我国火山地热流体地球化学研究新进展
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摘要
本文综述了最近几年来中国研究者在地热流体地球化学研究领域取得的主要进展。在国际上关于地球内部流体及其作用研究取得重要进展的大背景下,我国学者在地热流体地球化学研究上也取得了一些重要成果,主要表现在火山地热区和非火山地热区两大方面,在火山学、地热学、环境学、大地构造学、地震学等五个学科领域都取得了一些重要进展。
This paper reviews the main advances obtained by Chinese researchers at geochemistry of hydrothermal fluids in recent years.As very important progresses are making internationally in the studies of the earth's interior fluids and its role,Chinese scholars also obtain some important results in the geothermal fluid geochemistry,specifically in two major fields of volcanic and non-volcanic geothermal areas,and in five disciplines,such as volcanology,geothermics,environmental science,tectonics and seismology.
This paper reviews the main advances obtained by Chinese researchers at geochemistry of hydrothermal fluids in recent years.As very important progresses are making internationally in the studies of the earth's interior fluids and its role,Chinese scholars also obtain some important results in the geothermal fluid geochemistry,specifically in two major fields of volcanic and non-volcanic geothermal areas,and in five disciplines,such as volcanology,geothermics,environmental science,tectonics and seismology.
引文
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[5]Ohtani E,Litasov K,Hosoya T,Kubo T,Kondo T.Watertransport into the deep mantle and formation of a hydroustransition zone[J].Phys.Earth Planet.Inter.,2004,143:255-269.
[6]Kawakatsu H,Watada S.Seismic evidence for deep-watertransportation in the mantle[J].Science,2007,316:1468-1471.
[7]Kelbert A,Schultz A,Egbert G.Global electromagnetic in-duction constraints on transition-zone water content variations[EB/OL].2009,460,doi:10.1038/nature08257.
[8]Williams Q,Hemley R J.Hydrogen in the deep Earth[J].Ann.Rev.Earth Planet.Sci.,2001,29:365-418.
[9]Bercovici D,Karato S.Whole-mantle convection and the tran-sition-zone water filter[J].Nature,2003,425:39-44.
[10]Terabayashi M,Okamoto K,Yamamoto H,Chan Y C.The-matic section:Fluid-rock interaction in the bottom of the in-land seismogenic zone-preface[J].Island Arc,2010,19:1-3.
[11]Zhao D,Kanamori H,Hegishi H.Tomography of source ar-ea of the 1995Kobe earthquake:Evidence for fluids at thehypocenter[J].Science,1996,274:1891-1894.
[12]Zhao D P,Santosh M,Yamada A.Dissecting large earth-quakes in Japan:Role of arc magma and fluids[J].IslandArc,2010,19:4-16.
[13]Zhao D P,Pirajno F,Dobretsov N L,Liu L.Mantle struc-ture and dynamics under East Russia and adjacent regions[J].Russian Geology and Geophysics,2010,51:925-938.
[14]Zhao D P,Yu S,Ohtani E.East Asia:Seismotectonics,magmatism and mantle dynamics[J].Journal of Asian EarthSciences,2010,doi:10.1016/j.jseaes.2010.11.013.
[15]Trieloff M,Kunz J.Isotope systematics of noble gases in theEarth’s mantle:Possible sources of primordial isotopes andimplications for mantle structure[J].Physics of the Earthand Planetary Interiors,2005,148:13-38.
[16]Graham D W.Noble gas isotope geochemistry of mid-oceanridge and ocean island basalts:Characterization of mantlesource reservoirs[A].Porcelli D,Ballentine C J,Wieler R.Noble gases in geochemistry and cosmochemistry,reviews inmineralogy and geochemistry[M].Mineralogical Society ofAmerica,Washington,D.C.August 2002:247-318.
[17]Farley K A,Neroda E.Noble gases in the earth’s mantle[J].Ann.Rev.Earth Planet.Sci.,1998,26:189-218.
[18]Van Soest M C,Hilton D R,Kreulen R.Tracing crustal andslab contributions to arc magmatism in the Lesser Antilles is-land arc using helium and carbon relationships in geothermalfluids[J].Geochim.Cosmochim.Acta,1998,62:3323-3335.
[19]Ozima M.Noble gas state in the mantle[J].Reviews of Geo-physics,1994,32:405-426.
[20]Hilton D R,Hammerschmidt K,Teufel S,Friedrichsen H.Helium isotope characteristics of Andean geothermal fluidsand lavas[J].Earth Planet.Sci.Lett.,1993,120:265-282.
[21]Lupton J E.Terrestrial inert-gases-isotope tracer studies andclues to primordial components in the mantle[J].Annual Re-view of Earth and Planetary Sciences,1983,11:371-414.
[22]Shaw A M,Hauri E H,Fischer T P,Hilton D R,Kelley KA.Hydrogen isotopes in Mariana arc melt inclusions:Impli-cations for subduction dehydration and the deep-Earth watercycle[J].Earth Planet.Sci.Lett.,2008,275:138-145.
[23]陈辉.氢在地球演化过程中的同位素分馏[J].地质科学,1996,31(3):238-247.Chen Hui.Hydrogen isotope fractionation in evolution of theEarth[J].Scientia Geologica Sinica,1996,31(3):238-247.(in Chinese with English abstract)
[24]Horiguchi K,Ueki S,Sano Y,Takahata N,Hasegawa A,Igarashi G.Geographical distribution of helium isotope ratiosin northeastern Japan[J].Island Arc,2010,19:60-70.
[25]赵慈平,冉华,陈坤华.由相对地热梯度推断的腾冲火山区现存岩浆囊[J].岩石学报,2006,22(6):1517-1528.Zhao Ciping,Ran Hua,Chen Kunhua.Present-day magmachambers in Tengchong volcano area inferred from relativegeothermal gradient[J].Acta Petrologica Sinica,2006,22(6):1517-1528.(in Chinese with English abstract)
[26]Zhang G P,Liu C Q,Liu H,Jin Z S,Han G L,Li L.Geo-chemistry of the Rehai and Ruidian geothermal waters,Yun-nan Province,China[J].Geothermics,2008,37(1):73-83.
[27]刘虹,张国平,金志升,刘丛强,韩贵琳,李玲.云南腾冲地区地热流体的地球化学特征[J].矿物学报,2009,29(4):496-501.Liu Hong,Zhang Guoping,Jin Zhisheng,Liu Congqiang,Han Guilin,Li Ling.Geochemical characteristics of geother-mal fluid in Tengchong Area,Yunnan Province,China[J].Acta Mineralogica Sinica,2009,29(4):496-501.(in Chi-nese with English abstract)
[28]邓紫娟.云南省腾冲火山区热海地热田水化学和同位素特征[D].北京:中国地质大学(北京),2009.Deng Zijuan.Chemical and isotopic characteristics of Rehaigeothermal field in Tengchong,Yunnan[D].Beijing:ChinaUniversity of Geosciences(Beijing),2009.(in Chinese withEnglish abstract)
[29]Du J G,Liu C Q,Fu B H,Ninomiya Y,Zhang Y L,WangC Y,Wang H L,Sun Z G.Variations of geothermometryand chemical-isotopic compositions of hot spring fluids in theRehai geothermal field,southwestern China[J].Journal ofVolcanology and Geothermal Research,2005,142(3-4):243-261.
[30]Shangguan Z G,Zhao C P,Li H Z,Gao Q W,Sun M L.E-volution of hydrothermal explosions at Rehai geothermalfield,Tengchong volcanic region,China[J].Geothermics,2005,34(4):518-526.
[31]Zhao C P,Shangguan Z G,Chen K H,Xu S.Conceptualmodel of hydrothermal explosion in Rehai Geothermal Field,Tengchong volcanic-geothermal area,southwest China[J].Earthquake Research,2004,27(S2):101-112.
[32]上官志冠,武成智.中国休眠火山区岩浆来源气体地球化学特征[J].岩石学报,2008,24(11):2638-2646.Shangguan Zhiguan,Wu Chengzhi.Geochemical features ofmagmatic gases in the regions of dormant volcanoes in China[J].Acta Petrologica Sinica,2008,24(11):2638-2646.(in Chinese with English abstract)
[33]赵慈平.腾冲火山区现代幔源氦释放特征及深部岩浆活动研究[D].北京:中地震局地质研究所,2008.Zhao Ciping.Mantle-derived Helium release characteristicsand deep magma charmber activities of present day in theTengchong volcanic area[D].Beijing:Institute of Geology,China Earthquake Adiministration,2008:1-125.(in Chi-nese with English abstract)
[34]上官志冠,赵慈平,高玲.中国活动火山区甲烷的碳同位素研究[J].岩石学报,2006,22(6):1458-1464.Shangguan Zhiguan,Zhao Ciping,Gao Lin.Carbon isotopiccompositions of the methane derived from magma at the ac-tive volcanic regions in China[J].Acta Petrologica Sinica,2006,22(6):1458-1464.(in Chinese with English ab-stract)
[35]赵珂.云南深大断裂CO2释放规律研究[D].重庆:西南师范大学,2005.Zhao Ke.The sudy of CO2degassed from deep faults in Yun-nan[D].Chongqing:Southwestern China Normal Universi-ty,2005.(in Chinese with English abstract)
[36]赵珂,姜光辉,杨琰,刘德深,刘玉,王丽丽.滇东主要断裂带温泉CO2成因浅析[J].地球与环境,2005,33(2):11-15.Zhao Ke,Jiang Guanghui,Yang Yan,Liu Deishen,Liu Yu,Wang Lili.Brief analysis of the reasons of CO2degassingfrom hot springs on main faults within the east of Yunnan[J].Earth and Environment,2005,33(2):11-15.(in Chi-nese with English abstract)
[37]沈立成,袁道先,丁悌平,李延河,乐国良,林玉石.中国西南地区CO2释放点的He同位素分布不均一性及大地构造成因[J].地质学报,2007,81(4):465-478.Shen Licheng,Yuan Daoxian,Ding Tiping,Li Yanhe,LeGuoliang,Lin Yushi.Distributing inhomogeneity of helium i-sotope of CO2degasification point and its geotectogenesis insouthwest China[J].Acta Geologica Sinica,2007,81(4):465-478.(in Chinese with English abstract)
[38]侯增谦,李振清.印度大陆俯冲前缘的可能位置:来自藏南和藏东活动热泉气体He同位素约束[J].地质学报,2004,78(4):482-493.Hou Zengqian,Li Zhenqing.Possible location for under-thrusting front of the Indus continent:Constraints from heli-um isotope of the geothermal gas in southern Tibet and east-ern Tibet[J].Acta Geologica Sinica,2004,78(4):482-493.(in Chinese with English abstract)
[39]李振清,侯增谦,聂凤军,孟祥金.藏南上地壳低速高导层的性质与分布:来自热水流体活动的证据[J].地质学报,2005,79(1):68-77.Li Zhenqing,Hou Zengqian,Nie Fengjun,Meng Xiangjin.Characteristic and distribution of the partial melting layers inthe upper crust:Evidence from active hydrothermal fluid inthe south Tibet[J].Acta Geologica Sinica,2005,79(1):68-77.(in Chinese with English abstract)
[40]Du J G,Cheng W Z,Zhang Y L,Jie C L,Guan Z J,Liu W,Bai L P.Helium and carbon isotopic compositions of thermalsprings in the earthquake zone of Sichuan,southwestern Chi-na[J].Journal of Asian Earth Sciences,2006,26(5):533-539.
[2]Molchanov O A,Uyeda S.Upward migration of earthquakehypocenters in Japan,Kurile-Kamchatka and Sunda subduc-tion zones[J].Physics and Chemistry of the Earth,2009,34(6-7):423-430.
[3]Lallemand S,Funiciello F.Subduction zone geodynamics[A].Frontiers in Earth Sciences[M].Heidelberg:Berlin,Springer-Verlag:ISBN 978-3-540-87971-8,DOI:10.1007/978-3-540-87974-9.
[4]Maruyama S,Okamoto K.Water transportation from the sub-ducting slab into the mantle transition zone[J].Gondwana Re-search,2007,11:148-165.
[5]Ohtani E,Litasov K,Hosoya T,Kubo T,Kondo T.Watertransport into the deep mantle and formation of a hydroustransition zone[J].Phys.Earth Planet.Inter.,2004,143:255-269.
[6]Kawakatsu H,Watada S.Seismic evidence for deep-watertransportation in the mantle[J].Science,2007,316:1468-1471.
[7]Kelbert A,Schultz A,Egbert G.Global electromagnetic in-duction constraints on transition-zone water content variations[EB/OL].2009,460,doi:10.1038/nature08257.
[8]Williams Q,Hemley R J.Hydrogen in the deep Earth[J].Ann.Rev.Earth Planet.Sci.,2001,29:365-418.
[9]Bercovici D,Karato S.Whole-mantle convection and the tran-sition-zone water filter[J].Nature,2003,425:39-44.
[10]Terabayashi M,Okamoto K,Yamamoto H,Chan Y C.The-matic section:Fluid-rock interaction in the bottom of the in-land seismogenic zone-preface[J].Island Arc,2010,19:1-3.
[11]Zhao D,Kanamori H,Hegishi H.Tomography of source ar-ea of the 1995Kobe earthquake:Evidence for fluids at thehypocenter[J].Science,1996,274:1891-1894.
[12]Zhao D P,Santosh M,Yamada A.Dissecting large earth-quakes in Japan:Role of arc magma and fluids[J].IslandArc,2010,19:4-16.
[13]Zhao D P,Pirajno F,Dobretsov N L,Liu L.Mantle struc-ture and dynamics under East Russia and adjacent regions[J].Russian Geology and Geophysics,2010,51:925-938.
[14]Zhao D P,Yu S,Ohtani E.East Asia:Seismotectonics,magmatism and mantle dynamics[J].Journal of Asian EarthSciences,2010,doi:10.1016/j.jseaes.2010.11.013.
[15]Trieloff M,Kunz J.Isotope systematics of noble gases in theEarth’s mantle:Possible sources of primordial isotopes andimplications for mantle structure[J].Physics of the Earthand Planetary Interiors,2005,148:13-38.
[16]Graham D W.Noble gas isotope geochemistry of mid-oceanridge and ocean island basalts:Characterization of mantlesource reservoirs[A].Porcelli D,Ballentine C J,Wieler R.Noble gases in geochemistry and cosmochemistry,reviews inmineralogy and geochemistry[M].Mineralogical Society ofAmerica,Washington,D.C.August 2002:247-318.
[17]Farley K A,Neroda E.Noble gases in the earth’s mantle[J].Ann.Rev.Earth Planet.Sci.,1998,26:189-218.
[18]Van Soest M C,Hilton D R,Kreulen R.Tracing crustal andslab contributions to arc magmatism in the Lesser Antilles is-land arc using helium and carbon relationships in geothermalfluids[J].Geochim.Cosmochim.Acta,1998,62:3323-3335.
[19]Ozima M.Noble gas state in the mantle[J].Reviews of Geo-physics,1994,32:405-426.
[20]Hilton D R,Hammerschmidt K,Teufel S,Friedrichsen H.Helium isotope characteristics of Andean geothermal fluidsand lavas[J].Earth Planet.Sci.Lett.,1993,120:265-282.
[21]Lupton J E.Terrestrial inert-gases-isotope tracer studies andclues to primordial components in the mantle[J].Annual Re-view of Earth and Planetary Sciences,1983,11:371-414.
[22]Shaw A M,Hauri E H,Fischer T P,Hilton D R,Kelley KA.Hydrogen isotopes in Mariana arc melt inclusions:Impli-cations for subduction dehydration and the deep-Earth watercycle[J].Earth Planet.Sci.Lett.,2008,275:138-145.
[23]陈辉.氢在地球演化过程中的同位素分馏[J].地质科学,1996,31(3):238-247.Chen Hui.Hydrogen isotope fractionation in evolution of theEarth[J].Scientia Geologica Sinica,1996,31(3):238-247.(in Chinese with English abstract)
[24]Horiguchi K,Ueki S,Sano Y,Takahata N,Hasegawa A,Igarashi G.Geographical distribution of helium isotope ratiosin northeastern Japan[J].Island Arc,2010,19:60-70.
[25]赵慈平,冉华,陈坤华.由相对地热梯度推断的腾冲火山区现存岩浆囊[J].岩石学报,2006,22(6):1517-1528.Zhao Ciping,Ran Hua,Chen Kunhua.Present-day magmachambers in Tengchong volcano area inferred from relativegeothermal gradient[J].Acta Petrologica Sinica,2006,22(6):1517-1528.(in Chinese with English abstract)
[26]Zhang G P,Liu C Q,Liu H,Jin Z S,Han G L,Li L.Geo-chemistry of the Rehai and Ruidian geothermal waters,Yun-nan Province,China[J].Geothermics,2008,37(1):73-83.
[27]刘虹,张国平,金志升,刘丛强,韩贵琳,李玲.云南腾冲地区地热流体的地球化学特征[J].矿物学报,2009,29(4):496-501.Liu Hong,Zhang Guoping,Jin Zhisheng,Liu Congqiang,Han Guilin,Li Ling.Geochemical characteristics of geother-mal fluid in Tengchong Area,Yunnan Province,China[J].Acta Mineralogica Sinica,2009,29(4):496-501.(in Chi-nese with English abstract)
[28]邓紫娟.云南省腾冲火山区热海地热田水化学和同位素特征[D].北京:中国地质大学(北京),2009.Deng Zijuan.Chemical and isotopic characteristics of Rehaigeothermal field in Tengchong,Yunnan[D].Beijing:ChinaUniversity of Geosciences(Beijing),2009.(in Chinese withEnglish abstract)
[29]Du J G,Liu C Q,Fu B H,Ninomiya Y,Zhang Y L,WangC Y,Wang H L,Sun Z G.Variations of geothermometryand chemical-isotopic compositions of hot spring fluids in theRehai geothermal field,southwestern China[J].Journal ofVolcanology and Geothermal Research,2005,142(3-4):243-261.
[30]Shangguan Z G,Zhao C P,Li H Z,Gao Q W,Sun M L.E-volution of hydrothermal explosions at Rehai geothermalfield,Tengchong volcanic region,China[J].Geothermics,2005,34(4):518-526.
[31]Zhao C P,Shangguan Z G,Chen K H,Xu S.Conceptualmodel of hydrothermal explosion in Rehai Geothermal Field,Tengchong volcanic-geothermal area,southwest China[J].Earthquake Research,2004,27(S2):101-112.
[32]上官志冠,武成智.中国休眠火山区岩浆来源气体地球化学特征[J].岩石学报,2008,24(11):2638-2646.Shangguan Zhiguan,Wu Chengzhi.Geochemical features ofmagmatic gases in the regions of dormant volcanoes in China[J].Acta Petrologica Sinica,2008,24(11):2638-2646.(in Chinese with English abstract)
[33]赵慈平.腾冲火山区现代幔源氦释放特征及深部岩浆活动研究[D].北京:中地震局地质研究所,2008.Zhao Ciping.Mantle-derived Helium release characteristicsand deep magma charmber activities of present day in theTengchong volcanic area[D].Beijing:Institute of Geology,China Earthquake Adiministration,2008:1-125.(in Chi-nese with English abstract)
[34]上官志冠,赵慈平,高玲.中国活动火山区甲烷的碳同位素研究[J].岩石学报,2006,22(6):1458-1464.Shangguan Zhiguan,Zhao Ciping,Gao Lin.Carbon isotopiccompositions of the methane derived from magma at the ac-tive volcanic regions in China[J].Acta Petrologica Sinica,2006,22(6):1458-1464.(in Chinese with English ab-stract)
[35]赵珂.云南深大断裂CO2释放规律研究[D].重庆:西南师范大学,2005.Zhao Ke.The sudy of CO2degassed from deep faults in Yun-nan[D].Chongqing:Southwestern China Normal Universi-ty,2005.(in Chinese with English abstract)
[36]赵珂,姜光辉,杨琰,刘德深,刘玉,王丽丽.滇东主要断裂带温泉CO2成因浅析[J].地球与环境,2005,33(2):11-15.Zhao Ke,Jiang Guanghui,Yang Yan,Liu Deishen,Liu Yu,Wang Lili.Brief analysis of the reasons of CO2degassingfrom hot springs on main faults within the east of Yunnan[J].Earth and Environment,2005,33(2):11-15.(in Chi-nese with English abstract)
[37]沈立成,袁道先,丁悌平,李延河,乐国良,林玉石.中国西南地区CO2释放点的He同位素分布不均一性及大地构造成因[J].地质学报,2007,81(4):465-478.Shen Licheng,Yuan Daoxian,Ding Tiping,Li Yanhe,LeGuoliang,Lin Yushi.Distributing inhomogeneity of helium i-sotope of CO2degasification point and its geotectogenesis insouthwest China[J].Acta Geologica Sinica,2007,81(4):465-478.(in Chinese with English abstract)
[38]侯增谦,李振清.印度大陆俯冲前缘的可能位置:来自藏南和藏东活动热泉气体He同位素约束[J].地质学报,2004,78(4):482-493.Hou Zengqian,Li Zhenqing.Possible location for under-thrusting front of the Indus continent:Constraints from heli-um isotope of the geothermal gas in southern Tibet and east-ern Tibet[J].Acta Geologica Sinica,2004,78(4):482-493.(in Chinese with English abstract)
[39]李振清,侯增谦,聂凤军,孟祥金.藏南上地壳低速高导层的性质与分布:来自热水流体活动的证据[J].地质学报,2005,79(1):68-77.Li Zhenqing,Hou Zengqian,Nie Fengjun,Meng Xiangjin.Characteristic and distribution of the partial melting layers inthe upper crust:Evidence from active hydrothermal fluid inthe south Tibet[J].Acta Geologica Sinica,2005,79(1):68-77.(in Chinese with English abstract)
[40]Du J G,Cheng W Z,Zhang Y L,Jie C L,Guan Z J,Liu W,Bai L P.Helium and carbon isotopic compositions of thermalsprings in the earthquake zone of Sichuan,southwestern Chi-na[J].Journal of Asian Earth Sciences,2006,26(5):533-539.
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