云南腾冲全新世火山岩岩浆演化和岩石成因
|
摘要
腾冲火山岩区是我国全新世以来记载火山喷发的少数地区之一,该地区岩浆作用的性质与成因是揭示青藏高原东缘的现今侧向生长过程与深部作用的重要依据。本文对腾冲火山岩区的马鞍山、黑空山、打鹰山全新世火山岩开展了矿物化学和岩石地球化学研究,以期揭示岩石成因和深部动力学过程。腾冲全新世火山岩主体岩性为高钾钙碱性系列的玄武粗安岩和粗安岩。岩石的CaO、Fe_2O_3~T、TiO_2与SiO_2负相关,而K_2O与SiO_2正相关,表明岩浆演化过程中可能存在橄榄石、辉石和斜长石的分离结晶作用。岩石中存在酸性斜长石(更长石,An=28)大颗粒捕掳晶,其边部发育了基性斜长石(拉长石,An=65)增生边;在大颗粒石英捕掳晶的边部发育了辉石的反应边,这些结构表明在岩浆上升到地壳浅部时,曾受到了花岗岩围岩的混染,但岩石的Th/Nb值均小于1.16,表明地壳混染总体不显著。腾冲全新世火山岩大离子亲石元素富集、高场强元素相对亏损,高Th/U、低Ba/La,富集Sr-Nd同位素,其岩浆源区应为经历过洋壳沉积物交代后的富集地幔。腾冲火山岩属于大陆板内环境,是印度与亚洲大陆碰撞后岩浆作用的产物。火山岩是沿着腾冲盆地南北向展布,且熔岩分布面积有限。由于高原侧向生长过程中的区域性走滑断裂会引起局部的伸展,腾冲火山岩产出可能与富集岩石圈地幔的减压熔融有关。
Tengchong volcanic field is one of the areas with the records of Holocene volcanos in China.The magmatism nature and petrogenesis of this Tengchong Holocene Volcanics(THV)are essential evidences in revealing the present southeastward growth and deep processes of the Tibetan Plateau.This paper carried out mineral chemistry and whole rock geochemistry study on three volcanos(Maanshan,Heikongshan,and Dayingshan)of the THV,and discuss the origin and dynamics of the magmatism.The majority of the THV are high potassium calc-alkaline rocks,including basaltic trachyandesite and trachyandesite.We found negative correlations between SiO_2and CaO,Fe_2O_3~T,TiO_2,MgO,and positive correlation between SiO_2and K_2O,which indicate the fractional crystallization of olivine,pyroxene,and plagioclase.The xenocrysts of plagioclase with acidic composition(An=28)has overgrowth basic plagioclase rim(An=65),and xenocrysts of quartz with narrow pyroxene reaction rim,were found in the trachyandesite samples,which possibly suggest the crustal contamination by granitoid country rock during the magma upwelling processes in shallow level of the crust.On the contrary,the whole rock Th/Nb ratio is small(<1.16),which reflects a minor overall contamination.The THV show enrichment in large ion lithophile element(LILE),and depletion in high field strength element(HFSE),high Th/U and low Ba/La ratios,and enrichment of Sr-Nd isotopes,which as a whole implies that the magma should have come from an enriched upper mantle that have experienced metasomatism by subduction of pelagic sediments of the Neo-Tethys.The THV are formed in intraplate tectonic setting of post-collision regime after the collision between India and Asia.The volcanos are distributing in north-south trending along the Tengchong basin and erupted in limited volume.Considering the highly localized extension along regional strike-slip faults during the lateral spreading in the eastern Tibetan plateau,the trigger of the Tengchong Holocene volcanic rocks may be interpreted as resulting of the decompression melting of the enriched metasomatized mantle lithosphere.
Tengchong volcanic field is one of the areas with the records of Holocene volcanos in China.The magmatism nature and petrogenesis of this Tengchong Holocene Volcanics(THV)are essential evidences in revealing the present southeastward growth and deep processes of the Tibetan Plateau.This paper carried out mineral chemistry and whole rock geochemistry study on three volcanos(Maanshan,Heikongshan,and Dayingshan)of the THV,and discuss the origin and dynamics of the magmatism.The majority of the THV are high potassium calc-alkaline rocks,including basaltic trachyandesite and trachyandesite.We found negative correlations between SiO_2and CaO,Fe_2O_3~T,TiO_2,MgO,and positive correlation between SiO_2and K_2O,which indicate the fractional crystallization of olivine,pyroxene,and plagioclase.The xenocrysts of plagioclase with acidic composition(An=28)has overgrowth basic plagioclase rim(An=65),and xenocrysts of quartz with narrow pyroxene reaction rim,were found in the trachyandesite samples,which possibly suggest the crustal contamination by granitoid country rock during the magma upwelling processes in shallow level of the crust.On the contrary,the whole rock Th/Nb ratio is small(<1.16),which reflects a minor overall contamination.The THV show enrichment in large ion lithophile element(LILE),and depletion in high field strength element(HFSE),high Th/U and low Ba/La ratios,and enrichment of Sr-Nd isotopes,which as a whole implies that the magma should have come from an enriched upper mantle that have experienced metasomatism by subduction of pelagic sediments of the Neo-Tethys.The THV are formed in intraplate tectonic setting of post-collision regime after the collision between India and Asia.The volcanos are distributing in north-south trending along the Tengchong basin and erupted in limited volume.Considering the highly localized extension along regional strike-slip faults during the lateral spreading in the eastern Tibetan plateau,the trigger of the Tengchong Holocene volcanic rocks may be interpreted as resulting of the decompression melting of the enriched metasomatized mantle lithosphere.
引文
Bai DH,Meju MA and Liao ZJ.2001.Magnetotelluric images of deep crustal structure of the Rehai geothermal field near Tengchong,southern China.Geophysical Journal International,148(3):677-687
Boynton WV.1984.Cosmochemistry of the rare earth elements:Meteorite studies.In:Henderson P(ed.).Rare Earth Element Geochemistry.Amsterdam:Elsevier,2:63-114
Chen FK,Satir M,Ji J and Zhong D.2002.Nd-Sr-Pb isotopes of Tengchong Cenozoic volcanic rocks from western Yunnan,China:Evidence for an enriched-mantle source.Journal of Asian Earth Sciences,21(1):39-45
Chen FK,Li XH,Wang XL,Li QL and Siebel WG.2007.Zircon and Nd-Hf isotopic composition of the Yunnan Tethyan belt,southwestern China.International Journal of Earth Sciences,96(6):1179-1194
Chu MF,Chung SL,O’Reilly SY,Pearson NJ,Wu FY,Li XH,Liu DY,Ji JQ,Chu QH and Lee HY.2011.India’s hidden inputs to Tibetan orogeny revealed by Hf isotopes of Transhimalayan zircons and host rocks.Earth and Planetary Science Letters,307(3-4):479-486
Chung SL,Chu MF,Zhang YQ,Xie YW,Lo CH,Lee TY,Lan CY,Li XH,Zhang Q and Wang YZ.2005.Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism.Earth-Science Reviews,68(3-4):173-196
Class C,Miller DM,Goldstein SL and Langmuir CH.2000.Distinguishing melt and fluid subduction components in Umnak Volcanics,Aleutian Arc.Geochemistry,Geophysics,Geosystems,1:1004
Duan XZ,Fan HR,Zhang HF,Yaxley G,Santosh M,Tian HC,Tan KX,Tang ZP,Xie YS,Xiao YL,He ZH and Guo HF.2019.Melt inclusions in phenocrysts track enriched upper mantle source for Cenozoic Tengchong volcanic field,Yunnan Province,SW China.Lithos,324-325:180-201
Elburg MA,van Bergen M,Hoogewerff J,Foden J,Vroon P,Zulkarnain I and Nasution A.2002.Geochemical trends across an arc-continent collision zone:Magma sources and slab-wedge transfer processes below the Pantar Strait volcanoes,Indonesia.Geochimica et Cosmochimica Acta,66(15):2771-2789
Gao JF,Zhou MF,Robinson PT,Wang CY,Zhao JH and Malpas J.2015.Magma mixing recorded by Sr isotopes of plagioclase from dacites of the Quaternary Tengchong volcanic field,SE Tibetan Plateau.Journal of Asian Earth Sciences,98:1-17
Guo ZF,Hertogen J,Liu J,Pasteels P,Boven A,Punzalan L,He HY,Luo XJ and Zhang WH.2005.Potassic magmatism in western Sichuan and Yunnan provinces,SE Tibet,China:Petrological and geochemical constraints on petrogenesis.Journal of Petrology,46(1):33-78
Guo ZF,Wilson M,Zhang ML,Cheng ZH and Zhang LH.2013.Postcollisional,K-rich mafic magmatism in South Tibet:Constraints on Indian slab-to-wedge transport processes and plateau uplift.Contributions to Mineralogy and Petrology,165(6):1311-1340
Guo ZF,Cheng ZH,Zhang ML,Zhang LH,Li XH and Liu JQ.2015.Post-collisional high-K calc-alkaline volcanism in Tengchong volcanic field,SE Tibet:Constraints on Indian eastward subduction and slab detachment.Journal of the Geological Society,172(5):624-640
Hawkesworth CJ,Turner SP,Mc Dermott F,Peate DW and Van Calsteren P.1997.U-Th isotopes in arc magmas:Implications for element transfer from the subducted crust.Science,276(5312):551-555
Hébert R,Guilmette C,Dostal J,Bezard R,Lesage G,Bédardéand Wang CS.2014.Miocene post-collisional shoshonites and their crustal xenoliths,Yarlung Zangbo Suture Zone southern Tibet:Geodynamic implications.Gondwana Research,25(3):1263-1271
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Hou ZQ,Gao YF,Qu XM,Rui ZY and Mo XX.2004.Origin of adakitic intrusives generated during Mid-Miocene east-west extension in southern Tibet.Earth and Planetary Science Letters,220(1-2):139-155
Hu JH,Song XY,He HL,Zheng WQ,Yu SY,Chen LM and Lai CK.2018.Constraints of texture and composition of clinopyroxene phenocrysts of Holocene volcanic rocks on a magmatic plumbing system beneath Tengchong,SW China.Journal of Asian Earth Sciences,154:342-353
Huang JL and Zhao DP.2006.High-resolution mantle tomography of China and surrounding regions.Journal of Geophysical Research,11(B9):B09305
Huang XL,Niu YL,Xu YG,Chen LL and Yang QJ.2010.Mineralogical and geochemical constraints on the petrogenesis of postcollisional potassic and ultrapotassic rocks from Western Yunnan,SW China.Journal of Petrology,51(8):1617-1654
Huang XW,Zhou MF,Wang CY,Robinson PT,Zhao JH and Qi L.2013.Chalcophile element constraints on magma differentiation of Quaternary volcanoes in Tengchong,SW China.Journal of Asian Earth Sciences,76:1-11
Jiang CS.1998.Distribution characteristics of Tengchong volcano in the Cenozoic era.Journal of Seismological Research,21(4):309-319(in Chinese with English abstract)
Le Maitre RW.1989.A classification of Igneous Rock and Glossary of Terms.Oxford:Blackwell Science Publication
Lei HS,Ma Q,Liu Z,Zhao ZD,Zhu DC and Mo XX.2017.The geochemistry and petrogenesis of Cenozoic basalt in Sofular-Acig9l Marr,Central Turkey.Acta Petrologica Sinica,33(8):2619-2632(in Chinese with English abstract)
Lei JS,Zhao DP and Su YJ.2009.Insight into the origin of the Tengchong intraplate volcano and seismotectonics in Southwest China from local and teleseismic data.Journal of Geophysical Research,114:B05302
Li DM,Li Q and Chen WJ.2000.Volcanic activities in the Tengchong volcano area since Pliocene.Acta Petrologica Sinica,16(3):362-370(in Chinese with English abstract)
Li X and Liu JQ.2012.A study on the geochemical characteristics and petrogenesis of Holocene volcanic rocks in the Tengchong volcanic eruption field,Yunnan Province,SW China.Acta Petrologica Sinica,28(5):1507-1516(in Chinese with English abstract)
Lin MS,Peng SB and Qiao WT.2017.40Ar/30Ar geochronology and geochemistry of Pleistocene trachyandesite in Tengchong,western Yunnan,China,and its tectonic implication.Acta Petrologica Sinica,33(10):3137-3146(in Chinese with English abstract)
Liu D,Zhao ZD,Zhu DC,Niu YL and Harrison TM.2014a.Zircon xenocrysts in Tibetan ultrapotassic magmas:Imaging the deep crust through time.Geology,42(1):43-46
Liu D,Zhao ZD,Zhu DC,Niu YL,De Paolo DJ,Harrison TM,Mo XX,Dong GC,Zhou S,Sun CG,Zhang ZC and Liu JL.2014b.Postcollisional potassic and ultrapotassic rocks in southern Tibet:Mantle and crustal origins in response to India-Asia collision and convergence.Geochimica et Cosmochimica Acta,143:207-231
Liu D,Zhao ZD,Zhu DC,Niu YL,Widom E,Teng FZ,De Paolo DJ,Ke S,Xu JF,Wang Q and Mo XX.2015.Identifying mantle carbonatite metasomatism through Os-Sr-Mg isotopes in Tibetan ultrapotassic rocks.Earth and Planetary Science Letters,430:458-469
Liu D,Zhao ZD,Niu YL,Zhu DC and Li XH.2018.Perovskite U-Pb and Sr-Nd isotopic perspectives on melilitite magmatism and outward growth of the Tibetan Plateau.Geology,46(12):1027-1030
Liu F,Li X,Wang GQ,Liu YF,Zhu HL,Kan JT,Huang F,Sun WD,Xia XP and Zhang ZF.2017.Marine carbonate component in the mantle beneath the southeastern Tibetan Plateau:Evidence from magnesium and calcium isotopes.Journal of Geophysical ResearchSolid Earth,122(12):9729-9744
Liu S,Hu RZ,Gao S,Feng CX,Huang ZL,Lai SC,Yuan HL,Liu XM,Coulson IM,Feng GY,Wang T and Qi YQ.2009.U-Pb zircon,geochemical and Sr-Nd-Hf isotopic constraints on the age and origin of Early Palaeozoic I-type granite from the Tengchong-Baoshan Block,western Yunnan Province,SW China.Journal of Asian Earth Sciences,36(2-3):168-182
Liu YS,Zong KQ,Kelemen PB and Gao S.2008.Geochemistry and magmatic history of eclogites and ultramafic rocks from the Chinese Continental Scientific Drill Hole:Subduction and ultrahigh-pressure metamorphism of lower crustal cumulates.Chemical Geology,247(1-2):133-153
Luo ZH,Liu JQ,Zhao CP,Guo ZF,Cheng LL,Li XH and Li DP.2011.Deep fluids and magmatism:The deep processes beneath the Tengchong volcano group.Acta Petrologica Sinica,27(10):2855-2862(in Chinese with English abstract)
Marschall HR and Schumacher JC.2012.Arc magmas sourced from mélange diapirs in subduction zones.Nature Geoscience,5(12):862-867
Mo XX,Zhao ZD,Deng JF,Flower M,Yu XH,Luo ZH,Li YH,Zhou S,Dong GC,Zhu DC and Wang LL.2006.Petrology and geochemistry of postcollisional volcanic rocks from the Tibetan Plateau:Implications for lithosphere heterogeneity and collisioninduced asthenosphere mantle flow.Geological Society of America Special Paper,409:507-530
Mo XX,Hou ZQ,Niu YL,Dong GC,Qu XM,Zhao ZD and Yang ZM.2007.Mantle contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet.Lithos,96(1-2):225-242
Niu ZJ,Liu Y and Di YJ.2014.Zoning characteristics of the plagioclase from the Mesozoic trachyandesite in Wuchagou area of the Da Hinggan Mountains and its geological implications.Acta Petrologica et Mineralogica,33(1):102-108(in Chinese with English abstract)
Pearce JA and Parkinson IJ.1993.Trace element models for mantle melting:Application to volcanic arc petrogenesis.In:Prichard HM,Alabaster T,Harris NBW and Neary CR(eds.).Magmatic Processes and Plate Tectonics.Geological Society,London,Special Publications,76(1):373-403
Plank T and Langmuir CH.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle.Chemical Geology,145(3-4):325-394
Powell CM and Johnson BD.1980.Contraints on the Cenozoic position of Sundaland.Tectonophysics,63(1-4):91-109
Qin JZ,Huangfu G,Li Q,Qian XD,Su YJ and Cai MJ.2000.3-Dchromatography of velocity structure in Tengchong volcano areas and nearby.Journal of Seismological Research,23(2):157-164(in Chinese with English abstract)
Rehkmper M and Hofmann AW.1997.Recycled ocean crust and sediment in Indian Ocean MORB.Earth and Planetary Science Letters,147(1-4):93-106
Rowley DB.1996.Age of initiation of collision between India and Asia:A review of stratigraphic data.Earth and Planetary Science Letters,145(1-4):1-13
Sato H.1977.Nickel content of basaltic magmas:Identification of primary magmas and a measure of the degree of olivine fractionation.Lithos,10(2):113-120
Saunders AD,Storey M,Kent RW and Norry MJ.1992.Consequences of plume-lithosphere interactions.In:Storey BC,Alabasater T and Pankhurst RJ(eds.).Magmatism and the Causes of Continental Break-up.Geological Society,London,Special Publications,68:41-60
Sheppard S and Taylor WR.1992.Barium-and LREE-rich,olivinemica-lamprophyres with affinities to lamproites,Mt.Bundey,Northern Territory,Australia.Lithos,28(3-6):303-325
Smith RK and Lofgren GF.1983.An analytical and experimental study of zoning in plagioclase.Lithos,16(2):153-168
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313-345
Takagi D,Sato H and Nakagawa M.2005.Experimental study of a lowalkali tholeiite at 1~5kbar:Optimal condition for the crystallization of high-An plagioclase in hydrous arc tholeiite.Contributions to Mineralogy and Petrology,149(5):527-540
Thompson RN and Gibson SA.2000.Transient high temperatures in mantle plume heads inferred from magnesian olivines in Phanerozoic picrites.Nature,407(6803):502-506
Tian HC,Yang W,Li SG,Ke S and Duan XZ.2018.Lowδ26Mg volcanic rocks of Tengchong in southwestern China:A deep carbon cycle induced by supercritical liquids.Geochimica et Cosmochimica Acta,240:191-219
Ustunisik G,Kilinc A and Nielsen RL.2014.New insights into the processes controlling compositional zoning in plagioclase.Lithos,200-201:80-93
Vroon PZ,Van Bergen MJ,White WM and Varekamp JC.1993.Sr-NdPb isotope systematics of the Banda Arc,Indonesia:Combined subduction and assimilation of continental material.Journal of Geophysical Research,98(B12):22349-22366
Wang JH,Yin A,Harrison TM,Grove M,Zhang YQ and Xie GH.2001.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision Zone.Earth and Planetary Science Letters,188(1-2):123-133
Wang Q,Wyman DA,Xu JF,Dong YH,Vasconcelos PM,Pearson N,Wan YS,Dong H,Li CF,Yu YS,Zhu TX,Feng XT,Zhang QY,Zi F and Chu ZY.2008.Eocene melting of subducting continental crust and early uplifting of central Tibet:Evidence from centralwestern Qiangtang high-K calc-alkaline andesites,dacites and rhyolites.Earth and Planetary Science Letters,272(1-2):158-171
Workman RK and Hart SR.2005.Major and trace element composition of the depleted MORB mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72
Wu TF,Zhang SX,Li MK,Qin WB and Zhang CY.2016.Two crustal flowing channels and volcanic magma migration underneath the SEmargin of the Tibetan Plateau as revealed by surface wave tomography.Journal of Asian Earth Sciences,132:25-29
Xu CL,Zhao GT,He YY and Li DP.2012.Geochemistry of Cenozoic volcanic rocks from Tengchong,western Yunnan.Marine Geology and Quaternary Geology,32(2):65-75(in Chinese)
Xu Y,Li XL and Wang S.2017.Crustal thickness and Poisson’s ratio of the Tengchong volcanic area in southweatern China.Chinese Journal of Geophysics,60(6):2256-2264(in Chinese with English abstract)
Yan DP,Zhou MF,Wang CY and Xia B.2006.Structural and geochronological constraints on the tectonic evolution of the DulongSong Chay tectonic dome in Yunnan Province,SW China.Journal of Asian Earth Sciences,28(4-6):332-353
Yang F,Huang XL and Li J.2018.Magma processes and petrogenesis of the Late Cretaceous plagioclase-phyric basalt in the Changchengling area,South China.Acta Petrologica Sinica,34(1):157-171(in Chinese with English abstract)
Yu HM.2011.Microstructural study on volcanic products and its geological implications.Ph.D.Dissertation.Beijing:Institute of Geology,China Earthquake Administration(in Chinese with English summary)
Yu HM,Xu JD,Lin CY,Shi LB and Chen XD.2012.Magmatic processes inferred from chemical composition,texture and crystal size distribution of the Heikongshan lavas in the Tengchong volcanic field,SW China.Journal of Asian Earth Sciences,58:1-15
Zhang B,Zhang JJ and Zhong DL.2010.Structure,kinematics and ages of transpression during strain-partitioning in the Chongshan shear zone,western Yunnan,China.Journal of Structural Geology,32(4):445-463
Zhao CP,Ran H and Chen KH.2006.Present-day magma chambers in Tengchong volcano area inferred from relative geothermal gradient.Acta Petrologica Sinica,22(6):1517-1528(in Chinese with English abstract)
Zhao DP and Liu L.2010.Deep structure and origin of active volcanoes in China.Geoscience Frontiers,1(1):31-44
Zhao ZD,Mo XX,Dilek Y,Niu YL,De Paolo DJ,Robinson P,Zhu DC,Sun CG,Dong GC,Zhou S,Luo ZH and Hou ZQ.2009.Geochemical and Sr-Nd-Pb-O isotopic compositions of the postcollisional ultrapotassic magmatism in SW Tibet:Petrogenesis and implications for India intra-continental subduction beneath southern Tibet.Lithos,113(1-2):190-212
Zhou MF,Robinson PT,Wang CY,Zhao JH,Yan DP,Gao JF and Malpas J.2012.Heterogeneous mantle source and magma differentiation of Quaternary arc-like volcanic rocks from Tengchong,SE margin of the Tibetan Plateau.Contributions to Mineralogy and Petrology,163(5):841-860
Zhu BQ,Mao CX,Lugmair GW and Macdougall JD.1983.Isotopic and geochemical evidence for the origin of Plio-Pleistocene volcanic rocks near the Indo-Eurasian collisional margin at Tengchong,China.Earth and Planetary Science Letters,65(2):263-275
Zou HB,Fan QC,Schmitt AK and Sui JL.2010.U-Th dating of zircons from Holocene potassic andesites(Maanshan volcano,Tengchong,SE Tibetan Plateau)by depth profiling:Time scales and nature of magma storage.Lithos,118(1-2):202-210
Zou HB,Shen CC,Fan QC and Lin K.2014.U-series disequilibrium in young Tengchong volcanics:Recycling of mature clay sediments or mudstones into the SE Tibet mantle.Lithos,192-195:132-141
Zou HB,Ma MJ,Fan QC,Xu B,Li SQ,Zhao YW and King DT Jr.2017.Genesis and open-system evolution of Quaternary magmas beneath southeastern margin of Tibet:Constraints from Sr-Nd-Pb-Hf
isotope systematics.Lithos,272-273:278-290
姜朝松.1998.腾冲新生代火山分布特征.地震研究,21(4):309-319
雷杭山,马倩,刘泽,赵志丹,朱弟成,莫宣学.2017.土耳其中部阿哲格尔火山湖新生代玄武岩的地球化学与岩石成因.岩石学报,33(8):2619-2632
李大明,李齐,陈文寄.2000.腾冲火山区上新世以来的火山活动.岩石学报,16(3):362-370
李欣,刘嘉麒.2012.云南腾冲全新世火山岩地球化学特征及其成因.岩石学报,28(5):1507-1516
林木森,彭松柏,乔卫涛.2017.滇西腾冲更新世粗面安山岩Ar-Ar年代学、地球化学特征及其构造意义.岩石学报,33(10):3137-3146
罗照华,刘嘉琦,赵慈平,郭正府,程黎鹿,李晓惠,李大鹏.2011.深部流体与岩浆活动:兼论腾冲火山群的深部过程.岩石学报,27(10):2855-2862
牛之建,刘跃,狄永军.2014.大兴安岭五岔沟地区中生代粗安岩中斜长石环带特征及其地质意义.岩石矿物学杂志,33(1):102-108
秦嘉政,皇甫岗,李强,钱晓东,苏有锦,蔡明军.2000.腾冲火山及邻区速度结构的三维层析成象.地震研究,23(2):157-164
徐翠玲,赵广涛,何雨旸,李德平.2012.滇西腾冲新生代火山岩岩石地球化学特征.海洋地质与第四纪地质,32(2):65-75
胥颐,李雪垒,汪晟.2017.腾冲火山区的地壳厚度和平均泊松比研究.地球物理学报,60(6):2256-2264
杨帆,黄小龙,李洁.2018.华南长城岭晚白垩世斜斑玄武岩的岩浆作用过程与岩石成因制约.岩石学报,34(1):157-171
于红梅.2011.火山喷发物的显微构造研究及其地质意义.博士学位论文.北京:中国地震局地质研究所
赵慈平,冉华,陈坤华.2006.由相对地热梯度推断的腾冲火山区现存岩浆囊.岩石学报,22(6):1517-1528
(1)云南省地质局区域地质调查队.1982.1︰20万腾冲幅(G-47-XXV11)区域地质图
Boynton WV.1984.Cosmochemistry of the rare earth elements:Meteorite studies.In:Henderson P(ed.).Rare Earth Element Geochemistry.Amsterdam:Elsevier,2:63-114
Chen FK,Satir M,Ji J and Zhong D.2002.Nd-Sr-Pb isotopes of Tengchong Cenozoic volcanic rocks from western Yunnan,China:Evidence for an enriched-mantle source.Journal of Asian Earth Sciences,21(1):39-45
Chen FK,Li XH,Wang XL,Li QL and Siebel WG.2007.Zircon and Nd-Hf isotopic composition of the Yunnan Tethyan belt,southwestern China.International Journal of Earth Sciences,96(6):1179-1194
Chu MF,Chung SL,O’Reilly SY,Pearson NJ,Wu FY,Li XH,Liu DY,Ji JQ,Chu QH and Lee HY.2011.India’s hidden inputs to Tibetan orogeny revealed by Hf isotopes of Transhimalayan zircons and host rocks.Earth and Planetary Science Letters,307(3-4):479-486
Chung SL,Chu MF,Zhang YQ,Xie YW,Lo CH,Lee TY,Lan CY,Li XH,Zhang Q and Wang YZ.2005.Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism.Earth-Science Reviews,68(3-4):173-196
Class C,Miller DM,Goldstein SL and Langmuir CH.2000.Distinguishing melt and fluid subduction components in Umnak Volcanics,Aleutian Arc.Geochemistry,Geophysics,Geosystems,1:1004
Duan XZ,Fan HR,Zhang HF,Yaxley G,Santosh M,Tian HC,Tan KX,Tang ZP,Xie YS,Xiao YL,He ZH and Guo HF.2019.Melt inclusions in phenocrysts track enriched upper mantle source for Cenozoic Tengchong volcanic field,Yunnan Province,SW China.Lithos,324-325:180-201
Elburg MA,van Bergen M,Hoogewerff J,Foden J,Vroon P,Zulkarnain I and Nasution A.2002.Geochemical trends across an arc-continent collision zone:Magma sources and slab-wedge transfer processes below the Pantar Strait volcanoes,Indonesia.Geochimica et Cosmochimica Acta,66(15):2771-2789
Gao JF,Zhou MF,Robinson PT,Wang CY,Zhao JH and Malpas J.2015.Magma mixing recorded by Sr isotopes of plagioclase from dacites of the Quaternary Tengchong volcanic field,SE Tibetan Plateau.Journal of Asian Earth Sciences,98:1-17
Guo ZF,Hertogen J,Liu J,Pasteels P,Boven A,Punzalan L,He HY,Luo XJ and Zhang WH.2005.Potassic magmatism in western Sichuan and Yunnan provinces,SE Tibet,China:Petrological and geochemical constraints on petrogenesis.Journal of Petrology,46(1):33-78
Guo ZF,Wilson M,Zhang ML,Cheng ZH and Zhang LH.2013.Postcollisional,K-rich mafic magmatism in South Tibet:Constraints on Indian slab-to-wedge transport processes and plateau uplift.Contributions to Mineralogy and Petrology,165(6):1311-1340
Guo ZF,Cheng ZH,Zhang ML,Zhang LH,Li XH and Liu JQ.2015.Post-collisional high-K calc-alkaline volcanism in Tengchong volcanic field,SE Tibet:Constraints on Indian eastward subduction and slab detachment.Journal of the Geological Society,172(5):624-640
Hawkesworth CJ,Turner SP,Mc Dermott F,Peate DW and Van Calsteren P.1997.U-Th isotopes in arc magmas:Implications for element transfer from the subducted crust.Science,276(5312):551-555
Hébert R,Guilmette C,Dostal J,Bezard R,Lesage G,Bédardéand Wang CS.2014.Miocene post-collisional shoshonites and their crustal xenoliths,Yarlung Zangbo Suture Zone southern Tibet:Geodynamic implications.Gondwana Research,25(3):1263-1271
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Hou ZQ,Gao YF,Qu XM,Rui ZY and Mo XX.2004.Origin of adakitic intrusives generated during Mid-Miocene east-west extension in southern Tibet.Earth and Planetary Science Letters,220(1-2):139-155
Hu JH,Song XY,He HL,Zheng WQ,Yu SY,Chen LM and Lai CK.2018.Constraints of texture and composition of clinopyroxene phenocrysts of Holocene volcanic rocks on a magmatic plumbing system beneath Tengchong,SW China.Journal of Asian Earth Sciences,154:342-353
Huang JL and Zhao DP.2006.High-resolution mantle tomography of China and surrounding regions.Journal of Geophysical Research,11(B9):B09305
Huang XL,Niu YL,Xu YG,Chen LL and Yang QJ.2010.Mineralogical and geochemical constraints on the petrogenesis of postcollisional potassic and ultrapotassic rocks from Western Yunnan,SW China.Journal of Petrology,51(8):1617-1654
Huang XW,Zhou MF,Wang CY,Robinson PT,Zhao JH and Qi L.2013.Chalcophile element constraints on magma differentiation of Quaternary volcanoes in Tengchong,SW China.Journal of Asian Earth Sciences,76:1-11
Jiang CS.1998.Distribution characteristics of Tengchong volcano in the Cenozoic era.Journal of Seismological Research,21(4):309-319(in Chinese with English abstract)
Le Maitre RW.1989.A classification of Igneous Rock and Glossary of Terms.Oxford:Blackwell Science Publication
Lei HS,Ma Q,Liu Z,Zhao ZD,Zhu DC and Mo XX.2017.The geochemistry and petrogenesis of Cenozoic basalt in Sofular-Acig9l Marr,Central Turkey.Acta Petrologica Sinica,33(8):2619-2632(in Chinese with English abstract)
Lei JS,Zhao DP and Su YJ.2009.Insight into the origin of the Tengchong intraplate volcano and seismotectonics in Southwest China from local and teleseismic data.Journal of Geophysical Research,114:B05302
Li DM,Li Q and Chen WJ.2000.Volcanic activities in the Tengchong volcano area since Pliocene.Acta Petrologica Sinica,16(3):362-370(in Chinese with English abstract)
Li X and Liu JQ.2012.A study on the geochemical characteristics and petrogenesis of Holocene volcanic rocks in the Tengchong volcanic eruption field,Yunnan Province,SW China.Acta Petrologica Sinica,28(5):1507-1516(in Chinese with English abstract)
Lin MS,Peng SB and Qiao WT.2017.40Ar/30Ar geochronology and geochemistry of Pleistocene trachyandesite in Tengchong,western Yunnan,China,and its tectonic implication.Acta Petrologica Sinica,33(10):3137-3146(in Chinese with English abstract)
Liu D,Zhao ZD,Zhu DC,Niu YL and Harrison TM.2014a.Zircon xenocrysts in Tibetan ultrapotassic magmas:Imaging the deep crust through time.Geology,42(1):43-46
Liu D,Zhao ZD,Zhu DC,Niu YL,De Paolo DJ,Harrison TM,Mo XX,Dong GC,Zhou S,Sun CG,Zhang ZC and Liu JL.2014b.Postcollisional potassic and ultrapotassic rocks in southern Tibet:Mantle and crustal origins in response to India-Asia collision and convergence.Geochimica et Cosmochimica Acta,143:207-231
Liu D,Zhao ZD,Zhu DC,Niu YL,Widom E,Teng FZ,De Paolo DJ,Ke S,Xu JF,Wang Q and Mo XX.2015.Identifying mantle carbonatite metasomatism through Os-Sr-Mg isotopes in Tibetan ultrapotassic rocks.Earth and Planetary Science Letters,430:458-469
Liu D,Zhao ZD,Niu YL,Zhu DC and Li XH.2018.Perovskite U-Pb and Sr-Nd isotopic perspectives on melilitite magmatism and outward growth of the Tibetan Plateau.Geology,46(12):1027-1030
Liu F,Li X,Wang GQ,Liu YF,Zhu HL,Kan JT,Huang F,Sun WD,Xia XP and Zhang ZF.2017.Marine carbonate component in the mantle beneath the southeastern Tibetan Plateau:Evidence from magnesium and calcium isotopes.Journal of Geophysical ResearchSolid Earth,122(12):9729-9744
Liu S,Hu RZ,Gao S,Feng CX,Huang ZL,Lai SC,Yuan HL,Liu XM,Coulson IM,Feng GY,Wang T and Qi YQ.2009.U-Pb zircon,geochemical and Sr-Nd-Hf isotopic constraints on the age and origin of Early Palaeozoic I-type granite from the Tengchong-Baoshan Block,western Yunnan Province,SW China.Journal of Asian Earth Sciences,36(2-3):168-182
Liu YS,Zong KQ,Kelemen PB and Gao S.2008.Geochemistry and magmatic history of eclogites and ultramafic rocks from the Chinese Continental Scientific Drill Hole:Subduction and ultrahigh-pressure metamorphism of lower crustal cumulates.Chemical Geology,247(1-2):133-153
Luo ZH,Liu JQ,Zhao CP,Guo ZF,Cheng LL,Li XH and Li DP.2011.Deep fluids and magmatism:The deep processes beneath the Tengchong volcano group.Acta Petrologica Sinica,27(10):2855-2862(in Chinese with English abstract)
Marschall HR and Schumacher JC.2012.Arc magmas sourced from mélange diapirs in subduction zones.Nature Geoscience,5(12):862-867
Mo XX,Zhao ZD,Deng JF,Flower M,Yu XH,Luo ZH,Li YH,Zhou S,Dong GC,Zhu DC and Wang LL.2006.Petrology and geochemistry of postcollisional volcanic rocks from the Tibetan Plateau:Implications for lithosphere heterogeneity and collisioninduced asthenosphere mantle flow.Geological Society of America Special Paper,409:507-530
Mo XX,Hou ZQ,Niu YL,Dong GC,Qu XM,Zhao ZD and Yang ZM.2007.Mantle contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet.Lithos,96(1-2):225-242
Niu ZJ,Liu Y and Di YJ.2014.Zoning characteristics of the plagioclase from the Mesozoic trachyandesite in Wuchagou area of the Da Hinggan Mountains and its geological implications.Acta Petrologica et Mineralogica,33(1):102-108(in Chinese with English abstract)
Pearce JA and Parkinson IJ.1993.Trace element models for mantle melting:Application to volcanic arc petrogenesis.In:Prichard HM,Alabaster T,Harris NBW and Neary CR(eds.).Magmatic Processes and Plate Tectonics.Geological Society,London,Special Publications,76(1):373-403
Plank T and Langmuir CH.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle.Chemical Geology,145(3-4):325-394
Powell CM and Johnson BD.1980.Contraints on the Cenozoic position of Sundaland.Tectonophysics,63(1-4):91-109
Qin JZ,Huangfu G,Li Q,Qian XD,Su YJ and Cai MJ.2000.3-Dchromatography of velocity structure in Tengchong volcano areas and nearby.Journal of Seismological Research,23(2):157-164(in Chinese with English abstract)
Rehkmper M and Hofmann AW.1997.Recycled ocean crust and sediment in Indian Ocean MORB.Earth and Planetary Science Letters,147(1-4):93-106
Rowley DB.1996.Age of initiation of collision between India and Asia:A review of stratigraphic data.Earth and Planetary Science Letters,145(1-4):1-13
Sato H.1977.Nickel content of basaltic magmas:Identification of primary magmas and a measure of the degree of olivine fractionation.Lithos,10(2):113-120
Saunders AD,Storey M,Kent RW and Norry MJ.1992.Consequences of plume-lithosphere interactions.In:Storey BC,Alabasater T and Pankhurst RJ(eds.).Magmatism and the Causes of Continental Break-up.Geological Society,London,Special Publications,68:41-60
Sheppard S and Taylor WR.1992.Barium-and LREE-rich,olivinemica-lamprophyres with affinities to lamproites,Mt.Bundey,Northern Territory,Australia.Lithos,28(3-6):303-325
Smith RK and Lofgren GF.1983.An analytical and experimental study of zoning in plagioclase.Lithos,16(2):153-168
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313-345
Takagi D,Sato H and Nakagawa M.2005.Experimental study of a lowalkali tholeiite at 1~5kbar:Optimal condition for the crystallization of high-An plagioclase in hydrous arc tholeiite.Contributions to Mineralogy and Petrology,149(5):527-540
Thompson RN and Gibson SA.2000.Transient high temperatures in mantle plume heads inferred from magnesian olivines in Phanerozoic picrites.Nature,407(6803):502-506
Tian HC,Yang W,Li SG,Ke S and Duan XZ.2018.Lowδ26Mg volcanic rocks of Tengchong in southwestern China:A deep carbon cycle induced by supercritical liquids.Geochimica et Cosmochimica Acta,240:191-219
Ustunisik G,Kilinc A and Nielsen RL.2014.New insights into the processes controlling compositional zoning in plagioclase.Lithos,200-201:80-93
Vroon PZ,Van Bergen MJ,White WM and Varekamp JC.1993.Sr-NdPb isotope systematics of the Banda Arc,Indonesia:Combined subduction and assimilation of continental material.Journal of Geophysical Research,98(B12):22349-22366
Wang JH,Yin A,Harrison TM,Grove M,Zhang YQ and Xie GH.2001.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision Zone.Earth and Planetary Science Letters,188(1-2):123-133
Wang Q,Wyman DA,Xu JF,Dong YH,Vasconcelos PM,Pearson N,Wan YS,Dong H,Li CF,Yu YS,Zhu TX,Feng XT,Zhang QY,Zi F and Chu ZY.2008.Eocene melting of subducting continental crust and early uplifting of central Tibet:Evidence from centralwestern Qiangtang high-K calc-alkaline andesites,dacites and rhyolites.Earth and Planetary Science Letters,272(1-2):158-171
Workman RK and Hart SR.2005.Major and trace element composition of the depleted MORB mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72
Wu TF,Zhang SX,Li MK,Qin WB and Zhang CY.2016.Two crustal flowing channels and volcanic magma migration underneath the SEmargin of the Tibetan Plateau as revealed by surface wave tomography.Journal of Asian Earth Sciences,132:25-29
Xu CL,Zhao GT,He YY and Li DP.2012.Geochemistry of Cenozoic volcanic rocks from Tengchong,western Yunnan.Marine Geology and Quaternary Geology,32(2):65-75(in Chinese)
Xu Y,Li XL and Wang S.2017.Crustal thickness and Poisson’s ratio of the Tengchong volcanic area in southweatern China.Chinese Journal of Geophysics,60(6):2256-2264(in Chinese with English abstract)
Yan DP,Zhou MF,Wang CY and Xia B.2006.Structural and geochronological constraints on the tectonic evolution of the DulongSong Chay tectonic dome in Yunnan Province,SW China.Journal of Asian Earth Sciences,28(4-6):332-353
Yang F,Huang XL and Li J.2018.Magma processes and petrogenesis of the Late Cretaceous plagioclase-phyric basalt in the Changchengling area,South China.Acta Petrologica Sinica,34(1):157-171(in Chinese with English abstract)
Yu HM.2011.Microstructural study on volcanic products and its geological implications.Ph.D.Dissertation.Beijing:Institute of Geology,China Earthquake Administration(in Chinese with English summary)
Yu HM,Xu JD,Lin CY,Shi LB and Chen XD.2012.Magmatic processes inferred from chemical composition,texture and crystal size distribution of the Heikongshan lavas in the Tengchong volcanic field,SW China.Journal of Asian Earth Sciences,58:1-15
Zhang B,Zhang JJ and Zhong DL.2010.Structure,kinematics and ages of transpression during strain-partitioning in the Chongshan shear zone,western Yunnan,China.Journal of Structural Geology,32(4):445-463
Zhao CP,Ran H and Chen KH.2006.Present-day magma chambers in Tengchong volcano area inferred from relative geothermal gradient.Acta Petrologica Sinica,22(6):1517-1528(in Chinese with English abstract)
Zhao DP and Liu L.2010.Deep structure and origin of active volcanoes in China.Geoscience Frontiers,1(1):31-44
Zhao ZD,Mo XX,Dilek Y,Niu YL,De Paolo DJ,Robinson P,Zhu DC,Sun CG,Dong GC,Zhou S,Luo ZH and Hou ZQ.2009.Geochemical and Sr-Nd-Pb-O isotopic compositions of the postcollisional ultrapotassic magmatism in SW Tibet:Petrogenesis and implications for India intra-continental subduction beneath southern Tibet.Lithos,113(1-2):190-212
Zhou MF,Robinson PT,Wang CY,Zhao JH,Yan DP,Gao JF and Malpas J.2012.Heterogeneous mantle source and magma differentiation of Quaternary arc-like volcanic rocks from Tengchong,SE margin of the Tibetan Plateau.Contributions to Mineralogy and Petrology,163(5):841-860
Zhu BQ,Mao CX,Lugmair GW and Macdougall JD.1983.Isotopic and geochemical evidence for the origin of Plio-Pleistocene volcanic rocks near the Indo-Eurasian collisional margin at Tengchong,China.Earth and Planetary Science Letters,65(2):263-275
Zou HB,Fan QC,Schmitt AK and Sui JL.2010.U-Th dating of zircons from Holocene potassic andesites(Maanshan volcano,Tengchong,SE Tibetan Plateau)by depth profiling:Time scales and nature of magma storage.Lithos,118(1-2):202-210
Zou HB,Shen CC,Fan QC and Lin K.2014.U-series disequilibrium in young Tengchong volcanics:Recycling of mature clay sediments or mudstones into the SE Tibet mantle.Lithos,192-195:132-141
Zou HB,Ma MJ,Fan QC,Xu B,Li SQ,Zhao YW and King DT Jr.2017.Genesis and open-system evolution of Quaternary magmas beneath southeastern margin of Tibet:Constraints from Sr-Nd-Pb-Hf
isotope systematics.Lithos,272-273:278-290
姜朝松.1998.腾冲新生代火山分布特征.地震研究,21(4):309-319
雷杭山,马倩,刘泽,赵志丹,朱弟成,莫宣学.2017.土耳其中部阿哲格尔火山湖新生代玄武岩的地球化学与岩石成因.岩石学报,33(8):2619-2632
李大明,李齐,陈文寄.2000.腾冲火山区上新世以来的火山活动.岩石学报,16(3):362-370
李欣,刘嘉麒.2012.云南腾冲全新世火山岩地球化学特征及其成因.岩石学报,28(5):1507-1516
林木森,彭松柏,乔卫涛.2017.滇西腾冲更新世粗面安山岩Ar-Ar年代学、地球化学特征及其构造意义.岩石学报,33(10):3137-3146
罗照华,刘嘉琦,赵慈平,郭正府,程黎鹿,李晓惠,李大鹏.2011.深部流体与岩浆活动:兼论腾冲火山群的深部过程.岩石学报,27(10):2855-2862
牛之建,刘跃,狄永军.2014.大兴安岭五岔沟地区中生代粗安岩中斜长石环带特征及其地质意义.岩石矿物学杂志,33(1):102-108
秦嘉政,皇甫岗,李强,钱晓东,苏有锦,蔡明军.2000.腾冲火山及邻区速度结构的三维层析成象.地震研究,23(2):157-164
徐翠玲,赵广涛,何雨旸,李德平.2012.滇西腾冲新生代火山岩岩石地球化学特征.海洋地质与第四纪地质,32(2):65-75
胥颐,李雪垒,汪晟.2017.腾冲火山区的地壳厚度和平均泊松比研究.地球物理学报,60(6):2256-2264
杨帆,黄小龙,李洁.2018.华南长城岭晚白垩世斜斑玄武岩的岩浆作用过程与岩石成因制约.岩石学报,34(1):157-171
于红梅.2011.火山喷发物的显微构造研究及其地质意义.博士学位论文.北京:中国地震局地质研究所
赵慈平,冉华,陈坤华.2006.由相对地热梯度推断的腾冲火山区现存岩浆囊.岩石学报,22(6):1517-1528
(1)云南省地质局区域地质调查队.1982.1︰20万腾冲幅(G-47-XXV11)区域地质图
© 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 |