Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1082-1097.doi: 10.13278/j.cnki.jjuese.20200265

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Petrogenesis and Tectonic Implication of Late Paleozoic I-A Type Granites in the Northwest Heilongjiang Province

Sun Chao1, Gou Jun1, Sun Deyou1,2, Feng Zhao1, Tian Li1   

  1. 1. College of Earth Science, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China
  • Received:2021-03-26 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the National Natural Science Foundation of China (41502045) and the Nuclear Industry 243 Brigade Project of China Nuclear Industry Geological Bureau (202003)

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Abstract: Petrology, geochemistry and U-Pb geochronology of the Great Xing'an Range Tayuan and the Little Xing'an Range Erzhan Country granites in the northwest Heilongjiang Province were undertaken to determine the subduction and collisional processes of the Paleo-Asian Ocean. The Tayuan granites are mainly biotite monzogranites with zircon U-Pb age of 308 Ma, which is a Late Carboniferous intrusion, and they are characterized by high silica and total alkali contents, enrichment in light rare earth elements (LREE) and large ion lithophile elements (LILE), depletion in heavy rare earth elements (HREE) and high field strength elements (HFSE). Zircons from the Tayuan monzogranites have εHf(t) values ranging from 0.8 to 2.5, suggesting that the granitic magmas were generated by partial melting of newly-accreted lower crust. The Erzhan Country granites are dominantly monogranite and alkali-feldspar granite with zircon U-Pb ages of 305 Ma and 293 Ma. They have high silica and total alkali contents, and are characterised by enrichment in LREEs and LILE relative to HREE and HFSE, implying that they were generated by the melting of juvenile continental crust. The Late Carboniferous monogranites belong to I-type granite, and the Early Permian alkali-feldspar granite is typical A-type granite. Zircon δEu ratios can be used to estimate the melting depths of granites:The formation depth of Tayuan monzogranite and Erzhan Country monzogranite is 38.8 km and 34.7 km,respectively,while the alkali-feldspar granite formed at a shallow depth of 28.7 km. The crustal thinning during the Late Carboniferous to Early Permian might record the tectonic transition from subduction to post-collisional extension related to the final closure of the Paleo-Asian Ocean.

Key words: U-Pb geochronology, geochemistry, I-type granite, A-type granite, Paleo-Asian Ocean, the northwest of Heilongjiang Province

CLC Number: 

  • P595
[1] 景妍,张彦龙,王清海,等. 大兴安岭北段龙江地区早白垩世晶洞花岗岩的成因及构造意义[J].世界地质,2019, 38(3):655-667. Jing Yan, Zhang Yanlong, Wang Qinghai,et al. Petrogenesis of Early Cretaceous Miarolitic Monzogranite in Longjiang Region of Northern Great Xing'an Range and Its Tectonic Implications[J]. Global Geology, 2019, 38(3):655-667.
[2] 周传芳,杨华本,李向文,等. 大兴安岭北段新林地区晚石炭世花岗岩的岩石成因及地质意义[J].吉林大学学报(地球科学版),2020, 50(1):97-111. Zhou Chuanfang, Yang Huaben, Li Xiangwen,et al. Petrogenesis of Late Carboniferous Granitic Plutons in Xinlin Area, Northern Great Xing'an Range and Their Geological Significance[J]. Jouanal of Jilin University(Earth Science Edition), 2020,50(1):97-111.
[3] 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 China[J]. Geology in China, 2010, 37(4):943-951.
[4] Liu C, Xu M, Zhou Z, et al. Magmatic History During Late Carboniferous to Early Permian in the North of the Central Xing'an-Mongolia Orogenic Belt:A Case Study of the Houtoumiao Pluton, Inner Mongolia[J]. International Geology Review, 2018, 60(15):1918-1939.
[5] Ge W C, Wu F Y, Zhou C Y, 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 Mts[J]. Chinese Science Bulletin, 2005, 50(18):2097-2105.
[6] 徐备,赵盼,鲍庆中,等. 兴蒙造山带前中生代构造单元划分初探[J]. 岩石学报,2014, 30(7):1841-1857. Xu Bei, Zhao Pan, Bao Qingzhong, et al. Preliminary Study on the Pre-Mesozoic Tectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB)[J]. Acta Petrologica Sinica, 2014, 30(7):1841-1857.
[7] 马永非,刘永江,秦涛, 等. 大兴安岭中段扎赉特旗地区石炭纪花岗岩的岩石成因、构造背景及对增生造山作用的指示[J]. 岩石学报,2018, 34(10):2931-2955. Ma Yongfei, Liu Yongjiang, Qin Tao, et al. Carboniferous Granites in the Jalaid Banner Area, Middle Great Xing'an Range, NE China:Petrogenesis, Tectonic Background and Orogeny Accretionary Implications[J]. Acta Petrologica Sinica, 2018, 34(10):2931-2955.
[8] Feng Z Q, Li W M, Liu Y J, et al. Early Carboniferous Tectonic Evolution of the Northern Heihe-Nenjiang-Hegenshan Suture Zone, NE China:Constraints from the Mylonitized Nenjiang Rhyolites and the Moguqi Gabbros[J]. Geological Journal, 2018, 53(3):1005-1021.
[9] 崔芳华,郑常青,徐学纯,等. 大兴安岭全胜林场地区晚石炭世岩浆活动研究:对兴安地块与松嫩地块拼合时间的限定[J].地质学报,2013, 87(9):1247-1263. Cui Fanghua, Zheng Changqing, Xu Xuechun, et al. Late Carboniferous Magmatic Activities in the Quanshenglinchang Area, Great Xing'an Range:Constrains on the Timing of Amalgamation Between Xing'an and Songnen Massifs[J]. Acta Geologica Sinica, 2013, 87(9):1247-1263.
[10] Li Y, Xu W L, Wang F, et al. Geochronology and Geochemistry of Late Paleozoic Volcanic Rocks on the Western Margin of the Songnen-Zhangguangcai Range Massif, NE China:Implications for the Amalgamation History of the Xing'an and Songnen-Zhangguangcai Range Massifs[J]. Lithos, 2014, 205:394-410.
[11] Dong Y, Ge W C, Zhao Guo C, et al. Petrogenesis and Tectonic Setting of the Late Paleozoic Xing'an Complex in the Northern Great Xing'an Range, NE China:Constraints from Geochronology, Geochemi-stry and Zircon Hf Isotopes[J]. Journal of Asian Earth Sciences, 2016, 115:228-246.
[12] 赵芝. 大兴安岭北部晚古生代岩浆作用及其构造意义[D]. 长春:吉林大学,2011. Zhao Zhi. Late Paleozoic Magmatism and Its Tectonic Significance in Northern Great Xing'an Range, Northeastern China[D]. Changchun:Jilin University, 2011.
[13] Liu Y J, Li W M, Feng Z Q, et al. A Review of the Paleozoic Tectonic in the Eastern Part of Central Asian Orogenic Belt[J]. Gondwana Research, 2017, 43:123-148.
[14] Miao L C, Fan W M, Liu D Y, et al. Geochronology and Geochemistry of the Hegenshan Ophiolitic Complex:Implications for Late-Stage Tectonic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China[J]. Journal of Asian Earth Sciences, 2008, 32(5/6):348-370.
[15] 黄波,付冬,李树才,等. 内蒙古贺根山蛇绿岩形成时代及构造启示[J]. 岩石学报,2016, 32(1):158-176. Huang Bo, Fu Dong, Li Shucai, et al. The Age and Tectonic Implications of the Hegenshan Ophiolite in Inner Mongolia[J]. Acta Petrologica Sinica, 2016, 32(1):158-176.
[16] Jian P, Kr ner A, Windley B F, et al. Carboniferous and Cretaceous Mafic-Ultramafic Massifs in Inner Mongolia (China):A SHRIMP Zircon and Geochemical Study of the Previously Presumed Integral "Hegenshan Ophiolite"[J]. Lithos, 2012, 142/143:48-66.
[17] Zhou J B, Han J, Zhao G C, et al. The Emplacement Time of the Hegenshan Ophiolite:Constraints from the Unconformably Overlying Paleozoic Strata[J]. Tectonophysics, 2015, 662:398-415.
[18] 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(1/2):34-43.
[19] Andersen T. Correction of Common Lead in U-Pb Analyses that do not Report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
[20] Ludwig K R. User's Manual for Isoplot 3.1:A Geolocronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 2003, 4:25-32.
[21] Wu F Y, Yang Y H, Xie L W, et al. Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology[J]. Chemical Geology, 2006, 234(1/2):105-126.
[22] Vervoort J D, Blichert-Toft J. Evolution of the Depleted Mantle:Hf Isotope Evidence from Juvenile Rocks Through Time[J]. Geochimica et Cosmochimica Acta, 1999, 63(3/4):533-556.
[23] Griffin W L, Pearson N J, Belousova E, et al. The Hf Isotope Composition of Cratonic Mantle:LA-MC-ICPMS Analysis of Zircon Megacrysts in Kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1):133-147.
[24] Griffin W L, Wang X, Jackson S E, et al. Zircon Chemistry and Magma Mixing, SE China:In Situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes[J]. Lithos, 2002, 61(3):237-269.
[25] Belousova E A, Griffin W L, O'Reilly S Y, et al. Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-622.
[26] Whalen J B, Currie K L, Chappell B W. A-Type Granites:Geochemical Characteristics[J]. Contributions to Mineralogy and Petrology, 1987, 95:420-436.
[27] Tang M, Ji W Q, Chu X, et al. Reconstructing Crustal Thickness Evolution from Europium Anomalies in Detrital Zircons[J]. Geology, 2020, 49(1):76-80.
[28] Wyllie P J, Wolf M B, van der Laan S R. Conditions for Formation of Lonalites and Trondhjenites:Magmatic Sources and Products[M]. Oxford:Oxford University Press, 1997:256-266.
[29] 张旗,金惟俊,李承东,等. 再论花岗岩按照Sr-Yb的分类:标志[J]. 岩石学报,2010, 26(4):985-1015. Zhang Qi, Jin Weijun, Li Chengdong, et al. Revisiting the New Classification of Granitic Rocks Based on Whole-Rock Sr and Yb Contents:Index[J]. Acta Petrologica Sinica, 2010, 26(4):985-1015.
[30] Feng Z Q, Jia J, Liu Y J, et al. Geochronology and Geochemistry of the Carboniferous Magmatism in the Northern Great Xing'an Range, NE China:Constraints on the Timing of Amalgamation of Xing'an and Songnen Blocks[J]. Journal of Asian Earth Sciences, 2015, 113:411-426.
[31] 赵芝,迟效国,潘世语,等. 小兴安岭西北部石炭纪地层火山岩的锆石LA-ICP-MS U-Pb年代学及其地质意义[J]. 岩石学报,2010, 26(8):2452-2464. Zhao Zhi, Chi Xiaoguo, Pan Shiyu, et al. Zircon U-Pb LA-ICP-MS Dating of Carboniferous Volcanics and Its Geological Significance in the Northwestern Lesser Xing'an Range[J]. Acta Petrologica Sinica, 2010, 26(8):2452-2464
[32] Nozaka T, Liu Y. Petrology of the Hegenshan Ophiolite and Its Implication for the Tectonic Evolution of Northern China[J]. Earth and Planetary Science Letters, 2002, 202(1):89-104.
[33] 张彦龙,葛文春,高妍,等.龙镇地区花岗岩锆石U-Pb年龄和Hf同位素及地质意义[J].岩石学报,2010, 26(4):1059-1073. Zhang Yanlong, Ge Wenchun, Gao Yan, et al. Zircon U-Pb Ages and Hf Isotopes of Granites in Longzhen Area and Their Geological Implications[J]. Acta Petrologica Sinica, 2010, 26(4):1059-1073.
[34] Pearce J A, Harris N B W, Tindle A G. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J]. Journal of Petrology, 1984, 25:956-983.
[35] 孙德有,吴福元,李惠民,等. 小兴安岭西北部造山后A型花岗岩的时代及与索伦山-贺根山-扎赉特碰撞拼合带东延的关系[J]. 科学通报,2000, 20:2217-2222. Sun Deyou, Wu Fuyuan, Li Huimin, et al. The Age of Post-Orogenic A-Type Granites in the Northwest Xiaoxing'an Mountains and Its Relationship with the Eastern Extension of the Suolun-Hegan Mountain-Zalaiite Collision Belt[J]. Chinese Science Bulletin, 2000, 20:2217-2222.
[36] 郭奎城,张文龙,杨晓平,等. 黑河市五道沟地区早二叠世A型花岗岩成因[J].吉林大学学报(地球科学版),2011, 41(4):1077-1083. Guo Kuicheng, Zhang Wenlong, Yang Xiaoping, et al. Origin of Early Permian A-Type Granite in the Wudaogou Area, Heihe City[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(4):1077-1083.
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