摘要出露于小兴安岭西北部的"落马湖岩群"是多宝山矿集区重要的地质建造之一,由于缺少化石及顶底不全,其形成时代一直存在争议,制约了对区域构造演化及成矿背景的认识. 为了探讨其形成时代及古构造背景,采用锆石U-Pb(LA-ICP-MS)方法对卧都河乡附近的"落马湖岩群"变粉砂质泥岩的碎屑锆石进行了年代学研究,85个测点中68个有效测点年龄介于216~2 636 Ma,分为8个年龄组:216~347 Ma (n=8)、430~443 Ma (n=2)、463~502 Ma (加权平均485±5 Ma,n=21)、513~572 Ma (加权平均528±7 Ma,n=16)、596~613 Ma (加权平均606±12 Ma,n=7)、718~739 Ma (加权平均730±12 Ma,n=3)、830~882 Ma (加权平均850±26 Ma,n=5)、1 769~2 636 Ma (n=6),以第Ⅲ-第Ⅶ年龄组构成明显的峰值. 综合分析锆石晶态、CL图像、U含量特征及地质体宏观岩相学特点,认为第Ⅲ年龄组代表样品层位沉积下限. 结合区域研究成果,认为"落马湖岩群"形成于奥陶纪至志留纪罗德洛世;其碎屑锆石主要来源于"额尔古纳-兴安联合地块"及奥陶纪弧火山岩区,形成于弧后盆地构造背景;其与多宝山弧岩浆岩带共同构成早古生代弧-盆系.
Abstract：Due to the lack of fossils and incomplete roof and bottom, the forming age of Luomahu Complex, one of the important geological formations in Duobaoshan ore concentration area, has been controversial, restricting the cognition of regional tectonic evolution and metallogenic background. The geochronology of detrital zircons in meta-silty mudstones from Luomahu Complex near Wuduhe Township are studied by zircon U-Pb LA-ICP-MS dating method to investigate the formation age and paleotectonic setting. Among the 85 survey points, 68 effective ones range in age from 216 to 2 636 Ma and can be divided into eight age groups:216-347 Ma, 430-443 Ma, 463-502 Ma, 513-572 Ma, 596-613 Ma, 718-739 Ma, 830-882 Ma and 1 769-2 636 Ma, with the third to seventh groups forming obvious peak values. Based on the comprehensive analysis of zircon crystalline state, CL image, U content characteristics and macro petrographic features of geological body, it is considered that the third age group represents the maximum sedimentary age of sample layers. Combined with the regional research results, it is concluded that Luomahu Complex was formed in Ordovician-Silurian Ludlovian, with the detrital zircons mainly derived from the Erguna-Xing'an block and Ordovician arc volcanic rocks and formed in the tectonic setting of back-arc basin. The Luomahu Complex, together with Duobaoshan arc magmatic belt, formed the Early Paleozoic arc-basin system.
Şengör 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(6435):299-307.
[2]
张兴洲, 杨宝俊, 吴福元, 等. 中国兴蒙-吉黑地区岩石圈结构基本特征[J]. 中国地质, 2006, 33(4):816-823. Zhang X Z, Yang B J, Wu F Y, et al. The lithosphere structure in the Hingmong-Jihei (Hinggan-Mongolia-Jilin-Heilongjiang) region, northeastern China[J]. Geology in China, 2006, 33(4):816-823.
[3]
张兴洲, 周建波, 迟效国, 等. 东北地区晚古生代构造-沉积特征与油气资源[J]. 吉林大学学报(地球科学版), 2008, 38(5):719-725. Zhang X Z, Zhou J B, Chi X G, et al. Late Paleozoic tectonic- sedimentation and petroleum resources in northeastern China[J]. Journal of Jilin University (Earth Science Edition), 2008, 38(5):719-725.
[4]
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 Y J, Zhang X Z, Jin W, et al. Late Paleozoic tectonic evolution in Northeast China[J]. Geology in China, 2010, 37(4):943-951.
[5]
付俊彧, 朱群, 杨雅军, 等. 中华人民共和国地质图(东北) (1:1500000)说明书[M]. 北京:地质出版社, 2019:105-143. Fu J Y, Zhu Q, Yang Y J, et al. Geological map of the People's Republic of China (Northeast) (1:1500000)[M]. Beijing:Geological Publishing House, 2019:105-143. (in Chinese)
[6]
傅俊彧, 于荣文, 宋亚芹, 等. 黑龙江黑河西北洪业家推覆剪切构造带地质特征及其意义[J]. 地质力学学报, 2005, 11(2):145-152. Fu J Y, Yu R W, Song Y Q, et al. Geological characteristics of the Hongyejia thrust shear zone northwest of Heihe in the Heilongjiang River valley and its significance[J]. Journal of Geomechanics, 2005, 11(2):145-152.
[7]
刘晓佳, 赵立国, 田珺, 等. 漠河逆冲推覆构造活动时代的ESR年龄证据[J]. 地质力学学报, 2014, 20(3):299-303. Liu X J, Zhao L G, Tian J, et al. ESR ages evidences of Mohe overthrust structure stage[J]. Journal of Geomechanics, 2014, 20(3):299-303.
[8]
赵书跃, 郑全波, 韩彦东. 漠河逆冲推覆构造中段地质特征与构造演化[J]. 地质通报, 2016, 35(7):1095-1105. Zhao S Y, Zheng Q B, Han Y D. Geological characteristics and tectonic evolution of the middle segment of Mohe thrust nappe[J]. Geological Bulletin of China, 2016, 35(7):1095-1105.
[9]
韩国卿, 刘永江, Neubauer F, 等. 松辽盆地西缘边界断裂带中北段尼尔基L型构造岩构造年代学及其构造意义[J]. 岩石学报, 2014, 30(7):1922-1934. Han G Q, Liu Y J, Neubauer F, et al. Chronology of L-type tectonite from Nierji area in the northern-middle segment of the western boundary fault of the Songliao Basin and its tectonic implications[J]. Acta Petrologica Sinica, 2014, 30(7):1922-1934.
[10]
郑常青, 李娟, 金巍, 等. 松辽盆地西缘断裂带中花岗质糜棱岩的锆石SHRIMP和云母氩-氩年龄及其构造意义[J]. 吉林大学学报(地球科学版), 2015, 45(2):349-363. Zheng C Q, Li J, Jin W, et al. SHRIMP U-Pb zircon dating and mica laser 40Ar-39Ar ages of the granitic mylonites in ductile fracture belt in the western Songliao Basin and its tectonic implication[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(2):349-363.
[11]
汪岩, 钱程, 马永非, 等. 吉林白城岭下地区花岗质糜棱岩锆石U-Pb年代学与地球化学特征对松辽盆地西缘晚古生代以来的俯冲背景的制约[J]. 地质学报, 2019, 93(1):117-137. Wang Y, Qian C, Ma Y F, et al. Geochronologic and geochemistric evidence of granitic mylonites from Lingxia area of Baicheng City, Jinlin:Constraints on subduction in the western of the Songliao basin since the Late Paleozoic[J]. Acta Geologica Sinica, 2019, 93(1):117-137.
[12]
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, 1993:22-43. Heilongjiang Bureau of Geology and Mineral Resources. Regional geology of Heilongjiang Province[M]. Beijing:Geological Publishing House, 1993:22-43. (in Chinese)
[13]
苗来成, 刘敦一, 张福勤, 等. 大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-Pb年龄[J]. 科学通报, 2007, 52(5):591-601. Miao L C, Liu D Y, Zhang F Q, et al. Zircon SHRIMP U-Pb ages of the "Xinghuadukou Group" in Hanjiayuanzi and Xinlin areas and the "Zhalantun Group" in Inner Mongolia, Da Hinggan Mountains[J]. Chinese Science Bulletin, 2007, 52(8):1112-1124.
[14]
周建波, 张兴洲, Wilde S A, 等. 中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J]. 岩石学报, 2011, 27(4):1235-1245. Zhou J B, Zhang X Z, Wilde S A, et al. Confirming of the Heilongjiang~500 Ma Pan-African khondalite belt and its tectonic implications[J]. Acta Petrologica Sinica, 2011, 27(4):1235-1245.
[15]
Zhou J B, Wilde S A, Zhang X Z, et al. A >1300 km late Pan- African metamorphic belt in NE China:New evidence from the Xing' an block and its tectonic implications[J]. Tectonophysics, 2011, 509(3/4):280-292.
[16]
孙立新, 任邦方, 赵凤清, 等. 内蒙古额尔古纳地块古元古代末期的岩浆记录——来自花岗片麻岩的锆石U-Pb年龄证据[J]. 地质通报, 2013, 32(2/3):341-352. Sun L X, Ren B F, Zhao F Q, et al. Late Paleoproterozoic magmatic records in the Eerguna massif:Evidences from the zircon U-Pb dating of granitic gneisses[J]. Geological Bulletin of China, 2013, 32(2/3):341-352.
[17]
Ge W C, Chen J S, Yang H, et al. Tectonic implications of new zircon U-Pb ages for the Xinghuadukou complex, Erguna massif, northern Great Xing'an Range, NE China[J]. Journal of Asian Earth Sciences, 2015, 106:169-185.
[18]
赵院冬, 许逢明, 车继英, 等. 锆石U-Pb定年对大兴安岭东北部"兴华渡口群"形成时代和组成的约束[J]. 中国地质, 2017, 44(3):575-587. Zhao Y D, Xu F M, Che J Y, et al. Constraints from the zircon U-Pb dating on the formation age and composition of the Xinhuadukou Group in northeastern Da Hinggan Mountains[J]. Geology in China, 2017, 44(3):575-587.
[19]
佘宏全, 李进文, 向安平, 等. 大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J]. 岩石学报, 2012, 28(2):571-594. She H Q, Li J W, Xiang A P, et al. U-Pb ages of the zircons from primary rocks in middle-northern Daxinganling and its implications to geotectonic evolution[J]. Acta Petrologica Sinica, 2012, 28(2):571-594.
[20]
孙巍, 迟效国, 潘世语, 等. 大兴安岭北部新林地区倭勒根群大网子组锆石LA-ICP-MS U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2014, 44(1):176-185. Sun W, Chi X G, Pan S Y, et al. Zircon LA-ICP-MS U-Pb dating and its geological significance of the Dawangzi Formation from Wolegen Group in Xinlin area, northern Great Xing'an Range[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(1):176-185.
[21]
杜兵盈, 冯志强, 刘宇崴, 等. 大兴安岭环二库新元古代变质辉长岩的厘定及其地质意义[J]. 世界地质, 2017, 36(3):751-762. Du B Y, Feng Z Q, Liu Y W, et al. Determination of Neoproterozoic meta-gabbro from Huanerku, Da Hinggan Mountains and its geological significance[J]. Global Geology, 2017, 36(3):751-762.
[22]
表尚虎, 赵海滨, 傅俊彧. 黑龙江黑河变质地层微古植物化石的发现[J]. 中国区域地质, 2000, 19(4):445-447. Biao S H, Zhao H B, Fu J Y. Discovery of microflora fossils in metamorphic strata at Heihe, Heilongjiang[J]. Regional Geology of China, 2000, 19(4):445-447.
[23]
孙巍. 兴安地块"前寒武纪变质岩系"——下古生界锆石年代学研究及其构造意义[D]. 长春:吉林大学, 2014. Sun W. Zircon geochronology constraints on the age and nature of "Precambrian metamorphic rocks"and Lower Paleozoic in the Xing'an block of Northeast China[D]. Changchun:Jilin University, 2014.
[24]
赵院冬, 车继英, 许逢明, 等. 碎屑锆石U-Pb年龄谱系对兴安地块落马湖群原岩形成时代的约束[J]. 地球科学, 2020, 45(2):489-502. Zhao Y D, Che J Y, Xu F M, et al. Constraints on the forming age of the Luomahu Group in the Xing'an block from the detrital zircon population[J]. Earth Science, 2020, 45(2):489-502.
[25]
付俊彧, 那福超, 李仰春, 等. 蒙古-鄂霍茨克洋南向俯冲:小兴安岭西北部落马湖群中三叠世岩浆记录[J]. 地质通报, 2021, 40(6):889-904. Fu J Y, Na F C, Li Y C, et al. Southward subduction of the Mongo- Okhotsk Ocean:middle triassic magmatic records of the "Luomahu Group" in northwest of Lesser Khingan Mountains[J]. Geological Bulletin of China, 2021, 40(6):889-904.
[26]
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. Hou K J, Li Y H, Tian Y R. In situ U-Pb zircon dating using laser ablation-multi ion counting-ICP-MS[J]. Mineral Deposits, 2009, 28(4):481-492.
[27]
Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2):537-571.
[28]
Ludwig K R. ISOPLOT 3.00:A geochronological toolkit for Microsoft Excel[R]. Berkeley:Berkeley Geochronology Center, 2003.
[29]
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. Wu Y B, Zheng Y F. Genesis of zircon and its constraints on interpretation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(15):1554-1569.
[30]
刘敦一, 简平, 张旗, 等. 内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据[J]. 地质学报, 2003, 77(3):317-327. Liu D Y, Jian P, Zhang Q, et al. SHRIMP dating of adakites in the Tulingkai ophiolite, Inner Mongolia:Evidence for the Early Paleozoic subduction[J]. Acta Geologica Sinica, 2003, 77(3):317-327.
[31]
吴元保, 陈道公, 郑永飞, 等. 北大别漫水河混合岩化片麻岩中锆石微区微量元素特征及其地质意义[J]. 岩石学报, 2004, 20(5):1141-1150. Wu Y B, Chen D G, Zheng Y F, et al. Trace element geochemistry of zircons in migmatitic gneiss at Manshuihe, North Dabieshan and its geological implications[J]. Acta Petrologica Sinica, 2004, 20(5):1141-1150.
[32]
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, 1997:15-19. Heilongjiang Geology and Mineral Bureau. Stratigraphy (lithostratic) of Heilongjiang Province[M]. Wuhan:China University of Geosciences Press, 1997:15-19.
[33]
Cawood P A, Hawkesworth C J, Dhuime B. Detrital zircon record and tectonic setting[J]. Geology, 2012, 40(10):875-878.
[34]
Miao L C, Zhang F Q, Zhu M S, et al. Zircon SHRIMP U-Pb dating of metamorphic complexes in the conjunction of the Greater and Lesser Xing'an Ranges, NE China:Timing of formation and metamorphism and tectonic implications[J]. Journal of Asian Earth Sciences, 2015, 114:634-648.
[35]
黄永卫, 刘扬, 王喜臣, 等. 黑龙江北部多宝山矿区奥陶系的岩石特征和构造意义[J]. 地质科学, 2009, 44(1):245-256. Huang Y W, Liu Y, Wang X C, et al. Petrological features and tectonic significance of the Ordovician in Duobaoshan ore district, northern Heilongjiang[J]. Chinese Journal of Geology, 2009, 44(1):245-256.
[36]
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, 45(20):2217-2222. Sun D Y, Wu F Y, Li H M, et al. Emplacement age of the postorogenic A-type granites in northwestern Lesser Xing'an Ranges, and its relationship to the eastward extension of Suolushan-Hegenshan- Zhalaite collisional suture zone[J]. Chinese Science Bulletin, 2001, 46(5):427-432.
[37]
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 Z, Chi X G, Pan S Y, 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.
[38]
唐克东, 邵济安, 李永飞. 松嫩地块及其研究意义[J]. 地学前缘, 2011, 18(3):57-65. Tang K D, Shao J A, Li Y F. Songnen massif and its research significance[J]. Earth Science Frontiers, 2011, 18(3):57-65.
[39]
张兴洲, 乔德武, 迟效国, 等. 东北地区晚古生代构造演化及其石油地质意义[J]. 地质通报, 2011, 30(2/3):205-213. Zhang X Z, Qiao D W, Chi X G, et al. Late-Paleozoic tectonic evolution and oil-gas potentiality in northeastern China[J]. Geological Bulletin of China, 2011, 30(2/3):205-213.
[40]
那福超, 付俊彧, 汪岩, 等. 内蒙古莫力达瓦旗哈达阳绿泥石白云母构造片岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报, 2014, 33(9):1326-1332. Na F C, Fu J Y, Wang Y, et al. LA-ICP-MS zircon U-Pb age of the chlorite-muscovite tectonic schist in Hadayang, Morin Dawa Banner, Inner Mongolia, and its tectonic significance[J]. Geological Bulletin of China, 2014, 33(9):1326-1332.
[41]
汪岩, 付俊彧, 杨帆, 等. 嫩江-黑河构造带收缩与伸展——源自晚古生代花岗岩类的地球化学证据[J]. 吉林大学学报(地球科学版), 2015, 45(2):374-388. Wang Y, Fu J Y, Yang F, et al. Contraction and extension in Nenjiang-Heihe tectonic belt:Evidence from the Late Paleozoic granitoid geochemistry[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(2):374-388.
[42]
付俊彧, 汪岩, 那福超, 等. 内蒙古哈达阳镁铁-超镁铁质岩锆石U-Pb年代学及地球化学特征:对嫩江-黑河地区晚泥盆世俯冲背景的制约[J]. 中国地质, 2015, 42(6):1740-1753. Fu J Y, Wang Y, Na F C, et al. Zircon U-Pb geochronology and geochemistry of the Hadayang maficultramafic rocks in Inner Mongolia:Constraints on the Late Devonian subduction of Nenjiang-Heihe area, Northeast China[J]. Geology in China, 2015, 42(6):1740-1753.
[43]
Zhou Z G, Liu C F, Wang G S, et al. Geochronology, geochemistry and tectonic significance of the Dashizhai ophiolitic mélange belt, southeastern Xing'an-Mongolia orogenic belt[J]. International Journal of Earth Sciences, 2019, 108(1):67-88, doi:10.1007/s00531-018-1642-6.
[44]
刘永江, 冯志强, 蒋立伟, 等. 中国东北地区蛇绿岩[J]. 岩石学报, 2019, 35(10):3017-3047. Liu Y J, Feng Z Q, Jiang L W, et al. Ophiolite in the eastern Central Asian orogenic belt, NE China[J]. Acta Petrologica Sinica, 2019, 35(10):3017-3047.
[45]
邵军, 李永飞, 周永恒, 等. 中国东北额尔古纳地块新太古代岩浆事件——钻孔片麻状二长花岗岩锆石LA-ICP-MS测年证据[J]. 吉林大学学报(地球科学版), 2015, 45(2):364-373. Shao J, Li Y F, Zhou Y H, et al. Neo-Archaean magmatic event in Erguna Massif of Northeast China:Evidence from the zircon LA- ICP-MS dating of the gneissic monzogranite from the drill[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(2):364-373.
[46]
Wu F Y, 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.
[47]
佘宏全, 梁玉伟, 李进文, 等. 内蒙古莫尔道嘎地区早中生代岩浆作用及其地球动力学意义[J]. 吉林大学学报(地球科学版), 2011, 41(6):1831-1864. She H Q, Liang Y W, Li J W, et al. The Early-Mesozoic magmatic activity at Moerdaoga district in Inner Mongolia and its geodynamic implication[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6):1831-1864.
[48]
孙立新, 任邦方, 赵凤清, 等. 额尔古纳地块太平川巨斑状花岗岩的锆石U-Pb年龄和Hf同位素特征[J]. 地学前缘, 2012, 19(5):114-122. Sun L X, Ren B F, Zhao F Q, et al. Zircon U-Pb ages and Hf isotope characteristics of Taipingchuan large porphy-ritic granite pluton of Erguna massif in the Great Xing'an Range[J]. Earth Science Frontiers, 2012, 19(5):114-122.
[49]
Tang J, Xu W L, Wang F, et al. Geochronology and geochemistry of Neoproterozoic magmatism in the Erguna massif, NE China:Petrogenesis and implications for the breakup of the Rodinia supercontinent[J]. Precambrian Research, 2013, 224:597-611.
[50]
张丽, 刘永江, 李伟民, 等. 关于额尔古纳地块基底性质和东界的讨论[J]. 地质科学, 2013, 48(1):227-244. Zhang L, Liu Y J, Li W M, et al. Discussion on the basement properties and east boundary of the Ergun massif[J]. Chinese Journal of Geology, 2013, 48(1):227-244.
[51]
Gou J, Sun D Y, Ren Y S, et al. Petrogenesis and geodynamic setting of Neoproterozoic and Late Paleozoic magmatism in the Manzhouli-Erguna area of Inner Mongolia, China:Geochronological, geochemical and Hf isotopic evidence[J]. Journal of Asian Earth Sciences, 2013, 67-68:114-137.
[52]
郭宇飞, 杨言辰, 韩世炯, 等. 大兴安岭北部凤凰山地区英云闪长岩地球化学特征与锆石U-Pb定年[J]. 吉林大学学报(地球科学版), 2016, 46(5):1406-1417.Guo Y F, Yang Y C, Han S J, et al. Geochemistry and Zircon U-Pbdating of the Tonalite from Fenghuangshan area in northern Daxing'anling[J]. Journal of Jilin University (Earth Science Edition), 2016,46(5):1406-1417.
[53]
赵硕, 许文良, 唐杰, 等. 额尔古纳地块新元古代岩浆作用与微陆块构造属性:来自侵入岩锆石U-Pb年代学、地球化学和Hf同位素的制约[J]. 地球科学, 2016, 41(11):1803-1829.Zhao S, Xu W L, Tang J, et al. Neoproterozoic magmatic events andtectonic attribution of the Erguna massif:Constraints fromgeochronological, geochemical and Hf isotopic data of intrusive rocks[J]. Earth Science, 2016, 41(11):1803-1829.
[54]
赵硕, 张进, 李锦轶, 等. 额尔古纳地块新元古代花岗岩榍石原位微区LA-ICP-MS U-Pb定年及其地质意义[J]. 地质学报, 2020,94(3):757-767.Zhao S, Zhang J, Li J Y, et al. Titanite LA-ICP-MS U-Pb dating ofthe Neoproterozoic granites in the Erguna massif and their geologicalsignificance[J]. Acta Geologica Sinica, 2020, 94(3):757-767.
[55]
杨华本, 刘玉, 郑吉林, 等. 额尔古纳地块玻乌勒山地区新元古代斜长角闪岩-片麻状花岗岩的成因及其地质意义[J]. 地质通报,2017, 36(2/3):343-356.Yang H B, Liu Y, Zheng J L, et al. Petrogenesis and geologicalsignificance of Neoproterozoic amphibolite and granite in Bowuleshanarea, Erguna massif, Northeast China[J]. Geological Bulletin ofChina, 2017, 36(2/3):342-356.
[56]
葛文春, 吴福元, 周长勇, 等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J]. 科学通报, 2005, 50(12):1239-1247.Ge W C, Wu F Y, Zhou C Y, et al. Emplacement age of the Tahegranite and its constraints on the tectonic nature of the Ergun block inthe northern part of the Da Hinggan Range[J]. Chinese ScienceBulletin, 2005, 50(18):2097-2105.
[57]
葛文春, 隋振民, 吴福元, 等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J]. 岩石学报, 2007, 23(2):423-440.Ge W C, Sui Z M, Wu F Y, et al. Zircon U-Pb ages, Hf isotopiccharacteristics and their implications of the Early Paleozoic granites inthe northeastern Da Hinggan Mts., northeastern China[J]. Acta PetrologicaSinica, 2007, 23(2):423-440.
[58]
武广, 孙丰月, 赵财胜, 等. 额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义[J]. 科学通报, 2005, 50(20):2278-2288.Wu G, Sun F Y, Zhao C S, et al. Discovery of the Early Paleozoicpost-collisional granites in northern margin of the Erguna massif andits geological significance[J]. Chinese Science Bulletin, 2005, 50(23):2733-2743.
[59]
崔根, 王金益, 张景仙, 等. 黑龙江多宝山花岗闪长岩的锆石SHRIMP U-Pb年龄及其地质意义[J]. 世界地质, 2008, 27(4):387-394.Cui G, Wang J Y, Zhang J X, et al. U-Pb SHRIMP dating of zirconsfrom Duobaoshan granodiorite in Heilongjiang and its geologicalsignificance[J]. Global Geology, 2008, 27(4):387-394.
[60]
赵焕利, 朱春艳, 刘海洋, 等. 黑龙江多宝山铜矿床中花岗闪长岩锆石SHRIMP U-Pb测年及其构造意义[J]. 地质与资源, 2012, 21(5):421-424.Zhao H L, Zhu C Y, Liu H Y, et al. Zircon SHRIMP U-Pb datingand its tectonic implications of the granodiorite in Duobaoshan copperdeposit, Heilongjiang Province[J]. Geology and Resources, 2012, 21(5):421-424.
[61]
向安平, 杨郧城, 李贵涛, 等. 黑龙江多宝山斑岩Cu-Mo矿床成岩成矿时代研究[J]. 矿床地质, 2012, 31(6):1237-1248.Xiang A P, Yang Y C, Li G T, et al. Diagenetic and metallogenicages of Duobaoshan porphyry Cu-Mo deposit in Heilongjiang Province[J]. Mineral Deposits, 2012, 37(6):1237-1248.
[62]
刘军, 周振华, 何哲峰, 等. 黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征[J]. 矿床地质, 2015, 34(2):289-308.Liu J, Zhou Z H, He Z F, et al. Zircon U-Pb dating and geochemistryof ore-bearing tonalite in Tongshan copper deposit, HeilongjiangProvince[J]. Mineral Deposits, 2015, 34(2):289-308.
[63]
杨永胜, 吕新彪, 高荣臻, 等. 黑龙江争光金矿床英云闪长斑岩年代学、地球化学及地质意义[J]. 大地构造与成矿学, 2016, 40(4):674-700.Yang Y S, Lü X B, Gao R Z, et al. Geochronology, geochemistryand geological significance of the tonalite porphyry in Zhengguanggold deposit, Heilongjiang Province[J]. Geotectonica et Metallogenia,2016, 40(4):674-700.
[64]
Zhao C, Qin K Z, Song G X, et al. Early Palaeozoic high-Mg basalt-andesite suite in the Duobaoshan porphyry Cu deposit, NE China:Constraints on petrogenesis, mineralization, and tectonic setting[J].Gondwana Research, 2019, 71:91-116.
[65]
付艳丽, 杨言辰. 黑龙江省争光金矿床成因及找矿标志[J]. 黄金,2010, 31(6):13-18.Fu Y L, Yang Y C. Deposit genesis and prospecting criteria ofZhengguang gold deposit, Heilongjiang[J]. Gold, 2010, 31(6):13-18.
[66]
赵忠海, 郑卫政, 曲晖, 等. 黑龙江多宝山地区铜金成矿作用及成矿规律[J]. 矿床地质, 2012, 31(3):601-614.Zhao Z H, Zheng W Z, Qu H, et al. Cu-Au mineralization andmetallogenic regularity of Duobaoshan area, Heilongjiang Province[J]. Mineral Deposits, 2012, 31(3):601-614.
[67]
Hao Y J, Ren Y S, Duan M X, et al. Metallogenic events and tectonic setting of the Duobaoshan ore field in Heilongjiang Province, NE China[J]. Journal of Asian Earth Sciences, 2015, 97:442-458.
[68]
朱群, 李之彤. 大兴安岭古利库金矿区落马湖岩群变质岩系及其含矿性[J]. 地质与资源, 2001, 10(4):204-209. Zhu Q, Li Z T. The metamorphic rocks of Luomahu Group and its ore potentiality in Guliku gold field, Daxinganling Ridge[J]. Geology and Resources, 2001, 10(4):204-209.
[69]
李春诚, 吕新彪, 高荣臻, 等. 大兴安岭北段古利库金(银)矿床地质特征及成因分析[J]. 矿床地质, 2014, 33(S1):523-524. Li C C, Lv X B, Gao R Z, et al. Geological characteristics and genetic analysis of Guli Kui Gold (Ag) deposit in the northern Da Hinggan Mountains[J]. Mineral Deposits, 2014, 33(S1):523-524. (in Chinese)
[70]
刘宝山, 王少轶, 牛延宏, 等. 黑龙江黑河大新屯金矿区地质特征及成因机理初探[J]. 黄金, 2013, 34(11):16-19. Liu B S, Wang S Y, Niu Y H, et al. Geological characteristics and genetic mechanism of the Daxintun gold deposit in Heihe, Heilongjiang Province[J]. Gold, 2013, 34(11):16-19.
[71]
刘宝山, 李成禄. 黑河地区北宽河组地层含矿性地球化学评价——以黑河大新屯金锑矿区为例[J]. 地质调查与研究, 2016, 39(4):273-278. Liu B S, Li C L. Geochemical evaluation for ore potentiality of the Beikuanhe formation in Heihe area:A case study of the Daxintun gold deposit in Heihe[J]. Geological Survey and Research, 2016, 39(4):273-278.
2023, Vol. 32 
辽公网安备 21010502000112号