年龄及其地质意义. 长春地质学院学报, 24(4): 369-372
[66] 张兴洲, 张元厚. 1991. 蓝片岩与绿片岩共存: 龙江岩系构造演化的新证据. 长春地质学院学报, 21(3): 277-282
[67] 张兴洲. 1992. 黑龙江岩系-古佳木斯地块加里东缝合带的证据. 长春地质学院学报, 22(增): 94-101
[68] 张兴洲, 马玉霞, 迟效国, 张凤旭, 孙跃武, 郭冶, 曾振. 2012. 东北及内蒙古东部地区显生宙构造演化的有关问题. 吉林大学学报(地球科学版), 42(5): 1269-1285
[69] 赵亮亮, 张兴洲. 2011. 黑龙江杂岩构造折返的岩石学与年代学证据. 岩石学报, 27(4): 1227-1234
[70] 周建波, 张兴洲, Wilde SA, 郑常青, 金魏, 陈红, 韩杰. 2009. 黑龙江杂岩的碎屑锆石年代学及其大地构造意义. 岩石学报, 25(8): 1924-1936
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