吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1098-1118.doi: 10.13278/j.cnki.jjuese.20210031
赵越1,2, 刘敬党2, 张国宾2, 张艳飞2,3
Zhao Yue1,2, Liu Jingdang2, Zhang Guobin2, Zhang Yanfei2,3
摘要: 张广才岭是松嫩地块与佳木斯地块之间的碰撞造山带,是东北"巨型花岗岩省"的重要组成部分。本文通过锆石U-Pb定年和岩石地球化学分析,研究了张广才岭南部帽儿山二长花岗岩年代学、地球化学特征和构造背景。锆石U-Pb年代学结果显示:张广才岭南部细粒二长花岗岩成岩年龄为(176.4±1.1)Ma,中粒二长花岗岩成岩年龄为(178.9±1.3)、(177.7±1.1)Ma,粗粒二长花岗岩成岩年龄为(180.0±1.8)、(179.9±1.2)Ma,成岩时代均属于早侏罗世。岩石地球化学研究显示:细粒二长花岗岩、中粒二长花岗岩和粗粒二长花岗岩均具有富硅、贫铝、高碱、低钙,富集Zr、Hf、Rb、K,亏损Ba、Sr、Nb、P、Ti,燕式型稀土配分模式等特征,成岩类型属于造山后A2型花岗岩。结合年代学和地球化学特征,研究区早侏罗世二长花岗岩形成于碰撞后构造背景,代表佳木斯地块和松嫩地块碰撞—拼合过程中的一次伸展作用,表明早侏罗世区域构造环境逐渐由挤压造山向造山后伸展环境转变。
中图分类号:
[1] 句高,梁一鸿,孙晓,等.张广才岭南段两个侏罗纪花岗岩体的地球化学特征及其地质意义[J].世界地质,2018,37(2):374-384. Ju Gao, Liang Yihong, Sun Xiao, et al. Geochemical Characteristics and Geological Significance of Two Jurassic Granite Bodies in the Southern Section of Zhangguangcai Ling[J]. World Geology, 2018, 37(2):374-384. [2] 孙德有,吴福元,林强,等.张广才岭燕山早期白石山岩体成因与壳幔相互作用[J].岩石学报,2001,17(2):227-235. Sun Deyou, Wu Fuyuan, Lin Qiang, et al. Genesis and Crust Slow Interaction of Early Baishishan Pluton in Yanshan Mountain in Zhangguangcailing[J]. Acta Petrologica Sinica, 2001, 17(2):227-235. [3] Whalen J B,Currie K L,Chappell B W. A-Type Granites:Geochemical Characteristics, Discrimi-nation and Petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987,95(4):407-419. [4] 吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄[J].长春科技大学学报,1999,29(4):313-318. Wu Fuyuan, Sun Deyou.Mesozoic Magmatism and Lithospheric Thinning in Eastern China[J]. Journal of Changchun University of Science and Technology, 1999, 29(4):313-318. [5] Wu Fuyuan, Ming Jahnbor, Wilder S A, et al. Highly Fractionated I-Type Granites in NE China(I):Geochronology and Petrogenesis[J]. Lithos,2003,66:241-273. [6] Hoskin P W O, Black L P. Metamorphic Zircon Formation by Solid-State Recrystallization of Protolith Igneous Zircon[J]. Journal of Metamorphic Geology,2000,18:423-439. [7] Hoskin P W O, Schaltegger U. The Composition of Zircon and Igneous and Metamorphic Petrogenesis[J]. Reviews of Mineralogy and Geochemistry,2003,53(1):27-62. [8] 张国宾,韩超,杨言辰,等.完达山地块跃进山矽卡岩型铜金矿区酸性侵入岩锆石U-Pb年龄、地球化学特征及成因[J].中国地质,2018,45(5):977-991. Zhang Guobin, Han Chao, Yang Yanchen, et al. U-Pb Ages, Geochemical Characteristics and Genesis of Acidic Intrusive Rocks from Yuejinshan Skarn Copper-Gold Deposit in Wandashan Block[J].Chinese Geology,2018,45(5):977-991. [9] Peccerillo A, Taylor T S. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks form Kastamonu Area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976,56:63-81. [10] Middlemost E A K. Magmas and Magmatic Rocks:An Introduction to Igneous Petrology[M].London:Longman Grou, 1985:1-266. [11] Boynton W V. Geochemistry of the Rare Earth Elements:Meteorite Studies[C]//Henderson P.Rare Earth Element Geochemistry.Amsterdam:Elsevier,1984:63-114. [12] Sun S S, McDonough W F.Chemical and Isotopic Systematics of Oceanic Basalts:Implication for Mantle Composition and Processes[J]. Geological Society, 1989,42:313-345. [13] 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, 40(1):1-30. [14] Wu F Y, Jang 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, 328:89-113. [15] 孙德有,吴福元,高山,等.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘,2005,12(2):263-275. Sun Deyou, Wu Fuyuan, Gao Shan, et al. Determination of the Late Triassic and Early Jurassic Aluminous A-Type Granites in Central Jilin and Their Constraints on the Tectonic Framework of Eastern Jilin[J]. Earth Science Frontiers, 2005,12(2):263-275. [16] 孙晓. 张广才岭花岗岩带南段侏罗纪花岗岩的年代学特征及形成环境[D].长春:吉林大学,2016. Sun Xiao. Chronological Characteristics and Formation Environment of Jurassic Granites in the Southern Segment of Zhangguangcailing Granite Belt[D]. Changchun:Jilin University, 2016. [17] 魏红艳,孙德有,叶松青,等.小兴安岭东南部伊春-鹤岗地区花岗质岩石锆石U-Pb年龄测定及其地质意义[J].地球科学:中国地质大学学报,2012,37(增刊1):50-59. Wei Hongyan, Sun Deyou, Ye Songqing, et al. Determination of Zircon U-Pb Age of Granitic Rocks in the Yichun-Hegang Area in the Southeast of Xiaoxing'anling and Its Geological Significance[J]. Earth Science:Journal of China University of Geosciences, 2012, 37(Sup.1):50-59. [18] 邵济安,李永飞,唐克东.张广才岭造山过程的重构及其大地构造意义[J].岩石学报,2013,29(9):2959-2970. Shao Ji'an,Li Yongfei, Tang Kedong. The Reconstruction of the Zhangguangcailing Orogenic Process and Its Tectonic Significance[J]. Acta Petrologica Sinica, 2013, 29(9):2959-2970. [19] 王广婷,孙德有,孙如江,等.张广才岭南部横道河子岩体地球化学特征及其成因[J].世界地质,2015, 34(2):321-329. Wang Guangting, Sun Deyou, Sun Rujiang, et al. Geochemical Characteristics and Genesis of the Hengdaohezi Pluton in the Southern Part of Zhangguangcai Mountain[J]. Global Geology, 2015, 34(2):321-329. [20] 邹存铭. 张广才岭晚古生代A型花岗岩的年代学及构造环境分析[D].长春:吉林大学,2015. Zou Cunming. Analysis of the Geochronology and Tectonic Environment of Zhangguangcailing Late Paleozoic A-Type Granite[D]. Changchun:Jilin University, 2015. [21] 葛茂卉,张进江,刘恺,等.小兴安岭-张广才岭地区晚古生代至中生代花岗岩的成因及其地质意义[J].岩石矿物学杂志,2020,39(4):385-405. Ge Maohui, Zhang Jinjiang, Liu Kai, et al. The Genesis and Geological Significance of the Late Paleozoic to Mesozoic Granites in the Xiaoxing'anling-Zhangguangcailing Area[J]. Journal of Rock and Mineralogy, 2020, 39(4):385-405. [22] 王强,赵振华,简平,等.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约[J].岩石学报,2005,21(3):795-808. Wang Qiang, Zhao Zhenhua, Jian Ping, et al. Geochronology of Cretaceous A-Type Granitoids or Alkaline Intrusive Rocks in the Hinterland, South China:Constraints for Late-Mesozoic Evolution[J]. Acta Petrologica Sinica, 2005,21(3):795-808. [23] Eby G N.Chemical Subdivision of the A-Type Granitoids:Petrogenetic and Tectonic Implications[J]. Geology,1992, 20(7):641-644. [24] 洪大卫.两类碱性花岗岩的鉴别标志[C]//中国地质科学院地质研究所文集.北京:地质出版社,1995:123-124. Hong Dawei. Identification Marks of Two Types of Alkaline Granite[C]//Collected Works of Institute of Geology, Chinese Academy of Geological Sciences.Beijing:Geological Publishing House,1995:123-124. [25] 刘昌实,陈小明,陈培荣,等. A型岩套的分类、判别标志和成因[J].高校地质学报,2003,9(4):573-591. Liu Changshi, Chen Xiaoming, Chen Peirong, et al. Classification, Identification Signs and Genesis of A-Type Rock Sets[J]. Geological Journal of Universities, 2003,9(4):573-591. [26] 陈井胜.赤峰地区晚古生代-早中生代花岗岩成因及其构造意义[D].长春:吉林大学,2018. Chen Jingsheng. The Genesis and Tectonic Significance of Late Paleozoic-Early Mesozoic Granites in Chifeng Area[D]. Changchun:Jilin University, 2018. [27] 苏玉平,唐红峰. A型花岗岩的微量元素地球化学[J].矿物岩石地球化学通报,2005,24(3):245-251. Su Yuping, Tang Hongfeng. Trace Element Geochemistry of A-Type Granite[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2005,24(3):245-251. [28] 解洪晶,武广,朱明田,等.内蒙古道郎呼都格地区A型花岗岩年代学、地球化学及地质意义[J].岩石学报,2012,28(2):483-494. Xie Hongjing, Wu Guang, Zhu Mingtian, et al. Chronology,Geochemistry and Geological Significance of A-Type Granites in Daolang Huduge Area, Inner Mongolia[J]. Acta Petrologica Sinica, 2012, 28(2):483-494. [29] Weaver B L,Tarney J.Empirical Approach to Estimating the Composition of the Continental Crust[J]. Nature,1984,310:575-577. [30] Francis A. The Growth of Continental Crust[J].Tectonophysics,1998,296(1):241-265. [31] 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 Deyou, Wu Fuyuan, Zhang Yanbin, et al. The Last Closure Time of the Xilamulun River-Changchun-Yanji Plate Suture Zone-Evidence from Jilin Dayushan Granite Body[J]. Journal of Jilin University (Earth Science Edition), 2004,34(2):174-181. [32] 尹志刚,宫兆民,王春生,等.小兴安岭平顶山一带早侏罗世花岗岩类年代学、地球化学特征及其地质意义[J].吉林大学学报(地球科学版), 2021,51(1):107-125. Yin Zhigang, Gong Zhaomin,Wang Chunsheng, et al. Chronological, Geochemical Characteristics and Geological Significance of Early Jurassic Granites in Pingdingshan Area of Lesser Xing'an Range[J]. Journal of Jilin University (Earth Science Edition), 2021,51(1):107-125. [33] 周翔. 松辽盆地北部营城组火山岩地球化学特征及地质意义[J].吉林大学学报(地球科学版), 2019,49(4):1001-1014. Zhou Xiang. Geochemistry and Tectonic Implication of Volcanic Rocks of Yingcheng Formation in Northern Songliao Basin[J]. Journal of Jilin University (Earth Science Edition), 2019,49(4):1001-1014. [34] 董玉.佳木斯地块与松嫩-张广才岭地块拼合历史:年代学与地球化学证据[D].长春:吉林大学,2018. Dong Yu. The History of the Integration of the Jiamusi Block and the Songnen-Zhangguangcailing Block Chronological and Geochemical Evidence[D].Changchun:Jilin University, 2018. [35] 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 Fuyuan, Wilde S A, Sun Deyou. Zircon Ion Probe U-Pb Age of Gneissic Granites in the Jiamusi Block[J]. Acta Petrologica Sinica, 2001,17(3):443-452. [36] 黄映聪,任东辉,张兴洲,等.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[J].吉林大学学报(地球科学版),2008,38(4):631-638. Huang Yingcong, Ren Donghui, Zhang Xingzhou, et al. Zircon U-Pb Dating of the Meizuo Granite from the Huanan Uplift in Eastern Heilongjiang and Its Geological Significance[J]. Journal of Jilin University (Earth Science Edition),2008,38(4):631-638. [37] 张磊,李秋根,史兴俊,等.佳木斯地块中部二叠纪永清花岗闪长岩的锆石U-Pb年龄、地球化学特征及其地质意义[J].岩石矿物学杂志,2013,32(6):1022-1036. Zhang Lei, Li Qiugen, Shi Xingjun, et al. Zircon U-Pb Age, Geochemical Characteristics and Geological Significance of the Permian Yongqing Granodiorite in the Central Jiamusi Block[J]. Journal of Rock and Mineralogy, 2013,32(6):1022-1036. [38] 王志伟.小兴安岭-张广才岭早古生代火成岩的岩石学与地球化学:对块体拼合历史和地壳属性的制约[D].长春:吉林大学,2017. Wang Zhiwei. The Petrology and Geochemistry of Early Paleozoic Igneous Rocks in Xiaoxing'anling-Zhangguangcailing Mountains:Constraints on the History of Block Assembly and Crustal Properties[D]. Changchun:Jilin University, 2017. [39] Zhou J B, Wilde S A, Zhang X Z, et al. Detrital Zircons from Phanerozoic Rocks of the Songliao Block,NE China:Evidence and Tectonic Implications[J]. Journal of Asian Earth Sciences,2012,47:21-34. [40] Ge M H, Zhang J J, Li L, et al. Geochronology and Geochemistry of the Heilongjiang Complex and the Granitoids from the Lesser Xing'an-Zhangguangcai Range:Implications for the Late Paleozoic-Mesozoic Tectonics of Eastern NE China[J]. Tectonophysics, 2017,717:565-584. [41] 赵亮亮,张兴洲.黑龙江杂岩构造折返的岩石学与年代学证据[J].岩石学报,2011,27(4):1227-1234. Zhao Liangliang,Zhang Xingzhou.The Petrological and Chronological Evidence of the Structural Exhumation of the Heilongjiang Complex[J].Acta Petrologica Sinica,2011,27(4):1227-1234. [42] Yang H, Ge W C, Dong Y, et al. Record of Permian-Early Triassic Continental arc Magmatism in the Western Margin of the Jiamusi Block,NE China:Petro Genesis and Implications for Paleo-Pacific Subduction[J]. International Journal of Earth Sciences,2017,106:1919-1942. [43] Zhu C Y, Zhao G C, Sun M, et al. Subduction Between the Jiamusi and Songliao Blocks:Geochronological and Geochemical Constraints from Granitoids Within the Zhangguangcailing Orogen, Northern China[J]. Lithos Phere,2017,9:515-533. [44] Zhang X R, Zhao G C, Eizenhofer P R, et al. Late Ordovician Adakitic Rocks in the Central Tianshan Block, NW China:Partial Melting of Lower Continental Arccrust During Backarc Basin Opening[J].Geological Society of America Buletin,2016,128(9):302-315. [45] 吴志强,任云生,索良明,等.松嫩地块东缘金山屯地区晚三叠世双峰式侵入岩年代学、地球化学及其对构造演化的制约[J].世界地质,2020,39(4):796-808. Wu Zhiqiang, Ren Yunsheng, Suo Liangming, et al. Geochronology, Geochemistry and Its Constraintion Tectonic Evolution of Late Triassic Bimodal Intrusive Rocks in Jinshantun Area of Eastern Songnen Massif[J]. Global Geology, 2020,39(4):796-808. [46] 冯光英,牛晓露,刘飞,等.张广才岭地块早侏罗世晚期花岗闪长岩及其闪长质包体的岩石成因及构造意义[J].地质学报,2019, 93(10):2598-2616. Feng Guangying, Niu Xiaolu, Liu Fei, et al. Petrogenesis of Last Early Jurassic Granodiorites and Associated Dioritic Enclaves in the Zhangguangcai Range and Its Tectonic Implication[J]. Acta Geologica Sinica, 2019,93(10):2598-2616. [47] 王枫,许文良,葛文春,等.敦化-密山断裂带的平移距离:来自松嫩-张广才岭-佳木斯-兴凯地块古生代-中生代岩浆作用的制约[J]. 岩石学报, 2016,32(4):1129-1140. Wang Feng,Xu Wenliang,Ge Wenchun,et al.The Offset Distance of the Dunhua-Mishan Fault:Constraints from Paleozoic-Mesozoic Magmatism Within the Songnen-Zhangguangcai Range, Jiamusi, and Khanka Massifs[J].Acta Petrologica Sinica,2016, 32(4):1129-1140. [48] 李竞妍,郭锋,李超文,等.东北地区晚古生代-中生代I型和A型花岗岩Nd同位素变化趋势及其构造意义[J].岩石学报, 2014,30(7):1995-2008. Li Jingyan, Guo Feng, Li Chaowen, et al. Nd Isotopic Variations of Late Paleozoic to Mesozoic I-and A-Type Granitoids in NE China and Implications for Tectonic Evolution[J]. Acta Petrologica Sinica,2014,30(7):1995-2008. |
[1] | 张贵山, 邱红信, 温汉捷, 彭仁, 孟乾坤. 攀西红格钒钛磁铁矿矿田富钴硫化物中钴的地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2021, 51(6): 1740-1752. |
[2] | 宫昀迪, 李碧乐, 李治华, 于润涛, 孙永刚, 张森. 大兴安岭北段小柯勒河花岗斑岩脉成因及地质意义:锆石U-Pb年龄、岩石地球化学及Hf同位素制约[J]. 吉林大学学报(地球科学版), 2021, 51(6): 1753-1769. |
[3] | 张七道, 刘振南, 尹林虎. 深变质岩区地热流体化学特征及成因——以滇西陇川盆地温泉为例[J]. 吉林大学学报(地球科学版), 2021, 51(6): 1838-1852. |
[4] | 李天军, 黄志龙, 王瑞, 苟红光, 张品, 殷越. 银根—额济纳旗盆地天草凹陷下白垩统巴音戈壁组有效烃源岩地球化学特征及其形成环境[J]. 吉林大学学报(地球科学版), 2021, 51(4): 957-972. |
[5] | 史冬岩, 张坤, 张玉鹏, 高勇, 唐伟, 吕明奇. 黑龙江省浅覆盖区地物化特征与找矿标志——以黑河市340高地金矿化区为例[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1042-1053. |
[6] | 杨元江, 邓昌州, 李成禄, 张立, 高永志, 于喜洹. 大兴安岭大洋山钼矿区侵入岩年代学、岩石地球化学特征及岩石成因[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1064-1081. |
[7] | 孙超, 苟军, 孙德有, 冯钊, 田丽. 黑龙江省西北部晚古生代I-A型花岗岩的成因及构造意义[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1082-1097. |
[8] | 张雪, 翁凯, 赵晓健, 杜守礼, 尚颖. 新疆东天山卡拉塔格二叠纪火山岩成因及构造意义[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1119-1138. |
[9] | 史冀忠, 牛亚卓, 许伟, 宋博, 王宝文. 银额盆地石板泉西石炭系白山组碳酸盐岩地球化学特征及其环境意义[J]. 吉林大学学报(地球科学版), 2021, 51(3): 680-693. |
[10] | 曾志杰, 陈雷. 南秦岭山阳—柞水矿集区夏家店金矿床微量-铂族元素地球化学特征及其对矿床成因的指示[J]. 吉林大学学报(地球科学版), 2021, 51(3): 704-722. |
[11] | 张超, 石绍山, 时溢, 魏明辉, 杨帆, 郇恒飞, 李文博, 王路远. 华北板块北缘东段中三叠世构造演化——来自辽宁法库地区侵入岩的证据[J]. 吉林大学学报(地球科学版), 2021, 51(3): 734-748. |
[12] | 田梦宇, 狄永军, 王帅, 贾一龙. 广西云开地区那蓬岩体黑云母二长花岗岩年代学、地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2021, 51(3): 749-766. |
[13] | 邓红宾, 李培龙, 魏华财, 何文劲, 杨鹏涛, 李宁, 唐华. 东昆仑造山带低山头花岗岩体岩石地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2021, 51(3): 767-782. |
[14] | 康鹏宇, 刘传朋, 梁成, 冯爱平, 刘同, 宗传攀. 沂蒙山区土壤质量地球化学评价方法[J]. 吉林大学学报(地球科学版), 2021, 51(3): 877-886. |
[15] | 田兴旺, 罗冰, 孙奕婷, 刘冉, 李亚, 陈延贵, 周春林, 汪华, 李亚丁, 王尉, 王云龙, 杨岱林. 二叠系火山碎屑岩气藏天然气地球化学特征及气源分析——以四川盆地成都—简阳地区永探1井为例[J]. 吉林大学学报(地球科学版), 2021, 51(2): 325-335. |
|