澜沧江南带三叠纪碰撞后岩浆作用、岩石成因及其构造意义
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摘要
碰撞后岩浆作用记录了俯冲/碰撞过程壳幔物质循环的诸多信息,其源区属性及所揭示的深部动力学背景对理解造山带构造演化和壳幔相互作用尤为重要。澜沧江南带作为古特提斯主洋盆的缝合带,在该区的云县-景洪一带(忙怀组-小定西组-芒汇河组或相当地层)发育最大厚度可达8000m的与特提斯俯冲碰撞有关的三叠纪火山岩及相关侵入岩,因此,我们选择研究基础较为薄弱的三叠纪火山岩和临沧花岗岩基为研究对象,开展系统的岩石(相)学、精细的锆石单矿物SHRIMP和全岩(40)~Ar/(39)~Ar年代学、元素-同位素地球化学研究,以确立该火山岩带的时空分布格局,示踪其岩石成因与构造背景,探讨该区三叠纪岩浆形成的可能动力学机制及其对古特提斯构造演化的制约,从而更好地理解典型碰撞后岩浆作用的深部过程及壳-幔相互作用机制。本研究主要取得以下成果和认识:
1、澜沧江南带三叠纪火山岩锆石SHRIMP U-Pb年代学表明,景洪忙怀组下段中基性火山岩(20SM-408)形成于241.0±4.9Ma,其顶部流纹岩(02DX-95)形成于231.0±5.0Ma;临沧花岗岩基主体的2个二长花岗岩的代表性样品(02DX-137和20JH-10)分别给出了229.4±3.0 Ma和230.4±3.6Ma的谐和年龄;原划为小定西组的下部基性岩样品(02DX-103)给出了213.5±7.7Ma的谐和年龄,而原划为芒汇河组的上部火山岩(02DX-124)给出了216+20Ma的参考年龄。
2、忙怀组下段中基性火山岩为玄武质安山岩-安山岩系列,以亏损Nb-Ta、P等高场强元素和富集LILE、LREE为特征,((87)~Sr/(86)~Sr)_i=0.706116-0.707046,εNd(t)=-2.69～-4.02,((206)~Pb/(204)~pb)_t=18.541-18.800,((207)~Pb/(204)~Pb)_t=15.614-15.698,((208)~Pb/(204)~Pb)_t=38.478-38.820。其高于岛弧火山岩的Pb/Nd比值,与受俯冲沉积物改造的富集岩石圈地幔特征相似,模拟计算结果暗示其源区可能是印度洋MORB玄武岩源区与5-7%洋壳俯冲沉积物混合作用的结果。
3、忙怀组上段流纹岩显示 A-型酸性岩特征,具较低初始(87)~Sr/(86)~Sr(0.705717-0.707262)和较高εNd(t)(-4.64～-6.34)值及变化较大的初始Pb同位素组成((206)~Pb/(204)~Pb)_t=17.220-18.570,((207)~Pb/(204)~Pb)_t=15.601-15.570,((208)~Pb/(204)~Pb)_t=36.964-
The post-collisional magmatism can provide a great deal of important information on the interaction of crust and mantle during subduction and collision. In particular, the natures of magma source and the tectonic settings of generation of magmatism to understand the tectonic evolution of orogenic belt and the crust-mantle interaction are very important. As a major suture of paleo-Tethyan ocean, the Triassic volcanic rocks with a depth up to 8000 m and granitic intrusion correlated with subduction and collision of the paleo-Tethyan ocean were cropped out in the Yunxian-Jinghong area, Southern Lancangjiang zone. Thus, we chose the Triassic magmatism to conduct the study on systematic lithology (lithofacies), zircon SHRIMP U-Pb and whole-rock ~(40)Ar/~(39)Ar geochronology, elemental and Sr-Nd-Pb isotopic geochemistry. The main objectives are: (1) to confirm patterns of distribution of different magmatism belts;(2) to investigate the petrogenesis of magma and their tectonic settings relative to their generation;(3) to probe into the geodynamic mechanism of the Triassic magmatism and their constraint on the tectonic evolution of the paleo-Tethyan Ocean;(4) to better understand the deep process and mechanism of crust-mantle interaction of typical post-collisional magmatism. The major conclusions are summarized as follow:1、 The geochronological data of zircon SHRIMP U-Pb for the Triassic igneous rocks from the Southern Lancangjiang zone indicate that the intermediate-mafic volcanic rock (20SM-408) from the lower part of the Manghuai Formation and the rhyolite (02DX-95) from its uppermost part were erupted at ca. 241.0±4.9 Ma and ca. 231.0±5.0 Ma, respectively, and the main granitic intrusions in Lincang batholith
were mainly intruded at about ca. 230Ma, and the volcanic rocks from Xiaodingxi Formation and Manghuihe Formation could were generated at similar time(215-210 Ma).2 s The middle-Triassic intermediate-mafic volcanic rocks for the lower part of Manghuai Formation characterized by depletion in Nb-Ta and enrichment in LILE, LREE and initial Sr-Nd-Pb isotopic compositions ((87Sr/86Sr)r= 0.706116-0.707046, sNd(t)=-2.69~-4.02, (206Pb/204Pb)t=l 8.541-18.800, (207Pb/204Pb)t= 15.614-15.698, (208Pb/204Pb)t=3g.478_3g.820), with an affinity to basaltic andesite and andesite, show similar signatures to source of the enriched lithospheric mantle modified by the subducted pelagic sediments. Their higher Pb/Nd ratios than those of island arc volcanic rocks indicate a possible contribution of pelagic sediments. The result of simulating calculation further suggests that its origin source could be the product of the Indian MORB-type source mixed with 5-7% pelagic sediments.3 > The rhyolites for the uppermost of Manghuai Formation characterized by a relatively low initial 87Sr/86Sr (0.705717-0.707262) and high eNd(t) (-4.64~-6.34) ratios and variable initial Pb isotopic composition ((206Pb/204Pb)t==17.220-18.570), with the geochemical affinity to A-type granite, are distinct from the felsic rocks derived from partial melting of crust, but similar to Anorogenic A-type felsic rocks. The result of simulating calculation indicates that the rhyolites for the uppermost of Manghuai Formation might be originated from the underplated basic magma mixed with 5-7% lower crustal materials and 8-10% middle-upper crustal materials, and then underwent some mineral crystallization and fractionation during the ascent of magma.4^ The late-Triassic volcanic rocks for the Xiaodingxi and Manghuihe Formations possess the feature of high-Al basaltic rocks. In light of the discrepancy of their MgO contents, they are divided into two groups: group 1: high-Al and low-Mg basaltic series (Al2O3=16.00-16.85wt%, MgO=3.04-7.50wt%), and group 2: high-Al and high-Mg basaltic series (Al2O3=16.77-19.79wt%, MgO=7.74-11.00wt%). The group 1 possess Zr/Nb=9.29-15.42, Nb/La=0.26-0.66, La/Sm=4.19-6.86, ENd(t)= -2.30-3.44 (2O6Pb/2O4Pb)r=18.401-18.598. Group 2 have higher Zr/Nb (19.37-23.92) and ENd(t) (1.25-2.31) ratios and lower La/Sm (1.65-3.11) ratios. The corresponding results of
simulating calculation implies that the mantle source of Group 1 volcanism could be product of Indian MORB-type mantle source modified by mixing with 4-7% pelagic sediments, while the Group2 rocks could be derived from the interaction of low-Mg and high-Al magma and asthenospheric components.5> Based on the previous data of the evolution of paleo-Tethyan Ocean, we reconstruct the model of evolution of paleo-Tethyan Ocean (Cangning-Menglian Ocean) in the western Yunnan Province. The Cangning-Menglian Ocean had opened before the middle-Devonian. The continent-continent or continent-arc collision had developed from the late-Permian to early-Triassic. The evolution of post-orogenic phase had occurred in the region since the middle- to -Triassic time. Subducted slab had begun to slip off or delaminate since the early-Triassic, and resulted in the generation of the middle-Triassic igneous rocks. Following the slab slip-off or delamination, the ascending asthenosphere interacted with the enriched lithospheric mantle modified by the subducted pelagic sediments and produced the late-Triassic volcanic rocks (high-Al, low-Mg and high-Al, high-Mg basaltic rocks for the Xiaodingxi and Manghuihe Formation).
1、澜沧江南带三叠纪火山岩锆石SHRIMP U-Pb年代学表明,景洪忙怀组下段中基性火山岩(20SM-408)形成于241.0±4.9Ma,其顶部流纹岩(02DX-95)形成于231.0±5.0Ma;临沧花岗岩基主体的2个二长花岗岩的代表性样品(02DX-137和20JH-10)分别给出了229.4±3.0 Ma和230.4±3.6Ma的谐和年龄;原划为小定西组的下部基性岩样品(02DX-103)给出了213.5±7.7Ma的谐和年龄,而原划为芒汇河组的上部火山岩(02DX-124)给出了216+20Ma的参考年龄。
2、忙怀组下段中基性火山岩为玄武质安山岩-安山岩系列,以亏损Nb-Ta、P等高场强元素和富集LILE、LREE为特征,((87)~Sr/(86)~Sr)_i=0.706116-0.707046,εNd(t)=-2.69～-4.02,((206)~Pb/(204)~pb)_t=18.541-18.800,((207)~Pb/(204)~Pb)_t=15.614-15.698,((208)~Pb/(204)~Pb)_t=38.478-38.820。其高于岛弧火山岩的Pb/Nd比值,与受俯冲沉积物改造的富集岩石圈地幔特征相似,模拟计算结果暗示其源区可能是印度洋MORB玄武岩源区与5-7%洋壳俯冲沉积物混合作用的结果。
3、忙怀组上段流纹岩显示 A-型酸性岩特征,具较低初始(87)~Sr/(86)~Sr(0.705717-0.707262)和较高εNd(t)(-4.64～-6.34)值及变化较大的初始Pb同位素组成((206)~Pb/(204)~Pb)_t=17.220-18.570,((207)~Pb/(204)~Pb)_t=15.601-15.570,((208)~Pb/(204)~Pb)_t=36.964-
The post-collisional magmatism can provide a great deal of important information on the interaction of crust and mantle during subduction and collision. In particular, the natures of magma source and the tectonic settings of generation of magmatism to understand the tectonic evolution of orogenic belt and the crust-mantle interaction are very important. As a major suture of paleo-Tethyan ocean, the Triassic volcanic rocks with a depth up to 8000 m and granitic intrusion correlated with subduction and collision of the paleo-Tethyan ocean were cropped out in the Yunxian-Jinghong area, Southern Lancangjiang zone. Thus, we chose the Triassic magmatism to conduct the study on systematic lithology (lithofacies), zircon SHRIMP U-Pb and whole-rock ~(40)Ar/~(39)Ar geochronology, elemental and Sr-Nd-Pb isotopic geochemistry. The main objectives are: (1) to confirm patterns of distribution of different magmatism belts;(2) to investigate the petrogenesis of magma and their tectonic settings relative to their generation;(3) to probe into the geodynamic mechanism of the Triassic magmatism and their constraint on the tectonic evolution of the paleo-Tethyan Ocean;(4) to better understand the deep process and mechanism of crust-mantle interaction of typical post-collisional magmatism. The major conclusions are summarized as follow:1、 The geochronological data of zircon SHRIMP U-Pb for the Triassic igneous rocks from the Southern Lancangjiang zone indicate that the intermediate-mafic volcanic rock (20SM-408) from the lower part of the Manghuai Formation and the rhyolite (02DX-95) from its uppermost part were erupted at ca. 241.0±4.9 Ma and ca. 231.0±5.0 Ma, respectively, and the main granitic intrusions in Lincang batholith
were mainly intruded at about ca. 230Ma, and the volcanic rocks from Xiaodingxi Formation and Manghuihe Formation could were generated at similar time(215-210 Ma).2 s The middle-Triassic intermediate-mafic volcanic rocks for the lower part of Manghuai Formation characterized by depletion in Nb-Ta and enrichment in LILE, LREE and initial Sr-Nd-Pb isotopic compositions ((87Sr/86Sr)r= 0.706116-0.707046, sNd(t)=-2.69~-4.02, (206Pb/204Pb)t=l 8.541-18.800, (207Pb/204Pb)t= 15.614-15.698, (208Pb/204Pb)t=3g.478_3g.820), with an affinity to basaltic andesite and andesite, show similar signatures to source of the enriched lithospheric mantle modified by the subducted pelagic sediments. Their higher Pb/Nd ratios than those of island arc volcanic rocks indicate a possible contribution of pelagic sediments. The result of simulating calculation further suggests that its origin source could be the product of the Indian MORB-type source mixed with 5-7% pelagic sediments.3 > The rhyolites for the uppermost of Manghuai Formation characterized by a relatively low initial 87Sr/86Sr (0.705717-0.707262) and high eNd(t) (-4.64~-6.34) ratios and variable initial Pb isotopic composition ((206Pb/204Pb)t==17.220-18.570), with the geochemical affinity to A-type granite, are distinct from the felsic rocks derived from partial melting of crust, but similar to Anorogenic A-type felsic rocks. The result of simulating calculation indicates that the rhyolites for the uppermost of Manghuai Formation might be originated from the underplated basic magma mixed with 5-7% lower crustal materials and 8-10% middle-upper crustal materials, and then underwent some mineral crystallization and fractionation during the ascent of magma.4^ The late-Triassic volcanic rocks for the Xiaodingxi and Manghuihe Formations possess the feature of high-Al basaltic rocks. In light of the discrepancy of their MgO contents, they are divided into two groups: group 1: high-Al and low-Mg basaltic series (Al2O3=16.00-16.85wt%, MgO=3.04-7.50wt%), and group 2: high-Al and high-Mg basaltic series (Al2O3=16.77-19.79wt%, MgO=7.74-11.00wt%). The group 1 possess Zr/Nb=9.29-15.42, Nb/La=0.26-0.66, La/Sm=4.19-6.86, ENd(t)= -2.30-3.44 (2O6Pb/2O4Pb)r=18.401-18.598. Group 2 have higher Zr/Nb (19.37-23.92) and ENd(t) (1.25-2.31) ratios and lower La/Sm (1.65-3.11) ratios. The corresponding results of
simulating calculation implies that the mantle source of Group 1 volcanism could be product of Indian MORB-type mantle source modified by mixing with 4-7% pelagic sediments, while the Group2 rocks could be derived from the interaction of low-Mg and high-Al magma and asthenospheric components.5> Based on the previous data of the evolution of paleo-Tethyan Ocean, we reconstruct the model of evolution of paleo-Tethyan Ocean (Cangning-Menglian Ocean) in the western Yunnan Province. The Cangning-Menglian Ocean had opened before the middle-Devonian. The continent-continent or continent-arc collision had developed from the late-Permian to early-Triassic. The evolution of post-orogenic phase had occurred in the region since the middle- to -Triassic time. Subducted slab had begun to slip off or delaminate since the early-Triassic, and resulted in the generation of the middle-Triassic igneous rocks. Following the slab slip-off or delamination, the ascending asthenosphere interacted with the enriched lithospheric mantle modified by the subducted pelagic sediments and produced the late-Triassic volcanic rocks (high-Al, low-Mg and high-Al, high-Mg basaltic rocks for the Xiaodingxi and Manghuihe Formation).
引文
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