Zircon U-Pb age and geochemistry of the stratotype section of the Meiletu Formation in middle southern Da Hinggan Mountains and its geological significance

YANG Haixing; GAO Lidong; GAO Yushi; SUI Haitao; ZHAO Zhifei; LÜ Jing; ZHANG Weiyu; ZHAO Shengjin; LIU Zhihui; ZHOU Yingshuai

2019 Vol. 38, No. 5

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YANG Haixing, GAO Lidong, GAO Yushi, SUI Haitao, ZHAO Zhifei, LÜ Jing, ZHANG Weiyu, ZHAO Shengjin, LIU Zhihui, ZHOU Yingshuai. 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.

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YANG Haixing, GAO Lidong, GAO Yushi, SUI Haitao, ZHAO Zhifei, LÜ Jing, ZHANG Weiyu, ZHAO Shengjin, LIU Zhihui, ZHOU Yingshuai. 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.

Zircon U-Pb age and geochemistry of the stratotype section of the Meiletu Formation in middle southern Da Hinggan Mountains and its geological significance

1.
Inner Mongolia tenth geological mineral exploration and development Co., Ltd., Chifeng 024005, Innner Mongolia, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 11 May 2018

Revised Date: 15 June 2018

Publish Date: 15 May 2019

Abstract

Abstract

The Meiletu Formation is the highest strata volcanic rocks in Mesozoic in the southern central part of the Da Hinggan Mountains. The study of the layer section is of great significance for the division and regional correlation. In this paper, the authors carried out the study of the chronology and geochemistry of the Meiletu Formation layer section volcanic rocks, analyzed zircon UPb isotope dating for 4 pieces of andesite samples by using LA-ICP-MS technique, and yielded the ages of 127.7 ±1.4~133.4 ±1.5Ma, suggesting Early Cretaceous. A comparison with the similar volcanic rocks in China shows that the Meiletu Formation volcanic rocks have high content of SiO₂(57.95%~64.25%), TiO₂(0.69%~1.25%) and K₂O(0.55%~4.97%), low content of Fe₂O₃ (2.03%~4.32%), FeO(1.05%~3.77%), MgO(0.52%~2.44%) and CaO(2.22%~6.07%), and consistent MnO(0.05%~1.00%), Al₂O₃ (14.97%~17.61%)and Na₂O(2.61%~4.16%)content, suggesting aluminous-over-aluminous rock of high potassium Ca-alkali series. Lower rare earth (ΣREE) values are between 133.43×10^-6 and 181.7×10^-6, and there exists obvious regional difference in light and heavy rare earth elements(LREE/HREE=7.51~8.14, (La/Yb)_N=7.75~8.78), showing strong fractionation between the light rare earth and the heavy rare earth, with negative EU anomaly(δEu=0.78~0.95). The rocks are enriched in large ion lithophile elements (Rb, Ba, K, Pb, Sr) and LREE and depleted in high field-strength elements (Nb. Ta, Ti and P) and HREE. Magma came for the transitional mantle. The rocks were formed in a continental edge arc environment, and were related to the continental extension after the Pacific Plate subduction.
- Meiletu Formation /
- volcanic rocks /
- zircon U-Pb age /
- petrogeochemistry /
- stratotype section

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References

[1]	李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论评, 1998, 44(4):339-347. doi: 10.3321/j.issn:0371-5736.1998.04.002 CrossRef Google Scholar
[2]	吴福元, 曹林.东北亚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
[3]	刘兵.大兴安岭地区晚古生代构造演化研究[D].吉林大学博士学位论文, 2014. Google Scholar
[4]	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. Google Scholar
[5]	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
[6]	秦涛, 郑常青, 崔天日, 等.内蒙古扎兰屯地区白音高老组火山岩地球化学、年代学及其地质意义[J].地质与资源, 2014, 23(2):146-153. doi: 10.3969/j.issn.1671-1947.2014.02.011 CrossRef Google Scholar
[7]	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. doi: 10.3969/j.issn.1671-1947.2009.04.001 CrossRef Google Scholar
[8]	孙德有, 许文良, 周燕.大兴安岭地区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
[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):129-139. Google Scholar
[10]	Shao J A, Zang S X, Mou B L. Extensional tectonics and asthenospheric upwelling in the orogenic belt:a case study from Hinggan-Mongolia Orogenic belt[J]. Chin. Sci. Bull., 1994.39(6):533-537. Google Scholar
[11]	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):396-407. Google Scholar
[12]	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].地球科学, 2000, 25(2):172-178. Google Scholar
[13]	邵济安, 刘福田, 陈辉, 等.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J].地质学报, 2001, 75:56-63. doi: 10.3321/j.issn:0001-5717.2001.01.006 CrossRef Google Scholar
[14]	林强, 葛文春, 曹林, 等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学, 2003, 32(3):208-222. doi: 10.3321/j.issn:0379-1726.2003.03.002 CrossRef Google Scholar
[15]	谢鸣谦.拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M].北京:科学出版社, 2000. Google Scholar
[16]	Meng Q R. What drove Late Mesozoic extension of the northern China-Mongolia tract[J]. Tectonophysics, 2003, 369:155-174. doi: 10.1016/S0040-1951(03)00195-1 CrossRef Google Scholar
[17]	Fan W M, Guo F, Wang Y J, et al. Late Mesozoic calc -alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains, northeastern China[J]. Journal of Volcanology and Geothermal Research, 2003, 121:115-135. doi: 10.1016/S0377-0273(02)00415-8 CrossRef Google Scholar
[18]	高晓峰, 郭锋, 范蔚茗, 等.南兴安岭晚中生代中酸性火山岩的岩石成因[J].岩石学报, 2005, 21(3):734-748. Google Scholar
[19]	Wang P J, Chen F K, Shen S M, et al. Geochemical and Nd-SrPb 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]	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
[21]	苟军, 孙德有, 赵忠华, 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
[22]	赵国龙, 杨桂林, 傅嘉有, 等.大兴安岭中南部中生代火山岩[M].北京:科学技术出版社, 1989:1-252. Google Scholar
[23]	刘俊杰, 鞠文信, 赵九峰, 等.大兴安岭根河岩区晚侏罗世火山岩特征及构造环境探讨[J].华南地质与矿产, 2006, 22(1):38-47. doi: 10.3969/j.issn.1007-3701.2006.01.007 CrossRef Google Scholar
[24]	Wang F, Zhou X H, Zhang L C, et al.Late Mesozoic volcanis, in the Great Xing'an Range (NE China):Timing and implications for the dynamic setting of NE Asia[J]. Earth and Planetary Science Letters, 2006, 251:179-198. doi: 10.1016/j.epsl.2006.09.007 CrossRef Google Scholar
[25]	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
[26]	Zhang, L C, Zhou, X H, Ying, J F, et al.Geochemistry and SrNd-Pb-Hf isotopes of Early Cretaceous basalts from the Great Xinggan Range, NE China:Implications for their origin and mantle source characteristics[J].Chem. Geol., 2008, 256:12-23. doi: 10.1016/j.chemgeo.2008.07.004 CrossRef Google Scholar
[27]	吴华英, 张连昌, 周新华, 等.大兴安岭中段晚中生代安山岩年代学和地球化学特征及成因分析[J].岩石学报, 2008, 24(6):1339-1352. Google Scholar
[28]	张吉衡.大兴安岭中生代火山岩年代学及地球化学研究[D].吉林大学博士学位论文, 2009. Google Scholar
[29]	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
[30]	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, 276:144-165. doi: 10.1016/j.chemgeo.2010.05.013 CrossRef Google Scholar
[31]	聂立军, 贾海明, 王聪, 等.大兴安岭中段白音高老组流纹岩年代学、地球化学及其地质意义[J].世界地质, 2015, 34(2):296-304. doi: 10.3969/j.issn.1004-5589.2015.02.004 CrossRef Google Scholar
[32]	谭皓元, 和钟铧, 陈飞, 等.大兴安岭中段索伦地区白音高老组火山岩锆石U-Pb年龄、地球化学特征及构造意义[J].世界地质, 2017, 36(5):893-908. Google Scholar
[33]	杜岳丹, 和钟铧, 隋振民, 等.大兴安岭中段索伦地区玛尼吐组火山岩年代学、地球化学及其构造背景[J].世界地质, 2017, 36(2):346-360. doi: 10.3969/j.issn.1004-5589.2017.02.003 CrossRef Google Scholar
[34]	苟军, 孙德有, 赵忠华, 等.满洲里南部白音高老组流纹岩锆石U-Pb定年及岩石成因[J].岩石学报, 2010, 26(1):333-344. Google Scholar
[35]	杨文静, 程天赦, 王登红, 等.内蒙古色日崩地区白音高老组流纹岩岩石地球化学特征及地质意义[J].地质与资源, 2013, 22(2):30-35. Google Scholar
[36]	Dong Y, Ge W C, Yang H, et al. Geochronology and geochemistry of Early Cretaceous volcanic rocks from the Baiyingaolao Formation in the central Great Xing'an Range, NE China, and its tectonic implications[J].Lithos, 2014, 205:68-184. Google Scholar
[37]	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. Google Scholar
[38]	张乐彤, 李世超, 赵庆英, 等.大兴安岭中段白音高老组火山岩的形成时代及地球化学特征[J].世界地质, 2015, 34(1):44-54. doi: 10.3969/j.issn.1004-5589.2015.01.006 CrossRef Google Scholar
[39]	聂立军, 贾海明, 王聪, 等.大兴安岭中段白音高老组流纹岩年代学、地球化学及其地质意义[J].世界地质, 2015, 34(2):296-304. doi: 10.3969/j.issn.1004-5589.2015.02.004 CrossRef Google Scholar
[40]	孟宪锋, 张正平, 徐翠, 等.内蒙古东北部东乌珠穆沁旗乌兰哈德一带晚侏罗世满克头鄂博组的地质特征及岩性段划分[J].地质通报, 2010, 29(11):1649-1654. doi: 10.3969/j.issn.1671-2552.2010.11.007 CrossRef Google Scholar
[41]	张超, 杨伟红, 和钟铧, 等.大兴安岭中南段塔尔气地区满克头鄂博组流纹岩年代学和地球化学研究[J].世界地质, 2014, 33(2):255-265. doi: 10.3969/j.issn.1004-5589.2014.02.002 CrossRef Google Scholar
[42]	Zhang C, Yang W H, He Z H, et al. Chronology and geochemistry of rhyolites in Manketou'ebo Formation from Ta'erqi area, southerncentral Greater Xing'an Range[J].Global Geology, 2014, 33(2):255-265. Google Scholar
[43]	Ji Z, Ge W C, Wang Q H, et al. Petrogenesis of Early Cretaceous volcanic rocks of the Manketouebo Formation in the Wuchagou region, central Great Xing'an Range, NE China, and tectonic implications:geochronological, geochemical, and Hf isotopic evidence[J]. International Geology Review, 2015, 58(5):1-18. Google Scholar
[44]	王刚, 孙国胜, 张超, 等.内蒙古敖汉旗晚侏罗世满克头鄂博组火山岩地球化学特征及构造背景分析[J].世界地质, 2015, 34(2):354-361. doi: 10.3969/j.issn.1004-5589.2015.02.010 CrossRef Google Scholar
[45]	李鹏川, 李世超, 刘正宏.内蒙古林西地区满克头鄂博组火山岩形成时代及构造环境[J].世界地质, 2016, 35(1):77-88. doi: 10.3969/j.issn.1004-5589.2016.01.008 CrossRef Google Scholar
[46]	李尚启, 李俊涛, 朱小平.大兴安岭中南段塔尔气地区满克头鄂博组火山岩地球化学特征及地质意义[J].地质与资源, 2017, 26(6):534-541. doi: 10.3969/j.issn.1671-1947.2017.06.002 CrossRef Google Scholar
[47]	纪政.大兴安岭中段五岔沟地区满克头鄂博组火山岩的成因及其构造意义[D].吉林大学硕士学位论文, 2017. Google Scholar
[48]	李永飞, 郜晓勇, 孙守亮.大兴安岭中段突泉盆地玛尼吐组火山岩地球化学特征与⁴⁰Ar/³⁹Ar测年[J].地质与资源, 2013, 22(6):444-451. doi: 10.3969/j.issn.1671-1947.2013.06.002 CrossRef Google Scholar
[49]	李世超, 徐仲元, 刘正宏, 等.大兴安岭中段玛尼吐组火山岩LAICP-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. Google Scholar
[50]	陶传忠, 李伫民, 王大千, 等.乌兰浩特地区玛尼吐组火山岩LAICP-MS锆石U-Pb定年及地球化学特征[J].地质与资源, 2015, 24(2):102-109. doi: 10.3969/j.issn.1671-1947.2015.02.004 CrossRef Google Scholar
[51]	司秋亮, 崔天日, 唐振, 等.大兴安岭中段柴河地区玛尼吐组火山岩年代学、地球化学及岩石成因[J].吉林大学学报(地球科学版), 2015, 45(2):389-403. Google Scholar
[52]	陶楠, 宋维民, 杨佳林, 等.大兴安岭中段突泉盆地玛尼吐组火山岩地球化学特征及成因[J].地质与资源, 2016, 25(6):520-524. doi: 10.3969/j.issn.1671-1947.2016.06.002 CrossRef Google Scholar
[53]	张力强, 陈彪, 曹元宝, 等.内蒙古科尔沁右翼前旗玛尼吐组火山岩年代学及岩石地球化学特征[J].现代矿业, 2017, 3(3):16-20. Google Scholar
[54]	金玲, 杨伟红, 杨德明, 等.内蒙古科右中旗地区梅勒图组安山岩年代学特征及其地质意义[J].世界地质, 2014, 33(1):48-58. Google Scholar
[55]	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):351-372. doi: 10.3969/j.issn.1671-2552.1999.04.003 CrossRef Google Scholar
[56]	张吉衡.大兴安岭中生代火山岩年代学的年代学格架[D].吉林大学硕士学位论文, 2006. Google Scholar
[57]	邢光福.中国东部中新生代陆缘弧盆系大地构造图说明书(1:2500000)[M].北京:地质出版社, 2016. Google Scholar
[58]	内蒙古自治区地矿局.内蒙古自治区岩石地层[M].武汉:中国地质大学出版社, 1996. Google Scholar
[59]	范晨子, 胡明月, 赵令浩, 等.锆石铀-铅定年激光剥蚀-电感耦合等离子体质谱原位微区分析进展[J].岩矿测试, 2012, 31(1):29-46. doi: 10.3969/j.issn.0254-5357.2012.01.004 CrossRef Google Scholar
[60]	侯可军, 李延河, 田有荣. LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J].矿床地质, 2009, 28(4):481-492 doi: 10.3969/j.issn.0258-7106.2009.04.010 CrossRef Google Scholar
[61]	吴元保, 郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报, 2004, 49(16):1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002 CrossRef Google Scholar
[62]	章森桂, 张允白, 严惠君.《中国地层表》(2014)正式使用[J].地层学杂志, 2015, 39(4):359-366. Google Scholar
[63]	迟清华, 鄢明才.应用地球化学元素丰度手册[M].北京:地质出版社, 2007:1-148. Google Scholar
[64]	LeMaitre R W, Bateman P, Dudek A, et al. A classification of igneous rock and glossary of terms[M]. Oxford:Blackwell, 1989. Google Scholar
[65]	Middlemost E A K. A simple classification of volcanic rocks[J]. Bulletin Volcanologique, 1972, 36(2):382-397. doi: 10.1007/BF02596878 CrossRef Google Scholar
[66]	Peccerillo R, Taylor S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions Mineralogy Petrology, 1976, 58:63-81. doi: 10.1007/BF00384745 CrossRef Google Scholar
[67]	Middlemost E A K. Magmas and Magmatic Rocks:An Introduction to Igneous Petrology[M]. London:Longman, 1986:1-26. Google Scholar
[68]	Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes[C]//Saunders A D, Norry M J. Magmatism in the Ocean Basins. Geological Society London Special Publications, 1989, 42: 313-345. Google Scholar
[69]	欧阳京, 汪双双, 于漫, 等.岛弧环境中不同成因的火成岩组合及其地质意义[J].甘肃地质, 2010, 19(2):18-26. Google Scholar
[70]	赵振华.关于岩石微量元素构造环境判别图解使用的有关问题[J].大地构造与成矿学, 2007, 31(1):92-103. doi: 10.3969/j.issn.1001-1552.2007.01.011 CrossRef Google Scholar
[71]	唐勇举.内蒙古乌兰浩特地区早白垩世侵入岩的岩石学、岩石地球化学特征及地质意义[D].中国地质大学(北京)硕士学位论文, 2014. Google Scholar
[72]	杨奇荻, 郭磊, 王涛, 等.大兴安岭中南段甘珠尔庙地区晚中生代两期花岗岩的时代、成因、物源及其构造背景[J].岩石学报, 2014, 30(7):1961-1981. Google Scholar
[73]	葛文春, 吴福元, 周长勇, 等.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J].岩石学报, 2005, 21(3):749-762. Google Scholar
[74]	陈会军, 张彦龙, 王清海, 等.大兴安岭中段早白垩世花岗质岩石锆石U-Pb年龄及地球化学特征[J].地质与资源, 2015, 24(5):433-443. doi: 10.3969/j.issn.1671-1947.2015.05.008 CrossRef Google Scholar
[75]	胡享生, 莫宣学, 范例.西藏江达古沟-弧-盆体系的火山岩石学与地质学标志[C]//地质矿产部青藏高原地质文集编委会.青藏高原地质文集.北京: 地质出版社, 1990: 1-15. Google Scholar
[76]	Defant M J, Drurnmond M S. Derivation of some modern arcmagmas bymelting of young subducted lithosphere[J]. Natrue, 1990, 347:662-665. doi: 10.1038/347662a0 CrossRef Google Scholar
[77]	Pearce J A. Trace element characteristics of lavas from destructive plate boundaries[C]//Thorps R S. Andesites. New York: JohnWiley and Sons, 1982: 525-548. Google Scholar
[78]	汪云亮, 张成江, 修淑芝.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J].岩石学报, 2001, 17(3):413-421. Google Scholar
[79]	Bailey J C. Geochemical criteria for a refined tectonic discrimination of orogenic andesites[J]. Chemical Geology, 1981, 32(1):139-154. Google Scholar
[80]	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慢相互作用[J].岩石学报, 2001, 17(2):227-235. Google Scholar
[81]	张艳斌, 吴福元, 翟明国, 等.和龙地块的构造属性与华北地台北缘东段边界[J].中国科学:地球科学, 2004, 34(9):795-806. Google Scholar
[82]	邵济安, 张履桥.大兴安岭中生代伸展造山过程中的岩浆作用[J].地学前缘, 1999, 6(4):339-346. doi: 10.3321/j.issn:1005-2321.1999.04.017 CrossRef Google Scholar
[83]	Talwani M, Pitman Ⅲ W C. Island arcs, deep sea trench and backarc basins[M]. Washington, D C:American Geophysical Union, 1977:1-470. Google Scholar
[84]	Hilde T W C, Uyeda S, Kroenke L. Evolution of the western Pacific and its margin[J]. Tectonophysics, 1977, 38:145-165. doi: 10.1016/0040-1951(77)90205-0 CrossRef Google Scholar
[85]	Maruyama S. Pacific-type orogeny revisited:Miyashirotype orogeny proposed[J]. Island Arc, 1997, 6:91-120. doi: 10.1111/iar.1997.6.issue-1 CrossRef Google Scholar
[86]	Fukao Y, Obayashi M, Inoue H, et al. Subducting slabs stagnant in the mantle transition zone[J]. Journal of Geophysical Research:Solid Earth, 1992, 97:4809-4822. doi: 10.1029/91JB02749 CrossRef Google Scholar
[87]	张履桥, 邵济安, 郑广瑞.内蒙古甘珠尔庙变质核杂岩[J].地质学报, 1998, 33:140-146. Google Scholar
[88]	张晓东, 余青, 陈发景, 等.松辽盆地变质核杂岩和伸展断陷的构造特正及成因[J].地学前缘, 2000, 7:411-419. Google Scholar
[89]	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. doi: 10.1016/j.jseaes.2013.04.003 CrossRef Google Scholar