肖龙;何琦;黄定华;缪秉魁;张振飞;杨瑞琰;张志;

• 1:中国地质大学空间科学技术研究中心
• 2:中国地质大学地球科学学院
• 3:中国地质大学空间科学技术研究中心
• 4:桂林工学院资源与环境工程系

摘要(Abstract)：

火山活动是太阳系内所有行星和多数卫星共同经历过的地质作用。类地行星及它们的卫星表面普遍分布着多种火山和火山岩。其中金星、火星和月球与地球上的早期(始太古代)火山活动有许多相似性。现在,火星与月球上的火山活动早已停止,而金星和地球上仍有火山活动。类木行星的卫星上主要活动的是"冰火山",它们之中有些还有十分强烈的活火山活动(如爱莪和海卫一)。对太阳系天体火山作用的对比研究能够提供认识太阳系和行星演化、天体深部和浅部地质作用过程、矿产资源形成以及生命的起源和演化等重要信息,是比较行星学的重要组成部分。

关键词(KeyWords)： 火山;太阳系;天体;比较行星学

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(40572031)

作者(Author): 肖龙;何琦;黄定华;缪秉魁;张振飞;杨瑞琰;张志;

Email:

DOI:

参考文献(References)：

• [1]Lopes R M C,Gregg T K P.Volcanic words:Exploringthe solar system's volcanoes[M].Spinger:Praxis Publishing,2004:1-236.
• [2]Cattermole P.Planetary volcanism:Astudy of volcanic ac-tivity in the soalr system[M].2ndedition.Chichester:Ellis Horwood Ltd.,1997.
• [3]刘嘉麒.中国火山[M].北京:科学出版社,1999:1-219.
• [4]Sigudsson H.Encyclopediaof volcanoes[M].San Diego:Ac-ademic Press,2000:1-500.
• [5]Widdowson M.Planetary volcanism-ulti ma thule?[M]∥Mc-Bridge N,Gil mour I.An introduction to the solar system.Cambridge:Cambridge University Press,2003:83-126.
• [6]Condie K C.Platetectonics andcrustal evolution[M].3rdedi-tion.[S.l.]:Pergamon Press,1989:1-476.
• [7]http:∥www.jamstec.go.jp/jamstec-e/shinkai/
• [8]http:∥www.whoi.edu/marops/vehicles/alvin/index.ht ml
• [9]Condie K C.Mantle plume and their record in Earth history[M].Cambridge:Cambridge University Press,2002:1-306.
• [10]Coffin M F,Eldhol m O.Large igneous province:Crustal structure,di mensions,and external consequences[J].Review of Geophysics,1994,32:1-36.
• [11]http://www.mantleplumes.org/
• [12]Saki moto S.Volcanoes on Mars:The global view[M]∥Lopes R MC,Gregg T K P.Volcanic world:Exploringthe solar system's volcanoes.Springer:Praxis Publishing,2004:97-110.
• [13]Sleep N H.Martian plate tectonics[J].J.Geophys.Res.,1994,99:5639-5655.
• [14]Carr M H.Water on Mars[M].New York:Oxford Universi-ty Press,1996:1-1229.
• [15]Rieder R,Economou T,Wanke H,et al.The chemical com-position of martian soil and rocks returned by the mobile alpha proton X-ray spectrometer:Preli minary results fromthe X-ray mode[J].Science,1997,278:1771-1774.
• [16]Christensen P R,McSween H Y,jr Bandfield J L,et al.Evi-dence for igneous diversity and magmatic evolution on Mars from infrared observations[J/OL].Nature,2005,436(7050):504-509.
• [17]Bandfield J L,Hamilton V E,Christensen P R,et al.Identifi-cation of quartzofeldspathic materials on Mars[J/OL].J.Geo-phys.Res.,2004,109(E1009):doi:10.1029/2004JE002290.
• [18]Hart mann W K.Martian surface and crust:Review and syn-thesis[J].Icarus,1973,19:550-575.
• [19]Carr M H.Tectonism and volcanism of the tharsis region of Mars[J].J.Geophys.Res.,1974,79:3943-3949.
• [20]Phillips RJ,Ivins E R.Geophysical observations pertainingto solid-state convection in the terrestrial planets[J].Phys.Earth Planet.Inter.,1979,19:107-148.
• [21]M啨ge D,Masson P,A plume tectonic model for the Tharsis province,Mars[J].Planetary and Space Science,1996,44:1499-1546.
• [22]Reese C C,Solomatov VS,Baumgardner J R,et al.Magmat-ic evolution of i mpact-induced Martian mantle plumes and the origin of Tharsis[J/OL].J.Geophys.Res.,2004,109:(E08009):doi:10.1029/2003JE002222.
• [23]Xiao L,Huang D H,Yang R Y,et al.Tharsis large igneous province on Mars:Opposite giant i mpact induced mantle plumeand magmatism?[C].AOGS-3rd Annual Meeting(Singa-pore)Abstract.[S.l.]:[s.n.],2006.
• [24]Doran P T,Clifford S M,Forman S L,et al.Mars chronolo-gy:Assessing techniques for quantifying surficial processes[J].Earth-Science Reviews,2004,67:313-337.
• [25]李春来,欧阳自远.空间化学[M].哈尔滨:哈尔滨工业大学出版社,2005:1-369.
• [26]Britt R R.Mars volcanoes possibly still active,pictures show[EB/OL].2004.http:∥www.space.com/scienceastronomy/mars-vulcanism-041222.ht ml.
• [27]Picardi G,Plaut J J,Biccari D.Radar soundings of the subsur-face of Mars[J].Science,2005,310:1925-1928.
• [28]Catthermole P.Venus:The geological story[M].London:UCL Press,1994:1-250.
• [29]Head J W,Crumpler L S,Aubele J C,et al.Venus volcan-ism:Classification of volcanic features and structure,associa-tions,and global distribution from magellan data[J].J.Geo-phys.Res.,1992,97:13153-13197.
• [30]Guest J E,Bul mer M H,Aubele J C,et al.Small volcanic ed-ifices and volcanismin the plains of Venus[J].J.Geophys.Res.,1992,97:15949-15966.
• [31]Crumpler L S,Aubele J C,Senske D A,et al.Volcanoes and centers of volcanismon Venus[M]∥Brougher S W,Hunten D M,Phillips R J.VenusⅡ.Tucson:Unerversity of Arizona Press,1997:697-756.
• [32]Stofan E R,Guest J E,Copp D L.Development of large vol-canoes on Venus:Constraints from Sf,gula and kunapipi montes[J].Icarus,2001,152:75-95.
• [33]Pavri B,Head J W,Klose K B,et al.Steep-sided domes on Venus:Characteristics,geologic setting,and eruption condi-tions from Magellan data[J].J.Geophys.Res.,1992,97:13445-13478.
• [34]Stofan E R,Anderson S W,Crown D A,et al.Emplacement and composition of steep-sided domes on Venus[J].J.Geo-phys.Res.,2000,105:26757-26772.
• [35]Pronin A A,Stofan E R.Coronae on Venus:Morphology,classi-fication and distribution[J].Icarus,1990,87:452-474.
• [36]Stofan E R,Tapper S W,Guest J E,et al.Preli minary analy-sis of an expanded corona database for Venus[J].Geophys.Res.Lett.,2001,28:4267-4270.
• [37]Schaber G G,Strom R G,Moore HJ,et al.Geology and dis-tribution of i mpact craters on Venus:What are theytelling us?[J].J.Geophys.Res.,1992,97:13257-13302.
• [38]Shearer C K,Papike J J.Basaltic magmatismon the moon:A perspective fromvolcanic picritic glass beads[J].Geochi mica et Cosmochi mica Acta,1993,57:4785-4812.
• [39]Neal C R,Taylor L A.Petrogenesis of mare basalts:Arecord of lunar volcanism[J].Geochi mica et Cosmochi mica Acta,1992,56:2177-2211.
• [40]O′Keefe J A,Cameron WS.Evidence fromthe moon's surface features for the production of lunar granites[J].Icarus,1962-1963,1:271-285.
• [41]Ryder G.Lunar sample15405:Remnant of a KREEP basalt-granite differentiated pluton[J].Earth and Planet.Sci.Lett.,1976,29:255-268.
• [42]Bogard D D,Garrison D H,Shih C Y,et al.39Ar-40Ar dating of twolunar granites:The age of Copernicus?[J].Geochi mi-caet Cosmochi mica Acta,1994,58:3093-3100.
• [43]马昌前.月球花岗岩——比较行星学意义[J].地质科技情报,2004,23(4):19-24.
• [44]Adams J B,Pieters C,McCord T B.Orange glass:Evidence for regional deposits of pyroclastic origin on the moon[C]∥Proceedings of the5thLunar Planetary science Confernece.[S.l.]:[s.n.],1974:171-186.
• [45]Delano J W.Pristine lunar glasses:Criteria,data,and i mpli-cations[J].J.Geophys.Res.,1986,91(Suppl.):D201-D213.
• [46]Lopes R MC.Io,a world of great volcanoes[M]∥Lopes R M C,Gregg T K P.Volcanic words:Exploringthe solar system's volcanoes.Spinger:Praxis Publishing,2004:127-144.
• [47]Prockter S.Ice volcanism on Jupiter's moons and beyond[M]∥Lopes R M C,Gregg T K P.Volcanic world:Exploring the solar system's volcanoes.Spinger:Praxis Publishing,2004:145-178.
• [48]Lopes R M C,Gregg T,Lougen J.Lava Lakes on Io[C].AOGS-3rd Annual Meeting(Singapore)Abstract.[S.l.]:[s.n.],2006.
• [49]Johnson T A,Veeder G J,Matson D L,et al.Io:Evidence for silicate volcanismin1986[J].Science,1988,242:1280-1283.
• [50]McEwen A S,Keszthelyi L,Spencer J R,et al.Very high temperature volcanism on Jupiter's moon Io[J].Science,1998,281:87-90.
• [51]Geissler P E,McEwen A S,Keszthelyi L,et al.Global color variations on Io[J].Icarus,1999,140:265-281.
• [52]http://www.jpl.nasa.gov/solar-system/planets/jupiter-in-dex.ht ml.
• [53]Kivelson M G,Khurana K K,Russell C T,et al.Galileo magnetometer measurements:Astronger case for a subsurface ocean at Europa[J].Science,2000,289:1340-1343.
• [54]Smith B A,Soderblom L A,Batson R,et al.A newlook at the Saturn system:Voyager2I mages[J].Science,1982,215:504-536.
• [55]Cruikshank D.Triton,Pluto and Charon[M]∥Beatty J K,Peterson C C,Chaikin A.The newsolar system.Cambridge:Cambridge University Press,1999:285-296.
• [56]Stern S A,Mikinnon WB.Triton's age and i mpactor popula-tion revisited in the light of Kuiper Belt fluxes:Evidence for small Kuiper Belt object and recent geological activity[J].The Astronomical Journal,2002,119:945-952.
• [57]Kirk R L,Soderblom L A,Brown R H,et al.Triton's plumes:Discovery,characteristics,and models[M]∥Cruiks-hank D P.Neptune andtriton.Tucson:University of Arizona Press,1995:949-989.
• [58]Wilson J T.Apossible origin of the hawaiianislands[J].Can.J.Physics.,1963,41:863-868.
• [59]Morgan WJ.Convection plumes in the lower mantle[J].Na-ture,1971,230:42-43.
• [60]King S D,Anderson D L.Edge driven convection[J].Earth Planet.Sci.Lett.,1998,160:289-296.
• [61]King S D,Ritsema J.African hotspot volcanism:Small-scale convectionin the upper mantle beneath cratons[J].Science,2000,290:1137-1140.
• [62]Pirajno F,Kranendonk MJ V.Review of hydrothermal processesand systems on Earth and i mplications for Martian analogues[J].Australian J.Earth Sci.,2005,52:329-351.
• [63]Kamatsu G,Dohn J M,Hare T M.Hydrogeologic processes of large-scale tectonomagmatic complexes in Mongolia-southern Si-beria and on Mars[J].Geology,2004,32:325-328.
• [64]Kamatsu G,Ori G G,Ciarcelluti P,et al.Interior layered de-posits of Valles Marineris,Mars:Analogous subice volcanism related to the Baikal rifting,southern Siberia[J].Planetary and Space Science,2004,52:167-187.
• [65]Pirajno F,van Kranendonk MJ,Xiao L.Hydrothermal sys-tems in the solar system:Areview[J].Journal of Geological Science and Technology Information,2008,27(1):1-12.
• [66]Jakosky B M,Shock E L.The biological potential of Mars,the early Earth,and Europa[J].J.Geophys.Res.,1998,103(E8):19359-19364.
• [67]Zarnecki J.Mars[M]∥Gil mour I,Sephton M A.An intro-duction to astrobiology,Cambridge:Cambridge University Press,2003:85-126.