佳木斯地块构造演化—来自晚古生代沉积—火山岩的制约
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摘要
中国东北地区及临区包括俄罗斯远东地区位于中亚造山带东段，大地构造位置处于华北克拉通和西伯利亚克拉通之间，其主要受古亚洲洋构造域的影响，又经历了太平洋构造域的强烈改造与叠加增生，具有复杂的构造演化历史。中国东北地区由一系列微陆块组成，佳木斯地块位于中亚造山带的东部，是洞悉中亚造山带构造演化历史的一个重要窗口。
佳木斯地块东缘大面积分布着晚古生代地层，但关于其形成时代和构造属性也存在较大争议，本次以宝清地区泥盆系黑台组砂岩、石炭系珍子山组砂岩以及二叠系二龙山组安山岩为研究对象，通过砂岩骨架成分统计分析、地球化学分析、锆石LA-ICP-MS U-Pb年代学等手段，结合最新研究成果，探讨佳木斯地块晚古生代构造演化过程及东北地区构造演化历史。
宝清地区位于佳木斯地块东缘。大地构造背景上东部为那丹哈达地体，西南为牡丹江断裂带，南部为索伦克-西拉木伦河-长春缝合带，区域内晚古生代地层广泛发育。泥盆系黑台组和石炭系珍子山组沉积物均以长石岩屑砂岩为主。砂岩骨架成分分析结果表明，矿物颗粒组成以石英、岩屑，长石为主，并含少量云母类矿物。岩屑成分中多以火山岩屑为主，并且含有大量的具岩浆岩特征的单晶石英。上述研究表明黑台组、珍子山组整体反映其成分成熟度低，源区快速剥蚀、快速搬运、近源沉积的特点。Dickinson三角图解清晰地反映了黑台组样品倾向于克拉通内部以及再旋回造山带物源，而珍子山组样品更倾向于再旋回造山带和切割岩浆弧物源。
主量元素及其比值特征（Fe_2O_3/K_2O和Na_2O/K_2O）反映了黑台组具有长石砂岩和杂砂岩的特征，珍子山组具有杂砂岩的特征。两组砂岩的微量元素经上地壳岩石标准化的结果具有极为相似的特征，并与上地壳微量元素的含量基本一致，说明佳木斯地块东缘泥盆系黑台组和石炭系珍子山组砂岩所反映的源区具有亲缘性且具有上地壳岩石的特征。砂岩稀土元素分析结果表明，黑台组砂岩ΣLREE/ΣHREE=5.91～7.95，（La/Yb）_N＝4.67~7.80，δEu＝0.59～0.69，珍子山组砂岩ΣLREE/ΣHREE=6.54~9.51，（La/Yb）_N＝5.19~9.16，δEu＝0.69~0.87，两组砂岩均具有轻稀土元素富集，重稀土相对亏损，负Eu异常的特点，证实了泥盆系黑台组和石炭系珍子山组砂岩基本来自相同的物源区，可能属于亲上地壳长英质岩石的源区。
砂岩母岩风化作用指数（CIA，CIW）均反映了泥盆系黑台组和石炭系珍子山组砂岩的物源区经受相对较强的风化作用。在A-CN-K图解同样也揭示这两个组存在一定程度的钾交代作用。地球化学特征判别图解表明，泥盆系黑台组砂岩主要具有被动大陆边缘物源区的特点，并呈现由被动大陆边缘向活动大陆边缘物源区变化的趋势；石炭系珍子山组砂岩具有活动大陆边缘和大陆岛弧型物源的特点。
二叠系二龙山组火山岩主要由玄武安山岩、安山岩组成。具有低硅（54.7%～57.46%）、高铝（15.96%～17.83%）、高镁（Mg~#=44～48）、富钠（Na_2O/K_2O=1.81～3.53）的特征。为一套亚碱性岩石组合，具钙碱性演化趋势，主要表现为（中钾）钙碱性系列。在原始地幔标准化微量元素蛛网图解上，该组火山岩显示出高场强元素（HFSE）的相对亏损和大离子亲石元素（LILE）相对富集。球粒陨石标准化稀土元素配分图解上，各组火山岩配分形式以相对富含轻稀土元素（LREE）、贫重稀土元素（HREE）、基本上没有Eu异常的右倾型为特征，（La/Yb）_N=5.0～7.1，δEu=0.87～1.02。岩石学、地球化学研究表明早二叠世岩浆演化过程中分离结晶作用为主导机制，二龙山组火山岩为俯冲大洋板片产生的熔体交代岩石圈地幔楔部分熔融的产物，其形成于活动大陆边缘的构造环境。
锆石LA-ICPMS U-Pb年代学表明，黑台组砂岩锆石年龄谱峰期为～380Ma、～406Ma、～476Ma、～509Ma，黑台组的形成时代不早于381±3Ma，其最大沉积时限应为晚泥盆世；珍子山组砂岩锆石年龄谱峰期为～315Ma，珍子山组的沉积年龄应晚于315±3Ma，其形成时代应不早于晚石炭世；二龙山组安山岩锆石年龄谱峰期为～280Ma、～370Ma、～509Ma，二龙山组的形成年龄应为281±3Ma，其形成时代应为早二叠世。
研究区黑台组、珍子山组和二龙山组锆石年龄显示了421Ma～542Ma早古生代岩浆事件的存在，这与佳木斯地块麻山杂岩中片麻状花岗岩年龄相似，同时与宝清地区加里东期碱长花岗岩的形成时代相吻合，另外，该期岩浆事件在小兴安岭东北部和松辽盆地基底也均有所发现。此外，这三个组中还存在1035Ma、1466Ma、～1800Ma、～2700Ma、2822Ma的锆石年龄，结合最新研究表明，佳木斯地块应该存在从新元古代到中太古代晚期的结晶基底，黑台组和珍子山组的沉积物源可能来自佳木斯地块。
佳木斯地块晚古生代构造演化为：在～500Ma，中国东北地块群（包括额尔古纳、兴安、松辽以及佳木斯-兴凯地块）起源于西伯利亚克拉通南缘晚泛非期造山带。在450～475Ma，中亚造山带内早期弧-陆碰撞导致岩石圈加厚和同碰撞花岗岩类上侵产生新地壳。在450～420Ma，蒙古-鄂霍茨克洋开启，佳木斯-兴凯地块从统一的东北地块中分离出去。在420～250Ma，东北地块及佳木斯-兴凯地块向南漂移到现今位置，泥盆纪处于被动大陆边缘的构造背景，石炭纪处于被动大陆边缘向活动大陆边缘转化的构造背景，二叠纪处于活动大陆边缘的构造背景，由于古太平洋板块的俯冲作用，佳木斯地块发育二叠纪的火山作用。在～230Ma，华北克拉通与西伯利亚克拉通最终碰撞拼合，太平洋板块的俯冲作用开始活跃。在210～180Ma，由于太平洋板块向西俯冲作用，佳木斯-兴凯地块与松辽地块重新碰撞拼合在一起。
NE China and adjacent regions, including the Russian Far East, havetraditionally been considered as the eastern part of the Central Asian Orogenic Belt,located between the Siberia and North China cratons. This region was not onlyaffected by the closing of Paleo-Asian Ocean, but also influenced by the subsequentoverprint and reconstruction related to the Pacific subduction. NE China is consideredto consist of a collage of micro-continental blocks, The Jiamusi Massif, located ateastern of CAOB, is significant for understanding tectonics and evolution of theCentral Asian Orogenic Belt.
Late Paleozoic stata was widespread distributed in eastern margins of the JiamusiMassif, but its chronology and tectonic affinity is controversy. The current study ismainly focusing on the Devonian and Carboniferous sandstones and Permian basalticandesite exposed in Baoqing area, Jiamusi Massif, the systemically sandstone detritalclasts component analysis, geochemistry and LA-ICP-MS U-Pb detrital zircon ageshave been carried out on the studied Formatiom, The result presented in this papersuggests late Paleozoic tectonic evolution of Jiamusi Massif and tectonic history ofNE China.
Baoqing area geographically exposed in eastern of Jiamusi Massif. that isbounded by the Nadanhada Terrane to the east, truncated by the Mudanjiang suturezone in the southwest, and by the Solonker-Xar Moron-Changchun suture zone in thesouth, where late Paleozoic strata are widespread. The sediments of the Devonian Heitai Formation and Carboniferous Zhenzishan Formation are mostly classified asfeldsparthic litharenite, which consists mainly of quartz, lithic clasts, feldspar andmicas, with a small amount of accessory minerals. The lithic clasts are predominatelycharacterized by the volcanic lithic grains. Additionally, the monocrystalline quartzgrains are extremely high in the framework of total quartz grains. The detritalcompositions indicate that the sandstones are immature, probably due to the effects ofrapid erosion, transport, and diagenetic process and/or nearly supplying derived fromthe source. In addition, the detrital modal analysis applying the Dickinson’s trianglediagrams also indicate the sediments of Heitai Formation are mainly derived fromrecycled orogenic and Cration interior source, while the sediments of ZhenzishanFormation are mostly derived from recycled orogenic and dissected arc source.
The major elements and their radios (especially, Fe_2O_3/K_2O and Na_2O/K_2O) areclosely associated with arkose and greywacke for the sandstone from HeitaiFormation and wacke and greywacke for the sandstone from Zhenzishan Formation.Trace elements in the studied sandstones from the two formations mentioned aboveare upper crust-normalized patterns, and show the similar trends in the spider diagram,suggesting the similar provenances related to the rocks of upper crust. The rare earthelements and their chondrite-normalized patterns in the investigated sandstonesmostly show the LREE content enrichment and negative Eu abnormality, withΣLREE/ΣHREE=5.91~7.95,(La/Yb)_N＝4.67~7.80, δEu＝0.59~0.69in HeitaiFormation and ΣLREE/ΣHREE=6.54~9.51,(La/Yb)_N＝5.19~9.16, δEu＝0.69~0.87in Zhenzishan Formation, revealing that the similar provenances derived from thefelsic upper continent crustal rocks are reasonable to supplying for the sediments ofboth the Heitai and Zhenzishan formations.
The indexes of paleo-weathering and chemical alteration (CIA and CIW values)together with the A-CN-K projections have been widely investigated in the sandstonefrom two formations, and show medium source weathering and potassiummetasomatism in the Heitai and Zhenzishan Formations. The geochemicaldiscrimination diagrams exhibit that tectonic setting corresponded for the provenance of the Heitai sediments is characterized by PM and subsequently transferred to theACM, whereas the tectonic setting of provenance of the Zhenzishan sediments tendsto transfer progressively from ACM to CIA.
The Permian volcanic rocks in the Erlongshan Formation are mainly composedof basaltic andesite and andesite. They are characterized by low SiO_2contents(54.7%～57.46%), high Al (15.96%～17.83%) and Mg~#(44～48), enrichment in Na(Na_2O/K_2O=1.81～3.53). They belong to subalkaline series and show a calc-alkalineevolutionary trend, most of them are plotted within (medium-K) calc-alkaline series.On the primitive mantle-normalized spider diagram, the Permian volcanic rocks arecharacterized by enrichment in large ion lithophile elements (LILE) and relativelydepletion in high field strength elements (HFSE). The Chondrite-normalized REEpattern for the Permian volcanic rocks shows that The volcanic rocks arecharacterized by enrichment in light rare earth elements (LREE), relatively depletionin heavy rare earth elements (HREE), and no Eu anomalies,(La/Yb)_N=5.0～7.1,δEu=0.87～1.02. The characteristic of petrology and geochemistry imply that mineralfractional crystallization is the dominant mechanism to control magmatic evolution.Besides, the Erlongshan Formation volcanic rocks could be derived from the partialmelting of the lithosphere mantle wedge modified by the subducted oceanic slabunder the tectonic setting of the active continental margin.
LA-ICP-MS zircon U-Pb dating results indicate that the maximum age ofdeposition of the Heitai Formation sandstone was younger than～374Ma in the lateDevonian, with a peak age at～380Ma、～406Ma、～476Ma、～509Ma in agepopulations. the maximum age of deposition of the Zhenzishan Formation sandstonewas younger than~313Ma in the late Carboniferous, with a peak age at～315Ma inage populations. the Erlongshan Formation volcanic rocks formed at278Ma in theearly Permian, with a peak age at～280Ma、～370Ma、～509Ma in age populations.
Zircon U-Pb date of the Heitai, Zhenzishan and Erlongshan Formations exhibitthat the existence of the Early Paleozoic tectonic-magmatic event within421Ma～542Ma, which is consistent with the ages of the gneissic granites in the Jiamusi Massif and the Caledonian alkali-feldspar granites in the Baoqing area. This magmatic eventcan be also found in the basement of the Songliao Basin and the northeastern XiaoHinggan Mountains. Zircon ages of1035Ma,1466Ma,～1800Ma,～2700Ma,2822Ma, together with other studies, indicate that the Mesoarchean to Neoproterozoicbasement exist in Jiamusi Massif. The provenances of the Heitai and ZhenzishanFormations are derived from Jiamusi Massif.
We have proposed a tentative model of tectonic evolution, whereby the blocks ofNE China (including Erguna, Xing’an, Songliao, Jiamusi, Khanka, and Bureya)originated as part of the Late Pan-African (~500Ma) orogenic belt developed aroundthe southern margin of the Siberia Craton. The early stage of arc-continent collisionwithin the CAOB was accompanied by reworking of juvenile crust at450-475Ma,leading to melting of thickened lithosphere and intrusion of syn-tectonic granitoids.However, at450-420Ma, during the opening of the Mongol-Okhotsk Ocean, Jiamusiblock rifted away the combined NE China blocks. at420-250Ma, The Jiamusi blockand the combined NE China blocks moved farther south into what is now NE China,probably. Devonian tectonic setting is PM, Carboniferous tectonic transfer from PMto ACM, Permian volcanic distributed widely due to the subduction of the PPC. Thefinal collision between the North China and Siberia cratons occurred at~230Ma in theMiddle Triassic. However, the Jiamusi-Khanka block rifted away at~260Ma in theLate Permian. Final re-docking with the Songliao Block occurred between210and
佳木斯地块东缘大面积分布着晚古生代地层，但关于其形成时代和构造属性也存在较大争议，本次以宝清地区泥盆系黑台组砂岩、石炭系珍子山组砂岩以及二叠系二龙山组安山岩为研究对象，通过砂岩骨架成分统计分析、地球化学分析、锆石LA-ICP-MS U-Pb年代学等手段，结合最新研究成果，探讨佳木斯地块晚古生代构造演化过程及东北地区构造演化历史。
宝清地区位于佳木斯地块东缘。大地构造背景上东部为那丹哈达地体，西南为牡丹江断裂带，南部为索伦克-西拉木伦河-长春缝合带，区域内晚古生代地层广泛发育。泥盆系黑台组和石炭系珍子山组沉积物均以长石岩屑砂岩为主。砂岩骨架成分分析结果表明，矿物颗粒组成以石英、岩屑，长石为主，并含少量云母类矿物。岩屑成分中多以火山岩屑为主，并且含有大量的具岩浆岩特征的单晶石英。上述研究表明黑台组、珍子山组整体反映其成分成熟度低，源区快速剥蚀、快速搬运、近源沉积的特点。Dickinson三角图解清晰地反映了黑台组样品倾向于克拉通内部以及再旋回造山带物源，而珍子山组样品更倾向于再旋回造山带和切割岩浆弧物源。
主量元素及其比值特征（Fe_2O_3/K_2O和Na_2O/K_2O）反映了黑台组具有长石砂岩和杂砂岩的特征，珍子山组具有杂砂岩的特征。两组砂岩的微量元素经上地壳岩石标准化的结果具有极为相似的特征，并与上地壳微量元素的含量基本一致，说明佳木斯地块东缘泥盆系黑台组和石炭系珍子山组砂岩所反映的源区具有亲缘性且具有上地壳岩石的特征。砂岩稀土元素分析结果表明，黑台组砂岩ΣLREE/ΣHREE=5.91～7.95，（La/Yb）_N＝4.67~7.80，δEu＝0.59～0.69，珍子山组砂岩ΣLREE/ΣHREE=6.54~9.51，（La/Yb）_N＝5.19~9.16，δEu＝0.69~0.87，两组砂岩均具有轻稀土元素富集，重稀土相对亏损，负Eu异常的特点，证实了泥盆系黑台组和石炭系珍子山组砂岩基本来自相同的物源区，可能属于亲上地壳长英质岩石的源区。
砂岩母岩风化作用指数（CIA，CIW）均反映了泥盆系黑台组和石炭系珍子山组砂岩的物源区经受相对较强的风化作用。在A-CN-K图解同样也揭示这两个组存在一定程度的钾交代作用。地球化学特征判别图解表明，泥盆系黑台组砂岩主要具有被动大陆边缘物源区的特点，并呈现由被动大陆边缘向活动大陆边缘物源区变化的趋势；石炭系珍子山组砂岩具有活动大陆边缘和大陆岛弧型物源的特点。
二叠系二龙山组火山岩主要由玄武安山岩、安山岩组成。具有低硅（54.7%～57.46%）、高铝（15.96%～17.83%）、高镁（Mg~#=44～48）、富钠（Na_2O/K_2O=1.81～3.53）的特征。为一套亚碱性岩石组合，具钙碱性演化趋势，主要表现为（中钾）钙碱性系列。在原始地幔标准化微量元素蛛网图解上，该组火山岩显示出高场强元素（HFSE）的相对亏损和大离子亲石元素（LILE）相对富集。球粒陨石标准化稀土元素配分图解上，各组火山岩配分形式以相对富含轻稀土元素（LREE）、贫重稀土元素（HREE）、基本上没有Eu异常的右倾型为特征，（La/Yb）_N=5.0～7.1，δEu=0.87～1.02。岩石学、地球化学研究表明早二叠世岩浆演化过程中分离结晶作用为主导机制，二龙山组火山岩为俯冲大洋板片产生的熔体交代岩石圈地幔楔部分熔融的产物，其形成于活动大陆边缘的构造环境。
锆石LA-ICPMS U-Pb年代学表明，黑台组砂岩锆石年龄谱峰期为～380Ma、～406Ma、～476Ma、～509Ma，黑台组的形成时代不早于381±3Ma，其最大沉积时限应为晚泥盆世；珍子山组砂岩锆石年龄谱峰期为～315Ma，珍子山组的沉积年龄应晚于315±3Ma，其形成时代应不早于晚石炭世；二龙山组安山岩锆石年龄谱峰期为～280Ma、～370Ma、～509Ma，二龙山组的形成年龄应为281±3Ma，其形成时代应为早二叠世。
研究区黑台组、珍子山组和二龙山组锆石年龄显示了421Ma～542Ma早古生代岩浆事件的存在，这与佳木斯地块麻山杂岩中片麻状花岗岩年龄相似，同时与宝清地区加里东期碱长花岗岩的形成时代相吻合，另外，该期岩浆事件在小兴安岭东北部和松辽盆地基底也均有所发现。此外，这三个组中还存在1035Ma、1466Ma、～1800Ma、～2700Ma、2822Ma的锆石年龄，结合最新研究表明，佳木斯地块应该存在从新元古代到中太古代晚期的结晶基底，黑台组和珍子山组的沉积物源可能来自佳木斯地块。
佳木斯地块晚古生代构造演化为：在～500Ma，中国东北地块群（包括额尔古纳、兴安、松辽以及佳木斯-兴凯地块）起源于西伯利亚克拉通南缘晚泛非期造山带。在450～475Ma，中亚造山带内早期弧-陆碰撞导致岩石圈加厚和同碰撞花岗岩类上侵产生新地壳。在450～420Ma，蒙古-鄂霍茨克洋开启，佳木斯-兴凯地块从统一的东北地块中分离出去。在420～250Ma，东北地块及佳木斯-兴凯地块向南漂移到现今位置，泥盆纪处于被动大陆边缘的构造背景，石炭纪处于被动大陆边缘向活动大陆边缘转化的构造背景，二叠纪处于活动大陆边缘的构造背景，由于古太平洋板块的俯冲作用，佳木斯地块发育二叠纪的火山作用。在～230Ma，华北克拉通与西伯利亚克拉通最终碰撞拼合，太平洋板块的俯冲作用开始活跃。在210～180Ma，由于太平洋板块向西俯冲作用，佳木斯-兴凯地块与松辽地块重新碰撞拼合在一起。
NE China and adjacent regions, including the Russian Far East, havetraditionally been considered as the eastern part of the Central Asian Orogenic Belt,located between the Siberia and North China cratons. This region was not onlyaffected by the closing of Paleo-Asian Ocean, but also influenced by the subsequentoverprint and reconstruction related to the Pacific subduction. NE China is consideredto consist of a collage of micro-continental blocks, The Jiamusi Massif, located ateastern of CAOB, is significant for understanding tectonics and evolution of theCentral Asian Orogenic Belt.
Late Paleozoic stata was widespread distributed in eastern margins of the JiamusiMassif, but its chronology and tectonic affinity is controversy. The current study ismainly focusing on the Devonian and Carboniferous sandstones and Permian basalticandesite exposed in Baoqing area, Jiamusi Massif, the systemically sandstone detritalclasts component analysis, geochemistry and LA-ICP-MS U-Pb detrital zircon ageshave been carried out on the studied Formatiom, The result presented in this papersuggests late Paleozoic tectonic evolution of Jiamusi Massif and tectonic history ofNE China.
Baoqing area geographically exposed in eastern of Jiamusi Massif. that isbounded by the Nadanhada Terrane to the east, truncated by the Mudanjiang suturezone in the southwest, and by the Solonker-Xar Moron-Changchun suture zone in thesouth, where late Paleozoic strata are widespread. The sediments of the Devonian Heitai Formation and Carboniferous Zhenzishan Formation are mostly classified asfeldsparthic litharenite, which consists mainly of quartz, lithic clasts, feldspar andmicas, with a small amount of accessory minerals. The lithic clasts are predominatelycharacterized by the volcanic lithic grains. Additionally, the monocrystalline quartzgrains are extremely high in the framework of total quartz grains. The detritalcompositions indicate that the sandstones are immature, probably due to the effects ofrapid erosion, transport, and diagenetic process and/or nearly supplying derived fromthe source. In addition, the detrital modal analysis applying the Dickinson’s trianglediagrams also indicate the sediments of Heitai Formation are mainly derived fromrecycled orogenic and Cration interior source, while the sediments of ZhenzishanFormation are mostly derived from recycled orogenic and dissected arc source.
The major elements and their radios (especially, Fe_2O_3/K_2O and Na_2O/K_2O) areclosely associated with arkose and greywacke for the sandstone from HeitaiFormation and wacke and greywacke for the sandstone from Zhenzishan Formation.Trace elements in the studied sandstones from the two formations mentioned aboveare upper crust-normalized patterns, and show the similar trends in the spider diagram,suggesting the similar provenances related to the rocks of upper crust. The rare earthelements and their chondrite-normalized patterns in the investigated sandstonesmostly show the LREE content enrichment and negative Eu abnormality, withΣLREE/ΣHREE=5.91~7.95,(La/Yb)_N＝4.67~7.80, δEu＝0.59~0.69in HeitaiFormation and ΣLREE/ΣHREE=6.54~9.51,(La/Yb)_N＝5.19~9.16, δEu＝0.69~0.87in Zhenzishan Formation, revealing that the similar provenances derived from thefelsic upper continent crustal rocks are reasonable to supplying for the sediments ofboth the Heitai and Zhenzishan formations.
The indexes of paleo-weathering and chemical alteration (CIA and CIW values)together with the A-CN-K projections have been widely investigated in the sandstonefrom two formations, and show medium source weathering and potassiummetasomatism in the Heitai and Zhenzishan Formations. The geochemicaldiscrimination diagrams exhibit that tectonic setting corresponded for the provenance of the Heitai sediments is characterized by PM and subsequently transferred to theACM, whereas the tectonic setting of provenance of the Zhenzishan sediments tendsto transfer progressively from ACM to CIA.
The Permian volcanic rocks in the Erlongshan Formation are mainly composedof basaltic andesite and andesite. They are characterized by low SiO_2contents(54.7%～57.46%), high Al (15.96%～17.83%) and Mg~#(44～48), enrichment in Na(Na_2O/K_2O=1.81～3.53). They belong to subalkaline series and show a calc-alkalineevolutionary trend, most of them are plotted within (medium-K) calc-alkaline series.On the primitive mantle-normalized spider diagram, the Permian volcanic rocks arecharacterized by enrichment in large ion lithophile elements (LILE) and relativelydepletion in high field strength elements (HFSE). The Chondrite-normalized REEpattern for the Permian volcanic rocks shows that The volcanic rocks arecharacterized by enrichment in light rare earth elements (LREE), relatively depletionin heavy rare earth elements (HREE), and no Eu anomalies,(La/Yb)_N=5.0～7.1,δEu=0.87～1.02. The characteristic of petrology and geochemistry imply that mineralfractional crystallization is the dominant mechanism to control magmatic evolution.Besides, the Erlongshan Formation volcanic rocks could be derived from the partialmelting of the lithosphere mantle wedge modified by the subducted oceanic slabunder the tectonic setting of the active continental margin.
LA-ICP-MS zircon U-Pb dating results indicate that the maximum age ofdeposition of the Heitai Formation sandstone was younger than～374Ma in the lateDevonian, with a peak age at～380Ma、～406Ma、～476Ma、～509Ma in agepopulations. the maximum age of deposition of the Zhenzishan Formation sandstonewas younger than~313Ma in the late Carboniferous, with a peak age at～315Ma inage populations. the Erlongshan Formation volcanic rocks formed at278Ma in theearly Permian, with a peak age at～280Ma、～370Ma、～509Ma in age populations.
Zircon U-Pb date of the Heitai, Zhenzishan and Erlongshan Formations exhibitthat the existence of the Early Paleozoic tectonic-magmatic event within421Ma～542Ma, which is consistent with the ages of the gneissic granites in the Jiamusi Massif and the Caledonian alkali-feldspar granites in the Baoqing area. This magmatic eventcan be also found in the basement of the Songliao Basin and the northeastern XiaoHinggan Mountains. Zircon ages of1035Ma,1466Ma,～1800Ma,～2700Ma,2822Ma, together with other studies, indicate that the Mesoarchean to Neoproterozoicbasement exist in Jiamusi Massif. The provenances of the Heitai and ZhenzishanFormations are derived from Jiamusi Massif.
We have proposed a tentative model of tectonic evolution, whereby the blocks ofNE China (including Erguna, Xing’an, Songliao, Jiamusi, Khanka, and Bureya)originated as part of the Late Pan-African (~500Ma) orogenic belt developed aroundthe southern margin of the Siberia Craton. The early stage of arc-continent collisionwithin the CAOB was accompanied by reworking of juvenile crust at450-475Ma,leading to melting of thickened lithosphere and intrusion of syn-tectonic granitoids.However, at450-420Ma, during the opening of the Mongol-Okhotsk Ocean, Jiamusiblock rifted away the combined NE China blocks. at420-250Ma, The Jiamusi blockand the combined NE China blocks moved farther south into what is now NE China,probably. Devonian tectonic setting is PM, Carboniferous tectonic transfer from PMto ACM, Permian volcanic distributed widely due to the subduction of the PPC. Thefinal collision between the North China and Siberia cratons occurred at~230Ma in theMiddle Triassic. However, the Jiamusi-Khanka block rifted away at~260Ma in theLate Permian. Final re-docking with the Songliao Block occurred between210and
引文
1引用胡升奇《地球学报》文章《广西大黎铜钼矿石英二长(斑)岩年代学、地球化学特征及其地质意义》
2引用赵英利的博士论文《大兴安岭中南部二叠纪砂岩物源分析对晚古生代区域构造演化的制约》
3引用柏涛的博士论文《多物源示踪研究》
4引用纪伟强的硕士论文《吉黑东部中生代晚期火山岩的年代学和地球化学》
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4引用纪伟强的硕士论文《吉黑东部中生代晚期火山岩的年代学和地球化学》
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