Geochemistry of Cambrian High-Mg Andesites in North Qilian and Its Geodynamic Implications
-
摘要: 北祁连扎柯山高镁安山岩铷锶同位素年龄为早—中寒武世[(516±7)Ma(1σ)],高镁安山岩类(SiO2=51.45%~59.62%,平均为56.33%),具有比典型岛弧安山岩更高的MgO(4.85%~9.64%,平均为6.2%,Mg#=66.68~74.15,平均为71.44),高Cr(21.6×10-6~476×10-6,平均为196.26×10-6)、高Ni(14×10-6~102×10-6,平均为56.14×10-6),低Al贫Ca(Al2O3=13.22%~17.37%,均值为15.69%,CaO=2.01%~10.33%,均值为5.64%),富Na、贫K(Na2O=1.57%~5.2%,K2O=1.04%~2.79%,Na2O/K2O=0.59~5.0,均值为2.36),弱负Eu异常以及富集Rb、Th、K大离子不相容元素(LILE),亏损Sr、Ti、P、Nb、Ta等高场强元素(HFSE),富集LREE,强烈亏损HREE,LREE/HREE=7.19~13.58,Yb=1.47×10-6~3.26×10-6,Y=11.6×10-6~22.5×10-6,含有较低的Sr(119×10-6~278×10-6,平均为193×10-6)。综合区域地质背景等资料研究表明,扎柯山寒武纪高镁安山岩可能是蚀变洋壳和俯冲的沉积物熔融进入地幔楔诱发橄榄岩部分熔融的产物,形成于岛弧环境。Abstract: High-Mg andesites are occurred in Zakeshan area,North Qilian, which were formed in Early and Middle Cambrian, with Rb-Sr isotopic age of (516±7)Ma (1σ).These andesites (SiO2=51.45%~59.62%,averaging in 56.33%)have higher MgO contents (MgO contents are 4.85%~9.64%, averaging in 71.44%, Mg# values are 66.68~74.15, averaging in 71.44)than the ones of typical island arc andesite, with enrichment of Cr (21.6×10-6~476×10-6, averaging in 196.26×10-6), Ni (14×10-6~102×10-6, averaging in 56.14×10-6)and Na elements, but low Al (Al2O3=13.22%~17.37%, averaging in 15.69%), Ca (CaO=2.01%~10.33%, averaging in 5.64%)and K (K2O=1.04%~2.79%, Na2O/K2O=0.59~5.0, averaging in 2.36).Meanwhile, these rocks show weakly negative Eu anomaly, they are enriched in Rb, Th and K (LILE), but they are depleted in Sr, Ti, P, Nb and Ta (HFSE), with LREE/HREE ratios ranging from 7.19 to 13.58 (Yb=1.47×10-6~3.26×10-6, Y=11.6×10-6~22.5×10-6). Combined with regional geological setting, the results suggest that high-Mg andesite was formed in island arc setting and was sourced from the partial melting of the peridotites in mantle wedge, which were metasomated by the fluids from subducted sediments and altered oceanic crust.
-
Keywords:
- high-Mg andesite /
- Cambrian /
- geoehemistry /
- geodynamics /
- Zakeshan area /
- North Qilian
-
-
邓晋福,刘翠,冯艳芳,等.高镁安山岩/闪长岩(HMA)和镁安山岩/闪长岩类(Ma):与洋俯冲作用相关的两类典型的火成岩类[J].中国地质,2010,37(4):1112-1118. DENG Jinfu,LIU Cui,FENG Yanfang,et al.High magnesian andesitic/dioritic rocks(HMA)and magnesian andesitic/dioritic rocks(MA):two igneous rock types related to oceanic subduction[J].Geology in China,2010.,37(4):1112-1118.
冯备战,王晓伟,曾俊杰,等.北祁连西段古元古代大陆裂谷火山岩性质的确定[J].甘肃地质学报,2005,14(1):16-20. FENG Beizhan,WANG Xiaowei,ZENG Junjie,et al.Characteristics determination of paleoproterozoic era continental rift volcanic rock in the western section of north qilian[J].Acta Geologica Gansu,2005,14(1):16-20.
李承东,张福勤,苗来成,等.吉林色洛河晚二叠世高镁安山岩SHRIMP锆石年代学及其地球化学特征[J].岩石学报,2007,23(4):767-776. LI Chengdong ZHANG Fuqin,MIAO Laicheng,et al.Zircon SHRIMP geochronology and geochemistry of Late Permian high-Mg andesites in Seluohe area,Jilin province,China[J].Acta Petrologica Sinica,2007,23(4):767-776.
李兆,陈岳龙,刘长征,等.北祁连的形成与演化历史:来自河流沉积物地球化学及其碎屑锆石 U-Pb年龄、Hf同位素组成的证据[J].地质学报,2016,90(2):267-282. LI Zhao,CHEN Yuelong,LIU Changzhen et al.Formation and Evolution History on the Northern Qilian Orogen:the Evidences from Compositions of Rivers' Sediments and Their Zircon U-Pb Ages,Hf Isotopic Compositions[J].Acta Geologica Sinica,2016,90(2):267-282.
毛景文,张作衡,简平,等.北祁连西段花岗质岩体的锆石U-Pb年龄报道[J].地质论评,2000,46(6):616-620. MAO Jingwen,ZHANG Zuoheng,JIAN Ping,et al.U-Pb Zircon dating of the Yeniutan granitic intrusion in the western part of the North QiLian Mountains[J].Geological Review,2000,46(6):616-620.
孟繁聪,张建新,于胜尧,等.北阿尔金红柳泉早古生代枕状玄武岩及其大地构造意义[J].地质学报,2010, 84(7):981-990. MENG Fancong,ZHANG Jianxing,YU Shengyao,et al.The Early Paleozoic pillow basalt in Northern Altyn,Western China and its tectonic implications[J].Acta Geologica Sinica,2010,84(7):981-990.
唐功建,王强.高镁安山岩及其地球动力学意义[J].岩石学报,2010,26(8):2495-2512. TANG Gongjian,WANG Qiang.High-Mg andesites and their geodynamic implications[J]..Acta Petrologica Sinica,2010,26(8):2495-2512.
夏林圻,夏祖春,徐学义,等.北祁连山早古生代洋脊-洋岛和弧后盆地火山作用[J].地质学报,1998,72(4):301-312. XIA Liqi,XIA Zuchun,XU Xueyi.Early Palaeozoic mid-ocean ridge-ocean island and back-arc basin volcanism in the North Qilian Mountains[J].Acta Geologica Sinica,1998,72(4):301-312.
夏林折,夏祖春,徐学义.北祁连山构造-火山岩浆演化动力学[J].西北地质科学,1995,16(1):1-28. XIA Linqi,XIA Zuchun,XU Xueyi.Dynamics of tectono-volcano-magmatic evolution from North Qilian Mountains,China[J].Northwest Geoscience,1995,16(1):1-28.
肖序常,陈国铭,朱志直.连山古蛇绿岩带的地质构造意义[J].地质学报,1978,54(4):287-295. XIAO Xuchang,CHEN Guoming,ZHU Zhizhi.A preliminary study on the tectonlcs of ancient oPhiolites in the QiLian Mountain,Northwest China[J].Acta Geologica Sinica,1978,54(4):287-295.
张新虎,刘建宏,徐家乐,等.再论甘肃省的板块构造[J].甘肃地质,2005,14(2):1-10. ZHANG Xinhu,LIU Jianhong,XU Jiale,et al.Second study on plate tectonics in gansu province[J].Acta Geologica Gansu,2005,14(2):1-10.
张新虎,刘建宏,赵彦庆.甘肃省成矿区(带)研究[J].甘肃地质,2008,17(2):1-8. ZHANG Xinhu,LIU Jianhong,ZHAO Yanqing,et al.Study on metallogenic provinces(zones)in gansu province[J].Acta Geologica Gansu,2008, 17(2):1-8.
张招崇,毛景文,左国朝,等.北祁连山西段早元古代变质火山岩的地球化学特征及其构造背景[J].矿物岩石,1998,8(4):22-309. ZHANG Zhaochong,MAO Jingwen,ZUO Guochao,et al.Geochemistry of the proterozoic metamorphic volcanic rocks in the west part of north qilian mountains and their tectonic setting.Journal of mineralogy and petrology,1998,8(4):22-309.
左国朝,吴茂炳,毛景文,等.北祁连西段早古生代构造演化史[J].甘肃地质学报,1999,8(1):6-13. ZUO Guochao,WU Maobing,MAO Jingwen,et al.Structural evolution of early Paleozoic tectonic belt in the west section of northern qilian area[J].Actageologica gansu,1999,8(1):6-13.
BENOIT M,AGUILLON-Robles A,CALMUS T,et al.Geochemical diversity of Late Miocene volcanism in southern Baja California,Mexico:Implication of mantle and crustal sources during the opening of an asthenospheric window[J].Journal of Geology,2002,110(6):627-648.
CAMERON W E,MECULLOCH M T, WALKER D A..Boninite petrogenesis:Chemical and Nd-Sr isotopic constraints[J].EPSL,1983,60:78-89.
CAMERON W E,NISBET E G and DIETRICH V J.Boninites,komatiites and ophiolitic basalts[J].Nature,1979,280(5723):550-553.
CRAWFORD A J.Boninites[M].London:Unwin Hyman,1989.
FENG Yiming Geotectonics and orogeny of the QiLian Mountain,china[M].Beijing:Geological Publishing house,1996.
GAO S,Rudnick R L,YUAN H L,,et al.Recycling lowercontinental crust in the North China craton[J].Nature,2004,432(7019):892-897.
GILLJB.Orogenic Andesites and Plate Tectonics[M].New York,Berlin,Heidelberg:Springer-Verlag,1981.
GUIVELC,MORATA D,PELLETER E,,et al..Miocene to Late Quaternary Patagonian basalts (46~47°S):Geochronometric and eochemical evidence for slab tearing due to active spreading ridge subduction[J].Journal of Volcanology and Geothermal Research,2006,149(3-4):346-370.
KAMEIA, OWADA M, NAGAO T, et al..High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, southwest Japan arc:evidence from clinopyroxene and whole rock compositions[J].Lithosphere,2004,75:359-371.
KAWABATA H and SHUTO K..Magnla mixing reeodred in intermediate oreks assoeiated with high-Mg andesites from the Seotuehi voleanic belt,Japan:implications for AcrheanTTG frormation[J].Joumal of Voleanology and Geothermal Reseacrh,2005,140:241-271.
KAY R W.Aleutian magnesian andesites:Melts from subducted Pacific Ocean crust[J].Journal of Volcanology and Geothermal Research,1978,4(1-2):117-132.
KELEMENP B, HANGHOJ K, GREENE A R.One view of the geochemistry of subduction-related magmatic arcs, with an emphosis on primitive andesite and lower crust[J].Holland H D, Turekian KK.Treatise on Geochemistry.Amsterdam:Elsevier Press, 2003,3:593-660.
KELEMEN P B.Genesis of high Mg-number andesites and the continental-crust[J].Contributions to Mineralogy and Petrology,1995,120(1):1-19.
LEBas M J, IUGS reclassification of the High-Mg and picritic volcanic rocks[J].Journal of Peterology,2000,40(10):1467-1470.
PALLARES C,MAURY R C,BELLON H,et al..Slab-tearing following ridge-trench collision:Evidence from Miocene volcanism in Baja California,Mexico[J].Journal of Volcanology and Geothermal Research,2007,161(1-2):95-117.
TATSUMIY, HANYU T.Geochemical modeling of dehydration and partial melting of subducting lithosphere:Toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt, SW Japan[J].Geochemistry, Geophysics, Geosystems,2003,4(9):643-651.
TATSUMI Y,SUZUKI T,KAWABATA H,et al.The petrology and geochemistry of Oto-Zan Composite Iava flow on ShodoShima island,SW Japan:Remelting of a solidified high-Mg andesite magma[J].Journal of Petrology,2006,47(3):595-629.
TATSUMI Y.Melting experiments on a high-magnesium andesite[J].Earth and Planetary Science Letters,1981,54:357-365.
TATSUMI Y.Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt,southwest Japan[J].Geology,2001,29(4):323-326.
WOODB J,TURNER S P.Origin of primitive high-Mg andesite:Constraints from natural examples and experiments[J].Earth and Planetary Science Letters,2009,283:59-66.
XIA Liqi,XIA Zuchun,ZHAO Jiangtian,et al.Determination of properties of Proterozoic continental flood basalts of western part from North QiLian Mountains[J].Science in China(Series D),1999,42(5):506-514.
XIA Liqi.Tectonics-Volanic magmatism-mineralization dynamics on the North QiLian Mountains[M].Beijing:the Earth Publishing House of China,2001.
计量
- 文章访问数: 2429
- HTML全文浏览量: 0
- PDF下载量: 2396