华北板块北缘东段晚古生代—早中生代火成岩的年代学与地球化学研究
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摘要
本文以吉林中部地区晚古生代—早中生代火成岩为研究对象，通过对火成岩中锆石的LA-ICP-MS和SIMS U-Pb年代学和火成岩的主量元素、微量元素及锆石Hf同位素的地球化学研究，确定了研究区火成岩的形成时代，讨论了研究区不同时代火成岩的岩石组合和岩浆源区性质及其形成的构造背景。最终结合区域地质资料，探讨了研究区晚古生代—早中生代区域构造演化历史。
锆石U-Pb定年结果表明，该区晚古生代—早中生代岩浆作用可以进一步划分为五期：早二叠世（293～279Ma）、中二叠世（270Ma）、晚二叠世（262～255Ma）、早三叠世（249～247Ma）和晚三叠世（222Ma）。
吉林中部地区早二叠世发育一套由粗面英安岩、英安岩和流纹岩组成的中钾—高钾钙碱性系列火山岩，它们形成于活动陆缘背景，揭示早二叠世华北板块北缘处于古亚洲洋的俯冲作用之下。吉林中部地区中二叠世岩浆作用以含石榴石二长花岗岩的产出为代表，负的εHf(t)值，表明其岩浆起源于华北板块古老地壳物质的部分熔融；地球化学特征显示其为同碰撞花岗岩，揭示该区处于松嫩—张广才岭地块与华北板块之间的碰撞环境。吉林中部地区晚二叠世发育辉长岩—花岗岩组合，辉长岩原始岩浆起源于曾经遭受过俯冲流体交代的亏损岩石圈地幔，花岗质岩石的原始岩浆起源于新元古代新增生下地壳的部分熔融；该期辉长岩和花岗质岩石构成了典型的双峰式岩石组合，暗示其形成于早二叠世华北板块北缘与松嫩—张广才岭地块碰撞造山后的伸展环境。吉林中部地区早三叠世二长花岗岩具有埃达克质岩石的地球化学特征，形成于加厚玄武质下地壳的部分熔融，这种陆壳加厚过程也是一次重要的造山过程，表明华北板块北缘与松嫩—张广才岭地块再次发生了碰撞，古亚洲洋最终闭合。吉林中部地区晚三叠世侵入岩主要由方辉橄榄岩组成，来源于亏损的岩石圈地幔；研究区和邻区晚三叠世镁铁质—超镁铁质侵入岩和花岗质岩石构成了典型的双峰式火成岩组合，暗示它们形成于华北板块北缘和兴蒙造山带最终碰撞造山后的伸展环境。
This thesis studies the geochronology and geochemistry of the Late Paleozoic-EarlyMesozoic igneous rocks in the central Jilin Province, NE China, with the aim of providingconstraints on the Late Paleozoic-Early Mesozoic tectonic evolution in the eastern segment ofthe northern margin of the North China Block (NCB). Main achievements are as follows:
1. Late Paleozoic–Early Mesozoic magmatic events in the eastern segment of thenorthern margin of the NCB
Zircons from the Late Paleozoic-Early Mesozoic igneous rocks in the central JilinProvince, NE China are euhedral-subhedral in shape and display fine-scale oscillatory growthzoning and striped absorption as well as their high Th/U ratios, implying their magmatic origin.LA-ICP-MS and SIMS zircon U-Pb dating results indicate that the Late Paleozoic-EarlyMesozoic magmatic events can be subdivided into five stages, i.e., Early Permian (293–279Ma), Middle Permian (~270Ma), Late Permian (262–255Ma), Early Triassic (249–247Ma),and Late Triassic (~222Ma).
2. Early Permian–an active continental margin setting
The volcanic rocks from the Daheshen Formation are representative as the Early Permianmagmatic event in the central Jilin Province, and are composed mainly of the trachytic dacite,dacite, and rhyolite. They are rich in SiO2and alkali contents, poor in MgO, with their εHf(t)values and Hf two-stage model ages of+0.23~+10.37and1240~785Ma, respectively, suggesting that their primary magmas could be mainly derived from partial melting of theMeso-Neoproterozoic accretted lower crust. The volcanic rocks from the Daheshen Formationchemically belong to mid-K and high-K calc-alkaline series, and display an enrichment inLREEs and LILEs and depletion in HFSEs, implying that they could have formed under anactive continental margin setting, i.e., the subduction of the Paleo-Asiatic oceanic platebeneath the northern margin of the NCB happened in Early Permian.
3. Middle Permian–continent-continent collisional setting
The Middle Permian igneous rocks consist chiefly of the FNG garnet-bearingmonzogranites. They have high SiO2, Al2O3and alkali conctents, low TFe2O3and MgOcontents, relatively flat rare earth element (REE) patterns and low total REE abundances(REE), as well as negative Eu anomalies. Their εHf(t) values and Hf two-stage model agesrange from–17.1~–14.1and2.37~2.18Ga, respectively, indicating that their primary magmacould be probably derived from partial melting of the ancient lower continental crust of theNCB. The presence of the garnet and their peraluminous geochemical features suggest thatthey are the syn-collision granites. Combined with the presence of the late Middle Permianmolasse in central Jilin Province, we propose that the garnet-bearing monzogranites couldform under an initial collision setting between the northern margin of the NCB and theSongnen-Zhangguangcai Range Massif.
4. Late Permian–post-collisional extension setting
The Late Permian igneous rocks are composed mainly of the gabbros and the granitoids.The gabbros are characterized by low SiO2contents, high Mg#values, positive εHf(t) values,enrichment in LILEs, and depletion in HFSEs, implying that their primary magma could bederived from partial melting of a depleted lithospheric mantle modified by subducted slab-derived fluids. The granitoids have high SiO2, low MgO, Cr, and Ni contents, and positiveεHf(t) values, suggesting that their primary magma could be derived from partial melting of ajuvenile lower crust. The Late Permian gabbros and granitoids constitute a bimodal igneousrock association, suggesting that they could formed under a post-collisional extensionalenvironment related to collapse of thickened crust caused by Middle Permian collision between the northern margin of the NCB and the Songnen-Zhangguangcai Range Massif.
5. Early Triassic–final closure of the Paleo-Asian Ocean
The Early Triassic magmatism in the study area is dominated by biotite monzogranites.They are characterized by high Al2O3, Na2O, and Sr concentrations, low Y and Ybconcentrations, enrichment in LREEs and LILEs, and depletion in HREEs and HFSEs, beingaffinity of adakitic rocks, suggesting that they formed by partial melting of a thickened maficlower crust. This thickening process of the mafic lower crust implies that a Late Triassiccompressional tectonic setting occurred in the central Jilin Province. Together with theoccurrence of the coeval metamorphism of the Hulan Group in the eastern part of the studyarea and cessation of the marine deposition in the area, we propose that the final amalgamationof the northern margin of the NCB and the Songnen-Zhangguangcai Range Massif took placein the Early Triassic, which led to the final closure of the Paleo-Asian Ocean.
6. Late Triassic–post-orogenic extensional setting
Late Triassic intrusive rocks in the study area are mainly composed of harzburgites. Theirlow SiO2, high MgO, Cr, and Ni concentrations, and positive εHf(t) values, suggest that theirprimary basaltic magma could be derived from partial melting of a depleted lithospheric mantle.Late Triassic mafic-ultramafic intrusive rocks and coeval granitoids constitute a typicalbimodal igneous rock association in both the study area and adjacent regions, implying thatthey formed under a post-orogenic extensional environment related to the final amalgamationof the NCB and the XMOB.
锆石U-Pb定年结果表明，该区晚古生代—早中生代岩浆作用可以进一步划分为五期：早二叠世（293～279Ma）、中二叠世（270Ma）、晚二叠世（262～255Ma）、早三叠世（249～247Ma）和晚三叠世（222Ma）。
吉林中部地区早二叠世发育一套由粗面英安岩、英安岩和流纹岩组成的中钾—高钾钙碱性系列火山岩，它们形成于活动陆缘背景，揭示早二叠世华北板块北缘处于古亚洲洋的俯冲作用之下。吉林中部地区中二叠世岩浆作用以含石榴石二长花岗岩的产出为代表，负的εHf(t)值，表明其岩浆起源于华北板块古老地壳物质的部分熔融；地球化学特征显示其为同碰撞花岗岩，揭示该区处于松嫩—张广才岭地块与华北板块之间的碰撞环境。吉林中部地区晚二叠世发育辉长岩—花岗岩组合，辉长岩原始岩浆起源于曾经遭受过俯冲流体交代的亏损岩石圈地幔，花岗质岩石的原始岩浆起源于新元古代新增生下地壳的部分熔融；该期辉长岩和花岗质岩石构成了典型的双峰式岩石组合，暗示其形成于早二叠世华北板块北缘与松嫩—张广才岭地块碰撞造山后的伸展环境。吉林中部地区早三叠世二长花岗岩具有埃达克质岩石的地球化学特征，形成于加厚玄武质下地壳的部分熔融，这种陆壳加厚过程也是一次重要的造山过程，表明华北板块北缘与松嫩—张广才岭地块再次发生了碰撞，古亚洲洋最终闭合。吉林中部地区晚三叠世侵入岩主要由方辉橄榄岩组成，来源于亏损的岩石圈地幔；研究区和邻区晚三叠世镁铁质—超镁铁质侵入岩和花岗质岩石构成了典型的双峰式火成岩组合，暗示它们形成于华北板块北缘和兴蒙造山带最终碰撞造山后的伸展环境。
This thesis studies the geochronology and geochemistry of the Late Paleozoic-EarlyMesozoic igneous rocks in the central Jilin Province, NE China, with the aim of providingconstraints on the Late Paleozoic-Early Mesozoic tectonic evolution in the eastern segment ofthe northern margin of the North China Block (NCB). Main achievements are as follows:
1. Late Paleozoic–Early Mesozoic magmatic events in the eastern segment of thenorthern margin of the NCB
Zircons from the Late Paleozoic-Early Mesozoic igneous rocks in the central JilinProvince, NE China are euhedral-subhedral in shape and display fine-scale oscillatory growthzoning and striped absorption as well as their high Th/U ratios, implying their magmatic origin.LA-ICP-MS and SIMS zircon U-Pb dating results indicate that the Late Paleozoic-EarlyMesozoic magmatic events can be subdivided into five stages, i.e., Early Permian (293–279Ma), Middle Permian (~270Ma), Late Permian (262–255Ma), Early Triassic (249–247Ma),and Late Triassic (~222Ma).
2. Early Permian–an active continental margin setting
The volcanic rocks from the Daheshen Formation are representative as the Early Permianmagmatic event in the central Jilin Province, and are composed mainly of the trachytic dacite,dacite, and rhyolite. They are rich in SiO2and alkali contents, poor in MgO, with their εHf(t)values and Hf two-stage model ages of+0.23~+10.37and1240~785Ma, respectively, suggesting that their primary magmas could be mainly derived from partial melting of theMeso-Neoproterozoic accretted lower crust. The volcanic rocks from the Daheshen Formationchemically belong to mid-K and high-K calc-alkaline series, and display an enrichment inLREEs and LILEs and depletion in HFSEs, implying that they could have formed under anactive continental margin setting, i.e., the subduction of the Paleo-Asiatic oceanic platebeneath the northern margin of the NCB happened in Early Permian.
3. Middle Permian–continent-continent collisional setting
The Middle Permian igneous rocks consist chiefly of the FNG garnet-bearingmonzogranites. They have high SiO2, Al2O3and alkali conctents, low TFe2O3and MgOcontents, relatively flat rare earth element (REE) patterns and low total REE abundances(REE), as well as negative Eu anomalies. Their εHf(t) values and Hf two-stage model agesrange from–17.1~–14.1and2.37~2.18Ga, respectively, indicating that their primary magmacould be probably derived from partial melting of the ancient lower continental crust of theNCB. The presence of the garnet and their peraluminous geochemical features suggest thatthey are the syn-collision granites. Combined with the presence of the late Middle Permianmolasse in central Jilin Province, we propose that the garnet-bearing monzogranites couldform under an initial collision setting between the northern margin of the NCB and theSongnen-Zhangguangcai Range Massif.
4. Late Permian–post-collisional extension setting
The Late Permian igneous rocks are composed mainly of the gabbros and the granitoids.The gabbros are characterized by low SiO2contents, high Mg#values, positive εHf(t) values,enrichment in LILEs, and depletion in HFSEs, implying that their primary magma could bederived from partial melting of a depleted lithospheric mantle modified by subducted slab-derived fluids. The granitoids have high SiO2, low MgO, Cr, and Ni contents, and positiveεHf(t) values, suggesting that their primary magma could be derived from partial melting of ajuvenile lower crust. The Late Permian gabbros and granitoids constitute a bimodal igneousrock association, suggesting that they could formed under a post-collisional extensionalenvironment related to collapse of thickened crust caused by Middle Permian collision between the northern margin of the NCB and the Songnen-Zhangguangcai Range Massif.
5. Early Triassic–final closure of the Paleo-Asian Ocean
The Early Triassic magmatism in the study area is dominated by biotite monzogranites.They are characterized by high Al2O3, Na2O, and Sr concentrations, low Y and Ybconcentrations, enrichment in LREEs and LILEs, and depletion in HREEs and HFSEs, beingaffinity of adakitic rocks, suggesting that they formed by partial melting of a thickened maficlower crust. This thickening process of the mafic lower crust implies that a Late Triassiccompressional tectonic setting occurred in the central Jilin Province. Together with theoccurrence of the coeval metamorphism of the Hulan Group in the eastern part of the studyarea and cessation of the marine deposition in the area, we propose that the final amalgamationof the northern margin of the NCB and the Songnen-Zhangguangcai Range Massif took placein the Early Triassic, which led to the final closure of the Paleo-Asian Ocean.
6. Late Triassic–post-orogenic extensional setting
Late Triassic intrusive rocks in the study area are mainly composed of harzburgites. Theirlow SiO2, high MgO, Cr, and Ni concentrations, and positive εHf(t) values, suggest that theirprimary basaltic magma could be derived from partial melting of a depleted lithospheric mantle.Late Triassic mafic-ultramafic intrusive rocks and coeval granitoids constitute a typicalbimodal igneous rock association in both the study area and adjacent regions, implying thatthey formed under a post-orogenic extensional environment related to the final amalgamationof the NCB and the XMOB.
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