辽东古元古代热液铀矿床形成的大地构造背景
|
摘要
辽东半岛是胶-辽-吉古元古代造山带的一部分,经历了古元古代早期裂谷作用和古元古代末期碰撞造山过程。裂谷阶段形成了A型花岗岩(2.09~2.18 Ga)、辽河群沉积(2.05~1.93 Ga)。1.90~1.93 Ga期间裂谷闭合碰撞造山,辽河群遭受强烈变形、变质。1.83~1.90 Ga造山带构造折返,伴随垮塌、软流圈地幔上涌,发生区域退变质作用,形成造山后环斑花岗岩、斑状花岗岩、碱性正长岩和花岗伟晶岩。1.83 Ga辉绿岩的出现标志地壳进入伸展张裂阶段。尽管辽东地区古元古代铀矿化的类型多样,包括单铀型(3075铀矿床、410铀矿床)、铁-铀型(405铀矿床)、铁-硼-铀型(翁泉沟含铀铁硼矿床),但是铀的成矿时代一致,集中在1.83~1.90Ga。辽东地区古元古代末期的铀成矿作用形成于太古宙龙岗地块与狼林地块碰撞造山之后的伸展环境,可能与碰撞造山晚期俯冲陆块的构造折返和/或造山带垮塌及软流圈地幔上涌加热下地壳有关。
As part of the Paleoproterozoic Jiao-Liao-Ji orogenic belt, the eastern Liaoning peninsula underwent rifting in the early Paleoproterozoic and collisional orogenesis in the late Paleoproterozoic. The A-type granitoids(2.09 to 2.18 Ga) and Liaohe Group(2.05 to 1.93 Ga) were formed in the rifting process. The rift was closed due to collisional oogenesis at 1.90 to 1.93 Ga which led to the extensive deformation and metamorphism of the Liaohe Group. During 1.83 to 1.90 Ga, exhumation took place as a consequence of orogenic collapse and subsequent upwelling of asthenospheric mantle which is marked by the regional retrograde metamorphism, intrusion of post-orogenic rapakivi granites, porphyritic granites, alkaline syenites and granitic pegmatites. The ~1.83 Ga diabase dykes indicated a regional crustal extension. The types of uranium mineralization in the eastern Liaoning peninsula are diverse, including single U, Fe-U, Fe-B-U mineralization, however, they are coeval with ages of 1.83 to 1.90 Ga. Therefore, the regional uranium mineralization in the eastern Liaoning peninsula of the Paleoproterozoic Jiao-Liao-Ji orogenic belt was formed in post orogenic extensional setting following the collision between the Archean Longgang and Langlin blocks.
As part of the Paleoproterozoic Jiao-Liao-Ji orogenic belt, the eastern Liaoning peninsula underwent rifting in the early Paleoproterozoic and collisional orogenesis in the late Paleoproterozoic. The A-type granitoids(2.09 to 2.18 Ga) and Liaohe Group(2.05 to 1.93 Ga) were formed in the rifting process. The rift was closed due to collisional oogenesis at 1.90 to 1.93 Ga which led to the extensive deformation and metamorphism of the Liaohe Group. During 1.83 to 1.90 Ga, exhumation took place as a consequence of orogenic collapse and subsequent upwelling of asthenospheric mantle which is marked by the regional retrograde metamorphism, intrusion of post-orogenic rapakivi granites, porphyritic granites, alkaline syenites and granitic pegmatites. The ~1.83 Ga diabase dykes indicated a regional crustal extension. The types of uranium mineralization in the eastern Liaoning peninsula are diverse, including single U, Fe-U, Fe-B-U mineralization, however, they are coeval with ages of 1.83 to 1.90 Ga. Therefore, the regional uranium mineralization in the eastern Liaoning peninsula of the Paleoproterozoic Jiao-Liao-Ji orogenic belt was formed in post orogenic extensional setting following the collision between the Archean Longgang and Langlin blocks.
引文
蔡剑辉,阎国翰,牟保磊,许保良,邵宏翔,许荣华.2002.辽宁盖县梁屯?矿洞沟碱性正长岩杂岩体的U-Pb和Sm-Nd年龄及其地质意义.岩石学报,18(3):349-354.
陈树良,郇彦清,邴志波.2001.辽东地区古元古代侵入岩特征及构造岩浆大陆动力学演化.辽宁地质,18(1):43-50.
陈衍景.2013.大陆碰撞成矿理论的创建及应用.岩石学报,29(1):1-17.
陈衍景,翟明国,蒋少涌.2009.华北大陆边缘造山过程与成矿研究的重要进展和问题.岩石学报,25(11):2695-2726.
邓军,葛良胜,杨立强.2013.构造动力体制与复合造山作用--兼论三江复合造山带时空演化.岩石学报,29(4):1099-1114.
葛良胜,邓军,王长明.2012.构造动力体制与成矿环境及成矿作用--以三江复合造山带为例.岩石学报,29(4):1115-1128.
郭春影,李子颖,韩军,徐浩,白芸,任忠宝,韩愉,赵宇霆.2017.辽东大石桥组蛇纹石化大理岩中铀矿化特征及形成时代.地质通报,36(4):565-574.
郭智添.1982.辽东连山关早前寒武纪铀矿床地质特征及成矿模式.长春地质学院学报,(S1):84-94.
韩军.2009.鞍本地区早前寒武纪地球化学特征、年代学及铀成矿作用同位素示踪.北京:核工业北京地质研究院博士学位论文:119-124.
韩军,夏毓亮.2009.连山关?高家沟花岗岩体LA-ICP-MS锆石U-Pb年龄及其地质意义.铀矿地质,25(4):214-221.
郝德峰.2004.辽吉地区古元古代花岗岩的成因与地壳演化.青岛:中国海洋大学硕士学位论文:24-25.
核工业208大队.2013.四子王旗?多伦地区铀多金属成矿条件和靶区远景评价研究:26.
核工业西北地质局.1998.中国北西部铀矿地质:874.
贺品高,叶慧文.1998a.辽东?吉南地区早元古代变质地体的组成及主要特征.长春科技大学学报,28(2):121-134.
贺品高,叶慧文.1998b.辽东?吉南地区早元古代两种类型变质作用及其构造意义.岩石学报,14(2):152-162.
侯增谦.2010.大陆碰撞成矿论.地质学报,84(1):30-58.
侯增谦,潘佳棠,王安建,莫宣学,田世红,孙晓明,丁林,王二七,高永丰,谢玉玲,曾普胜,秦克章,许继峰,曲晓明,杨志明,杨竹森,费红彩,孟祥金,李振清.2006b.青藏高原碰撞造山带:II.晚碰撞转换成矿作用.矿床地质,25(5):521-533.
侯增谦,曲晓明,杨竹森,孟祥金,李振清,杨志明,郑绵平,郑有业,聂凤军,高永丰,江思宏,李光明.2006c.青藏高原碰撞造山带:III.后碰撞伸展成矿作用.矿床地质,25(6):629-651.
侯增谦,杨竹森,徐文艺,莫宣学,丁林,高永丰,董方浏,李光明,曲晓明,李光明,赵志丹,江思宏,孟祥金,李振清,秦克章,杨志明.2006a.青藏高原碰撞造山带:I.主碰撞造山成矿作用.矿床地质,25(4):337-358.
李大力.2011.翁泉沟硼铁矿床矿石成分特征及矿石类型分析.中国科技博览,27:238-240.
李东明.1988.翁泉沟硼铁矿床地质特征.辽宁地质,(1):26-37.
李三忠,韩宗珠,刘永江,杨振升,马瑞.2001.辽河群区域变质特征及其大陆动力学意义.地质论评,47(1):9-18.
李三忠,郝德芳,韩宗珠,赵国春,孙敏.2003.胶辽地块古元古代构造?热演化与深部过程.地质学报,77(3):318-340.
李三忠,杨振升.1997.胶辽地块古元古代花岗岩类型及成因.西北地质,18(3):21-27.
李三忠,杨振升,刘永江,刘俊来.1997.胶辽吉地区古元古代早期花岗岩的侵位模式及其与隆滑构造的关系.岩石学报,13(2):189-202.
辽宁省地质矿产调查院.2008.辽宁省凤城市翁泉沟硼铁矿资源储量核实报告:17.
林强,吴福元,刘树文,葛文春,孙景贵,尹京柱.1992.华北地台东部太古宙花岗岩.北京:科学出版社:168-199.
刘福来,刘平华,王舫,刘超辉,蔡佳.2015.胶?辽?吉古元古代造山/活动带巨量变沉积岩系的研究进展.岩石学报,31(10):2816-2846.
刘敬党,肖荣阁,王文武,王翠志.2007.辽东硼矿区域成矿模型.北京:地质出版社:1-426.
刘永江,李三忠.1996.辽宁海城?大石桥?吉洞地区早元古代花岗岩.辽宁地质,(1):10-18.
路孝平,吴福元,林景仟,孙德有,张艳斌,郭春丽.2004.辽东半岛南部早前寒武纪花岗质岩浆作用的年代学格架.地质科学,39(1):123-138.
彭齐鸣,许虹.1994.辽东?吉南地区早元古宙变质蒸发岩系及硼矿床.长春:东北师范大学出版社:60-97.
秦亚.2013.辽吉古元古裂谷带构造演化的年代学制约.长春:吉林大学博士学位论文:1-156.
王惠初,陆松年,初航,相振群,张长捷,刘欢.2011.辽阳河栏地区辽河群中变质基性熔岩的锆石U-Pb年龄与形成构造背景.吉林大学学报(地球科学版),41(5):1322-1361.
王驹.1987.3075矿床形成的物理化学条件及富矿成因.北京:核工业北京地质研究院硕士学位论文:1-173.
王驹,杜乐天.1988.早元古代连山关铀矿床的地质地球化学特征.铀矿地质,4(6):321-331.
王文广,陶铨,张守本.1993.辽东海城?鞍山?八河川地区区域铀成矿地质特征及其成矿远景评价.北京:核工业北京地质研究院:1-321.
吴迪,庄廷新,刘晓东,王策.2013.辽东连山关地区重熔混合岩岩石地球化学特征.世界核地质科学,30(4):210-216.
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145-1174.
夏毓亮,韩军.2008.中国最古老铀矿床成矿年龄及铅同位素示踪铀成矿省.地球学报,29(6):752-760.
徐义刚,李洪颜,庞崇进,何斌.2009.论华北克拉通破坏的时限.科学通报,54(14):1974-1989.
许保良,阎国翰,牟保磊,谭林坤,何中甫,乔广生,张任祜.1998.辽宁盖县梁屯?矿洞沟碱性正长岩Rb-Sr年龄及其意义.科学通报,43(17):1885-1887.
杨凤超,孙景贵,宋运红,张朋,毕中伟.2016.辽东连山关地区新太古代花岗杂岩SHRIMP U-Pb、Hf同位素组成及地质意义.地球科学,41(12):2008-2018.
翟明国,彭澎.2007.华北克拉通古元古代构造事件.岩石学报,23(11):2665-2682.
翟裕生,姚书振,蔡克勤.2011.矿床学.北京:地质出版社:1-369.
张秋生.1988.辽东半岛早期地壳与矿床.北京:地质出版社:1-552.
张艳飞.2011.辽东地区硼矿床区域成矿系统研究.阜新:辽宁工程技术大学博士学位论文:1-108.
钟家蓉.1983.连山关地区下元古界中混合交代作用与铀成矿的关系.矿床地质,2:77-86.
Bonin B,Azzouni-Sekkal A,Bussy F and Ferrag S.1998.Alkali-calcic and alkaline post-orogenic(PO)granite magmatism:Petrologic constraints and geodynamic settings.Lithos,45(1-4):45-70.
Crawford A J,Corbett K U and Everard J L.1992.Geochemistry of the Cambrian volcanic-hosted massive sulfide-rich mount read volcanics,Tasmania,and some tectonic implications.Economic Geology,87(3):597-619.
Groves D I,Goldfarb D I,Gebre-Mariam M,Hagemann S Gand Robert F.1998.Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other Au deposit types.Ore Geology Reviews,13(1-5):7-27.
Hou Z Q and Nigel J C.2009.Metallogenesis of the Tibetan collisional orogen:A review and introduction to the special issue.Ore Geology Reviews,36(1):2-24.
Kerrich R and Feng R.1992.Archean geodynamics and the Abitibi-Pontiac collision:Implications for advection of fluid at transpressive collisional boundaries and the origin of giant quartz vein systems.Earth Science Reviews,32(1-2):33-60.
Koons P O.1991.Gold mineralization as a consequence of continental collision:An example from the Southern Alps,New Zealand.Earth and Planetary Science Letter,103(1-4):1-9.
Li S Z and Zhao G C.2007.SHRIMP U-Pb zircon geochronology of the Liaoji granitoids:Constraints on the evolution of the Paleoproterozoic Jiao-Liao-Ji belt in the Eastern Block of the North China Craton.Precambrian Research,158(1):1-16.
Li S Z,Zhao G C,Sun M,Han Z Z,Zhao G T and Hao D F.2006.Are the South and North Liaohe Groups of North China Craton different exotic terranes?Nd isotope constraints.Gondwana Research,9(1):198-208.
Li S Z,Zhao G C,Sun M,Liu J Z,Hao D F,Han Z Z,Luo Yand Yang Z Z.2004.Not all the Liaoji granitoids are Paleoproterozoic:Evidence from SHRIMP U-Pb zircon ages.International Geology Review,46(2):162-176.
Li S Z,Zhao G C,Sun M,Wu F Y,Hao D F,Han Z Z,Luo Yand Xia X P.2005.Deformational history of the Paleoproterozoic Liaohe Group in the Eastern Block of the North China Craton.Journal of Asian Earth Sciences,24(5):654-669.
Li Z and Chen B.2014.Geochronology and geochemistry of the Paleoproterozoic meta-basalts from the Jiao-Liao-Ji Belt,North China Craton:Implications for petrogenesis and tectonic setting.Precambrian Research,255:653-667.
Liu J L,Liu Y J,Chen H,Sha D M and Wang H C.1997.The inner zone of the Liaoji Paleo-rift:Its early structural styles and structural evolution.Journal of Asian Earth Sciences,15(1):19-31.
Lu X P,Wu F Y,Guo J H,Wilde S A,Yang J H,Liu X M and Zhang X O.2006.Zircon U-Pb geochronological constraints on the Paleoproterozoic crustal evolution of the Eastern block in the North China Craton.Precambrian Research,146(3):138-164.
Lu Y F,Chen Y C,Li H Q,Xue C J and Chen F W.2005.Metallogenic chronology study of boron deposits in early Proterozoic rift in east Liaoning.Acta Geologica Sinica,79(3):414-425.
Luo Y,Sun M,Zhao G C,Li S Z,Ayers J C,Xia X P and Zhang J H.2008.A comparison of U-Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups:Constraints on the evolution of the Jiao-Liao-Ji Belt,North China Craton.Precambrian Research,163(3):279-306.
Luo Y,Sun M,Zhao G C,Li S Z,Xu P,Ye K and Xia X P.2004.LA-ICPMS U-Pb zircon ages of the Liaohe Group in the Eastern Block of the North China Craton:Constraints on the evolution of the Jiao-Liao-Ji Orogen.Precambrian Research,134(3):349-371.
Marignac C and Cuney M.1999.Ore deposits of the French Massif Central:Insight into the metallogenesis of the Variscan collision belt.Mineralium Deposita,34(5-6):472-504.
Meng E,Liu F L,Liu P H,Liu C H and Yang H.2014.Petrogenesis and tectonic significance of Paleoproterozoic meta-mafic rocks from central Liaodong Peninsula,northeast China:Evidence from zircon U-Pb dating and in situ Lu-Hf isotopes,and whole-rock geochemistry.Precambrian Research,247(1):92-109.
Peng Q M and Palmer M R.1995.The Palaeoproterozoic boron deposits in eastern Liaoning,China:A metamorphosed evaporite.Precambrian Research,72(3-4):185-197.
Pirajno F.2009.Hydrothermal Processes and Mineral Systems.Berlin:Springer:1-1250.
Pirajno F.2012.The Geology and Tectonic Settings of China’s Mineral Deposits.Berlin:Springer:1-679.
Richard S P.1992.Collision-related alkalic magmatism and associated gold mineralization:Early magmatic fluids in the meso-epithermal Porgera gold deposit,Papua New Guinea.EOS,73(14):372.
Robb L.2005.Introduction to ore-Forming Processes.Malden:Blackwell:1-384.
Seltmann R,Kampf H and Moller P.1994.Metallogeny of Collisional Orogens.Czech Geological Survey,Prague:1-434.
Tam P Y,Zhao G C,Liu F L,Zhou X W,Sun M and Li S Z.2011.Timing of metamorphism in the Paleoproterozoic Jiao-Liao-Ji Belt:New SHRIMP U-Pb zircon dating of granulites,gneisses and marbles of the Jiaobei massif in the North China Craton.Gondwana Research,19(1):150-162.
Wan Y S,Song B,Liu D Y,Wilde S A,Wu J S,Shi Y R,Yin X Y and Zhou H Y.2006.SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:Evidence for a major Late Palaeoproterozoic tectonothermal event.Precambrian Research,149(3):249-271.
Xie L W,Yang J H,Wu F Y,Yang Y H and Wilde S A.2011.PbSL dating of garnet and staurolite:Constraints on the Paleoproterozoic crustal evolution of the Eastern Block,North China Craton.Journal of Asian Earth Sciences,42(1):142-154.
Yang Z S,Li S G,Yu B X,Gao D H and Gao C G.1988.Structural deformation and mineralization in the Early Proterozoic Liaojitite suite,eastern Liaoning province,China.Precambrian Research,39(1):31-38.
Zhai M G,Li T S,Peng P,Hu B,Liu F,Zhang Y B and Guo JH.2010.Precambrian key tectonic events and evolution of the North China Craton//Kusky T M,Zhai M G and Xiao W J.The Evolving Continents.Geological Society of London,Special Publication,338(1):235-262.
Zhao G C and Zhai M G.2013.Lithotectonic elements of Precambrian basement in the North China Craton:Review and tectonic implications.Gondwana Research,23(4):1207-1240.
Zhao G C,Cao L,Wilde S A,Sun M and Li S Z.2006.Implications based on the first SHRIMP U-Pb zircon dating on Precambrian granitoid rocks in North Korea.Earth and Planetary Science Letters,251(3):365-379.
Zhao G C,Sun M,Wilde S A and Li S Z.2005.Late Archean to Paleoproterozoic evolution of the North China Craton:Key issues revisited.Precambrian Research,136(2):177-202.
陈树良,郇彦清,邴志波.2001.辽东地区古元古代侵入岩特征及构造岩浆大陆动力学演化.辽宁地质,18(1):43-50.
陈衍景.2013.大陆碰撞成矿理论的创建及应用.岩石学报,29(1):1-17.
陈衍景,翟明国,蒋少涌.2009.华北大陆边缘造山过程与成矿研究的重要进展和问题.岩石学报,25(11):2695-2726.
邓军,葛良胜,杨立强.2013.构造动力体制与复合造山作用--兼论三江复合造山带时空演化.岩石学报,29(4):1099-1114.
葛良胜,邓军,王长明.2012.构造动力体制与成矿环境及成矿作用--以三江复合造山带为例.岩石学报,29(4):1115-1128.
郭春影,李子颖,韩军,徐浩,白芸,任忠宝,韩愉,赵宇霆.2017.辽东大石桥组蛇纹石化大理岩中铀矿化特征及形成时代.地质通报,36(4):565-574.
郭智添.1982.辽东连山关早前寒武纪铀矿床地质特征及成矿模式.长春地质学院学报,(S1):84-94.
韩军.2009.鞍本地区早前寒武纪地球化学特征、年代学及铀成矿作用同位素示踪.北京:核工业北京地质研究院博士学位论文:119-124.
韩军,夏毓亮.2009.连山关?高家沟花岗岩体LA-ICP-MS锆石U-Pb年龄及其地质意义.铀矿地质,25(4):214-221.
郝德峰.2004.辽吉地区古元古代花岗岩的成因与地壳演化.青岛:中国海洋大学硕士学位论文:24-25.
核工业208大队.2013.四子王旗?多伦地区铀多金属成矿条件和靶区远景评价研究:26.
核工业西北地质局.1998.中国北西部铀矿地质:874.
贺品高,叶慧文.1998a.辽东?吉南地区早元古代变质地体的组成及主要特征.长春科技大学学报,28(2):121-134.
贺品高,叶慧文.1998b.辽东?吉南地区早元古代两种类型变质作用及其构造意义.岩石学报,14(2):152-162.
侯增谦.2010.大陆碰撞成矿论.地质学报,84(1):30-58.
侯增谦,潘佳棠,王安建,莫宣学,田世红,孙晓明,丁林,王二七,高永丰,谢玉玲,曾普胜,秦克章,许继峰,曲晓明,杨志明,杨竹森,费红彩,孟祥金,李振清.2006b.青藏高原碰撞造山带:II.晚碰撞转换成矿作用.矿床地质,25(5):521-533.
侯增谦,曲晓明,杨竹森,孟祥金,李振清,杨志明,郑绵平,郑有业,聂凤军,高永丰,江思宏,李光明.2006c.青藏高原碰撞造山带:III.后碰撞伸展成矿作用.矿床地质,25(6):629-651.
侯增谦,杨竹森,徐文艺,莫宣学,丁林,高永丰,董方浏,李光明,曲晓明,李光明,赵志丹,江思宏,孟祥金,李振清,秦克章,杨志明.2006a.青藏高原碰撞造山带:I.主碰撞造山成矿作用.矿床地质,25(4):337-358.
李大力.2011.翁泉沟硼铁矿床矿石成分特征及矿石类型分析.中国科技博览,27:238-240.
李东明.1988.翁泉沟硼铁矿床地质特征.辽宁地质,(1):26-37.
李三忠,韩宗珠,刘永江,杨振升,马瑞.2001.辽河群区域变质特征及其大陆动力学意义.地质论评,47(1):9-18.
李三忠,郝德芳,韩宗珠,赵国春,孙敏.2003.胶辽地块古元古代构造?热演化与深部过程.地质学报,77(3):318-340.
李三忠,杨振升.1997.胶辽地块古元古代花岗岩类型及成因.西北地质,18(3):21-27.
李三忠,杨振升,刘永江,刘俊来.1997.胶辽吉地区古元古代早期花岗岩的侵位模式及其与隆滑构造的关系.岩石学报,13(2):189-202.
辽宁省地质矿产调查院.2008.辽宁省凤城市翁泉沟硼铁矿资源储量核实报告:17.
林强,吴福元,刘树文,葛文春,孙景贵,尹京柱.1992.华北地台东部太古宙花岗岩.北京:科学出版社:168-199.
刘福来,刘平华,王舫,刘超辉,蔡佳.2015.胶?辽?吉古元古代造山/活动带巨量变沉积岩系的研究进展.岩石学报,31(10):2816-2846.
刘敬党,肖荣阁,王文武,王翠志.2007.辽东硼矿区域成矿模型.北京:地质出版社:1-426.
刘永江,李三忠.1996.辽宁海城?大石桥?吉洞地区早元古代花岗岩.辽宁地质,(1):10-18.
路孝平,吴福元,林景仟,孙德有,张艳斌,郭春丽.2004.辽东半岛南部早前寒武纪花岗质岩浆作用的年代学格架.地质科学,39(1):123-138.
彭齐鸣,许虹.1994.辽东?吉南地区早元古宙变质蒸发岩系及硼矿床.长春:东北师范大学出版社:60-97.
秦亚.2013.辽吉古元古裂谷带构造演化的年代学制约.长春:吉林大学博士学位论文:1-156.
王惠初,陆松年,初航,相振群,张长捷,刘欢.2011.辽阳河栏地区辽河群中变质基性熔岩的锆石U-Pb年龄与形成构造背景.吉林大学学报(地球科学版),41(5):1322-1361.
王驹.1987.3075矿床形成的物理化学条件及富矿成因.北京:核工业北京地质研究院硕士学位论文:1-173.
王驹,杜乐天.1988.早元古代连山关铀矿床的地质地球化学特征.铀矿地质,4(6):321-331.
王文广,陶铨,张守本.1993.辽东海城?鞍山?八河川地区区域铀成矿地质特征及其成矿远景评价.北京:核工业北京地质研究院:1-321.
吴迪,庄廷新,刘晓东,王策.2013.辽东连山关地区重熔混合岩岩石地球化学特征.世界核地质科学,30(4):210-216.
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145-1174.
夏毓亮,韩军.2008.中国最古老铀矿床成矿年龄及铅同位素示踪铀成矿省.地球学报,29(6):752-760.
徐义刚,李洪颜,庞崇进,何斌.2009.论华北克拉通破坏的时限.科学通报,54(14):1974-1989.
许保良,阎国翰,牟保磊,谭林坤,何中甫,乔广生,张任祜.1998.辽宁盖县梁屯?矿洞沟碱性正长岩Rb-Sr年龄及其意义.科学通报,43(17):1885-1887.
杨凤超,孙景贵,宋运红,张朋,毕中伟.2016.辽东连山关地区新太古代花岗杂岩SHRIMP U-Pb、Hf同位素组成及地质意义.地球科学,41(12):2008-2018.
翟明国,彭澎.2007.华北克拉通古元古代构造事件.岩石学报,23(11):2665-2682.
翟裕生,姚书振,蔡克勤.2011.矿床学.北京:地质出版社:1-369.
张秋生.1988.辽东半岛早期地壳与矿床.北京:地质出版社:1-552.
张艳飞.2011.辽东地区硼矿床区域成矿系统研究.阜新:辽宁工程技术大学博士学位论文:1-108.
钟家蓉.1983.连山关地区下元古界中混合交代作用与铀成矿的关系.矿床地质,2:77-86.
Bonin B,Azzouni-Sekkal A,Bussy F and Ferrag S.1998.Alkali-calcic and alkaline post-orogenic(PO)granite magmatism:Petrologic constraints and geodynamic settings.Lithos,45(1-4):45-70.
Crawford A J,Corbett K U and Everard J L.1992.Geochemistry of the Cambrian volcanic-hosted massive sulfide-rich mount read volcanics,Tasmania,and some tectonic implications.Economic Geology,87(3):597-619.
Groves D I,Goldfarb D I,Gebre-Mariam M,Hagemann S Gand Robert F.1998.Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other Au deposit types.Ore Geology Reviews,13(1-5):7-27.
Hou Z Q and Nigel J C.2009.Metallogenesis of the Tibetan collisional orogen:A review and introduction to the special issue.Ore Geology Reviews,36(1):2-24.
Kerrich R and Feng R.1992.Archean geodynamics and the Abitibi-Pontiac collision:Implications for advection of fluid at transpressive collisional boundaries and the origin of giant quartz vein systems.Earth Science Reviews,32(1-2):33-60.
Koons P O.1991.Gold mineralization as a consequence of continental collision:An example from the Southern Alps,New Zealand.Earth and Planetary Science Letter,103(1-4):1-9.
Li S Z and Zhao G C.2007.SHRIMP U-Pb zircon geochronology of the Liaoji granitoids:Constraints on the evolution of the Paleoproterozoic Jiao-Liao-Ji belt in the Eastern Block of the North China Craton.Precambrian Research,158(1):1-16.
Li S Z,Zhao G C,Sun M,Han Z Z,Zhao G T and Hao D F.2006.Are the South and North Liaohe Groups of North China Craton different exotic terranes?Nd isotope constraints.Gondwana Research,9(1):198-208.
Li S Z,Zhao G C,Sun M,Liu J Z,Hao D F,Han Z Z,Luo Yand Yang Z Z.2004.Not all the Liaoji granitoids are Paleoproterozoic:Evidence from SHRIMP U-Pb zircon ages.International Geology Review,46(2):162-176.
Li S Z,Zhao G C,Sun M,Wu F Y,Hao D F,Han Z Z,Luo Yand Xia X P.2005.Deformational history of the Paleoproterozoic Liaohe Group in the Eastern Block of the North China Craton.Journal of Asian Earth Sciences,24(5):654-669.
Li Z and Chen B.2014.Geochronology and geochemistry of the Paleoproterozoic meta-basalts from the Jiao-Liao-Ji Belt,North China Craton:Implications for petrogenesis and tectonic setting.Precambrian Research,255:653-667.
Liu J L,Liu Y J,Chen H,Sha D M and Wang H C.1997.The inner zone of the Liaoji Paleo-rift:Its early structural styles and structural evolution.Journal of Asian Earth Sciences,15(1):19-31.
Lu X P,Wu F Y,Guo J H,Wilde S A,Yang J H,Liu X M and Zhang X O.2006.Zircon U-Pb geochronological constraints on the Paleoproterozoic crustal evolution of the Eastern block in the North China Craton.Precambrian Research,146(3):138-164.
Lu Y F,Chen Y C,Li H Q,Xue C J and Chen F W.2005.Metallogenic chronology study of boron deposits in early Proterozoic rift in east Liaoning.Acta Geologica Sinica,79(3):414-425.
Luo Y,Sun M,Zhao G C,Li S Z,Ayers J C,Xia X P and Zhang J H.2008.A comparison of U-Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups:Constraints on the evolution of the Jiao-Liao-Ji Belt,North China Craton.Precambrian Research,163(3):279-306.
Luo Y,Sun M,Zhao G C,Li S Z,Xu P,Ye K and Xia X P.2004.LA-ICPMS U-Pb zircon ages of the Liaohe Group in the Eastern Block of the North China Craton:Constraints on the evolution of the Jiao-Liao-Ji Orogen.Precambrian Research,134(3):349-371.
Marignac C and Cuney M.1999.Ore deposits of the French Massif Central:Insight into the metallogenesis of the Variscan collision belt.Mineralium Deposita,34(5-6):472-504.
Meng E,Liu F L,Liu P H,Liu C H and Yang H.2014.Petrogenesis and tectonic significance of Paleoproterozoic meta-mafic rocks from central Liaodong Peninsula,northeast China:Evidence from zircon U-Pb dating and in situ Lu-Hf isotopes,and whole-rock geochemistry.Precambrian Research,247(1):92-109.
Peng Q M and Palmer M R.1995.The Palaeoproterozoic boron deposits in eastern Liaoning,China:A metamorphosed evaporite.Precambrian Research,72(3-4):185-197.
Pirajno F.2009.Hydrothermal Processes and Mineral Systems.Berlin:Springer:1-1250.
Pirajno F.2012.The Geology and Tectonic Settings of China’s Mineral Deposits.Berlin:Springer:1-679.
Richard S P.1992.Collision-related alkalic magmatism and associated gold mineralization:Early magmatic fluids in the meso-epithermal Porgera gold deposit,Papua New Guinea.EOS,73(14):372.
Robb L.2005.Introduction to ore-Forming Processes.Malden:Blackwell:1-384.
Seltmann R,Kampf H and Moller P.1994.Metallogeny of Collisional Orogens.Czech Geological Survey,Prague:1-434.
Tam P Y,Zhao G C,Liu F L,Zhou X W,Sun M and Li S Z.2011.Timing of metamorphism in the Paleoproterozoic Jiao-Liao-Ji Belt:New SHRIMP U-Pb zircon dating of granulites,gneisses and marbles of the Jiaobei massif in the North China Craton.Gondwana Research,19(1):150-162.
Wan Y S,Song B,Liu D Y,Wilde S A,Wu J S,Shi Y R,Yin X Y and Zhou H Y.2006.SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary rocks in the North China Craton:Evidence for a major Late Palaeoproterozoic tectonothermal event.Precambrian Research,149(3):249-271.
Xie L W,Yang J H,Wu F Y,Yang Y H and Wilde S A.2011.PbSL dating of garnet and staurolite:Constraints on the Paleoproterozoic crustal evolution of the Eastern Block,North China Craton.Journal of Asian Earth Sciences,42(1):142-154.
Yang Z S,Li S G,Yu B X,Gao D H and Gao C G.1988.Structural deformation and mineralization in the Early Proterozoic Liaojitite suite,eastern Liaoning province,China.Precambrian Research,39(1):31-38.
Zhai M G,Li T S,Peng P,Hu B,Liu F,Zhang Y B and Guo JH.2010.Precambrian key tectonic events and evolution of the North China Craton//Kusky T M,Zhai M G and Xiao W J.The Evolving Continents.Geological Society of London,Special Publication,338(1):235-262.
Zhao G C and Zhai M G.2013.Lithotectonic elements of Precambrian basement in the North China Craton:Review and tectonic implications.Gondwana Research,23(4):1207-1240.
Zhao G C,Cao L,Wilde S A,Sun M and Li S Z.2006.Implications based on the first SHRIMP U-Pb zircon dating on Precambrian granitoid rocks in North Korea.Earth and Planetary Science Letters,251(3):365-379.
Zhao G C,Sun M,Wilde S A and Li S Z.2005.Late Archean to Paleoproterozoic evolution of the North China Craton:Key issues revisited.Precambrian Research,136(2):177-202.