Geochemistry of the Zhanbeicun Formation volcanic rocks in Xinlin area of northern Great Xing'an Range and its tectonic environment

ZHENG Jilin; LIU Zhijie; WANG Wendong; WEI Xiaoyong; GUO Xiaoyu; LIU Junshuai; SUN Jingyao

2021 Vol. 40, No. 4

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ZHENG Jilin, LIU Zhijie, WANG Wendong, WEI Xiaoyong, GUO Xiaoyu, LIU Junshuai, SUN Jingyao. Geochemistry of the Zhanbeicun Formation volcanic rocks in Xinlin area of northern Great Xing'an Range and its tectonic environment[J]. Geological Bulletin of China, 2021, 40(4): 512-519.

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ZHENG Jilin, LIU Zhijie, WANG Wendong, WEI Xiaoyong, GUO Xiaoyu, LIU Junshuai, SUN Jingyao. Geochemistry of the Zhanbeicun Formation volcanic rocks in Xinlin area of northern Great Xing'an Range and its tectonic environment[J]. Geological Bulletin of China, 2021, 40(4): 512-519.

Geochemistry of the Zhanbeicun Formation volcanic rocks in Xinlin area of northern Great Xing'an Range and its tectonic environment

Harbin Center for Integrated Natural Resources Survey of China Geological Survey, Harbin 150086, Heilongjiang, China

Received Date: 15 March 2019

Revised Date: 26 January 2021

Publish Date: 15 April 2021

Abstract

Abstract

The Lower Jurassic volcanic rocks of the Zhanbeicun Formation in Xinlin area of the northern Great Xing'an Range are petrographically composed of rhyolite and rhyolitic pyroclastic rocks.Chemically, these rhyolites belong to high-K calc-alkaline series characterized by high contents of silica, alkalis, low abundances of calcium and magnesium.The volcanic rocks have the characteristics of low ΣREE content(ΣREE=81.84×10^-6~110.32×10^-6), obvious differentiation between light rare earth and heavy rare earth elements[(La/Yb)_N=21.57~40.21], with moderate negative Eu anomaly(δEu=0.42~0.62).These rocks also have characteristics of crust-derived magma with enrichment of large ion lithophile elements(LILEs, such as Rb, K, Th and U), depletion of high field strength elements(HFSEs, such as Nb, Ta, Ti and P)and lower content of basic compatible elements(such as Cr, Co and Ni)and Mg^#.The low Sr and Yb content of rhyolites indicates that it is similar to Himalayan type.Combined with tectonic characteristics of the regional Early Jurassic volcanic rocks, it is suggested that the Zhanbeicun Formation volcanic rocks were formed in the tectonic background of the southeastward subduction of the Mongolia-Okhotsk ocean.
- Lower Jurassic /
- Zhanbeicun Formation /
- tectonic setting /
- Great Xing'an Range

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[1]	孙德有, 苟军, 任云生, 等. 满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究[J]. 岩石学报, 2011, 27(10): 3083-3094. Google Scholar
[2]	许文良, 王枫, 裴福萍, 等. 中国东北中生代构造体制与区域成矿背景: 来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 2013, 29(2): 339-353. Google Scholar
[3]	唐杰, 许文良, 王枫, 等. 张广才岭帽儿山组双峰式火岩成因: 年代学与地球化学证据[J]. 世界地质, 2011, 30(4): 508-513. doi: 10.3969/j.issn.1004-5589.2011.04.002 CrossRef Google Scholar
[4]	郑吉林, 王文东, 杨华本, 等. 大兴安岭北部下侏罗统战备村组的建立及其地质意义[J]. 地质通报, 2016, 35(7): 1106-1114. doi: 10.3969/j.issn.1671-2552.2016.07.006 CrossRef Google Scholar
[5]	王泉, 表尚虎, 李喜明, 等. 黑龙江省孙吴地区早侏罗世火山岩的识别及其地质意义[J]. 矿产与地质, 2017, 31(2): 378-388. doi: 10.3969/j.issn.1001-5663.2017.02.026 CrossRef Google Scholar
[6]	李研, 王建, 韩志滨, 等. 大兴安岭北段八大关地区早侏罗世流纹岩锆石U-Pb定年与岩石成因[J]. 中国地质, 2017, 44(2): 346-357. Google Scholar
[7]	赵胜金, 于海洋, 申亮, 等. 大兴安岭北段下侏罗统柴河组的厘定及地质意义[J]. 地质通报, 2018, 37(7): 1302-1313. Google Scholar
[8]	赵国龙, 杨桂林, 王忠, 等. 大兴安岭中南部中生代火山岩[M]. 北京: 科学技术出版社, 1989: 1-260. Google Scholar
[9]	马家骏, 方大赫. 黑龙江省中生代火山岩初步研究[J]. 黑龙江地质, 1991, 2(2): 1-6. Google Scholar
[10]	孙德有, 许文良, 周燕, 等. 大兴安岭中生代火山岩的形成机制[J]. 矿物岩石地球化学通讯, 1994, 3: 162-164. Google Scholar
[11]	Zhang J H, Ge W C, Wu F Y, et al. Large-scale Early Cretaceous volcanic events in the northern Great Xing'an Range, Northeastern China[J]. Lithos, 2008, 102: 138-157. doi: 10.1016/j.lithos.2007.08.011 CrossRef Google Scholar
[12]	Zhang J H, Gao S, Ge W C, et al. Geochronology of the Mesozoic volcanic rocks in the Great Xing'an Range, northeastern China: Implications for subduction-induced delamination[J]. Chemical Geology, 2010, 27(6): 144-165. Google Scholar
[13]	张宏, 马俊孝, 权恒, 等. 大兴安岭北段中生代火山岩形成的动力学环境[J]. 贵金属地质, 1999, 8(1): 56-64. Google Scholar
[14]	邵济安, 张履桥, 牟堡垒, 等. 大兴安岭中生代伸展造山过程中的岩浆作用[J]地学前缘, 1996, (4): 339-346. Google Scholar
[15]	林强, 葛文春, 孙德有, 等. 东北地区中生代火山岩的大地构造意义[J]. 地质科学, 1998, 3(32): 129-139. Google Scholar
[16]	葛文春, 林强, 孙德有, 等. 大兴安岭中生代玄武岩的地球化学特征: 壳慢相互作用的证据[J]. 岩石学报, 1999, 15(3): 396-407. Google Scholar
[17]	吴福元, 曹林. 东北地区的若干重要基础地质问题[J]. 世界地质, 1999, 18(2): 1-13. Google Scholar
[18]	Meng Q R. What drove Late Mesozoic extension of the northern China-Mongolia tract[J]. Tectonophysics, 2003, 36(9): 155-174. Google Scholar
[19]	Wang P J, Chen F K, Shen S M, et al. Geochemical and Nd-Sr-Pb isotopic composition of Mesozoic volcanic rocks in the Songliao basin, NE China[J]. Geochemical Journal, 2006, 40: 149-159. doi: 10.2343/geochemj.40.149 CrossRef Google Scholar
[20]	陈志广, 张连昌, 周新华, 等. 满洲里新右旗火山岩剖面年代学和地球化学特征[J]. 岩石学报, 2006, 22(12): 1-14. Google Scholar
[21]	张玉涛, 张连昌, 英基丰, 等. 大兴安岭北段塔河地区早白垩世火山岩地球化学及源区特征[J]. 岩石学报2007, 23(11): 2811-2822. doi: 10.3969/j.issn.1000-0569.2007.11.012 CrossRef Google Scholar
[22]	Ying J F, Zhou X H, Zhang L C, et al. Geochronological framework of Mesozoic volcanic rocks in the Great Xing'an Range, NE China, and their geodynamic implications[J]. Journal of Asian Earth Sciences, 2010, 39(6): 786-793. doi: 10.1016/j.jseaes.2010.04.035 CrossRef Google Scholar
[23]	徐美君, 许文良, 孟恩, 等. 内蒙古东北部额尔古纳地区上护林-向阳盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J]. 地质通报, 2011, 30(9): 1321-1338. doi: 10.3969/j.issn.1671-2552.2011.09.001 CrossRef Google Scholar
[24]	Yu J J, Wang F, Xu W L, et al. Early Jurassic mafic magmatism in the Lesser Xing'an-Zhangguangcai Range, NE China and its tectonic implications: Constrains from zircon U-Pb chronology and geochemistry[J]. Lithos, 2012, 142/143: 256-266. doi: 10.1016/j.lithos.2012.03.016 CrossRef Google Scholar
[25]	Wu F F, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1): 1-30. doi: 10.1016/j.jseaes.2010.11.014 CrossRef Google Scholar
[26]	Liu Y S, Hu Z C, Gao S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(s1/2): 34-43. Google Scholar
[27]	Winchester J A, Floyd P A. Geochemical magma type discrimination: application to altered and metamorphosed basic igneous rocks[J]. Earth & Planetary Science Letters, 1976, 28(3): 459-469. Google Scholar
[28]	Le Maitre R W, Bakteman P, Dudek A, et al. A Classification of Igneous Rocks and Glossary of Terms Oxford: Blackwell[M]. Scientific Publications, 1989: 1-193. Google Scholar
[29]	Boynton W V. Geochemistry of the rare earth elements: Meteorite studies[C]//Henderson P. Rare Earth Element Geochemistry. Elsevier, 1984: 63-114. Google Scholar
[30]	Sun S S, McDonough W F. Chemical and isotopic systematics of ocean basalts: Implications for mantle composition and processes[C]//Saunders A D, Norry M J. Magmatism in Oceanic Basins. Geological Society, London, Special Publications, 1989, 42: 313-345. Google Scholar
[31]	Hirose K. Melting experiments on lherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts[J]. Geology, 1997, 25(1): 42-44. doi: 10.1130/0091-7613(1997)025<0042:MEOLKU>2.3.CO;2 CrossRef Google Scholar
[32]	Tischendorf G, Paelchen W. Zur Klassifikation von Granitoiden. Classification of granitoids[J]. Zeitschrift fuer Geologische Wissenschaften, 1985, 13(5): 615-627. Google Scholar
[33]	Rudnick R L, Gao S. Composition of the continental crust[C]//Rudnick R L. Treatiseo Geochemisty. Elsevier, 2003, 3: 1-64. Google Scholar
[34]	Hofmann A W. Chemical differentiation of the Earth: the relationship between mantle, continental, and oceanic crust[J]. Earth and Planetary Scientific Letters, 1988, 90(3): 297-314. doi: 10.1016/0012-821X(88)90132-X CrossRef Google Scholar
[35]	Wedepohl K H. The composition of the continental crust[J]. Geochimica et Cosmochimica Acta, 1995, 59(7): 1217-1232. doi: 10.1016/0016-7037(95)00038-2 CrossRef Google Scholar
[36]	张遵忠, 顾连兴, 吴昌志, 等. 东天山印支早期尾亚石英正正长岩: 成岩作用及成岩意义[J]. 岩石学报, 2006, 22(5): 1135-1149. Google Scholar
[37]	Xu M J, Xu W L, Wang F, et al. Geochronology and geochemistry of the Early Jurassic granitoids in then orthwestern Lesser Xing an Range, NE Chaina and its tectonic implications[J]. Acta Petrologina Sinica, 2013, 29(2): 34-368. Google Scholar
[38]	王召林, 金浚, 李占龙, 等. 大兴安岭中北段莫尔道嘎地区含矿斑岩的U-Pb锆石年龄Hf同位素特征及成矿意义[J]. 岩石矿物学杂志, 2010, 29(6): 796-810. doi: 10.3969/j.issn.1000-6524.2010.06.015 CrossRef Google Scholar
[39]	Chen Z G, Zhang L C, Wan B, et al. Geochronology and geochemistry of the Wunugetushan porphyry Cu-Mo deposit in NE China, and their geological significance[J]. Ore Geology Reviews, 2011, 43(1): 92-105. doi: 10.1016/j.oregeorev.2011.08.007 CrossRef Google Scholar
[40]	Li N, Chen Y J, Ulrich T, et al. Fluid inclusion study of the Wunugtu Cu-Mo deposit, InnerMongolia, China[J]. Mineralium Deposita, 2012, 47(5): 467-482. doi: 10.1007/s00126-011-0384-1 CrossRef Google Scholar
[41]	李宇, 丁磊磊, 许文良, 等. 孙吴地区中侏罗世白云母花岗岩的年代学与地球化学: 对蒙古-鄂霍茨克洋闭合时间的限定[J]. 岩石学报, 2015, 31(1): 56-66. Google Scholar
[42]	徐美君, 许文良, 王枫, 等. 小兴安岭中部早侏罗世花岗质岩石的年代学与地球化学及其构造意义[J]. 岩石学报, 2013, 29(2): 354-368. Google Scholar
[43]	张旗, 王焰, 李承东, 等. 花岗岩的Sr-Yb分类及其地质意义[J]. 岩石学报, 2006, 22: 2249-2269. Google Scholar
[44]	张旗, 王焰, 李承东, 等. 花岗岩按照压力的分类[J]. 地质通报, 2006, 25: 1274-1278. doi: 10.3969/j.issn.1671-2552.2006.11.004 CrossRef Google Scholar
[45]	张旗, 王焰, 熊小林, 等. 埃达克岩和花岗岩: 挑战与机遇[M]. 北京: 中国大地出版社, 2008: 1-344. Google Scholar
[46]	杨华本, 王文东, 闫永生, 等. 大兴安岭北段新林区塔木兰沟组火山岩成因及地幔富集作用[J]. 地质论评, 2016, 62(6): 1471-1486. Google Scholar
[47]	Kravchinsky V A, Cogne J P, Harbrt W P, et al. Evolution of the Mongol-Ocean as constrained by newpalaeomagnetic data from the Mongol-Okhotsk suture zone, Sliberia[J]. GeophysicalJourmal International, 2002, 148(1): 34-57. doi: 10.1046/j.1365-246x.2002.01557.x CrossRef Google Scholar
[48]	Sorokin A A, Sorokin A P, Ponomarchuk VA, et al. The age and geochemistry of volcaic rocks on the eastern flank of the Umlekan-Ogodzha volcanoplutonic belt(Amurregion)[J]. Russian Geology and Geophysics, 2010, 51(4): 369-379. doi: 10.1016/j.rgg.2010.03.004 CrossRef Google Scholar
[49]	Pearce J A, Lippard S J, Roberts S. Charactesitcs and tectonic significance of supra-subducion zone ophiolites. Geological Society[M]. London, Special Publications, 1984: 77-94. Google Scholar
①	黑龙江省地质调查院. 黑龙江1: 25万漠河县、漠河、兴安幅区调(修测)报告. 2016. Google Scholar
②	中国人民武装警察部队黄金第三支队. 1: 5万战备村、二中队幅区域地质矿产调查报告. 2014. Google Scholar