太行山南段丰峪蚀变正长花岗岩LA-ICP-MS锆石U-Pb年龄及构造意义
|
摘要
在华北克拉通中东部的太行山南段丰峪一带,发现一处不整合于长城系大河组之下的蚀变正长花岗岩体。岩石类型为黑云母正长花岗岩,钾化、绢云母化蚀变明显。岩体低硅(SiO_2=67.46%～68.89%)、富碱(K_2O+Na_2O=8.09～9.62,K_2O/Na_2O远大于1),铝指数A/CNK=1.20～1.57,属过铝质、钙碱性A型花岗岩。岩石富集大离子亲石元素,显著亏损Nb、Ba、Ta、Sr、P、Ti元素,稀土元素含量高(192～774μg/g,平均483μg/g)。用LA-ICPMS技术测得锆石的207Pb/206Pb年龄为(1790±22)Ma(n=22,MSWD=0.80),这是迄今为止太行山南段长城系底界直接的控制年龄。岩石主、微量元素地球化学以及同位素年代学表明,丰峪蚀变正长花岗岩形成于板内伸展构造环境,为熊耳期三叉裂谷东北一支的存在提供了重要的岩浆岩石学证据,其所处的太行山区与熊耳群火山岩所处的豫西地区均为熊耳期三叉裂谷的组成部分,进而为太行山区与豫西地区的长城系对比提供了重要支撑。
An altered syenogranite pluton was found in Fengyu area, southern Taihang Mountain of central-eastern North China Craton, which unconformably underlies the Changcheng System. The rock type is biotite granite, which has undergone obvious Kfeldspar alteration and sericitization. The rocks are characterized by low SiO_2(SiO_2= 67.46%-68.89%) and high K_2O + Na_2O(K_2O+ Na_2O = 8.09-9.62, K_2O/Na_2O ? 1) content, with aluminum index A/CNK being 1.20-1.57, showing features of peraluminous,calc-alkaline A-type granite. The pluton is also characterized by enrichment of LILE and depletion of Ba, Nb, Ta, Sr, P, Ti, as well as high ∑REE values(192-774 μg/g, 483 ug/g om average). LA-ICP-MS zircon U-Pb dating of Fengyu altered syenogranite pluton yielded an207 Pb/206 Pb age of(1790±22)Ma(n=22, MSWD=0.80), which is by far the most direct control of the lower limit age of Changcheng System in southern Taihang Mountain. Petrochemistry, rare earth elements, trace element geochemistry and isotopic geochronology all prove that Fengyu altered syenogranite pluton was formed in an intraplate extensional environment in the Paleoproterozoic period, thus providing an important magmatism evidence for the existence of northeast Xiongerrian trident continental rift; they also show that the Taihang Mountain area where Fengyu altered syenogranite pluton was formed and the western Henan Province where Xiong'er Group volcanic rocks were developed constitute part of the Xiongerrian trident continental rift, which thus provides an important support for the stratigraphic correlation of the Changcheng System between Taihang Mountain area and western Henan Province.
An altered syenogranite pluton was found in Fengyu area, southern Taihang Mountain of central-eastern North China Craton, which unconformably underlies the Changcheng System. The rock type is biotite granite, which has undergone obvious Kfeldspar alteration and sericitization. The rocks are characterized by low SiO_2(SiO_2= 67.46%-68.89%) and high K_2O + Na_2O(K_2O+ Na_2O = 8.09-9.62, K_2O/Na_2O ? 1) content, with aluminum index A/CNK being 1.20-1.57, showing features of peraluminous,calc-alkaline A-type granite. The pluton is also characterized by enrichment of LILE and depletion of Ba, Nb, Ta, Sr, P, Ti, as well as high ∑REE values(192-774 μg/g, 483 ug/g om average). LA-ICP-MS zircon U-Pb dating of Fengyu altered syenogranite pluton yielded an207 Pb/206 Pb age of(1790±22)Ma(n=22, MSWD=0.80), which is by far the most direct control of the lower limit age of Changcheng System in southern Taihang Mountain. Petrochemistry, rare earth elements, trace element geochemistry and isotopic geochronology all prove that Fengyu altered syenogranite pluton was formed in an intraplate extensional environment in the Paleoproterozoic period, thus providing an important magmatism evidence for the existence of northeast Xiongerrian trident continental rift; they also show that the Taihang Mountain area where Fengyu altered syenogranite pluton was formed and the western Henan Province where Xiong'er Group volcanic rocks were developed constitute part of the Xiongerrian trident continental rift, which thus provides an important support for the stratigraphic correlation of the Changcheng System between Taihang Mountain area and western Henan Province.
引文
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb[J].Chemical Geology,192:59-79.
Bureau of Geology and Mineral Resources of Henan Provinece.1989.Regional Geology of Henan Provice[M].Beijing:Geological Publishing House,1-772(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Henan Provinece.1997.Lithostratigraphy of Henan[M].Wuhan:China University of Geosciences Press,1-229(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1989.Regional Geology of Shanxi Provice[M].Beijing:Geological Publishing House,1-780(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1997.Lithostratigraphy of Shanxi[M].Wuhan:Press of China University of Geosciences,1-353(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1989.Regional Geology of Shanxi Provice[M].Beijing:Geological Publishing House,1-698(in Chinese with English abstract).
Collins W J,Beams S D,White A J R.1982.Nature and origin of A-type granites with particular reference to south-eastern Australia[J].Contr.Minera1.Petrol.,80:189-200.
Cui Minli,Zhang Baolin,Peng Peng,Zang Lianchang,Shen Xiaoli,Guo Zhihua,Huang Xuefei.2010.Zircon/baddeleyite U-Pb dating for the Paleo-proterozoic intermediate-acid intrusive in Xiaoshan Mountains,west of Henan Province and their constraints on the age of the Xiong’er Volcanic Province[J].Acta Petrologica Sinica,26(5):1541-1549(in Chinese with English abstract).
Eby G N.1990.The A-type granitoids:A review of their occurrence andchemicial characteristics and speculations on their petrogenesis[J].Lithos,26:115-134.
Eby G N.1992.Chemical subdivision of the A-type granitoids:petrogenetic and tectonic implications[J].Geology,20:641-644.
Gao Wei,Zhang Chuanheng,Liu Xiaoming,Gao Linzhi,Shi Xiaoying,Liu Yaoming,Song Biao.2008.Zircon SHRIMP U-Pb age of rapakivi granite in Miyun,Beijing,China,and its tectonostratigraphic implications[J].Geological Bulletin of China,27(6):793-798(in Chinese with English abstract).
He ZhengJun,Niu Baogui,Zhang Xinyuan,Zhao Lei,Liu Renyan.2011.Discovery of the paleoweathered mantle of the rapakivi granite covered by the Proterozoic Changzhougou Formation in the Miyun area,Beijing and their detrital zircon dating[J].Geological Bulletin of China,30(5):798-802(in Chinese with English abstract).
Hu Guohui,Hu Junliang,Chen Wei,Zhao Taiping.2010.Geochemistry and tectonic setting of the 1.78 Ga mafic dyke swarms in the Mt.Zhongtiao and Mt.Song areas,the southern margin of the North China Craton[J].Acta Petrologica Sinica,26(5):1563-1576(in Chinese with English abstract).
Hong Dawei,Wang Guangguang,Han Baofu,Jin Manyuan.1995.Tectonic setting classifications and disrimination criteria for alkaline granites[J].Science in China(B),25(4):418-426(in Chinese with English abstract).
Kalsbeek F,Jepsen H and Nutman A.2001.From source migmatites toplutons:Tracking the origin of ca.435 Ma S-type granites in the East Greenland Caledonian orogen[J].Lithos,57(1):1-21.
Li Huaikun,Su Wenbo,Zhou Hongying,Geng Jianzhen,Xiang Zhenqun,Cui Yurong,Liu Wencan,Lu Songyian.2011.The base age of the Changchengian System at the northern North China Craton should be younger than 1670 Ma:Constraints from zircon U-Pb LA-MC-ICPMS dating of a granite-porphyry dike in Miyun County,Beijing[J].Earth Science Frontiers,18(3):108-120(in Chinese with English abstract).
Li Changmin.2009.A review on the minerageny and situ microanalytical dating techniques of zircons[J].Geological Survey and Research,33(3):161-174(in Chinese with English abstract).
Li Chengdong,Zhao Ligang,Chang Qingsong,Xu Yawen,Wang Shiyan,Xu Teng.2017.Zircon U-Pb dating of tuff bed from Luoyukou Formation in western Henan Province on the southern margin of the North China Craton and its dtratigraphic attribution discussion[J].Geology in China,44(3):511-525(in Chinese with English abstract).
Lu Songnian,Li Huaikun,Li Huimin,Song Biao,Wang Shiyan,Zhou Hongying,Chen Zhihong.2003.U-Pb isotopic ages and their significance of alkaline granite in the southern margin of the North China Craton[J].Geological Bulletin of China,22(12):762-768(in Chinese with English abstract).
Liao Chaolin,Wang Yuejin,Peng Touping.2003.40Ar-39Ar Geochronology of paleoproterozoic mafic dykes from southern Taihang mountains and its gellogical significance[J].Geotectonica et Metallogenia,27(4):354-361(in Chinese with English abstract).
Liu Changshi,Chen Xiaoming,Chen Peirong,Wang Rucheng,Hu Huan.2003.Subdivision,Discrim ination criteria and genesis for a type rock suites[J].Geological Journal of China Universities,9(4):573-591(in Chinese with English abstract).
Liu Y,Gao S,Hu Z.2010.Continental and oceanic crust recy-clinginduced 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,51(1/2):537-571.
Ludwig K R.1991.Isoplot-A plotting and regression program for radio-genic-isotope data[A].US Geological Survey Open-File Report,39:91-445.
Peng Peng,Liu Fu,Zhai Mingguo,Guo Jinghui.2012.Age of the Miyun dyke swarm:Constraints on the maximum depositional age of the Changcheng System[J].Chinese Science Bulletin,57(in Chinese).
Pearce N J G,Perkins W T,Westgate J A.1997.A compilation of new and published major and trace element data for NIST SRM610 and NIST SRM 612 glass reference materials[J].Geostandards Newletters,21:115-144.
Qiao Xiufu,Wang Yanbin.2014.Discussions on the lower boundary age of the Mesoproterozoic and basin tectonic evolution of the Mesoproterozoic in North China Craton[J].Acta Geologica Sinica,88(9):1623-1637.
Su Dechen,Li Chunwang,Sun Aiping,Qiao Xiufu.2017.Mesoproterozoic mud volcanoes discovered in North Taihang Mountain:Preliminary results[J].Geology in China,44(2):399-400(in Chinese with English abstract).
Su Wenbo,Li Huaikun,Xu Li,Jia Songhai,Geng Jianzhen,Zhou Hongying,Wang Zhihong,Pu Hanyong.2012.Luoyu and Ruyang Group at the south margin of the North China Craton(NCC)should belong in the Mesoproterozoic Changchengian System:Direct constraints from the LA-MC-ICPMS U-Pb age of the tuffite in the Luoyukou Formation,Ruzhou,Henan,China[J].Geological Survey and Research,35(2):96-108(in Chinese with English abstract).
Sun S S,McDonough W F.1989.Chemical and isotope systematics of ocean baslt:Implications for mantle composition and processes.In:Saunders A D and Norry M J(eds.).Magmatism in the Ocean Basins.Geological Society Special Publication,42:313-345.
Wu Tieshan.1979.The Sinian Department of Shanxi Province,Summary of the 1:20 Fault Zone Formation in Shanxi Province[R].Geological Survey Team of Shanxi Provincial Bureau of Geology and Mineral Resources(in Chinese).
Wang Qichao,Wu Tieshang,Xu Chaolei.1980.Taihang-Wutai district of Sinian subkingdom and its relationship with the chaotuo supergroup[C]//Tianjin Institute of Geology and Mineral Resources'CAGS(ed.).Research on Precambrian Geology.Tianjin:Tianjin Science and Technology Press(in Chinese with English abstract).
Wang Tonghe.1992.Characteristics and Evolution of Mid-latitude zonal structural belt in North China Craton[J].Geology of Shanxi,7(3):301-312(in Chinese with English abstract).
Wiedenbeck M,Alle P,Corfu F,Griffin W L,Meier M,Oberli F,Von quadt A,Roddick J C,Spiegel W.1995.Three natural zircon standards for U-Th-Pb,Lu-Hf,trace element and REE analyses[J].Geostandards Newsletter,19:1-23.
Wu Cailai,Dong Shuwen,Wang Lutai,et al.The discovery of the syenogranite with an age of 126 Ma in the depth of Tongling:Evidence from 3000meters scientific drilling[J].Geology in China,2016,43(5):1495-1513(in Chinese with English abstract).
Wu Suoping,Wang Meiying,Qi Kaijing.2007.Present situation of researches on A-type granites:Areview[J].Acta petrologica et mineralogica,26(1):57-66(in Chinese with English abstract).
Whalen J B,Currie K L,Chappell B W.1987.A-type granites:Geochemical characteristics,discriminations and petrogenesis[J].Contrib.Mineral.Petrol.,95:407-419.
Wan Yusheng,Liu Dunyi,Wang Shiyan,Zhao Xun,Dong Chunyan,Zhou Hongying,Yin Xiaoyan,Yang Changxiu,Gao Linzhi.2009.Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China):Constraints from geochemistry and SHRIMP U-Pb zircon dating[J].Acta Geologica Sinica,83(7):982-999(in Chinese with English abstract).
Xue Liangwei,Yu Xangdong,Zhao Taiping.1996.The geochemical characteristics of A-type granite in Songshan aera and its structural environment[J].Acta Petrologica Sinica,12(1):137-144(in Chinese with English abstract).
Zeng Xi,Chen Shouyu,Zhao Jiangnan.2016.Geochemical characteristics of Kafang altered granitein Gejiu City and its relationship with mineralization[J].Contributions to Geology and Mineral Resources Research,31(2):163-171(in Chinese with English abstract).
Zhang J,Zhang H F,Lu X X.2013.Zircon U-Pb age and Lu-Hf isotope constraints on Precambrian evolution of continental crust in the Songshan area,the south-central North China Craton[J].Precambrian Research,226:1-20.
Zhang Qi,Ran Hao,Li Chengdong.2012.A-type granite:What is the essence?[J].Acta Petrologica et Mineralogica,31(4):621-626(in Chinese with English abstract).
Zhang Qi.2013.The criteria and discrimination for A-type granites:Areply to the question put forward by Wang Yang and some other persons for“A-type granite:what is the essence?”[J].Acta Petrologica et Mineralogica,32(2):267-272(in Chinese with English abstract).
Zhao Tiaping,Deng Xiaoqin,Hu Guohui,Zhou Yanyan,Peng Peng,Zhai Mingguo.2015.The Paleoproterozoic-Mesoproterozoic boundary of the North China Craton and the related geological issues:Areview[J].Acta Petrologica Sinica,31(6):1495-1508(in Chinese with English abstract).
Zhao Taiping,Zhou Meifu,Jin Chengwei,Guan Hong,Li Huimin.2001.Discussion on age of the xiong’er group in southern margin of north China craton[J].Chinese Journal of Geology,36(3):326-334(in Chinese with English abstract).
Zhao Taiping,Jin Chengwei,zhai Mingguo,Xia Bin,Zhou Meifu.2002.Geoehemistry and Petrogenesis of the Xiong'er Group in the southern regions of the North China Craton[J].Acta Petrologica Sinica,18(1):59-69(in Chinese with English abstract).
Zhao Taiping,Xu Yonghang,Zhai Mingguo.2007.Petrogenesis and Tectonic Setting of the Paleoproterozoic Xiong’er Group in the Southern Part of the North China Craton:A review[J].Geological Journal of China Universities,13(2):191-206(in Chinese with English abstract).
河南省地质矿产局.1989.河南省区域地质志[M].北京:地质出版社,1-772.
河南省地质矿产局.1997.河南省岩石地层[M].武汉:中国地质大学出版社,1-299.
山西省地质矿产局.1989.山西省区域地质志[M].北京:地质出版社.1-780.
山西省地质矿产局.1997.山西省岩石地层[M].武汉:中国地质大学出版社,1-353.
陕西省地质矿产局.1989.陕西省区域地质志[M].北京:地质出版社,1-698.
崔敏利,张宝林,彭澎,张连昌,沈晓丽,郭志华,黄雪飞.2010.豫西崤山早元古代中酸性侵入岩锆石/斜锆石U-Pb测年及其对熊耳火山岩系时限的约束[J].岩石学报,26(5):1541-1549.
高维,张传恒,柳晓明,高林志,史晓颖,刘耀明,宋彪.2008.北京密云环斑花岗岩的锆石SHRIMP U-Pb年龄及其构造意义[J].地质通报,27(6):793-798.
和政军,牛宝贵,张新元,赵磊,刘仁燕.2011.北京密云元古宙常州沟组之下环斑花岗岩古风化壳岩石的发现及其碎屑锆石年龄[J].地质通报,30(5):798-802.
胡国辉,胡俊良,陈伟,赵太平.华北克拉通南缘中条山-嵩山地区1.78 Ga基性岩墙群的地球化学特征及构造环境[J].岩石学报,2010,26(6):1563-1576.
洪大卫,王光洸,韩宝福,靳满元.1995.碱性花岗岩的构造环境分类及其鉴别标志[J].中国科学(B辑),25(4):418-426.
李怀坤,苏文博,周红英,耿建珍,相振群,崔玉荣,刘文灿,陆松年.2011.华北克拉通北部长城系底界年龄小于1670 Ma:来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束[J].地学前缘,18(3):108-120.
刘昌实,陈小明,陈培荣,王汝成,胡欢.2003.A型岩套的分类、判别标志和成因[J].高校地质学报,9(4):573-591.
陆松年,李怀坤,李惠民,宋彪,王世炎,周红英,陈志宏.2003.华北克拉通南缘龙王石童碱性花岗岩U-Pb年龄及其地质意义[J].地质通报,22(12):762-768.
李长民.2009.锆石成因矿物学与锆石微区定年综述[J],地质调查与研究,33(3):161-174.
李承东,赵利刚,常青松,许雅雯,王世炎,许腾.2017.豫西洛峪口组凝灰岩锆石LA-MC-ICPMS U-Pb年龄及地层归属讨论[J].中国地质,44(3):511-525.
廖超林,王岳军,彭头平.2003.太行山南段早元古代基性脉岩的40Ar-39Ar年代学及其构造意义[J].大地构造与成矿学,27(4):354-361.
澎澎,刘富,翟明国,郭敬辉.2011.密云岩墙群的时代对长城系底界年龄的制约[J].科学通报,56(35):2975-2980.
乔秀夫,王彦斌.华北克拉通中元古界底界年龄与盆地性质讨论[J].地质学报,2014,88(9):1623-1637.
苏德辰,李春旺,孙爱萍,乔秀夫.2017.太行山北缘中元古界发现泥火山群[J].中国地质,44(2):399-400.
苏文博,李怀坤,徐莉,贾松海,耿建珍,周红英,王志宏,蒲含勇.2012.华北克拉通南缘洛峪群-汝阳群属于中元古界长城系--河南汝州洛峪口组层凝灰岩锆石LA-MC-ICPMS U-Pb年龄的直接约束[J].地质调查与研究,35(2):96-108.
万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志.2009.登封地区早前寒武纪地壳演化--地球化学和锆石SHRIMP U-Pb年代学制约[J].地质学报,83(7):982-999.
武铁山,1979.山西的震旦系,山西省1∶20万断代地层总结[R].山西省地矿局区调队.
王启超,武铁山,徐朝雷.1980.太行-五台区震旦亚界及其与滹沱超群的关系[C]//中国地质科学院天津地质矿产研究所编.中国震旦亚界.天津:天津科学技术出版社.
王同和,1992.华北克拉通中腰纬向构造带的特征及演化[J].山西地质,7(3):301-312.
吴才来,董树文,王陆太,王次松,雷敏,吴迪.2015.铜陵矿集区深部发现126 Ma的正长花岗岩:来自3000 m科学钻探的证据[J].中国地质,2016,43(5):1495-1513.
吴锁平,王梅英,戚开静.2007.A型花岗岩研究现状及其述评[J].岩石矿物学杂志,26(1):57-66.
薛良伟,尉向东,赵太平.1996.嵩山A型花岗岩的地质地球化学特征和构造环境[J].岩石学报,12(1):137-144.
曾茜,陈守余,赵江南.2016.个旧卡房蚀变花岗岩地球化学特征及其与成矿的关系[J].地质找矿论丛,31(2):163-171.
赵太平,邓小芹,胡国辉,周艳艳,彭澎,翟明国.2015.华北克拉通古/中元古代界线和相关地质问题讨论[J].岩石学报,31(6):1495-1508.
赵太平,周美夫,金成伟,关鸿,李惠民.2001.华北陆块南缘熊耳群形成时代讨论[J].地质科学,36(3):326-334.
赵太平,金成伟,翟明国,夏斌,周美夫.2002.华北陆块南部熊耳群火山岩的地球化学特征与成因[J].岩石学报,18(1):59-69.
赵太平,徐勇航,翟明国.2007.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议[J].高校地质学报,13(2):191-206.
张旗,冉皞,李承东.2012.A型花岗岩的实质是什么?[J]岩石矿物学杂志,31(4):621-626.
张旗.2013.A型花岗岩的标志和判别--兼答汪洋等对“A型花岗岩的实质是什么”的质疑[J].岩石矿物学杂志,32(2):267-272.
(1)河南省地质调查院.2015.河南1∶5万东姚集、临淇镇、鹤壁、庙口幅区域地质调查报告.
(2)山西省地质调查院.2007.1∶25万新乡市幅区域地质调查报告.
Bureau of Geology and Mineral Resources of Henan Provinece.1989.Regional Geology of Henan Provice[M].Beijing:Geological Publishing House,1-772(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Henan Provinece.1997.Lithostratigraphy of Henan[M].Wuhan:China University of Geosciences Press,1-229(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1989.Regional Geology of Shanxi Provice[M].Beijing:Geological Publishing House,1-780(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1997.Lithostratigraphy of Shanxi[M].Wuhan:Press of China University of Geosciences,1-353(in Chinese with English abstract).
Bureau of Geology and Mineral Resources of Shanxi Provinece.1989.Regional Geology of Shanxi Provice[M].Beijing:Geological Publishing House,1-698(in Chinese with English abstract).
Collins W J,Beams S D,White A J R.1982.Nature and origin of A-type granites with particular reference to south-eastern Australia[J].Contr.Minera1.Petrol.,80:189-200.
Cui Minli,Zhang Baolin,Peng Peng,Zang Lianchang,Shen Xiaoli,Guo Zhihua,Huang Xuefei.2010.Zircon/baddeleyite U-Pb dating for the Paleo-proterozoic intermediate-acid intrusive in Xiaoshan Mountains,west of Henan Province and their constraints on the age of the Xiong’er Volcanic Province[J].Acta Petrologica Sinica,26(5):1541-1549(in Chinese with English abstract).
Eby G N.1990.The A-type granitoids:A review of their occurrence andchemicial characteristics and speculations on their petrogenesis[J].Lithos,26:115-134.
Eby G N.1992.Chemical subdivision of the A-type granitoids:petrogenetic and tectonic implications[J].Geology,20:641-644.
Gao Wei,Zhang Chuanheng,Liu Xiaoming,Gao Linzhi,Shi Xiaoying,Liu Yaoming,Song Biao.2008.Zircon SHRIMP U-Pb age of rapakivi granite in Miyun,Beijing,China,and its tectonostratigraphic implications[J].Geological Bulletin of China,27(6):793-798(in Chinese with English abstract).
He ZhengJun,Niu Baogui,Zhang Xinyuan,Zhao Lei,Liu Renyan.2011.Discovery of the paleoweathered mantle of the rapakivi granite covered by the Proterozoic Changzhougou Formation in the Miyun area,Beijing and their detrital zircon dating[J].Geological Bulletin of China,30(5):798-802(in Chinese with English abstract).
Hu Guohui,Hu Junliang,Chen Wei,Zhao Taiping.2010.Geochemistry and tectonic setting of the 1.78 Ga mafic dyke swarms in the Mt.Zhongtiao and Mt.Song areas,the southern margin of the North China Craton[J].Acta Petrologica Sinica,26(5):1563-1576(in Chinese with English abstract).
Hong Dawei,Wang Guangguang,Han Baofu,Jin Manyuan.1995.Tectonic setting classifications and disrimination criteria for alkaline granites[J].Science in China(B),25(4):418-426(in Chinese with English abstract).
Kalsbeek F,Jepsen H and Nutman A.2001.From source migmatites toplutons:Tracking the origin of ca.435 Ma S-type granites in the East Greenland Caledonian orogen[J].Lithos,57(1):1-21.
Li Huaikun,Su Wenbo,Zhou Hongying,Geng Jianzhen,Xiang Zhenqun,Cui Yurong,Liu Wencan,Lu Songyian.2011.The base age of the Changchengian System at the northern North China Craton should be younger than 1670 Ma:Constraints from zircon U-Pb LA-MC-ICPMS dating of a granite-porphyry dike in Miyun County,Beijing[J].Earth Science Frontiers,18(3):108-120(in Chinese with English abstract).
Li Changmin.2009.A review on the minerageny and situ microanalytical dating techniques of zircons[J].Geological Survey and Research,33(3):161-174(in Chinese with English abstract).
Li Chengdong,Zhao Ligang,Chang Qingsong,Xu Yawen,Wang Shiyan,Xu Teng.2017.Zircon U-Pb dating of tuff bed from Luoyukou Formation in western Henan Province on the southern margin of the North China Craton and its dtratigraphic attribution discussion[J].Geology in China,44(3):511-525(in Chinese with English abstract).
Lu Songnian,Li Huaikun,Li Huimin,Song Biao,Wang Shiyan,Zhou Hongying,Chen Zhihong.2003.U-Pb isotopic ages and their significance of alkaline granite in the southern margin of the North China Craton[J].Geological Bulletin of China,22(12):762-768(in Chinese with English abstract).
Liao Chaolin,Wang Yuejin,Peng Touping.2003.40Ar-39Ar Geochronology of paleoproterozoic mafic dykes from southern Taihang mountains and its gellogical significance[J].Geotectonica et Metallogenia,27(4):354-361(in Chinese with English abstract).
Liu Changshi,Chen Xiaoming,Chen Peirong,Wang Rucheng,Hu Huan.2003.Subdivision,Discrim ination criteria and genesis for a type rock suites[J].Geological Journal of China Universities,9(4):573-591(in Chinese with English abstract).
Liu Y,Gao S,Hu Z.2010.Continental and oceanic crust recy-clinginduced 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,51(1/2):537-571.
Ludwig K R.1991.Isoplot-A plotting and regression program for radio-genic-isotope data[A].US Geological Survey Open-File Report,39:91-445.
Peng Peng,Liu Fu,Zhai Mingguo,Guo Jinghui.2012.Age of the Miyun dyke swarm:Constraints on the maximum depositional age of the Changcheng System[J].Chinese Science Bulletin,57(in Chinese).
Pearce N J G,Perkins W T,Westgate J A.1997.A compilation of new and published major and trace element data for NIST SRM610 and NIST SRM 612 glass reference materials[J].Geostandards Newletters,21:115-144.
Qiao Xiufu,Wang Yanbin.2014.Discussions on the lower boundary age of the Mesoproterozoic and basin tectonic evolution of the Mesoproterozoic in North China Craton[J].Acta Geologica Sinica,88(9):1623-1637.
Su Dechen,Li Chunwang,Sun Aiping,Qiao Xiufu.2017.Mesoproterozoic mud volcanoes discovered in North Taihang Mountain:Preliminary results[J].Geology in China,44(2):399-400(in Chinese with English abstract).
Su Wenbo,Li Huaikun,Xu Li,Jia Songhai,Geng Jianzhen,Zhou Hongying,Wang Zhihong,Pu Hanyong.2012.Luoyu and Ruyang Group at the south margin of the North China Craton(NCC)should belong in the Mesoproterozoic Changchengian System:Direct constraints from the LA-MC-ICPMS U-Pb age of the tuffite in the Luoyukou Formation,Ruzhou,Henan,China[J].Geological Survey and Research,35(2):96-108(in Chinese with English abstract).
Sun S S,McDonough W F.1989.Chemical and isotope systematics of ocean baslt:Implications for mantle composition and processes.In:Saunders A D and Norry M J(eds.).Magmatism in the Ocean Basins.Geological Society Special Publication,42:313-345.
Wu Tieshan.1979.The Sinian Department of Shanxi Province,Summary of the 1:20 Fault Zone Formation in Shanxi Province[R].Geological Survey Team of Shanxi Provincial Bureau of Geology and Mineral Resources(in Chinese).
Wang Qichao,Wu Tieshang,Xu Chaolei.1980.Taihang-Wutai district of Sinian subkingdom and its relationship with the chaotuo supergroup[C]//Tianjin Institute of Geology and Mineral Resources'CAGS(ed.).Research on Precambrian Geology.Tianjin:Tianjin Science and Technology Press(in Chinese with English abstract).
Wang Tonghe.1992.Characteristics and Evolution of Mid-latitude zonal structural belt in North China Craton[J].Geology of Shanxi,7(3):301-312(in Chinese with English abstract).
Wiedenbeck M,Alle P,Corfu F,Griffin W L,Meier M,Oberli F,Von quadt A,Roddick J C,Spiegel W.1995.Three natural zircon standards for U-Th-Pb,Lu-Hf,trace element and REE analyses[J].Geostandards Newsletter,19:1-23.
Wu Cailai,Dong Shuwen,Wang Lutai,et al.The discovery of the syenogranite with an age of 126 Ma in the depth of Tongling:Evidence from 3000meters scientific drilling[J].Geology in China,2016,43(5):1495-1513(in Chinese with English abstract).
Wu Suoping,Wang Meiying,Qi Kaijing.2007.Present situation of researches on A-type granites:Areview[J].Acta petrologica et mineralogica,26(1):57-66(in Chinese with English abstract).
Whalen J B,Currie K L,Chappell B W.1987.A-type granites:Geochemical characteristics,discriminations and petrogenesis[J].Contrib.Mineral.Petrol.,95:407-419.
Wan Yusheng,Liu Dunyi,Wang Shiyan,Zhao Xun,Dong Chunyan,Zhou Hongying,Yin Xiaoyan,Yang Changxiu,Gao Linzhi.2009.Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China):Constraints from geochemistry and SHRIMP U-Pb zircon dating[J].Acta Geologica Sinica,83(7):982-999(in Chinese with English abstract).
Xue Liangwei,Yu Xangdong,Zhao Taiping.1996.The geochemical characteristics of A-type granite in Songshan aera and its structural environment[J].Acta Petrologica Sinica,12(1):137-144(in Chinese with English abstract).
Zeng Xi,Chen Shouyu,Zhao Jiangnan.2016.Geochemical characteristics of Kafang altered granitein Gejiu City and its relationship with mineralization[J].Contributions to Geology and Mineral Resources Research,31(2):163-171(in Chinese with English abstract).
Zhang J,Zhang H F,Lu X X.2013.Zircon U-Pb age and Lu-Hf isotope constraints on Precambrian evolution of continental crust in the Songshan area,the south-central North China Craton[J].Precambrian Research,226:1-20.
Zhang Qi,Ran Hao,Li Chengdong.2012.A-type granite:What is the essence?[J].Acta Petrologica et Mineralogica,31(4):621-626(in Chinese with English abstract).
Zhang Qi.2013.The criteria and discrimination for A-type granites:Areply to the question put forward by Wang Yang and some other persons for“A-type granite:what is the essence?”[J].Acta Petrologica et Mineralogica,32(2):267-272(in Chinese with English abstract).
Zhao Tiaping,Deng Xiaoqin,Hu Guohui,Zhou Yanyan,Peng Peng,Zhai Mingguo.2015.The Paleoproterozoic-Mesoproterozoic boundary of the North China Craton and the related geological issues:Areview[J].Acta Petrologica Sinica,31(6):1495-1508(in Chinese with English abstract).
Zhao Taiping,Zhou Meifu,Jin Chengwei,Guan Hong,Li Huimin.2001.Discussion on age of the xiong’er group in southern margin of north China craton[J].Chinese Journal of Geology,36(3):326-334(in Chinese with English abstract).
Zhao Taiping,Jin Chengwei,zhai Mingguo,Xia Bin,Zhou Meifu.2002.Geoehemistry and Petrogenesis of the Xiong'er Group in the southern regions of the North China Craton[J].Acta Petrologica Sinica,18(1):59-69(in Chinese with English abstract).
Zhao Taiping,Xu Yonghang,Zhai Mingguo.2007.Petrogenesis and Tectonic Setting of the Paleoproterozoic Xiong’er Group in the Southern Part of the North China Craton:A review[J].Geological Journal of China Universities,13(2):191-206(in Chinese with English abstract).
河南省地质矿产局.1989.河南省区域地质志[M].北京:地质出版社,1-772.
河南省地质矿产局.1997.河南省岩石地层[M].武汉:中国地质大学出版社,1-299.
山西省地质矿产局.1989.山西省区域地质志[M].北京:地质出版社.1-780.
山西省地质矿产局.1997.山西省岩石地层[M].武汉:中国地质大学出版社,1-353.
陕西省地质矿产局.1989.陕西省区域地质志[M].北京:地质出版社,1-698.
崔敏利,张宝林,彭澎,张连昌,沈晓丽,郭志华,黄雪飞.2010.豫西崤山早元古代中酸性侵入岩锆石/斜锆石U-Pb测年及其对熊耳火山岩系时限的约束[J].岩石学报,26(5):1541-1549.
高维,张传恒,柳晓明,高林志,史晓颖,刘耀明,宋彪.2008.北京密云环斑花岗岩的锆石SHRIMP U-Pb年龄及其构造意义[J].地质通报,27(6):793-798.
和政军,牛宝贵,张新元,赵磊,刘仁燕.2011.北京密云元古宙常州沟组之下环斑花岗岩古风化壳岩石的发现及其碎屑锆石年龄[J].地质通报,30(5):798-802.
胡国辉,胡俊良,陈伟,赵太平.华北克拉通南缘中条山-嵩山地区1.78 Ga基性岩墙群的地球化学特征及构造环境[J].岩石学报,2010,26(6):1563-1576.
洪大卫,王光洸,韩宝福,靳满元.1995.碱性花岗岩的构造环境分类及其鉴别标志[J].中国科学(B辑),25(4):418-426.
李怀坤,苏文博,周红英,耿建珍,相振群,崔玉荣,刘文灿,陆松年.2011.华北克拉通北部长城系底界年龄小于1670 Ma:来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMS U-Pb年龄的约束[J].地学前缘,18(3):108-120.
刘昌实,陈小明,陈培荣,王汝成,胡欢.2003.A型岩套的分类、判别标志和成因[J].高校地质学报,9(4):573-591.
陆松年,李怀坤,李惠民,宋彪,王世炎,周红英,陈志宏.2003.华北克拉通南缘龙王石童碱性花岗岩U-Pb年龄及其地质意义[J].地质通报,22(12):762-768.
李长民.2009.锆石成因矿物学与锆石微区定年综述[J],地质调查与研究,33(3):161-174.
李承东,赵利刚,常青松,许雅雯,王世炎,许腾.2017.豫西洛峪口组凝灰岩锆石LA-MC-ICPMS U-Pb年龄及地层归属讨论[J].中国地质,44(3):511-525.
廖超林,王岳军,彭头平.2003.太行山南段早元古代基性脉岩的40Ar-39Ar年代学及其构造意义[J].大地构造与成矿学,27(4):354-361.
澎澎,刘富,翟明国,郭敬辉.2011.密云岩墙群的时代对长城系底界年龄的制约[J].科学通报,56(35):2975-2980.
乔秀夫,王彦斌.华北克拉通中元古界底界年龄与盆地性质讨论[J].地质学报,2014,88(9):1623-1637.
苏德辰,李春旺,孙爱萍,乔秀夫.2017.太行山北缘中元古界发现泥火山群[J].中国地质,44(2):399-400.
苏文博,李怀坤,徐莉,贾松海,耿建珍,周红英,王志宏,蒲含勇.2012.华北克拉通南缘洛峪群-汝阳群属于中元古界长城系--河南汝州洛峪口组层凝灰岩锆石LA-MC-ICPMS U-Pb年龄的直接约束[J].地质调查与研究,35(2):96-108.
万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志.2009.登封地区早前寒武纪地壳演化--地球化学和锆石SHRIMP U-Pb年代学制约[J].地质学报,83(7):982-999.
武铁山,1979.山西的震旦系,山西省1∶20万断代地层总结[R].山西省地矿局区调队.
王启超,武铁山,徐朝雷.1980.太行-五台区震旦亚界及其与滹沱超群的关系[C]//中国地质科学院天津地质矿产研究所编.中国震旦亚界.天津:天津科学技术出版社.
王同和,1992.华北克拉通中腰纬向构造带的特征及演化[J].山西地质,7(3):301-312.
吴才来,董树文,王陆太,王次松,雷敏,吴迪.2015.铜陵矿集区深部发现126 Ma的正长花岗岩:来自3000 m科学钻探的证据[J].中国地质,2016,43(5):1495-1513.
吴锁平,王梅英,戚开静.2007.A型花岗岩研究现状及其述评[J].岩石矿物学杂志,26(1):57-66.
薛良伟,尉向东,赵太平.1996.嵩山A型花岗岩的地质地球化学特征和构造环境[J].岩石学报,12(1):137-144.
曾茜,陈守余,赵江南.2016.个旧卡房蚀变花岗岩地球化学特征及其与成矿的关系[J].地质找矿论丛,31(2):163-171.
赵太平,邓小芹,胡国辉,周艳艳,彭澎,翟明国.2015.华北克拉通古/中元古代界线和相关地质问题讨论[J].岩石学报,31(6):1495-1508.
赵太平,周美夫,金成伟,关鸿,李惠民.2001.华北陆块南缘熊耳群形成时代讨论[J].地质科学,36(3):326-334.
赵太平,金成伟,翟明国,夏斌,周美夫.2002.华北陆块南部熊耳群火山岩的地球化学特征与成因[J].岩石学报,18(1):59-69.
赵太平,徐勇航,翟明国.2007.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议[J].高校地质学报,13(2):191-206.
张旗,冉皞,李承东.2012.A型花岗岩的实质是什么?[J]岩石矿物学杂志,31(4):621-626.
张旗.2013.A型花岗岩的标志和判别--兼答汪洋等对“A型花岗岩的实质是什么”的质疑[J].岩石矿物学杂志,32(2):267-272.
(1)河南省地质调查院.2015.河南1∶5万东姚集、临淇镇、鹤壁、庙口幅区域地质调查报告.
(2)山西省地质调查院.2007.1∶25万新乡市幅区域地质调查报告.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |