内蒙古头道桥地区蓝闪石片岩和相关变质岩石岩石学特征及其构造意义

doi:10.13278/j.cnki.jjuese.20170272

吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (2): 534-544.doi: 10.13278/j.cnki.jjuese.20170272

内蒙古头道桥地区蓝闪石片岩和相关变质岩石岩石学特征及其构造意义

赵立敏¹, 刘永江¹, 滕加雨², 李伟民¹

1. 吉林大学地球科学学院, 长春 130061;
2. 吉林省第一地质调查所, 长春 130033

收稿日期:2017-09-29 出版日期:2018-03-26 发布日期:2018-03-26
通讯作者: 刘永江(1964-),男,教授,博士生导师,主要从事大地构造学、构造年代学研究,E-mail:yongjiang@jlu.edu.cn E-mail:yongjiang@jlu.edu.cn
作者简介:赵立敏(1985-),女,助理工程师,主要从事构造地质学、变质岩石学研究,E-mail:zhaolimin@jlu.edu.cn
基金资助:
国家重点基础研究发展计划（"973"计划）项目（2013CB429802）；国家自然科学基金项目（41302175）

Character of Blueschist and Related Metamorphic Rocks from the Toudaoqiao Area, Inner Mongolia and Its Tectonic Implication

Zhao Limin¹, Liu Yongjiang¹, Teng Jiayu², Li Weimin¹

1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. The First Geologic Survey of Jilin Province, Changchun 130033, China

Received:2017-09-29 Online:2018-03-26 Published:2018-03-26
Supported by:
Supported by National Key Basic Research Program ("973" Program) of China(2013CB429802)and National Natural Science Foundation of China (41302175)

摘要/Abstract

摘要： 内蒙古头道桥地区出露了一套经高压变质形成的岩石组合。本次研究通过岩相学和矿物化学分析，根据矿物组合的不同，识别出蓝片岩、绿片岩两种不同类型的岩石类型。其中，蓝片岩的矿物组合为角闪石（蓝闪石、蓝透闪石）+绿帘石+钠长石+绿泥石+石英+赤铁矿±多硅白云母±方解石±榍石；绿片岩的矿物组合为绿泥石+钠长石+石英±绿帘石±角闪石（阳起石、镁角闪石、蓝透闪石、冻蓝闪石等）±多硅白云母±赤铁矿。确定了蓝片岩的峰期变质级别为绿帘-蓝闪片岩相，峰期变质温度为400~600℃，压力为1.2~1.4 GPa。绿片岩的峰期变质级别为绿帘-角闪岩相。结合前人研究成果，认为蓝片岩和绿片岩的形成与额尔古纳地块和兴安地块的碰撞拼合有关。

关键词: 头道桥地区, 蓝片岩, 绿片岩, 高压变质, 缝合带

Abstract: A set of high pressure metamorphic rocks are exposed in the Toudaoqiao area, Inner Mongolia. In this study,the investigations on petrography and mineral chemistry are carried out, and two types of metamorphic rocks are classified to blueschist and greenschist on the basis of the mineral assemblages. The mineral assemblage of the blueschist is amphibole+epidote+albite+chlorite+quartz+hematite±phengite±calcite±titanite, and the mineral assemblage of the greenschist is chlorite+albite+quartz±amphibole±epidote±phengite±hematite. The blueschists were suffered from the epidote-blueschist facies metamorphism, with the peak metamorphic conditions of T=400-600℃, p=1.2-1.4 GPa. The greenschists were suffered from the epidote-amphibole facies metamorphism. According to the previous geochronology data, the high pressure blueschist and greenschist are related to the suture zone between Eerguna and Xing'an massifs.

Key words: Toudaoqiao area, blueschist, greenschist, high-pressure metamorphism, suture zone

中图分类号:

赵立敏, 刘永江, 滕加雨, 李伟民. 内蒙古头道桥地区蓝闪石片岩和相关变质岩石岩石学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2018, 48(2): 534-544.

Zhao Limin, Liu Yongjiang, Teng Jiayu, Li Weimin. Character of Blueschist and Related Metamorphic Rocks from the Toudaoqiao Area, Inner Mongolia and Its Tectonic Implication[J]. Journal of Jilin University(Earth Science Edition), 2018, 48(2): 534-544.

参考文献

[1] Ernst W G. Tectonic History of Subduction Zones Inferred from Retrograde Blueschist p-T Path[J]. Geology, 1988, 16(12):1081-1084.
[2] 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):273-284. Dong Shenbao. The General Features and Distributions of the Glaucophane Schist Belts of China[J]. 1989, 16(12):1081-1084.
[3] 黑龙江省区域地质调查第二队一分队. 塔尔其幅1:20万区域地质调查报告[R]. 齐齐哈尔:黑龙江省地质局,1981:202-205. The Second Team of Regional Geological Survey of the Heilongjiang Province. 1:200000 Regional Geological Survey Report of the Tarq[R]. Qiqihaer:Bureau of Geology and Mineral Resources of Heilongjiang Province, 1981:202-205.
[4] 叶慧文,张兴洲,周裕文. 从蓝片岩及蛇绿岩特点看满洲里-绥芬河断面岩石圈结构与演化[M]//M-SGT地质课题组. 中国满洲里-绥芬河地学断面域内岩石圈结构及其演化的地质研究. 北京:地震出版社,1994:73-83. Ye Huiwen, Zhang Xingzhou, Zhou Yuwen. The Texture and Evolution of Manzhouli-Suifenhe Lithosphere:Study Based on Features of Blueschist and Ophiolites[M]//M-SGT Geology Group. Geological Studies of Lithospheric Structure and Evolution of Manzhouli-Suifenhe Geotransect, China. Beijing:Seismic Press, 1994:73-83.
[5] 张庆奎, 邵学峰, 关培彦, 等. 内蒙古苏布格塔蓝闪石片岩基本特征及成因分析[J]. 中国地质, 2014, 41(4):1205-1214. Zhang Qingkui, Shao Xuefeng, Guan Peiyan, et al. Basic Characteristics and Genetic Analysis of Glaucophane Schist in Subugeta, Inner Mongolia[J]. Geology in China, 2014, 41(4):1205-1214.
[6] Zhou J B, Wang B, Wilde S A, et al. Geochemistry and U-Pb Zircon Dating of the Toudaoqiao Blueschists in the Great Xing'an Range, Northeast China, and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2015, 97:197-210.
[7] Miao L C, Zhang F C, Jiao S J. Age, Protoliths and Tectonic Implications of the Toudaoqiao Blueschists, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 2015, 105:360-373.
[8] Zhao L M, Takasu A, Liu Y J, et al. Blueschist from the Toudaoqiao Area, Inner Mongolia, NE China:Evidence for the Suture Between the Ergun and the Xing'an Blocks[J]. Earth Science, 2017, 28(2):241-248.
[9] Wu F Y, Zhao G C, Sun D Y, et al. The Hulan Group:Its Role in the Evolution of the Central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences, 2007, 30:542-556.
[10] 黄汲清, 任纪舜, 姜春发, 等. 中国大地构造基本轮廓[J]. 地质学报, 1977, 51(2):117-135. Huang Jiqing, Ren Jishun, Jiang Chunfa, et al. An Outline of the Tectonic Characteristics of China[J]. Acta Geological Sinica, 1977, 51(2):117-135.
[11] 黄汲清,任纪舜,姜春发,等. 中国大地构造及其演化[M]. 北京:科学出版社,1980:29-47. Huang Jiqing, Ren Jishun, Jiang Chunfa, et al. Geotectonic Evolution of China[M]. Beijing:Science Press, 1980:29-47.
[12] 任纪舜,王作勋,陈炳蔚,等. 新一代中国大地构造[J]. 中国区域地质,1997, 16(3):225-248. Ren Jishun, Wang Zuoxun, Chen Bingwei, et al. A New Generation of Tectonic Map of China[J]. Regional Geology of China, 1997, 16(3):225-248.
[13] 张梅生, 彭向东, 孙晓猛. 中国东北区古生代构造古地理格局[J]. 辽宁地质, 1998(2):91-96. Zhang Meisheng, Peng Xiangdong, Sun Xiaomeng. The Paleozoic Tectonic Geographical Pattern of Northeast China[J]. Liaoning Geology, 1998(2):91-96.
[14] Badarch G, Cunningham W D, Windley B F. A New Terrane Subdivision for Mongolia:Implication for the Phanerozoic Crustal Growth of Central Asia[J]. Journal of Asian Earth Science, 2002, 21:87-110.
[15] 内蒙古自治区地质矿产局. 内蒙古自治区区域地质[M]. 北京:地质出版社,1991:7-498. Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region. Regional Geology of the Inner Mongolia Autonomous Region[M]. Beijing:Geological Publishing House, 1991:7-498.
[16] 黑龙江省地质矿产局. 黑龙江省地质志[M].北京:地质出版社,1993:1-734. Bureau of Geology and Mineral Resources of Heilongjiang Province. Regional Geology of Heilongjiang Province[M]. Beijing:Geological Publishing House, 1993:1-734.
[17] 苗来成,刘敦一,张福勤,等. 大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-P年龄[J]. 科学通报,2007, 52(5):591-601. Miao Laicheng, Liu Dunyi, Zhang Fuqin, et al. The SHRIMP U-P Ages of the Zircons from the Xinghuadukou Group and Zhalantun Group in the Hanjiayuanzi and Xinlin Area, Great Xing'an Range[J]. Chinese Science Bulletin, 2007, 52(5):591-601.
[18] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Science, 2011, 41(1):1-30.
[19] 周建波,张兴洲,Wilde S A. 中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J]. 岩石学报,2011, 27(4):1235-1245. Zhou Jianbo, Zhang Xingzhou, Wilde S A, et al. Confirming of the Heilongjiang~500 Ma Pan African Hhondalite Belt and Its Tectonic Implications[J]. Acta Petrologica Sinica, 2011, 27(4):1235-1245.
[20] 李锦轶. 中国东北及邻区若干地质构造问题的新认识[J]. 地质论评, 1998, 44(4):339-347. Li Jinyi. Some New Ideas on Tectonics of NE China and Its Neighboring Areas[J]. Geological Review, 1998, 44(4):339-347.
[21] 李锦轶,莫申国,和政军,等. 大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J]. 地学前缘,2004, 11(3):157-168. Li Jinyi, Mo Shenguo, He Zhengjun, et al. The Timing of Crustal Sinistral Strike-Slip Movement in the Northern Great Khing an Ranges and Its Constraint on Reconstruction of the Crustal Tectonic Evolution of NE China and Adjacent Areas Since the Mesozoic[J]. Earth Science Frontiers, 2004, 11(3):157-168.
[22] 李瑞山. 新林蛇绿岩[J]. 黑龙江地质, 1991, 2(1):19-31. Li Ruishan. Xinlin Ophiolite[J]. Heilongjiang Geology, 1991, 2(1):19-31.
[23] 葛文春, 吴福元, 周长勇, 等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J]. 科学通报, 2005, 50(12):1239-1247. Ge Wenchun, Wu Fuyuan, Zhou Changyong, et al. Emplacement Age of the Tahe Granite and Its Constraints on the Tectonic Nature of the Ergun Block in the Northern Part of the Da Hinggan Range[J]. Chinese Science Bulletin, 2005, 50(12):1239-1247.
[24] 刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J]. 中国地质, 2010, 37(4):943-951. Liu Yongjiang, Zhang Xingzhou, Jin Wei, et al. Late Paleozoic Tectonic Evolution in Northeast[J]. Geology in China, 2010, 37(4):943-951.
[25] Leake B E, Woolley A R, Arps C E S, et al. Nomenclature of Amphiboles:Reports of the Subcommiittee on Amphiboles of the International Mineralogical Association, Commission on New Mineral and Mineral Names[J]. Mineralogical Magazine, 1997, 61:295-321.
[26] Otsuki M, Banno S. Prograde andRetrograde Meta-morphism of Hematite-Bearing Basic Schists in the Sanbagawa Belt in Central Shikoku[J]. Journal of Metamorphic Geology, 1990, 8:425-439.
[27] Evans B W. Phase Relations of Epidoe-Blueschists[J]. Lithos, 1990, 25(1/2/3):3-23.
[28] Massonne H J, Schreyer W. Phengite Geobarometry Based on the Limiting Assemblage with K-Feldspar, Phlogopite, and Quartz[J]. Contributions to Mineralogy and Petrology, 1987, 96:212-224.
[29] Holland T J B. The Experimental Determination of Activities in Disordered and Short-Range Ordered Jadeitic Pyroxenes[J]. Contributions to Mineralogy and Petrology, 1983, 82(2/3):214-220.
[30] Owen C. Magmatic Differentiation and Alteration in Isofacial Greenschists and Blueschists, Shuksan Suite, Washington:Statistical Analysis of Major Element Variation[J]. Journal of Petrology, 1989, 30:739-761.
[31] 胡道功,谭成轩,张海. 内蒙古阿里河地区中元古代蛇绿岩[J]. 中国区域地质,1995(4):334-343. Hu Daogong, Tan Chengxuan, Zhang Hai. Middle Proterozoic Ophiolites in the Alihe Area, Inner Mongolia[J]. Regional Geology of China, 1995(4):334-343.
[32] 胡道功,李洪文,刘旭光,等. 大兴安岭吉峰科马提岩Sm-Nd等时线年龄测定[J]. 地球学报,2003, 24(5):405-408. Hu Daogong, Li Hongwen, Liu Xuguang, et al. Dating of Sm-Nd Isochron Ages of the Jifeng Komatiites from the Da Hinggan Ling[J]. Acta Geoscientia Sinica, 2003, 24(5):405-408.
[33] 胡道功,郑庆道,傅俊彧,等. 大兴安岭吉峰科马提岩地球化学特征[J]. 地质力学学报, 2001, 7(2):111-115. Hu Daogong, Zheng Qingdao, Fu Junyu, et al. The Geological and Geochemical Charecteristics of the Jifeng Komatiites in the Da Hinggan Ling Mountains[J]. Journal of Geomechanics, 2001, 7(2):111-115.
[34] 李仰春,赵海滨,杨晓平,等. 大兴安岭吉峰地区中元古代科马提岩及成因类型[J]. 地质与资源,2002,11(2):76-88. Li Yangchun, Zhao Haibin, Yang Xiaoping, et al. The Mesoproterozoic Komatiites and Their Genetic Type in the Jifeng Area of Daxinganling[J]. Geology and Resources, 2002, 11(2):76-88.
[35] 佘宏全,李进文,向安平,等. 大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J]. 岩石学报,2012, 28(2):571-594. She Hongquan, Li Jinwen, Xiang Anping, et al. U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution[J]. Acta Petrologica Sinica, 2012, 28(2):571-594.
[36] 冯志强. 大兴安岭北段古生代构造-岩浆演化[D]. 长春:吉林大学,2015. Feng Zhiqiang. Palezoic Tectonic-Magmatic Evolution of Northern Great Xing'an Range[D]. Changchun:Jilin University, 2015.
[37] 姚婕,贺灿. 大兴安岭新林-吉峰地区蛇绿岩中超基性岩特征及其地质意义[J]. 城市地理,2016(20):78. Yao Jie, He Can. The Characteristics of Ultramafic Rocks of Ophiolite and Its Geological Significance in Xinlin-Jifeng Area, Da Xing'an Mountian[J]. Global City Geography, 2016(20):78.
[38] 张德明. 大兴安岭北部嘎仙蛇绿岩的物质组成、地球化学特征及其构造意义[J]. 黑龙江科技信息, 2017(1):127. Zhang Deming. The Material Composition, Geochemical Characteristics and Tectonic Significance of Gaxian Ophiolite in Northern Daxing'an Mountain[J]. Heilongjiang Science and Technology Information, 2017(1):127.
[39] 沙春梅. 大兴安岭鄂伦春自治旗吉峰蛇绿岩的物质组成、地球化学特征及地质意义[J]. 大科技,2016(13):127. Sha Chunmei. The Material Composition, Geochemical Character and Geological Significance of Jifeng Ophiolite in Elun Chun Autonomous Region in Daxing'an Mountain[J]. Super Science, 2016(13):127.
[40] 杜兵盈, 冯志强, 刘宇崴,等. 大兴安岭环二库新元古代变质辉长岩的厘定及其地质意义[J]. 世界地质,2017, 36(3):751-762. Du Bingying, Feng Zhiqiang, Liu Yuwei, et al. Early Neoproterozoic Meta-Gabbro (~697 Ma) from the Huanerku, the Great Xing'an Range and Its Geological Significance[J]. Global Geology, 2017, 36(3):751-762.
[41] 邵学峰. 内蒙古塔源-头道桥拼合带西南段迈罕特乌拉蛇绿岩地球化学特征及其地质意义[J]. 世界地质,2016, 35(2):429-440. Shao Xuefeng. Geochemical Characteristics and Geological Significance of Ophiolite from Maihantewula, Southwest Section of Tayuan-Toudaoqiao Matching Belt in Inner Mongolia[J]. Global Geology, 2016, 35(2):429-440.
[42] 吕斌,王涛,童英,等. 中亚造山带东部岩浆热液矿床时空分布特征及其构造背景[J]. 吉林大学学报(地球科学版),2017, 47(2):305-343. Lü Bin, Wang Tao, Tong Ying, et al. Distribution and Tectonic Settings of Magmatic-Hydrothermal Ore Deposits in the Eastern Central Asia Orogen Belt[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(2):305-343.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

内蒙古头道桥地区蓝闪石片岩和相关变质岩石岩石学特征及其构造意义

Character of Blueschist and Related Metamorphic Rocks from the Toudaoqiao Area, Inner Mongolia and Its Tectonic Implication

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 11

Metrics

本文评价

推荐阅读 0

[1]	张志, 管志超, 王少军. 结合实测光谱的ASTER TIR数据岩性划分与构造样式分析:以新疆阿克苏蓝片岩为例[J]. 吉林大学学报(地球科学版), 2018, 48(1): 334-342.
[2]	孙跃武, 丁海生, 刘欢, 张德军, 公繁浩, 郑月娟. 华北板块北缘中二叠统于家北沟组植物化石及其大地构造意义[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1268-1283.
[3]	周建波, 石爱国, 景妍. 东北地块群:构造演化与古大陆重建[J]. 吉林大学学报(地球科学版), 2016, 46(4): 1042-1055.
[4]	刘永江, 刘宾强, 冯志强, 温泉波, 李伟民, 张铁安, 李小玉, 杜兵盈. 大兴安岭中北段老道口闪长岩锆石U-Pb年龄、地球化学特征及构造意义[J]. 吉林大学学报(地球科学版), 2016, 46(2): 482-498.
[5]	段志明, 李光明, 张晖, 李应栩, 段瑶瑶. 色那金矿石英二长闪长岩锆石U-Pb年龄与地球化学特征及其对成矿背景的约束[J]. 吉林大学学报(地球科学版), 2013, 43(6): 1864-1877.
[6]	周建波, 曾维顺, 曹嘉麟, 韩杰, 郭晓丹. 中国东北地区的构造格局与演化：从500 Ma到180 Ma[J]. J4, 2012, 42(5): 1298-1316.
[7]	肖根如, 甘卫军, 陈为涛, 程佳. 青藏高原班公-怒江缝合带现今运动状况的GPS观测研究[J]. J4, 2010, 40(6): 1496-1502.
[8]	周建波, 韩杰, 张兴洲, 曾维顺. 牡丹江地区蓝片岩的地球化学特征及其大地构造意义[J]. J4, 2010, 40(1): 93-103.
[9]	王跃, 张兴洲, 宋海峰, 张春艳, 熊小松. 牡丹江地区黑龙江杂岩的变质变形特征[J]. J4, 2009, 39(6): 1066-1072.
[10]	马瑞，田海民，张刚. 差应力与石英组构关系的实验研究[J]. J4, 2009, 39(1): 89-0092.
[11]	覃小锋，夏斌，李江，黎春泉，陆济璞，许华，周府生，胡贵昂，李乾. 阿尔金南缘构造带西段新元古代-早古生代变质岩系的变质作用[J]. J4, 2007, 37(5): 856-0867.