大兴安岭中南段霍林河地区火山喷发旋回划分及特征

doi:10.19388/j.zgdzdc.2023.331

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Abstract Huolinhe area in the central and southern Greater Khingan Mountain has experienced strong volcanic activities since Mesozoic Era, and widely distributed intermediate acidic volcanic rocks were formed from Middle Jurassic to Early Cretaceous, which is a desirable area for evolution characteristics research of volcanic eruption during Mesozoic Era. The triple mapping method of “volcanic lithology and lithofacies, volcanic structure, and rock strata” was used in Huolinhe area to summarize and analyze the lithology, lithofacies, volcanic eruption cycles, and rhythmic characteristics. The result shows that the types of exposed rock types in this area can be divided into six categories, including ordinary pyroclastic rocks, fused pyroclastic rocks, lava, sedimentary pyroclastic rocks and pyroclastic sedimentary rocks, and latent volcanic rock. And there are eight types of lithofacies, including explosive facies, pyroclastic flow facies, volcanic eruption collapse facies, overflow facies, volcanic eruption sedimentary facies, volcanic neck facies, intrusive facies, and subvolcanic lithofacies. The volcanic activity in this area can be divided into six volcanic eruption cycles: Xinmin period ((163.7±1.7)~(160.0±4.0) Ma), Tamulangou period ((164.2±4.1)~(159.7±2.7) Ma), Manketouebo period ((163.4±1.3)~(157.0±1.1) Ma), Manitu period ((151.4±2.6)~(144.0±2.8) Ma), Baiyingaolao period ((141.7±1.3)~(128.6±1.4) Ma), and Meiletu period ((133.4±1.5)~(127.7±1.4) Ma), corresponding to the six volcanic rock stratigraphic formation. Volcanic activity was unstable in Huolinhe area during Middle Jurassic. A small amount of acidic volcanic debris erupted and were accompanied by many intermittent periods, followed by mainly calm overflow of neutral lava in the late phase. There was a strong eruption of acidic volcanic clastic rocks during Late Jurassic, accompanied by a small amount of medium acidic volcanic lava overflow. In the early stages of Early Cretaceous, the early stage volcanic activities were characterized by strong eruption of acidic volcanic clastic rocks, and the late stage volcanic activities were characterized by calm overflow of medium basic volcanic lava. The volcanic activities in this area could represent the characteristics of the eruption cycles of Mesozoic volcanic rocks in the central and southern Greater Khingan Mountain. Therefore, the research result is of great significance to the reasonable division of the eruption cycles of Mesozoic volcanic rocks in the central and southern Greater Khingan Mountain, and could help promote in-depth comparative studies of volcanic rock combinations, volcanic activity characteristics, lithofacies construction, and volcanic stratigraphy in different regions.

Key words： volcanic mapping volcanic eruption cycle rhythm volcanic structure lithology lithofacies

Received: 04 December 2023

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LIU Yonggao. Volcanic eruption cycles division and characteristics in Huolinhe area of the central and southern Greater Khingan Mountain[J]. , 2024, 11(4): 50-61.

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http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2023.331 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2024/V11/I4/50

[1] 任纪舜,姜春发,张正坤,等.中国大地构造及其演化[M].北京:科学出版社,1980:1-124.
Ren J S,Jiang C F,Zhang Z K,et al.Geotectonic Evolution of China[M].Beijing:Science Press,1980:1-124.
[2] 孙德有,许文良,周燕.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,1994,13(3):162-164.
Sun D Y,Xu W L,Zhou Y,et al.Forming mechanism of the Mesozoic volcanic rocks in Da Hinggan Mountain,NE China[J].Bulletin of Mineralogy,Petrology and Geochemistry,1994,13(3):162-164.
[3] 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.
[4] 孙卫东,凌明星,汪方跃,等.太平洋板块俯冲与中国东部中生代地质事件[J].矿物岩石地球化学通报,2008,27(3):218-225.
Sun W D,Ling M X,Wang F Y,et al.Pacific plate subduction and Mesozoic geological event in Eastern China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2008,27(3):218-225.
[5] 孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226.
Meng E,Xu W L,Yang D B,et al.Zircon U-Pb chronology,geochemistry of Mesozoic volcanic rocks from the Lingquan Basin in Manzhouli area,and its tectonic implications[J].Acta Petrologica Sinica,2011,27(4):1209-1226.
[6] Xu W L,Pei F P,Wang F,et al.Spatial-temporal relationships of Mesozoic volcanic rocks in NE China:Constraints on tectonic overprinting and transformations between multiple tectonic regimes[J].Journal of Asian Earth Sciences,2013,74:167-193.
[7] 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.
Xu W L,Wang F,Pei F P,et al.Mesozoic tectonic regimes and regional ore-forming background in NE China:Constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[8] 张丽,刘永江,冯志强,等.额尔古纳地块中生代火山岩盆地基底构造特征:来自灵泉盆地的启示[J].地球科学,2017,42(12):2229-2242.
Zhang L,Liu Y J,Feng Z Q,et al.Basement structural features of Mesozoic volcanic basins in Erguna Massif:Implications from Lingquan Basin[J].Earth Science,2017,42(12):2229-2242.
[9] 林强,葛文春,孙德有,等.中国东北地区中生代火山岩的大地构造意义[J].地质科学,1998,33(2):3-13.
Lin Q,Ge W C,Sun D Y,et al.Tectonic significance of Mesozoic volcanic rocks in Northeastern China[J].Scientia Geologica Sinica,1998,33(2):3-13.
[10] 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:壳幔相互作用的证据[J].岩石学报,1999,15(3):396-406.
Ge W C,Lin Q,Sun D Y,et al.Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling:Evidence of the mantle-crust interaction[J].Acta Petrologica Sinica,1999,15(3):396-407.
[11] 孟凡超,刘嘉麒,崔岩,等.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约[J].岩石学报,2014,30(12):3569-3586.
Meng F C,Liu J Q,Cui Y,et al.Mesozoic tectonic regimes transition in the Northeast China:Constriants from temporal-spatial distribution and associations of volcanic rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[12] 张学斌,周长红,来林,等.锡林浩特东部早白垩世白音高老组岩石地球化学特征、LA-MC-ICP-MS锆石U-Pb年龄及地质意义[J].地质与勘探,2015,51(2):290-302.
Zhang X B,Zhou C H,Lai L,et al.Geochemistry and zircon U-Pb dating of volcanic rocks in eastern Xilin Hot,Inner Mongolia and their geological implications[J].Geology and Exploration,2015,51(2):290-302.
[13] 杨晓平,江斌,杨雅军.大兴安岭早白垩世火山岩的时空分布特征[J].地球科学,2019,44(10):3237-3251.
Yang X P,Jiang B.Yang Y J.Spatial-temporal distribution characteristics of Early Cretaceous volcanic rocks in Great Xing'an range area[J].Earth Science,2019,44(10):3237-3251.
[14] 杨雅军,杨晓平,江斌,等.大兴安岭中生代火山岩地层时空分布与蒙古—鄂霍茨克洋、古太平洋板块俯冲作用响应[J].地学前缘,2022,29(2):115-131.
Yang Y J,Yang X P,Jiang B,et al.Spatio-temporal distribution of Mesozoic volcanic strata in the Great Xing'an Range:Response to the subduction of the Mongol-Okhotsk Ocean and Paleo-Pacific Ocean[J].Earth Science Frontiers,2022,29(2):115-131.
[15] 周新华,英基丰,张连昌,等.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约[J].中国地质大学学报:地球科学版,2009,34(1):1-10.
Zhou X H,Ying J F,Zhang L C,et al.The Petrogenesis of Late Mesozoic volcanic rock and the contributions from ancient micro-continents:constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hf isotopic systematics[J].Earth Science-Journal of China University of Geosciences,2009,34(1):1-10.
[16] 刘世伟. 大兴安岭地区中生代火山岩岩石地层的划分与对比问题[J].地质与资源,2009,18(4):241-244.
Liu S W.Division and correlation of the Mesozoic volcanic rocks and strata in Daxinganling region[J].Geology and Resources,2009,18(4):241-244.
[17] 赵海玲,邓晋福,陈发景,等.中国东北地区中生代火山岩岩石学特征与盆地形成[J].现代地质,1998,12(1):56-62.
Zhao H L,Deng J F,Chen F J,et al.Petrology of the Mesozoic volcanic rocks and the basin formation in the Northeast China[J].Geoscience,1998,12(1):56-62.
[18] 葛文春,林强,孙德有,等.大兴安岭中生代两类流纹岩成因的地球化学研究[J].中国地质大学学报:地球科学版,2000,25(2):172-178.
Ge W C,Lin Q,Sun D Y,et al.Geochemical research into origins of two types of Mesozoic rhyolites in Daxing'anling[J].Earth Science-Journal of China University of Geosciences,2000,25(2):172-178.
[19] 李世超,徐仲元,刘正宏,等.大兴安岭中段玛尼吐组火山岩LA-ICP-MS锆石U-Pb年龄及地球化学特征[J].地质通报,2013,32(2/3):399-407.
Li S C,Xu Z Y,Liu Z H,et al.Zircon U-Pb dating and geochemical study of volcanic rocks in Manitu formation of central Da Hinggan Mountains[J].Geological Bulletin of China,2013,32(2/3):399-407.
[20] 邵济安,赵国龙,王忠,等.大兴安岭中生代火山活动构造背景[J].地质论评,1999,45(S1):422-430.
Shao J A,Zhao G L,Wang Z,et al.Tectonic setting of Mesozoic volcanism in Da Hinggan Mountains,Northeastern China[J].Geological Review,1999,45(S1):422-430.
[21] 徐智涛,李萌萌,孙景贵,等.大兴安岭得耳布尔地区中侏罗世流纹岩成因及成岩地球动力学背景[J].吉林大学学报:地球科学版,2023,53(3):866-886.
Xu Z T,Li M M,Sun J G,et al.Genesis and Diagenetic geodynamic background of Middle Jurassic rhyolites in Derbur area,Great Xing'an Range[J].Journal of Jilin University (Earth Science Edition),2023,53(3):866-886.
[22] 秦涛. 大兴安岭中段晚中生代火山岩地球化学与岩石成因研究[D].长春:吉林大学,2022.
Qin T.The Geochemical and Petrogenetic Studies on Late Mesozoic Volcanic Rocks in the Central Segment of Great Xing'an Range[D].Changchun:Jilin University,2022.
[23] 王亚东,姜山,王之晟,等.大兴安岭南段工农屯地区上侏罗统玛尼吐组火山岩U-Pb年龄、地球化学特征及其成因[J].地质论评,2023,69(3):973-986.
Wang Y D,Jiang S,Wang Z S,et al.U-Pb age,geochemical characteristics and genesis of volcanic rocks from the Upper Jurassic Manitu formation in Gongnongtun area,southern Great Hinggan Mountains[J].Geological Review,2023,69(3):973-986.
[24] 陈超,吕新彪,李杰,等.大兴安岭中段塔尔气地区中酸性火山岩成因及构造背景[J].地球科学,2020,45(12):4446-4462.
Chen C,Lü X B,Li J,et al.Petrogenesis and tectonic setting of intermediate-felsic volcanics in Ta'erqi area,central Great Xing'an Range[J].Earth Science,2020,45(12):4446-4462.
[25] 李中会,李睿杰,李阳,等.大兴安岭满归地区变中酸性火山岩LA-ICP-MS 锆石U-Pb年龄及其地质意义[J].中国地质调查,2020,7(1):47-52.
Li Z H,Li R J,Li Y,et al.LA-ICP-MS zircon U-Pb ages and geological significance of the meta-intermediate-acidic volcanic rocks in Mangui area of Da Hinggan Mountains[J].Geological Survey of China,2020,7(1):47-52.
[26] 张超. 大兴安岭南段巴林左旗-扎鲁特旗地区晚中生代岩浆作用及其构造背景[D].长春:吉林大学,2020.
Zhang C.Late Mesozoic Magmatism and Tectonic Setting of Bairin Left Banner-Jarud Banner Area in the Southern Great Xing'an Range[D].Changchun:Jilin University,2020.
[27] 王忠,朱洪森.大兴安岭中南段中生代火山岩特征及演化[J].中国区域地质,1999,18(4):351-358,372.
Wang Z,Zhu H S.Temporal and spatial evolution of the Mesozoic volcanism in mid-southern Daxinganling Mountain[J].Regional Geology of China,1999,18(4):351-358,372.
[28] 尹志刚,张跃龙,杨晓平,等.大兴安岭北部中生代火山岩特征及岩浆演化[J].世界地质,2006,25(2):120-128.
Yin Z G,Zhang Y L,Yang X P,et al.Characteristics of Mesozoic volcanic rocks and magma evolution in northern Daxinganling[J].World Geology,2006,25(2):120-128.
[29] 何雨栗,李小强,杨国林,等.内蒙古阿巴嘎旗北部侏罗纪火山岩地质特征与喷发旋回[J].兰州大学学报:自然科学版,2014,50(2):161-167.
He Y L,Li X Q,Yang G L,et al.Geological characteristics and eruption cycle partition of Jurassic volcanic rocks from northern Abagaqi,Inner Mongolia[J].Journal of Lanzhou University (Natural Sciences),2014,50(2):161-167.
[30] 张顺新,黄新华,刘伟,等.大兴安岭中段央格力雅山火山喷发盆地火山活动旋回和构造特征[J].现代矿业,2022,38(6):42-46,50.
Zhang S X,Huang X H,Liu W,et al.Volcanic activity cycles and volcanic structure characteristics of Yanggeliya Eruption Basin,central Great Xing'an Range[J].Modern Mining,2022,38(6):42-46,50.
[31] 石好果,林会喜.准中4区块侏罗系储层成岩及油气充注特征研究[J].特种油气藏,2017,24(6):18-22.
Shi H G,Lin H X.Study on the characteristics of Jurassic reservoir diagenesis and hydrocarbon filling in middle 4 block of Jungar Basin[J].Special Oil and Gas Reservoirs,2017,24(6):18-22.
[32] 邢光福. 中国东部中新生代陆缘弧盆系大地构造图说明书(1:2 500 000)[M].北京:地质出版社,2016.
Xing G F.Explanatory Note to the Mesozoic-Cenozoic Tectonic Map of Continental Marginal Arc-Basin Systems of China (1:2 500 000)[M].Beijing:Geology Press,2016.
[33] 赵国龙,杨桂林,傅嘉友,等.大兴安岭中南部中生代火山岩[M].北京:北京科学技术出版社,1989.
Zhao G L,Yang G L,Fu J Y,et al.Mesozoic Vol-Canic Rocks in the Middle South Great Xing'an Range[M].Beijing:Beijing Science and Technology Press,1989.
[34] 杨海星,高利东,高玉石,等.内蒙古霍林河地区晚石炭世本巴图组火山岩年代学、地球化学特征及构造背景[J].中国地质,2020,47(4):1173-1185.
Yang H X,Gao L D,Gao Y S,et al.The chronology,geochemical characteristics and tectonic setting of the volcanic rocks in the Benbatu formation of Huolinhe area,Inner Mongolia[J].Geology in China,2020,47(4):1173-1185.
[35] 谢家莹,徐忠连.括苍山地区中生代火山旋回划分[J].中国地质科学院南京地质矿产研究所所刊,1988,(2):68-80.
Xie J Y,Xu Z L.Mesozoic Volcano-Active Cycle and Feature in Kuochangshan District Zhejiang[J].Bull.Nanjing lnst.Geol.M.R.,Chinese Acad.Geol.Sci.,1988,(2):68-80.
[36] 尹家衡,黄光昭.中国东南沿海中、新生代火山旋回[J].火山地质与矿产,1997,18(3):167-190.
Yin J H,Huang G Z.Mesozoic-Cenozoic volcanic cycles of southeast coast of China[J].Volcanology & Mineral Resources,1997,18(3):167-190.
[37] 柳青. 地层、地层单位及其表示方法[J].科技与出版,2011(10):50-51.
Liu Q.Strata,stratigraphic units and their representation me-thods[J].Technology and Publishing,2011(10):50-51.
[38] 高利东,杨海星,隋海涛,等.1:50 000包尔呼吉尔塔拉等8幅区域地质调查报告[R].2019.
Gao L D,Yang H X,Sui H X,et al.1:50 000 Regional Geological Survey Report of Baoerhujiertala and Other 4 Regional[R].2019.
[39] 杨海星,赵胜金,柳志辉,等.大兴安岭中南段满克头鄂博组正层型剖面火山岩年代学及地球化学特征[J].世界地质,2023,42(2):213-229.
Yang H X,Zhao S J,Liu Z H,et al.Geochronological and geochemical characteristics of orthostratigraphic section volcanic rocks of Manketouebo formation in south-central sector of Great Xing'an Range[J].World Geology,2023,42(2):213-229.
[40] 杨海星,高利东,高玉石,等.大兴安岭中南段罕山林场地区玛尼吐组安山岩年代学、地球化学特征及其地质意义[J].地质与勘探,2019,55(5):1223-1240.
Yang H X,Gao L D,Gao Y S,et al.Geochronology and geochemistry of the andesites from the Manitu formation in the Hanshanlinchang area,central-southern Daxinganling Mountains and their geological implications[J].Geology and Exploration,2019,55(5):1223-1240.
[41] 杨海星,高利东,高玉石,等.大兴安岭中南段梅勒图组层型剖面锆石U-Pb年龄、地球化学特征及其地质意义[J].地质通报,2019,38(5):845-857.
Yang H X,Gao L D,Gao Y S,et al.Zircon U-Pb age and geochemistry of the stratotype section of the Meiletu formation in middle southern Da Hinggan Mountains and its geological significance[J].Geological Bulletin of China,2019,38(5):845-857.
[42] 周其林,王献忠,吉峰,等.大兴安岭中生代火山岩地层对比[J].地质论评,2013,59(6):1077-1084.
Zhou Q L,Wang X Z,Ji F,et al.Corresponding relations of Mesozoic volcanic formations in the Da Hinggan Mountains[J].Geological Review,2013,59(6):1077-1084.