突泉盆地突D2井林西组碎屑岩LA-ICP-MS锆石U-Pb年龄及地质意义
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摘要
内蒙古突泉盆地南部突D2井钻遇厚层的暗色泥岩,发现具有晚二叠世特征的孢粉化石。为获取精确的地层同位素年龄,对500.0m井段发育的粉砂岩进行碎屑锆石LA-ICP-MS U-Pb同位素测试分析,得到100颗锆石的谐和—近谐和年龄。结果表明:碎屑锆石按年龄和频率分布特征可以分为5组:245.0～279.0 Ma(12颗,占12%),峰值年龄为263.0 Ma;282.0～346.0Ma(48颗,占48%);355.0～531.0Ma(21颗,占21%);615.0～993.0Ma(6颗,占6%);1.022～2.163Ga(13颗,占13%,207Pb/206Pb年龄)。最小年龄段年龄的加权平均为(261.7±6.2)Ma(MSWD=0.93,12颗),与最小峰值263.0 Ma的年龄吻合,测年样品沉积时间下限为263.0 Ma,沉积时代为晚二叠世,证实突泉盆地存在林西组暗色泥岩,以及大地电磁测深剖面上存在的第二套广泛连续发育的低阻层为林西组。沉积物源具有多样性和复杂性,主体来自东北各地块,同时存在华北板块和西伯利亚板块的物源信息((1.658±0.023)、(1.877±0.016)、(1.891±0.041)、(2.163±0.011)Ga)。林西组沉积时期,华北板块与西伯利亚板块开始俯冲碰撞过程,最终闭合时间在晚二叠世之后。
A geologic well TD2 was deployed in the southern part of the Tuquan Basin,and thick layersof dark mudstone were drilled.Sphale fossils of the Late Permian age were found in the mudstone.The LA-ICP-MS U-Pb isotope test was performed on the zircons from the sample TD2-500 TWS of siltstone.The harmonic-near harmonics and ages of the 100 zircons were obtained and cited.The 100 detrital zircons can be divided into five groups according to age and frequency distribution characteristics:245.0～279.0 Ma(n=12,ca.12%)with peak age at 263.0 Ma,282.0～346.0 Ma(n=48,ca.48%),355.0～531.0 Ma(n=21,ca.21%),615.0～993.0 Ma(n=6,ca.6%),1.022～2.163 Ga(n=13,ca.13%,207 Pb/206 Pb age).The weighted average age for the youngest age group is(261.7±6.2)Ma(MSWD=0.93,n=12),which coincided with the minimum peak age of 263.0 Ma.It was speculated that the maximum depositional age of the Linxi Formation is 263.0 Ma.Combined with paleontological fossil data,it indicates that the sedimentary age should be the Late Permian,which confirms the existence of thick layered dark mudstones in the Tuquan Basin.It is also proved that the second set of widely-developed conductive layers on the magnetotelluric survey profile is the Linxi Formation,which is great significance for the deep-seated oil and gas geological exploration in the northeast.The detrital zircon age spectrum value indicates the diversity and complexity of its sediment source,the main body should come from all over the northeast,and there are provenance information of North China plate and Siberian plate((1.658±0.023),(1.877±0.016),(1.891±0.041),(2.163±0.011)Ga),suggesting that the North China plate and the Siberian plate may begin the subduction collision process during the deposition period of the Linxi Formation.The peak age of the youngest group of detrital zircons obtained this time is 263.0 Ma,indicating that the final closing time of the North China plate and the Siberian plate should be after the Late Permian.
A geologic well TD2 was deployed in the southern part of the Tuquan Basin,and thick layersof dark mudstone were drilled.Sphale fossils of the Late Permian age were found in the mudstone.The LA-ICP-MS U-Pb isotope test was performed on the zircons from the sample TD2-500 TWS of siltstone.The harmonic-near harmonics and ages of the 100 zircons were obtained and cited.The 100 detrital zircons can be divided into five groups according to age and frequency distribution characteristics:245.0～279.0 Ma(n=12,ca.12%)with peak age at 263.0 Ma,282.0～346.0 Ma(n=48,ca.48%),355.0～531.0 Ma(n=21,ca.21%),615.0～993.0 Ma(n=6,ca.6%),1.022～2.163 Ga(n=13,ca.13%,207 Pb/206 Pb age).The weighted average age for the youngest age group is(261.7±6.2)Ma(MSWD=0.93,n=12),which coincided with the minimum peak age of 263.0 Ma.It was speculated that the maximum depositional age of the Linxi Formation is 263.0 Ma.Combined with paleontological fossil data,it indicates that the sedimentary age should be the Late Permian,which confirms the existence of thick layered dark mudstones in the Tuquan Basin.It is also proved that the second set of widely-developed conductive layers on the magnetotelluric survey profile is the Linxi Formation,which is great significance for the deep-seated oil and gas geological exploration in the northeast.The detrital zircon age spectrum value indicates the diversity and complexity of its sediment source,the main body should come from all over the northeast,and there are provenance information of North China plate and Siberian plate((1.658±0.023),(1.877±0.016),(1.891±0.041),(2.163±0.011)Ga),suggesting that the North China plate and the Siberian plate may begin the subduction collision process during the deposition period of the Linxi Formation.The peak age of the youngest group of detrital zircons obtained this time is 263.0 Ma,indicating that the final closing time of the North China plate and the Siberian plate should be after the Late Permian.
引文
[1]刘晓艳,杜鸿烈,陈章明,等.松辽盆地边缘石炭—二叠系地表石油显示及其地质意义[J].地球化学,2001,30(4):390-394.LIU Xiaoyan,DU Honglie,CHEN Zhangming,et al.Show of petroleum of C-P systems on the earth's surface at the edge of Songliao Basin and its geological significance[J].Geochimica,2001,30(4):390-394.
[2]徐浩,解启来,王嗣敏,等.内蒙古东部中上二叠统烃源岩地化特征与生烃潜力评价[J].大庆石油地质与开发,2017,36(1):35-42.XU Hao,XIE Qilai,WANG Simin,et al.Geochemical characteristics and hydrocarbonge generating potential for Middle-Upper Permian source rocks in east Inner Mongolia[J].Pertoleum Geology and Oilfield Development in Daqing,2017,36(1):35-42.
[3]张健,卞雄飞,陈树旺,等.大兴安岭中南部上二叠统林西组页岩气资源前景[J].地质通报,2013,32(8):1297-1306.ZHANG Jian,BIAN Xiongfei,CHEN Shuwang,et al.Shale gas resources prospect of Late Permian Linxi Formation in the middlesouthern part of the Da Hinggan Mountains[J].Geological Bulletin of China,2013,32(8):1297-1306.
[4]任战利,萧德铭,迟元林.松辽盆地基底石炭—二叠系烃源岩生气期研究[J].自然科学进展,2006,16(8):974-979.REN Zhanli,XIAO Deming,CHI Yuanlin,et al.Study on the gasification period of the Carboniferous-Permian source rocks in the Songliao Basin[J].Natural Science Progress,2006,16(8):974-979.
[5]陈章明,关德师.东北地区深层石油地质综合研究与目标评价[R].安达:大庆石油学院,2000:115-128.CHEN Zhangming,GUAN Deshi.Comprehensive research and target evaluation of deep petroleum geology in Northeast China[R].Anda:Daqing Petroleum Institute,2000:115-128.
[6]张鹏辉,钟清,方慧,等.突泉盆地南部结构及含油气远景[J].物探与化探,2015,39(6):1284-1291.ZHANG Penghui,ZHONG Qing,FANG Hui,et al.A study of the structure of southern Tuquan Basin and oil-gas prospect based on magnetotelluric sounding[J].Geophysical and Geochemical Exploration,2015,39(6):1284-1291.
[7]方慧,钟清,陈树旺.内蒙古突泉盆地双低阻层的发现及其地质意义[J].地质通报,2013,32(8):1253-1259.FANG Hui,ZHONG Qing,CHEN Shuwang.The discovery of two conductive layers in Tuquan Basin,Inner Mongolia,and its geological significance[J].Geological Bulletin of China,2013,32(8):1253-1259.
[8]李世臻,周新桂,王丹丹,等.内蒙古突泉盆地突参1井原油地球化学特征与油源分析[J].地质通报,2015,34(10):1946-1951.LI Shizhen,ZHOU Xingui,WANG Dandan,et al.Geochemical characteristics of crude oil and oil-source correlation of well Tucan 1,Tuquan Basin,Inner Mongolia[J].Geological Bulletin of China,2015,34(10):1946-1951.
[9]陈树旺,张健,公繁浩,等.内蒙古突泉盆地侏罗系油气发现及工作展望[J].地质与资源,2015,24(1):1-6.CHEN Shuwang,ZHANG Jian,GONG Fanhao,et al.Discovery and prospects of the Jurassic oil and gas in Tuquan Basin,Inner Mongolia[J].Geology and Resources,2015,24(1):1-6.
[10]苏飞,李臻,张健,等.内蒙古突泉盆地突D2井上二叠统林西组烃源岩新发现[J].地质与资源,2017,26(3):268-274.SU Fei,LI Zhen,ZHANG Jian,et al.Discovery of the soure rock from Upper Permain Linxi Formation In Tuquan Basin,Inner Mongolia[J].Geology and Resources,2017,26(3):268-274.
[11]王杰,陈树旺,丁秋红.内蒙古突泉盆地中侏罗统万宝组碎屑岩LAICP-MS锆石U-Pb测年、地球化学特征及对源区的制约[J].地质通报,2013,32(8):1224-1235.WANG Jie,CHEN Shuwang,DING Qiuhong.Zircon U-Pb dating and geochemical characteristics of detrital rocks and their constraints on the provenance of Middle Jurassic Wanbao Formation in Tuquan Basin[J].Geological Bulletin of China,2013,32(8):1224-1235.
[12]丁秋红,陈树旺,张立君,等.松辽盆地外围油气新区中生代地层研究新进展[J].地质通报,2013,32(8):1159-1176.DING Qiuhong,CHEN Shuwang,ZHANG Lijun,et al.New research progress of the Mesozoic strata in new areas on the periphery of Songliao Basin[J].Geological Bulletin of China,2013,32(8):1159-1176.
[13]丁秋红,陈树旺,郑月娟,等.大兴安岭地区突泉盆地侏罗系充填序列及暗色泥岩发育特征[J].地质与资源,2010,19(3):203-207.DING Qiuhong,CHEN Shuwang,ZHENG Yuejuan,et al.The development of melamudstone and the Jurassic filling sequence in Tuquan Basin,Daxinganling Region[J].Geology and Resources,2010,19(3):203-207.
[14]王丹丹,李世臻,周新桂,等.大兴安岭地区突泉盆地高精度重磁电特征及其构造格架[J].吉林大学学报(地球科学版),2016,46(1):240-253.WANG Dandan,LI Shizhen,ZHOU Xingui,et al.Lithology lithofacies identification and deep structure of Tuquan Basin in Great Xinggan Range Area based on high-precision gravity-magnetic-electrical survey[J].Journal of Jilin University(Earth Science Edition),2016,46(1):240-253.
[15]宋彪,张玉海,万渝生,等.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论[J].地质论评,2002,48(增刊):26-30.SONG Biao,ZHANG Yuhai,WAN Yusheng,et al.Mount making and procedure of the SHRIMP dating[J].Geological Review,2002,48(Supp.):26-30.
[16]PEARCE N J G,PERKINS W T,WESTGATE J A,et al.Acompilation of new and published major and trace element data for NIST SRM 610and NIST SRM 612glass reference materials[J].Geostandards Newsletter,1997,21(1):115-144.
[17]BLACK L P,KAMO S L,ALLEN C M,et al.TEMORA 1:a new zircon standard for Phanerozoic U-Pb geochronology[J].Chemical Geology,2003,200,155-170.
[18]李献华,唐国强,龚冰,等.Qinghu(清湖)锆石:一个新的U-Pb年龄和O,Hf同位素微区分析工作标样[J].科学通报,2013,58(20):1954-1961.LI Xianhua,TANG Guoqiang,GONG Bing,et al.Qinghu zircon:a working reference for microbeam analysis of U-Pb age and Hf and O isotopes[J].Chinese Science Bulletin,2013,58(20):1954-1961.
[19]ANDERSON T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192:59-79.
[20]郑月娟,张健,陈树旺,等.内蒙古阿鲁科尔沁旗陶海营子剖面林西组化石新发现[J].地质通报,2013,23(8):1269-1276.ZHENG Yuejuan,ZHANG Jian,CHEN Shuwang,et al.New fossil discovery along the section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner,Inner Mongolia[J].Geological Bulletin of China,2013,32(8):1269-1276.
[21]张永生,牛绍武,田树刚,等.内蒙古林西地区上二叠统林西组叶肢介化石的发现及其意义[J].地质通报,2012,31(9):1394-1403.ZHANG Yongsheng,NIU Shaowu,TIAN Shugang,et al.The discovery of conchostracan fossils in the Upper Permian Linxi Formation of Linxi Area,Inner Mongolia,and its geological significance[J].Geological Bulletin of China,2012,31(9):1394-1403.
[22]张渝金,张超,郭威,等.内蒙古阿鲁科尔沁旗林西组植物化石新材料[J].地质与资源,2017,26(4):333-338.ZHANG Yujin,ZHANG Chao,GUO Wei,et al.New fossil materials of Late Permian plants from Linxi Formation In Ar Horqin Qi,Inner Mongolia[J].Geology and Resources,2017,26(4):333-338.
[23]张兴州,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):205-212.ZHANG Xingzhou,QIAO Dewu,CHI Xiaoguo,et al.Late Paleozoic tectonic evolution and oilgas potentiality in Northeastern China[J].Geological Bulletin of China,2011,30(2/3):205-212.
[24]宋卫卫,周建波,郭晓丹,等.松辽地块大地构造属性:古生界碎屑锆石年代学的制约[J].世界地质,2012,31(3):522-535.SONG Weiwei,ZHOU Jianbo,GUO Xiaodan,et al.Geotectonic setting of Songliao Block:reatriction from Paleozoic detrital zircon U-Pb dating[J].Global Geology,2012,31(3):522-535.
[25]韩国卿,刘永江,温泉波,等.西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J].地球科学,2011,36(4):687-702.HAN Guoqing,LIU Yongjiang,WEN Quanbo,et al.LA-ICP-MS U-Pb dating of detrital zircons from the Permian sandstones in north side of Xar Moron River suture belt and its tectonic implications[J].Earth Science,2011,36(4):687-702.
[26]韩杰,周建波,张兴洲,等.内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义[J].地质通报,2011,30(2/3):258-269.HAN Jie,ZHOU Jianbo,ZHANG Xingzhou,et al.Detrital zircon U-Pb dating from sandstone of the Upper Permian Linxi Formation,Linxi Area,Inner Mongolia,China and its tectonic implications[J].Geological Bulletin of China,2011,30(2/3):258-269.
[27]张海华,郑月娟,陈树旺,等.内蒙古巴林左旗二叠系碎屑锆石LA-ICP-MS U-Pb年龄及构造意义[J].地质学报,2015,89(10):1703-1717.ZHANG Haihua,ZHENG Yuejuan,CHEN Shuwang,et al.LA-ICP-MS U-Pb geochronology of detrital zircons from Permian in Baarin Left Banner of Inner Mogolia and its tectonic significance[J].Acta Geologica Sinica,2015,89(10):1703-1717.
[28]郑月娟,张海华,陈树旺,等.内蒙古阿鲁科尔沁旗林西组砂岩LA-ICP-MS锆石U-Pb年龄及意义[J].地质通报,2014,33(9):1293-1307.ZHENG Yuejuan,ZHANG Haihua,CHEN Shuwang,et al.U-Pb age of detrital zircons from Late Permian Linxi Formation in Aluke'erqin Qi,Inner Mogolia[J].Geological Bulletin of China,2014,33(9):1293-1307.
[29]陈树旺,张海华,郑月娟,等.内蒙古科右中旗—突泉地区晚二叠世林西组碎屑岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2015,34(10):1869-1877.CHEN Shuwang,ZHANG Haihua,ZHENG Yuejuan,et al.Detrital zircon LA-ICP-MS U-Pb age of the Late Permian Linxi Formation in Horqin Right Wing Middle Banner-Tuquan area of Inner Mongolia and its geological significance[J].Geological Bulletin of China,2015,34(10):1869-1877.
[30]李益龙,周汉文,钟增球,等.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据[J].地球科学,2009,34(6):931-938.LI Yilong,ZHOU Hanwen,ZHONG Zengqiu,et al.Collision processes of North China and Siberian Plates:evidence from LA-ICP-MS zircon U-Pb age on deformed granite in Xar Moron suture zone[J].Earth Science,2009,34(6):931-938.
[31]李益龙,周汉文,肖文交,等.古亚洲构造域和西太平洋构造域在索伦缝合带东段的叠加:来自内蒙古林西县西拉木伦断裂带内变形闪长岩的岩石学、地球化学和年代学证据[J].地球科学,2012,37(3):433-450.LI Yilong,ZHOU Hanwen,XIAO Wenjiao,et al.Superposition of Paleo-Asian and West-Pacific tectonic domains in the eastern section of the Solonker suture zone:insight from petrology,geochemistry and geochronology of deformde diorite in Xar Moron fault zone,Inner Mongolia[J].Earth Science,2012,37(3):433-450.
[32]郑月娟,黄欣,陈树旺,等.内蒙古巴林右旗下三叠统幸福之路组凝灰岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2015,33(2/3):370-377.ZHENG Yuejuan,HUANG Xin,CHEN Shuwang,et al.LA-ICP-MS zircon U-Pb age of the tuffs of the Lower Triassic Xingfuzhilu Formation in Bairin Right Banner,Inner Mongolia[J].Geological Bulletin of China,2013,33(2/3):370-377.
[33]高德臻,将干清.内蒙古苏尼特左旗二叠系的重新厘定及大地构造演化分析[J].中国区域地质,1998,17(4):403-411.GAO Dezhen,JIANG Ganqing.Revision of the stratigraphic division of the Permian and tectonic evolution in the sonid left Banner,Inner Mongolia[J].Region Geology of China,1998,17(4):403-411.
[34]邓胜徽,万传彪,杨建国.黑龙江阿城晚二叠世安加拉—华夏混生植物群—兼述古亚洲洋的关闭问题[J].中国科学(D辑:地球科学),2009,39(12):1744-1752.DENG Shenghui,WAN Chuanbiao,YANG Jianguo,et al.Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean[J].Science China(Series D:Earth Sciences),2009,39(12):1744-1752.
[35]李朋武,高锐,管烨,等.内蒙古中部索伦林西缝合带封闭时代的古地磁分析[J].吉林大学学报(地球科学版),2006,36(5):744-758.LI Pengwu,GAO Rui,GUAN Ye,et al.Palaeomagnetic constraints on the final closure time of Solonker Linxi Suture[J].Journal of Jilin University(Earth Science Edition),2006,36(5):744-758.
[36]秦华峰,李永飞,黄晟,等.内蒙古阿鲁科尔沁旗二叠纪地层古地磁研究结果及其构造意义[J].地质通报,2013,32(2/3):388-398.QIN Huafeng,LI Yongfei,HUANG Sheng,et al.Palaeomagnetic investigation of Permain sandstone in Taohaiyingzi Area of Inner Mongolia and its tectonic significance[J].Geological Bulletin of China,2013,32(2/3):388-398.
[37]洪大卫,黄怀曾,肖宜君,等.内蒙古中部二叠纪碱性花岗岩及其地球动力学意义[J].地质学报,1994,68(3):219-230.HONG Dawei,HUANG Huaizeng,XIAO Yijun,et al.The Permian alkaline granites in central Inner Mongolia and thelr geodynamic significance[J].Acta geologica sinica,1994,68(3):219-230.
[38]CHEN B,JAHN B M,TIAN W.Evolution of the Solonker suture zone:constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and fo-rearc sediments[J].Journal of Asian Earth Sciences,2009,34(3):245-257.
[39]石玉若,刘敦一,简平,等.内蒙古中部苏尼特左旗富钾花岗岩锆石SHRIMP U-Pb年龄[J].地质通报,2005,24(5):424-428.SHI Yuruo,LIU Dunyi,JIAN Ping,et al.Zircon SHRIMP dating of K-rich granites in Sonid Zuoqi,central Inner Mongolia[J].Geological Bulletin of China,2005,24(5):424-428.
[40]石玉若,刘敦一,张旗,等.内蒙古中部苏尼特左旗地区三叠纪A型花岗岩锆石SHRIMP U-Pb年龄及其区域构造意义[J].地质通报,2007,26(2):183-189.SHI Yuruo,LIU Dunyi,ZHANG Qi,et al.SHRIMP U-Pb zircon dating of Triassic A-type granites in Sonid Zuoqi,central Inner Mongolia,China and its tectonic implications[J].Geological Bulletin of China,2007,26(2):183-189.
[41]刘建峰.内蒙古林西—东乌旗地区晚古生代岩浆作用及其对区域构造演化的制约[D].长春:吉林大学,2009:58-64.LIU Jianfeng.Late Paleozoic magmatism in the Linxi-Dongwuqi Area,Inner Mongolia,and its constraints on regional tectonic evolution[D].Changchun:Jilin University,2009:58-64.
[42]施光海,刘敦一,张福勤,等.中国内蒙古锡林郭勒杂岩SHRIMP锆石U-Pb年代学及意义[J].科学通报,2003,48:2187-2192.SHI Guanghai,LIU Dunyi,ZHANG Fuqin,et al.SHRIMP zircon U-Pb geochronology and its significance in the Xilinguole Complex rock,Inner Mongolia,China[J].Chinese Science Bulletin,2003,48:2187-2192.
[43]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,2011,4:1-30.
[44]辛后田,滕学建,程银行.内蒙古东乌旗宝力高庙组地层划分及其同位素年代学研究[J].地质调查与研究,2011,34(1):1-9.XIN Houtian,TENG Xuejian,CHENG Yinhang.Stratigraphic subdivision and isotope geochronology study on the Baoligaomiao Formation in the East Ujimqin County,Inner Mongolia[J].Geological Survey and Research,2011,34(1):1-9.
[45]潘世语,迟效国,孙巍,等.内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义[J].世界地质,2012,31(1):40-50.PAN Shiyu,CHI Xiaoguo,SUN Wei,et al.Geochemical characteristics and tectonic significance of Late Carboniferous volcanic rocks in Benbatu Formation of Sonid Youqi,Inner Mongolia[J].Global Geology,2012,31(1):40-50.
[46]鲍庆中,张长捷,吴之理,等.内蒙古白音高勒地区石炭纪石英闪长岩SHRIMP锆石U-Pb年代学及其意义[J].吉林大学学报(地球科学版),2007,37(1):15-23.BAO Qingzhong,ZHANG Changjie,WU Zhili,et al.SHRIMP U-Pb zircon geochronology of a Carboniferous quartz diorite in Baiyingaole Area,Inner Mongolia and its implications[J].Journal of Jilin University(Earth Science Edition),2007,37(1):15-23.
[47]裴福萍,许文良,杨德彬,等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J].科学通报,2006,51(24):2881-2887.PEI Fuping,XU Wenliang,YANG Debin,et al.Zircon U-Pb Geochronology and its geological significance in basal metamorphic rocks,Songliao Basin[J].Chinese Science Bulletin,2006,51(24):2881-2887.
[48]LIU J F,CHI X G,DONG C Y,et al.Discovery of Early Paleozoic granites in the eastern Xiao Hinggan Mountains,Northeastern China and their tectonic significance[J].Geological Bulletin of China,2008,27:534-544.
[49]ZHOU J B,WILDE S A,ZHANG X Z,et al.Pan-African metamorphic rocks of the Erguna massif in the Great Xing'an Range,NE China:evidence and tectonic implications[J].Tectonophysics,2011,499(1/2/3/4):105-117.
[50]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(5):591-601.
[51]STEM J R.Neoproterozoic crustal growth:the solid earth system during a critical episode of earth history[J].Gondwana Research,2008,14:33-50.
[52]WILDE S A,ZHANG X Z,WU F Y.Extension of a newly-identified 500Ma metamorphic terrain in Northeast China:further U-Pb SHRIMP dating of the Mashan Complex,Heilongjiang Province,China[J].Tectonophysics,2000,328:115-130.
[53]颉颃强,张福勤,苗来成,等.东北牡丹江地区“黑龙江群”中斜长角闪岩与花岗岩的锆石SHRIMP U-Pb定年及其地质意义[J].岩石学报,2008,24(6):1237-1250.XIE Heqiang,ZHANG Fuqin,MIAO Laicheng,et al.Zircon SHRIMP U-Pb dating of the amphibolite from"Heilongjiang Group"and the granite in Mudanjiang Area,NE China,and its geological significance[J].Acta Petrologica Sinica,2008,24(6):1237-1250.
[54]章凤奇,陈汉林,董传万,等.松辽盆地北部存在前寒武纪基底的证据[J].中国地质,2008,35(3):421-428.ZHANG Fengqi,CHEN Hanlin,DONG Chuanwan,et al.Evidence for the existence of Precambrian basement under the northern Songliao Basin[J].Chinese Geology,2008,35(3):421-428.
[55]葛文春,隋振民,吴福元,等.2007.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义[J].岩石学报,2007,23(2):423-440.GEWenchun,SUIZhenmin,WUFuyuan,etal.ZirconU-Pbages,Hfisotopiccharacterristicsandtheir implications of the Early Paleozoic granites in the northeastern Da Hinggan Mts.,Northeastern China[J].Acta Petrologica Sinica,2007,23(2):423-440.
[56]GUO J H,SUN M,CHEN F K,et al.Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan Area,North China Craton:timing of Paleoproterozoic continental collision[J].Journal of Asian Earth Sciences,2005,24:629-642.
[57]KELTY T K,YIN A,DASH B,et al.Detrital-zircon geochronology of Paleozoic sedimentary rock in the Hangay-Hentey Basin,north-central Mongolia:implications for the tectonic evolution of the Mongol-Okhotsk Ocean in central Asia[J].Tectonophysics,2008,451:97-122.
[2]徐浩,解启来,王嗣敏,等.内蒙古东部中上二叠统烃源岩地化特征与生烃潜力评价[J].大庆石油地质与开发,2017,36(1):35-42.XU Hao,XIE Qilai,WANG Simin,et al.Geochemical characteristics and hydrocarbonge generating potential for Middle-Upper Permian source rocks in east Inner Mongolia[J].Pertoleum Geology and Oilfield Development in Daqing,2017,36(1):35-42.
[3]张健,卞雄飞,陈树旺,等.大兴安岭中南部上二叠统林西组页岩气资源前景[J].地质通报,2013,32(8):1297-1306.ZHANG Jian,BIAN Xiongfei,CHEN Shuwang,et al.Shale gas resources prospect of Late Permian Linxi Formation in the middlesouthern part of the Da Hinggan Mountains[J].Geological Bulletin of China,2013,32(8):1297-1306.
[4]任战利,萧德铭,迟元林.松辽盆地基底石炭—二叠系烃源岩生气期研究[J].自然科学进展,2006,16(8):974-979.REN Zhanli,XIAO Deming,CHI Yuanlin,et al.Study on the gasification period of the Carboniferous-Permian source rocks in the Songliao Basin[J].Natural Science Progress,2006,16(8):974-979.
[5]陈章明,关德师.东北地区深层石油地质综合研究与目标评价[R].安达:大庆石油学院,2000:115-128.CHEN Zhangming,GUAN Deshi.Comprehensive research and target evaluation of deep petroleum geology in Northeast China[R].Anda:Daqing Petroleum Institute,2000:115-128.
[6]张鹏辉,钟清,方慧,等.突泉盆地南部结构及含油气远景[J].物探与化探,2015,39(6):1284-1291.ZHANG Penghui,ZHONG Qing,FANG Hui,et al.A study of the structure of southern Tuquan Basin and oil-gas prospect based on magnetotelluric sounding[J].Geophysical and Geochemical Exploration,2015,39(6):1284-1291.
[7]方慧,钟清,陈树旺.内蒙古突泉盆地双低阻层的发现及其地质意义[J].地质通报,2013,32(8):1253-1259.FANG Hui,ZHONG Qing,CHEN Shuwang.The discovery of two conductive layers in Tuquan Basin,Inner Mongolia,and its geological significance[J].Geological Bulletin of China,2013,32(8):1253-1259.
[8]李世臻,周新桂,王丹丹,等.内蒙古突泉盆地突参1井原油地球化学特征与油源分析[J].地质通报,2015,34(10):1946-1951.LI Shizhen,ZHOU Xingui,WANG Dandan,et al.Geochemical characteristics of crude oil and oil-source correlation of well Tucan 1,Tuquan Basin,Inner Mongolia[J].Geological Bulletin of China,2015,34(10):1946-1951.
[9]陈树旺,张健,公繁浩,等.内蒙古突泉盆地侏罗系油气发现及工作展望[J].地质与资源,2015,24(1):1-6.CHEN Shuwang,ZHANG Jian,GONG Fanhao,et al.Discovery and prospects of the Jurassic oil and gas in Tuquan Basin,Inner Mongolia[J].Geology and Resources,2015,24(1):1-6.
[10]苏飞,李臻,张健,等.内蒙古突泉盆地突D2井上二叠统林西组烃源岩新发现[J].地质与资源,2017,26(3):268-274.SU Fei,LI Zhen,ZHANG Jian,et al.Discovery of the soure rock from Upper Permain Linxi Formation In Tuquan Basin,Inner Mongolia[J].Geology and Resources,2017,26(3):268-274.
[11]王杰,陈树旺,丁秋红.内蒙古突泉盆地中侏罗统万宝组碎屑岩LAICP-MS锆石U-Pb测年、地球化学特征及对源区的制约[J].地质通报,2013,32(8):1224-1235.WANG Jie,CHEN Shuwang,DING Qiuhong.Zircon U-Pb dating and geochemical characteristics of detrital rocks and their constraints on the provenance of Middle Jurassic Wanbao Formation in Tuquan Basin[J].Geological Bulletin of China,2013,32(8):1224-1235.
[12]丁秋红,陈树旺,张立君,等.松辽盆地外围油气新区中生代地层研究新进展[J].地质通报,2013,32(8):1159-1176.DING Qiuhong,CHEN Shuwang,ZHANG Lijun,et al.New research progress of the Mesozoic strata in new areas on the periphery of Songliao Basin[J].Geological Bulletin of China,2013,32(8):1159-1176.
[13]丁秋红,陈树旺,郑月娟,等.大兴安岭地区突泉盆地侏罗系充填序列及暗色泥岩发育特征[J].地质与资源,2010,19(3):203-207.DING Qiuhong,CHEN Shuwang,ZHENG Yuejuan,et al.The development of melamudstone and the Jurassic filling sequence in Tuquan Basin,Daxinganling Region[J].Geology and Resources,2010,19(3):203-207.
[14]王丹丹,李世臻,周新桂,等.大兴安岭地区突泉盆地高精度重磁电特征及其构造格架[J].吉林大学学报(地球科学版),2016,46(1):240-253.WANG Dandan,LI Shizhen,ZHOU Xingui,et al.Lithology lithofacies identification and deep structure of Tuquan Basin in Great Xinggan Range Area based on high-precision gravity-magnetic-electrical survey[J].Journal of Jilin University(Earth Science Edition),2016,46(1):240-253.
[15]宋彪,张玉海,万渝生,等.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论[J].地质论评,2002,48(增刊):26-30.SONG Biao,ZHANG Yuhai,WAN Yusheng,et al.Mount making and procedure of the SHRIMP dating[J].Geological Review,2002,48(Supp.):26-30.
[16]PEARCE N J G,PERKINS W T,WESTGATE J A,et al.Acompilation of new and published major and trace element data for NIST SRM 610and NIST SRM 612glass reference materials[J].Geostandards Newsletter,1997,21(1):115-144.
[17]BLACK L P,KAMO S L,ALLEN C M,et al.TEMORA 1:a new zircon standard for Phanerozoic U-Pb geochronology[J].Chemical Geology,2003,200,155-170.
[18]李献华,唐国强,龚冰,等.Qinghu(清湖)锆石:一个新的U-Pb年龄和O,Hf同位素微区分析工作标样[J].科学通报,2013,58(20):1954-1961.LI Xianhua,TANG Guoqiang,GONG Bing,et al.Qinghu zircon:a working reference for microbeam analysis of U-Pb age and Hf and O isotopes[J].Chinese Science Bulletin,2013,58(20):1954-1961.
[19]ANDERSON T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192:59-79.
[20]郑月娟,张健,陈树旺,等.内蒙古阿鲁科尔沁旗陶海营子剖面林西组化石新发现[J].地质通报,2013,23(8):1269-1276.ZHENG Yuejuan,ZHANG Jian,CHEN Shuwang,et al.New fossil discovery along the section of Linxi Formation at Taohaiyingzi in Ar Horqin Banner,Inner Mongolia[J].Geological Bulletin of China,2013,32(8):1269-1276.
[21]张永生,牛绍武,田树刚,等.内蒙古林西地区上二叠统林西组叶肢介化石的发现及其意义[J].地质通报,2012,31(9):1394-1403.ZHANG Yongsheng,NIU Shaowu,TIAN Shugang,et al.The discovery of conchostracan fossils in the Upper Permian Linxi Formation of Linxi Area,Inner Mongolia,and its geological significance[J].Geological Bulletin of China,2012,31(9):1394-1403.
[22]张渝金,张超,郭威,等.内蒙古阿鲁科尔沁旗林西组植物化石新材料[J].地质与资源,2017,26(4):333-338.ZHANG Yujin,ZHANG Chao,GUO Wei,et al.New fossil materials of Late Permian plants from Linxi Formation In Ar Horqin Qi,Inner Mongolia[J].Geology and Resources,2017,26(4):333-338.
[23]张兴州,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):205-212.ZHANG Xingzhou,QIAO Dewu,CHI Xiaoguo,et al.Late Paleozoic tectonic evolution and oilgas potentiality in Northeastern China[J].Geological Bulletin of China,2011,30(2/3):205-212.
[24]宋卫卫,周建波,郭晓丹,等.松辽地块大地构造属性:古生界碎屑锆石年代学的制约[J].世界地质,2012,31(3):522-535.SONG Weiwei,ZHOU Jianbo,GUO Xiaodan,et al.Geotectonic setting of Songliao Block:reatriction from Paleozoic detrital zircon U-Pb dating[J].Global Geology,2012,31(3):522-535.
[25]韩国卿,刘永江,温泉波,等.西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J].地球科学,2011,36(4):687-702.HAN Guoqing,LIU Yongjiang,WEN Quanbo,et al.LA-ICP-MS U-Pb dating of detrital zircons from the Permian sandstones in north side of Xar Moron River suture belt and its tectonic implications[J].Earth Science,2011,36(4):687-702.
[26]韩杰,周建波,张兴洲,等.内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义[J].地质通报,2011,30(2/3):258-269.HAN Jie,ZHOU Jianbo,ZHANG Xingzhou,et al.Detrital zircon U-Pb dating from sandstone of the Upper Permian Linxi Formation,Linxi Area,Inner Mongolia,China and its tectonic implications[J].Geological Bulletin of China,2011,30(2/3):258-269.
[27]张海华,郑月娟,陈树旺,等.内蒙古巴林左旗二叠系碎屑锆石LA-ICP-MS U-Pb年龄及构造意义[J].地质学报,2015,89(10):1703-1717.ZHANG Haihua,ZHENG Yuejuan,CHEN Shuwang,et al.LA-ICP-MS U-Pb geochronology of detrital zircons from Permian in Baarin Left Banner of Inner Mogolia and its tectonic significance[J].Acta Geologica Sinica,2015,89(10):1703-1717.
[28]郑月娟,张海华,陈树旺,等.内蒙古阿鲁科尔沁旗林西组砂岩LA-ICP-MS锆石U-Pb年龄及意义[J].地质通报,2014,33(9):1293-1307.ZHENG Yuejuan,ZHANG Haihua,CHEN Shuwang,et al.U-Pb age of detrital zircons from Late Permian Linxi Formation in Aluke'erqin Qi,Inner Mogolia[J].Geological Bulletin of China,2014,33(9):1293-1307.
[29]陈树旺,张海华,郑月娟,等.内蒙古科右中旗—突泉地区晚二叠世林西组碎屑岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2015,34(10):1869-1877.CHEN Shuwang,ZHANG Haihua,ZHENG Yuejuan,et al.Detrital zircon LA-ICP-MS U-Pb age of the Late Permian Linxi Formation in Horqin Right Wing Middle Banner-Tuquan area of Inner Mongolia and its geological significance[J].Geological Bulletin of China,2015,34(10):1869-1877.
[30]李益龙,周汉文,钟增球,等.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据[J].地球科学,2009,34(6):931-938.LI Yilong,ZHOU Hanwen,ZHONG Zengqiu,et al.Collision processes of North China and Siberian Plates:evidence from LA-ICP-MS zircon U-Pb age on deformed granite in Xar Moron suture zone[J].Earth Science,2009,34(6):931-938.
[31]李益龙,周汉文,肖文交,等.古亚洲构造域和西太平洋构造域在索伦缝合带东段的叠加:来自内蒙古林西县西拉木伦断裂带内变形闪长岩的岩石学、地球化学和年代学证据[J].地球科学,2012,37(3):433-450.LI Yilong,ZHOU Hanwen,XIAO Wenjiao,et al.Superposition of Paleo-Asian and West-Pacific tectonic domains in the eastern section of the Solonker suture zone:insight from petrology,geochemistry and geochronology of deformde diorite in Xar Moron fault zone,Inner Mongolia[J].Earth Science,2012,37(3):433-450.
[32]郑月娟,黄欣,陈树旺,等.内蒙古巴林右旗下三叠统幸福之路组凝灰岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2015,33(2/3):370-377.ZHENG Yuejuan,HUANG Xin,CHEN Shuwang,et al.LA-ICP-MS zircon U-Pb age of the tuffs of the Lower Triassic Xingfuzhilu Formation in Bairin Right Banner,Inner Mongolia[J].Geological Bulletin of China,2013,33(2/3):370-377.
[33]高德臻,将干清.内蒙古苏尼特左旗二叠系的重新厘定及大地构造演化分析[J].中国区域地质,1998,17(4):403-411.GAO Dezhen,JIANG Ganqing.Revision of the stratigraphic division of the Permian and tectonic evolution in the sonid left Banner,Inner Mongolia[J].Region Geology of China,1998,17(4):403-411.
[34]邓胜徽,万传彪,杨建国.黑龙江阿城晚二叠世安加拉—华夏混生植物群—兼述古亚洲洋的关闭问题[J].中国科学(D辑:地球科学),2009,39(12):1744-1752.DENG Shenghui,WAN Chuanbiao,YANG Jianguo,et al.Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean[J].Science China(Series D:Earth Sciences),2009,39(12):1744-1752.
[35]李朋武,高锐,管烨,等.内蒙古中部索伦林西缝合带封闭时代的古地磁分析[J].吉林大学学报(地球科学版),2006,36(5):744-758.LI Pengwu,GAO Rui,GUAN Ye,et al.Palaeomagnetic constraints on the final closure time of Solonker Linxi Suture[J].Journal of Jilin University(Earth Science Edition),2006,36(5):744-758.
[36]秦华峰,李永飞,黄晟,等.内蒙古阿鲁科尔沁旗二叠纪地层古地磁研究结果及其构造意义[J].地质通报,2013,32(2/3):388-398.QIN Huafeng,LI Yongfei,HUANG Sheng,et al.Palaeomagnetic investigation of Permain sandstone in Taohaiyingzi Area of Inner Mongolia and its tectonic significance[J].Geological Bulletin of China,2013,32(2/3):388-398.
[37]洪大卫,黄怀曾,肖宜君,等.内蒙古中部二叠纪碱性花岗岩及其地球动力学意义[J].地质学报,1994,68(3):219-230.HONG Dawei,HUANG Huaizeng,XIAO Yijun,et al.The Permian alkaline granites in central Inner Mongolia and thelr geodynamic significance[J].Acta geologica sinica,1994,68(3):219-230.
[38]CHEN B,JAHN B M,TIAN W.Evolution of the Solonker suture zone:constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and fo-rearc sediments[J].Journal of Asian Earth Sciences,2009,34(3):245-257.
[39]石玉若,刘敦一,简平,等.内蒙古中部苏尼特左旗富钾花岗岩锆石SHRIMP U-Pb年龄[J].地质通报,2005,24(5):424-428.SHI Yuruo,LIU Dunyi,JIAN Ping,et al.Zircon SHRIMP dating of K-rich granites in Sonid Zuoqi,central Inner Mongolia[J].Geological Bulletin of China,2005,24(5):424-428.
[40]石玉若,刘敦一,张旗,等.内蒙古中部苏尼特左旗地区三叠纪A型花岗岩锆石SHRIMP U-Pb年龄及其区域构造意义[J].地质通报,2007,26(2):183-189.SHI Yuruo,LIU Dunyi,ZHANG Qi,et al.SHRIMP U-Pb zircon dating of Triassic A-type granites in Sonid Zuoqi,central Inner Mongolia,China and its tectonic implications[J].Geological Bulletin of China,2007,26(2):183-189.
[41]刘建峰.内蒙古林西—东乌旗地区晚古生代岩浆作用及其对区域构造演化的制约[D].长春:吉林大学,2009:58-64.LIU Jianfeng.Late Paleozoic magmatism in the Linxi-Dongwuqi Area,Inner Mongolia,and its constraints on regional tectonic evolution[D].Changchun:Jilin University,2009:58-64.
[42]施光海,刘敦一,张福勤,等.中国内蒙古锡林郭勒杂岩SHRIMP锆石U-Pb年代学及意义[J].科学通报,2003,48:2187-2192.SHI Guanghai,LIU Dunyi,ZHANG Fuqin,et al.SHRIMP zircon U-Pb geochronology and its significance in the Xilinguole Complex rock,Inner Mongolia,China[J].Chinese Science Bulletin,2003,48:2187-2192.
[43]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,2011,4:1-30.
[44]辛后田,滕学建,程银行.内蒙古东乌旗宝力高庙组地层划分及其同位素年代学研究[J].地质调查与研究,2011,34(1):1-9.XIN Houtian,TENG Xuejian,CHENG Yinhang.Stratigraphic subdivision and isotope geochronology study on the Baoligaomiao Formation in the East Ujimqin County,Inner Mongolia[J].Geological Survey and Research,2011,34(1):1-9.
[45]潘世语,迟效国,孙巍,等.内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义[J].世界地质,2012,31(1):40-50.PAN Shiyu,CHI Xiaoguo,SUN Wei,et al.Geochemical characteristics and tectonic significance of Late Carboniferous volcanic rocks in Benbatu Formation of Sonid Youqi,Inner Mongolia[J].Global Geology,2012,31(1):40-50.
[46]鲍庆中,张长捷,吴之理,等.内蒙古白音高勒地区石炭纪石英闪长岩SHRIMP锆石U-Pb年代学及其意义[J].吉林大学学报(地球科学版),2007,37(1):15-23.BAO Qingzhong,ZHANG Changjie,WU Zhili,et al.SHRIMP U-Pb zircon geochronology of a Carboniferous quartz diorite in Baiyingaole Area,Inner Mongolia and its implications[J].Journal of Jilin University(Earth Science Edition),2007,37(1):15-23.
[47]裴福萍,许文良,杨德彬,等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J].科学通报,2006,51(24):2881-2887.PEI Fuping,XU Wenliang,YANG Debin,et al.Zircon U-Pb Geochronology and its geological significance in basal metamorphic rocks,Songliao Basin[J].Chinese Science Bulletin,2006,51(24):2881-2887.
[48]LIU J F,CHI X G,DONG C Y,et al.Discovery of Early Paleozoic granites in the eastern Xiao Hinggan Mountains,Northeastern China and their tectonic significance[J].Geological Bulletin of China,2008,27:534-544.
[49]ZHOU J B,WILDE S A,ZHANG X Z,et al.Pan-African metamorphic rocks of the Erguna massif in the Great Xing'an Range,NE China:evidence and tectonic implications[J].Tectonophysics,2011,499(1/2/3/4):105-117.
[50]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(5):591-601.
[51]STEM J R.Neoproterozoic crustal growth:the solid earth system during a critical episode of earth history[J].Gondwana Research,2008,14:33-50.
[52]WILDE S A,ZHANG X Z,WU F Y.Extension of a newly-identified 500Ma metamorphic terrain in Northeast China:further U-Pb SHRIMP dating of the Mashan Complex,Heilongjiang Province,China[J].Tectonophysics,2000,328:115-130.
[53]颉颃强,张福勤,苗来成,等.东北牡丹江地区“黑龙江群”中斜长角闪岩与花岗岩的锆石SHRIMP U-Pb定年及其地质意义[J].岩石学报,2008,24(6):1237-1250.XIE Heqiang,ZHANG Fuqin,MIAO Laicheng,et al.Zircon SHRIMP U-Pb dating of the amphibolite from"Heilongjiang Group"and the granite in Mudanjiang Area,NE China,and its geological significance[J].Acta Petrologica Sinica,2008,24(6):1237-1250.
[54]章凤奇,陈汉林,董传万,等.松辽盆地北部存在前寒武纪基底的证据[J].中国地质,2008,35(3):421-428.ZHANG Fengqi,CHEN Hanlin,DONG Chuanwan,et al.Evidence for the existence of Precambrian basement under the northern Songliao Basin[J].Chinese Geology,2008,35(3):421-428.
[55]葛文春,隋振民,吴福元,等.2007.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义[J].岩石学报,2007,23(2):423-440.GEWenchun,SUIZhenmin,WUFuyuan,etal.ZirconU-Pbages,Hfisotopiccharacterristicsandtheir implications of the Early Paleozoic granites in the northeastern Da Hinggan Mts.,Northeastern China[J].Acta Petrologica Sinica,2007,23(2):423-440.
[56]GUO J H,SUN M,CHEN F K,et al.Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan Area,North China Craton:timing of Paleoproterozoic continental collision[J].Journal of Asian Earth Sciences,2005,24:629-642.
[57]KELTY T K,YIN A,DASH B,et al.Detrital-zircon geochronology of Paleozoic sedimentary rock in the Hangay-Hentey Basin,north-central Mongolia:implications for the tectonic evolution of the Mongol-Okhotsk Ocean in central Asia[J].Tectonophysics,2008,451:97-122.