ZIRCON U-Pb CHRONOLOGY OF THE HEILONGJIANG COMPLEX IN MUDANJIANG AREA: Geological Implication
-
摘要:
黑龙江杂岩主要出露在佳木斯地块西缘，沿牡丹江断裂分布，为佳木斯地块与松嫩地块拼合过程中形成的构造混杂岩.杂岩以强烈变形的长英质糜棱岩为主体，其中含有大量具洋壳性质的超基性岩、变基性熔岩（蓝片岩）及变硅质岩和大理岩等岩块或岩片.对出露于黑龙江省东部牡丹江地区的长英质糜棱岩进行了锆石LA-ICP-MS研究.获得两组206Pb/238U年龄数据，其加权平均年龄分别为509.4±7.1 Ma（n=9，MSWD=1.3）和269±1.9 Ma（n=22，MSWD=0.93）.其中最老2 420和2 459 Ma锆石年龄的出现，表明杂岩中有来自古元古界古老物质；509 Ma左右是佳木斯地块中麻山群的高级变质和花岗质岩浆作用年龄；约269 Ma年龄说明黑龙江杂岩变形基质形成于晚二叠世之后，可能与晚古生代古亚洲洋闭合事件相关.
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.
-
Key words:
- Heilongjiang complex /
- detrital zircon dating /
- Late Permian /
- Jiamusi massif /
- Mudanjiang area
-
-
表 1 黑龙江杂岩样品(10MD-07)锆石LA-ICP-MS U-Pb年龄数据表
Table 1. Zircon LA-ICP-MS U-Pb dating data of Heilongjiang complex sample 10MD-07
测试点位 元素含量/10-6 Th/U 同位素比值 年龄/Ma Conc. Th U 207Pb*/206Pb* 1σ 207Pb*/235U 1σ 206Pb*/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 10MD-07-1-01 318.5 695.8 0.46 0.0535 0.0030 0.3211 0.0191 0.0426 0.0009 350 126 283 15 269 5 95% 10MD-07-1-02 277.8 468.4 0.59 0.0535 0.0027 0.3079 0.0151 0.0419 0.0006 346 113 273 12 264 4 96% 10MD-07-1-03 252.3 633.2 0.40 0.0508 0.0026 0.3015 0.0155 0.0427 0.0006 232 120 268 12 270 4 99% 10MD-07-1-04 295.0 719.7 0.41 0.0503 0.0022 0.3034 0.0135 0.0434 0.0007 209 102 269 11 274 4 98% 10MD-07-1-05 359.2 875.2 0.41 0.0546 0.0031 0.3273 0.0180 0.0431 0.0006 394 130 288 14 272 4 94% 10MD-07-1-06 621.0 1477.7 0.42 0.0565 0.0021 0.3447 0.0129 0.0435 0.0005 472 81 301 10 275 3 90% 10MD-07-1-07 137.7 267.4 0.51 0.1612 0.0041 9.6725 0.2787 0.4303 0.0082 2468 43 2404 27 2307 37 95% 10MD-07-1-08 144.7 300.0 0.48 0.1566 0.0036 9.7653 0.3024 0.4441 0.0093 2420 40 2413 29 2369 42 98% 10MD-07-1-09 542.5 2654.5 0.20 0.0559 0.0013 0.6534 0.0156 0.0837 0.0009 456 54 511 10 518 5 98% 10MD-07-1-10 104.5 2044.0 0.05 0.0569 0.0016 0.6630 0.0182 0.0834 0.0010 487 56 516 11 516 6 99% 10MD-07-1-11 73.2 608.3 0.12 0.0522 0.0053 0.3052 0.0336 0.0423 0.0021 295 233 270 26 267 13 98% 10MD-07-1-12 184.0 307.9 0.60 0.0495 0.0030 0.2940 0.0172 0.0431 0.0006 172 144 262 13 272 4 96% 10MD-07-1-13 167.4 1986.8 0.08 0.0881 0.0034 0.8096 0.0292 0.0665 0.0012 1384 74 602 16 415 7 63% 10MD-07-1-14 102.1 1020.2 0.10 0.0807 0.0027 0.8971 0.0281 0.0799 0.0009 1215 67 650 15 496 6 73% 10MD-07-1-15 173.1 825.8 0.21 0.0566 0.0052 0.3056 0.0279 0.0406 0.0028 476 236 271 22 257 17 94% 10MD-07-1-16 338.4 410.5 0.82 0.0514 0.0027 0.3027 0.0155 0.0428 0.0006 257 120 268 12 270 4 99% 10MD-07-1-17 261.1 766.0 0.34 0.0518 0.0019 0.3095 0.0134 0.0436 0.0011 280 85 274 10 275 7 99% 10MD-07-1-18 160.2 396.7 0.40 0.0475 0.0023 0.2825 0.0132 0.0431 0.0005 72 117 253 10 272 3 92% 10MD-07-1-19 184.8 672.6 0.27 0.0564 0.0077 0.4005 0.0559 0.0510 0.0016 478 307 342 41 321 10 93% 10MD-07-1-20 748.7 1544.9 0.48 0.0532 0.0017 0.3121 0.0102 0.0421 0.0005 339 38 276 8 266 3 96% 10MD-07-1-21 11.8 93.6 0.13 0.0702 0.0185 0.3320 0.0573 0.0399 0.0042 1000 532 291 44 252 26 85% 10MD-07-1-22 630.0 377.7 1.67 0.0520 0.0062 0.2874 0.0345 0.0402 0.0012 283 317 257 27 254 8 98% 10MD-07-1-23 104.1 154.7 0.67 0.0601 0.0058 0.3202 0.0287 0.0409 0.0011 609 211 282 22 258 7 91% 10MD-07-1-24 117.5 134.7 0.87 0.0581 0.0045 0.3306 0.0234 0.0432 0.0009 600 164 290 18 272 5 93% 10MD-07-1-25 812.9 2353.1 0.35 0.0584 0.0058 0.6445 0.0773 0.0791 0.0028 546 214 505 48 491 16 97% 10MD-07-1-26 1172.5 2750.8 0.43 0.0594 0.0016 0.6735 0.0210 0.0817 0.0015 583 57 523 13 506 9 96% 10MD-07-1-27 249.3 717.4 0.35 0.0593 0.0062 0.6581 0.0773 0.0797 0.0025 576 230 513 47 494 15 96% 10MD-07-1-28 136.8 370.6 0.37 0.0569 0.0022 0.6456 0.0254 0.0820 0.0011 487 87 506 16 508 6 99% 10MD-07-1-29 1.1 81.1 0.01 0.0627 0.0125 0.3079 0.0445 0.0411 0.0022 698 432 273 35 260 13 95% 10MD-07-1-30 276.8 1003.6 0.28 0.0571 0.0029 0.6315 0.0301 0.0798 0.0019 498 114 497 19 495 12 99% 10MD-07-1-32 36.8 87.1 0.42 0.0745 0.0040 0.5677 0.0309 0.0552 0.0011 1054 108 457 20 346 7 72% 10MD-07-1-35 3.8 173.6 0.02 0.0547 0.0104 0.3072 0.0619 0.0410 0.0018 467 309 272 48 259 11 95% 10MD-07-1-36 320.3 767.9 0.42 0.0552 0.0029 0.3324 0.0175 0.0428 0.0006 420 151 291 13 270 3 92% 10MD-07-1-37 265.8 255.3 1.04 0.0542 0.0034 0.3178 0.0192 0.0424 0.0007 389 145 280 15 268 4 95% 10MD-07-1-38 139.0 446.4 0.31 0.0613 0.0028 0.6892 0.0319 0.0805 0.0015 650 100 532 19 499 9 93% 10MD-07-1-39 197.9 305.7 0.65 0.0601 0.0059 0.6555 0.0567 0.0790 0.0031 606 208 512 35 490 18 95% 10MD-07-1-40 206.8 688.1 0.30 0.0539 0.0026 0.3189 0.0146 0.0431 0.0007 369 111 281 11 272 5 96% 
下载: 导出CSV
-
[1] 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. doi: 10.3321/j.issn:0001-5717.1989.03.003
Dong S B. The general features and distributions of the glaucophane schist belts of China[J]. Acta Geologica Sinica, 1989, 63(3): 273-275. doi: 10.3321/j.issn:0001-5717.1989.03.003
[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. http://www.sciencedirect.com/science/article/pii/0743954789900354
[3] Liou J G, Maruyama S, Wang X, et al. Precambrian blueschist terranes of the world[J]. Tectonophysics, 1990, 181(1/4): 97-111. http://www.sciencedirect.com/science/article/pii/0040195190900106
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199303011.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199303011.htm
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199103005.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199103005.htm
[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. http://www.sciencedirect.com/science/article/pii/S1367912005001598
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199501001.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199501001.htm
[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. http://www.sciencedirect.com/science/article/pii/S0040195100001803
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200101005.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200101005.htm
[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. http://www.sciencedirect.com/science/article/pii/S0301926802002176
[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. doi: 10.1111/j.1440-1738.2007.00564.x
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908019.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908019.htm
[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. http://www.sciencedirect.com/science/article/pii/S0040195109004260
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908017.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908017.htm
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201007006.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201007006.htm
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW199202000.htm
Jiang J S. Regional metamorphism and evolution of Mashan khondalite series[J]. Acta Petrologicaet Mineralogica, 1992, 11(2): 97-110. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW199202000.htm
[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. doi: 10.1016/S1342-937X(05)70125-8
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200103012.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200103012.htm
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201001012.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201001012.htm
[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. http://www.sciencedirect.com/science/article/pii/S0009254103001657
[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. doi: 10.1007/s11434-007-0160-x
[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. http://www.sciencedirect.com/science/article/pii/S000925410200195X
[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. http://www.researchgate.net/publication/303107803_User's_manual_for_Isoplot_36_A_geochronological_toolkit_for_microsoft_excel_Berkeley_Geochronology_Center
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201607005.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201607005.htm
[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. http://www.sciencedirect.com/science/article/pii/S0040195100001797
[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. http://www.sciencedirect.com/science/article/pii/S1464189501001284
[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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402003.htm
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. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402003.htm
-
图(3)
表(1)
计量
- 文章访问数: 690
- PDF下载数: 53
- 施引文献: 0