吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (6): 1725-1740.doi: 10.13278/j.cnki.jjuese.20180050

• 地质与资源 • 上一篇    下一篇

黑龙江省东部早古生代晨明组物源区特征及其构造背景

高福红, 何雨思, 王枫, 修铭   

  1. 吉林大学地球科学学院, 长春 130061
  • 收稿日期:2018-05-26 出版日期:2018-11-26 发布日期:2018-11-26
  • 通讯作者: 何雨思(1993-),女,硕士研究生,主要从事岩石学方面的研究,E-mail:heys16@mails.jlu.edu.cn E-mail:heys16@mails.jlu.edu.cn
  • 作者简介:高福红(1963-),女,教授,博士生导师,主要从事岩石学方面的研究,E-mail:gaofh@mails.jlu.edu.cn
  • 基金资助:
    国家自然科学基金项目(41272075)

Provenance Characteristics and Tectonic Setting of Early Paleozoic Chenming Formation in Eastern Heilongjiang Province

Gao Fuhong, He Yusi, Wang Feng, Xiu Ming   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2018-05-26 Online:2018-11-26 Published:2018-11-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41272075)

摘要: 为揭示黑龙江省东部早古生代晨明组沉积物源区特征及其沉积构造背景,对晨明组进行了地球化学特征研究。结果表明:晨明组岩石样品化学蚀变指数(ICA)值和斜长石蚀变指数(IPA)值较低、成分变异指数(ICV)值中等偏高,指示晨明组沉积物来源于不成熟的物质源区,并经历了较弱的化学风化作用和活动构造背景下的初次循环;LREE富集、HREE稳定和明显的负Eu异常,指示沉积物源区物质具有明显的上地壳特征且沉积物源岩为长英质火成岩;主量、微量和稀土元素特征共同指示晨明组形成于活动大陆边缘环境或大陆岛弧环境。结合前人研究成果,判定晨明组沉积物来源于经历了弱-中等程度化学风化作用的早古生代花岗质岩,沉积构造背景可能为靠近大陆岛弧的活动大陆边缘环境。

关键词: 黑龙江省东部, 晨明组, 地球化学, 沉积物源区, 构造背景

Abstract: To constrain the characteristics of sedimentary provenance and sedimentary tectonic setting of the Early Paleozoic Chenming Formation located in the eastern Heilongjiang Province, its geochemical characteristics were studied. The results show that the ICA and IPA values measured from the rock samples of Chenming Formation are relatively low, while their ICV values are moderate, indicating that the sediments of Chenming Formation came from an immature source, and experienced weak chemical weathering and initial circulation in an active tectonic environment. The enriched LREE, flat HREE pattern and obvious negative Eu-anomaly are suggestive to the obvious upper crustal characteristics of the materials in sedimentary provenance, and the source rocks of the sediments might be felsic igneous rocks.The geochemical analyses on major, trace elements as well as rare earth elements demonstrate that Chenming Formation might be deposited in an active continental margin or continental island arc environment. Combined with the previous literatures, the source rocks of Chenming Formation might be the Early Paleozoic granite, which were altered by weak to moderate weathering, and the sedimentary tectonic setting might be an active continental margin that was adjacent to island arcs.

Key words: eastern Heilongjiang Province, Chenming Formation, geochemistry, sedimentary provenance, tectonic setting

中图分类号: 

  • P588.2
[1] 李锦轶,张进,杨天南,等.北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J].吉林大学学报(地球科学版),2009,39(4):587-605. Li Jinyi, Zhang Jin, Yang Tiannan, et al. Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J].Journal of Jilin University(Earth Science Edition), 2009, 39(4):587-605.
[2] Sengör A M C, Natal'in B A, Burtman V S.Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia[J].Nature, 1993, 364:299-307.
[3] 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.
[4] Jia D C, Hu R Z, Lu Y, et al. Collision Belt Between the Khanka Block and the North China Block in the Yanbian Region, Northeast China[J].Journal of Asian Earth Sciences, 2004, 23(2):211-219.
[5] Zhang Y B, Wu F Y, Wilde S A, et al. Zircon U-Pb Ages and Tectonic Implications of 'Early Paleozoic' Granitoids at Yanbian, Jilin Province, Northeast China[J].The Island Arc, 2004, 13:484-505.
[6] Meng E, Xu W L, Pei F P, et al. Permian Bimodal Volcanism in the Zhangguangcai Range of Eastern Heilongjiang Province, NE China:Zircon U-Pb-Hf Isotopes and Geochemical Evidence[J].Journal of Asian Earth Sciences, 2011, 41:119-132.
[7] Xu W L, Ji W Q, Pei F P, et al. Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces, NE China:Chronology, Geochemistry, and Tectonic Implications[J].Journal of Asian Earth Sciences, 2009, 34:392-402.
[8] 孟恩,许文良,裴福萍,等.黑龙江省东部中泥盆世火山作用及其构造意义:来自岩石地球化学、锆石U-Pb年代学和Sr-Nd-Hf同位素的制约[J].岩石矿物学杂志,2011,30(5):883-900. Meng En, Xu Wenliang, Pei Fuping, et al. Middle Devonian Volcanism in Eastern Heilongjiang Province and Its Tectonic Implications:Constraints from Petro-Geochemistry, Zircon U-Pb Chronology and Sr-Nd-Hf Isotopes[J].Acta Petrologica et Mineralogica, 2011, 30(5):883-900.
[9] 唐杰,许文良,王枫,等.张广才岭帽儿山组双峰式火山岩成因:年代学与地球化学证据[J].世界地质,2011,30(4):508-513. Tang Jie, Xu Wenliang, Wang Feng, et al. Petrogenesis of Bimodal Volcanic Rocks from Maoershan Formation in Zhangguangcai Range:Evidence from Geochronology and Geochemistry[J].Global Geology, 2011, 30(4):508-513.
[10] Wang F, Xu W L, Meng E, et al. Late Triassic Bimodal Magmatism in the Lesser Xing'an-Zhangguangcai Range, NE China:Geochronological and Geochemical Evidence[J].Mineralogical Magazine, 2011, 75:2116.
[11] Wang F, Xu W L, Meng E, et al. Early Paleozoic Amalgamation of the Songnen-Zhangguangcai Range and Jiamusi Massifs in the Eastern Segment of the Central Asian Orogenic Belt:Geochronological and Geochemical Evidence from Granitoids and Rhyolites[J].Journal of Asian Earth Sciences, 2012, 49:234-248.
[12] Yu J J, Wang F, Xu W L, et al. Late Permian Tectonic Evolution at the Southeastern Margin of the Songnen-Zhangguangcai Range Massif, NE China:Constraints from Geochronology and Geochemistry of Granitoids[J]. Gondwana Research, 2013, 24:635-647.
[13] Wang F, Xu W L, Gao F H, et al. Tectonic History of the Zhangguangcailing Group in Eastern Heilongjiang Province, NE China:Constraints from U-Pb Geochronology of Detrital and Magmatic Zircons[J].Tectonophysics, 2012, 566/567:105-122.
[14] 高福红,王枫,许文良,等.小兴安岭"古元古代"东风山群的形成时代及其构造意义:锆石U-Pb年代学证据[J].吉林大学学报(地球科学版),2013,43(2):440-456. Gao Fuhong, Wang Feng, Xu Wenliang, et al. Age of the "Paleoproterozoic" Dongfengshan Group in the Lesser Xing'an Range, NE China, and Its Tectonic Implications:Constraints from Zircon U-Pb Geochronology[J].Journal of Jilin University(Earth Science Edition), 2013, 43(2):440-456.
[15] 高福红,杨扬,王枫,等.黑龙江省东部早古生代地层的确定:地质与碎屑锆石U-Pb年代学证据[J].地球科学,2014,39(5):499-508. Gao Fuhong, Yang Yang, Wang Feng, et al. Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province:Evidence from Field Geology and Detrital Zircon U-Pb Geochronology[J].Earth Science, 2014, 39(5):499-508.
[16] 郝文丽,许文良,王枫,等.张广才岭"新元古代"一面坡群的形成时代:来自岩浆锆石和碎屑锆石U-Pb年龄的制约[J].岩石学报,2014,30(7):1867-1878. Hao Wenli, Xu Wenliang, Wang Feng, et al. Geochronology of the "Neoproterozoic" Yimianpo Group in the Zhangguangcai Range, NE China:Constraints from U-Pb Ages of Detrial and Magmatic Zircons[J].Acta Petrologica Sinica, 2014, 30(7):1867-1878.
[17] 龙晓平,袁超,孙敏,等.北疆阿尔泰南缘泥盆系浅变质碎屑沉积岩地球化学特征及其形成环境[J].岩石学报,2008,24(4):718-732. Long Xiaoping, Yuan Chao, Sun Min, et al. Geochemical Characteristics and Sedimentary Environments of Devonian Low Metamorphic Clastic Sedimentary Rocks in the Southern Margin of the Chinese Altai, North Xinjiang[J].Acta Petrologica Sinica, 2008, 24(4):718-732.
[18] 沈瑞峰,张辉,唐勇,等.阿尔泰造山带古生代地层的地球化学特征及其对沉积环境的制约[J].地球化学,2015,44(1):43-60. Shen Ruifeng, Zhang Hui, Tang Yong, et al. Geochemical Characteristics of Paleozoic Strata and Its Restriction on Depositional Environment in Altay Orogen, North Xinjiang, China[J].Geochimica, 2015, 44(1):43-60.
[19] 李想,于泓超,许俸源,等.黑龙江黄松群的地球化学特征及形成环境分析[J].世界地质,2016,35(3):697-707. Li Xiang, Yu Hongchao, Xu Fengyuan, et al. Geochemical Characteristics of Huangsong Group in Heilongjiang and Its Tectonic Environments[J].Global Geology, 2016, 35(3):697-707.
[20] 石海岩,苗卫良,马海州,等.云南思茅盆地白垩纪-古新世碎屑岩地球化学特征及地质意义[J].现代地质,2016,30(3):541-554. Shi Haiyan, Miao Weiliang, Ma Haizhou, et al. Geochemistry of Cretaceous-Palaeocene Detrital Rocks in Simao Basin, Yunnan Province and Its Geological Significances[J].Geoscience, 2016, 30(3):541-554.
[21] Li D F, Chen H Y, Zhang L, et al. Geochemistry of Fine-Grained Clastic Rocks in the Mesoproterozoic Kawabulake Group:Implications for Provenance and the Tectonic Model of the Eastern Tianshan, Xinjiang, NW China[J].Int J Earth Sci (Geol Rundsch), 2017, 106:115-129.
[22] 许文良,王枫,孟恩,等.黑龙江省东部古生代-早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据[J].吉林大学学报(地球科学版),2012,42(5):1378-1389. Xu Wenliang, Wang Feng, Meng En, et al. Paleozoic-Early Mesozoic Tectonic Evolution in the Eastern Heilongjiang Province, NE China:Evidence from Igneous Rock Association and U-Pb Geochronology of Detrital Zircons[J].Journal of Jilin University(Earth Science Edition), 2012, 42(5):1378-1389.
[23] 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 Resource.Regional Geology of Heilongjiang Province[M].Beijing:Geological Publishing House,1993.
[24] 黑龙江省地质矿产局.黑龙江省岩石地层[M].武汉:中国地质大学出版社,2008. Heilongjiang Bureau of Geology and Mineral Resource.Lithostratigraphy of Heilongjiang Province[M].Wuhan:China University of Geosciences Press,2008.
[25] McLennan S M.Weathering and Global Denudation[J].The Journal of Geology, 1993, 101(2):295-303.
[26] Taylor S R, McLennan S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell Scientific Publications, 1985.
[27] Sun S S, McDonough W F.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society of London, 1989, 42:313-345.
[28] Nesbitt H W, Young G M.Early Proterozoic Climates and Plate Motions Inferred from Major Element Chemistry of Lutites[J].Nature, 1982, 299:715-717.
[29] Cox R, Lowe D R, Cullers R L.The Influence of Sediment Recycling and Basement Composition on Evolution of Mudrock Chemistry in the Southwestern United States[J].Geochimica et Cosmochimica Acta, 1995, 59(14):2919-2940.
[30] Kamp P C, Leake B E.Petrography and Geochemistry of Feldspathic and Mafic Sediments of the Northeastern Pacific Margin[J].Transactions of the Royal Society of Edinburgh:Earth Sciences, 1985, 76:411-449.
[31] Fedo C M, Nesbitt H W, Young G M.Unraveling the Effects of Potassium Metasomatism in Sedimentary Rocks and Paleosols, with Implications for Paleoweathering Conditions and Provenance[J].Geology, 1995, 23(10):921-924.
[32] Nesbitt H W, Young G M.Prediction of Some Weathering Trends of Plutonic and Volcanic Rocks Based on Thermodynamic and Kinetic Considerations[J].Geochimica et Cosmochimica Acta, 1984, 48:1523-1534.
[33] McLennan S M, Taylor S R.Th and U in Sedimentary Rocks:Crustal Evolution and Sedimentary Recycling[J].Nature, 1980, 285:621-624.
[34] McLennan S M, Hemming S, McDaniel D K, et al. Geochemical Approaches to Sedimentation, Provenance, and Tectonics[J].Geological Society of America Special Paper, 1993, 284:21-40.
[35] Cullers R L, Basu A, Suttner L.Geochemical Signa-ture of Provenance in Sand-size Material in Soils and Stream Sediments Near the Tobacco Root Batholith, Montana, USA[J].Chemical Geology, 1988, 70:335-348.
[36] McLennan S M, Taylor S R, McCulloch M T, et al. Geochemical and Nd-Sr Isotopic Composition of Deep-Sea Turbidites:Crustal Evolution and Plate Tectonic Associations[J].Geochimica et Cosmochimica Acta, 1990, 54(7):2015-2050.
[37] Cullers R L.The Chemical Signature of Source Rocks in Size Fractions of Holocene Stream Sediment Derived from Metamorphic Rocks in the Wet Mountains Region, Colorado, USA[J].Chemical Geology, 1994, 113:327-343.
[38] McLennan S M.Rare Earth Elements in Sedimentary Rocks:Influence of Provenance and Sedimentary Processes[J].Review of Mineralogy, 1989, 21:169-200.
[39] Hayashi K I, Fujisawa H, Holland H D, et al. Geochemistry of~1.9 Ga Sedimentary Rocks from Northeastern Labrador, Canada[J].Geochimica et Cosmochimica Acta, 1997, 16(19):4115-4137.
[40] Girty G H, Ridge D L, Knaack C, et al. Provenance and Depositional Setting of Paleozoic Chert and Argillite, Sierra Nevada, California[J].Journal of Sedimentary Research, 1996, 66(1):107-118.
[41] Bhatia M R.Rare Earth Element Geochemistry of Australian Paleozoic Graywacks and Mudrocks:Provenance and Tectonic Control[J].Sedimentary Geology, 1985, 45:97-113.
[42] Gu X X, Liu J M, Zhang M H, et al. Provenance and Tectonic Setting of the Proterozoic Turbidites in Hunan, South China:Geochemical Evidence[J].Journal of Sedimentary Research, 2002, 72(3):393-407.
[43] Floyd P A, Leveridge B E.Tectonic Environment of Devonia Gramscatho Basin, South Cornwall:Framework Mode and Geochemical Evidence from Turbiditic Sandstones[J].Geological Society of London Journal, 1987, 144(4):531-542.
[44] Shao L, Stattegger K, Garbe Schoenberg C D.Sand-stone Petrology and Geochemistry of the Turpan Basin(NW China):Implications for the Tectonic Evolution of a Continental Basin[J].Journal of Sedimentary Research, 2001, 71(1):37-49.
[45] Bhatia M R, Crook K A W.Trace Element Charac-teristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins[J].Contributions to Mineralogy and Petrology, 1986, 92:181-193.
[46] McLennan S M, Taylor S R.Sedimentary Rocks and Crustal Evolution:Tectonic Setting and Secular Trends[J]. The Journal of Geology, 1991, 99(1):1-21.
[47] Bhatia M R.Plate Tectonics and Geochemical Com-position of Sandstones[J].The Journal of Geology, 1983, 91(6):611-627.
[48] Roser B P, Korsch R J.Determination of Tectonic Setting of Sandstone-Mudstone Suites Using SiO2 Content and K2O/Na2O Ratio[J].The Journal of Geology, 1986, 94(5):635-650.
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