引文
[1]Wang Pinxian.Interactions between Earth's deep and surface[J].Advances in Earth Science,2003,24(12):1 331-1 338.[汪品先.地球深部与表层的相互作用[J].地球科学进展,2003,24(12):1 331-1 338.]
[2]Liu Zhifei,Tuo Shouting.Scientific ocean drilling programs:Re-view and prospect[J].Chinese Journal of Nature,2007,29(3):141-151.[刘志飞,拓守廷.科学大洋钻探回顾与展望[J].自然杂志,2007,29(3):141-151.]
[3]Expedition 334 Scientists.Costa Rica Seismogenesis Project(CRISP):Sampling and Quantifying Input to the SeismogenicZone and Fluid Output[R].Integrated Ocean Drilling ProgramExpedition 334 Preliminary Report,2011:1-67.
[4]Vannucchi P,Ujiie K,Gamage K.Costa Rica Seismogenesis Pro-ject(CRISP):Sampling and Quantifying Input to the SeismogenicZone and Fluid Output[R].Integrated Ocean Drilling ProgramExpedition 334 Scientific Prospectus,2010:1-53.
[5]Zhu J,Kopp H,Flueh E R,et al.Crustal structure of the centralCosta Rica subduction zone:Implications for basal erosion fromseismic wide-angle data[J].Geophysical Journal International,2009,178:1 112-1 131.
[6]Mann P,Rogers R D,Gahagan L.Overview of plate tectonic his-tory and its unresolved tectonic problems[M]∥Bunddchuh J,Al-varado G,eds.Central America:Geology,Resources and Haz-ards,2007:267-274.
[7]Hoernle K,Van den Bogaard P,Werner R,et al.Tectonic andbiological evolution of the Americas Missing history(16-71 Ma)ofthe Galpagos hotspot:Implications for the tectonic and biologicalevolution of the Americas[J].Geology,2002,30:795-798.
[8]Von Huene R,Ranero C R,Weinrebe W.Quaternary convergentmargin tectonics of Costa Rica,segmentation of the Cocos Plate,and Central American volcanism[J].Tectonics,2000,19:314-334.
[9]Hey R.Tectonic evolution of the Cocos-Nazca spreading center[J].Geological Society of America Bulletin,1977,88(12):1 404-1 420.
[10]Lonsdale P,Klitgord K D.Structure and tectonic history of theeastern Panama Basin[J].Geological Society of America Bulletin,1978,89(7):981-999.
[11]Van Andel T H,Heath G R,Malfait B T,et al.Tectonics of thePanama Basin,eastern equatorial Pacific[J].Geological Societyof America Bulletin,1971,82(6):1 489-1 508.
[12]Sigurdsson H,Kelley S,Leckie R M,et al.History of circum-Caribbean explosive volcanism:40Ar/39Ar dating of tephra layers[C]∥Leckie R M,Sigurdsson H,Acton G D,eds.Proceedingsof the Ocean Drilling Program Scientific Results 165[R/OL].ht-tp:∥www-odp.tamu.edu/publications/165_SR/165 TOCHTM,2011.
[13]Jordan B R,Sigurdsson H,Carey S N,et al.Geochemical corre-lation of Caribbean Sea tephra layers with ignimbrites in CentralAmerica[M]∥Siebe C,Macias Gerardo J L,Aguirre-Díaz G J,eds.Neogene-Quaternary Continental Margin Volcanism:A Per-spective from México.Special Paper:Geological Society of Amer-ica,2006,402:175-208.
[14]Reagan M K,Gill J B.Coexisting calcalkaline and high-niobiumbasalts from Turrialba Volcano,Costa Rica:Implications for re-sidual titanates in arc magma sources[J].Journal of GeophysicalResearch,1989,94(B4):4 619-4 633.
[15]Kutterolf S,Freundt A,Peréz W,et al.Pacific offshore record ofplinian arc volcanism in Central America:1.Along-arc correla-tions[J].Geochemistry,Geophysics,Geosystems,2008,9(2):Q02S01-Q02S26.
[16]Werner R,Hoernle K,Van den Bogaard P,et al.Drowned 14-m.y.-old Galápagos archipelago off the coast of Costa Rica:Im-plications for tectonic and evolutionary models[J].Geology,1999,27(6):499-502.
[17]Barckhausen U,Ranero C R,Von Huene R,et al.Revised tec-tonic boundaries in the Cocos plate off Costa Rica:Implicationsfor the segmentation of the convergent margin and for plate tecton-ic models[J].Journal of Geophysical Research,2001,106(B9):19 207-19 220.
[18]Ye S,Bialas J,Flueh E R,et al.Crustal structure of the MiddleAmerican Trench off Costa Rica from wide-angle seismic data[J].Tectonics,1996,15:1 006-1 021.
[19]Hinz K,Von Huene R,Ranero C R,et al.Tectonic structure ofthe convergent Pacific margin offshore Costa Rica from multichan-nel seismic reflection data[J].Tectonics,1996,15(1):54-66.
[20]Kimura G.Proceedings of the Ocean Drilling Program Initial Re-ports[R].Ocean Drilling Program,College Station,Texas,1997.
[21]Vannucchi P,Scholl D W,Meschede M,et al.Tectonic erosionand consequent collapse of the Pacific margin of Costa Rica:Combined implications from ODP Leg 170,seismic offshore data,and regional geology of the Nicoya Peninsula[J].Tectonics,2001,20(5):649-668.
[22]Vannucchi P,Fisher D M,Bier S,et al.From seamount accre-tion to tectonic erosion:Formation of Osa mélange and the effectsof Cocos Ridge subduction in southern Costa Rica[J].Tectonics,2006,25(4):TC2004.
[23]Buchs D M,Baumgartner P O.The Osa-Cao Accretionary Com-plex(southern Costa Rica):Sedimentary processes in the MiddleAmerican Trench recorded in an emerged Eocene-Miocene accre-tionary prism[C]∥10th Meeting of Swiss Sedimentologists(SWISS SED),Fribourg,Switzerland,2003.
[24]Meschede M,Zweigel P,Kiefer E.Subsidence and extension ata convergent plate margin:Evidence for subduction erosion offCosta Rica[J].Terra Nova,1999,11(2/3):112-117.
[25]Jannasch H W,Davis E E,Kastner M,et al.CORK-II:Long-term monitoring of fluid chemistry,fluxes,and hydrology in in-strumented boreholes at the Costa Rica subduction zone[R]∥Morris J D,Villinger H W,Klaus A.Proceedings of the OceanDrilling Program,Initial Report,205:College Station,TX(O-cean Drilling Program),2003:1-36.
[26]Morris J,Valentine R,Harrison T.10Be imaging of sediment ac-cretion and subduction along the northeast Japan and Costa Ricaconvergent margins[J].Geology,2002,30(1):59-62.
[27]Solomon E A,Kastner M,Wheat C G,et al.Long-term hydro-geochemical records in the oceanic basement and forearc prism atthe Costa Rica subduction zone[J].Earth and Planetary ScienceLetters,2009,282(1/4):240-251.
[28]Von Herzen R P,Uyeda S.Heat flow through the Eastern PacificOcean floor[J].Journal of Geophysical Research,1963,68:4 219-4 250.
[29]Vacquier V,Sclater J G,Correy C E.Studies of the thermalstate of the Earth:Heat flow,Eastern Pacific[J].Bulletin of theEarthquake Research Institute,1967,45:375-393.
[30]Stavenhagen A U,Flueh E R,Ranero C R,et al.Seismic wide-angle investigations in Costa Rica—A crustal velocity model fromthe Pacific to the caribbean coast[J].Zentralblatt für Geologicalund Palontologie,TeilΙ,1997,3/6:393-408.
[31]Walther C.The crustal structure of the Cocos ridge off Costa Rica[J].Journal of Geophysical Research,2003,108(B3):21-36.
[32]Zhu J,Kopp H,Klaeschen D,et al.Margin architecture andseismic attenuation in the central Costa Rican forearc[J].MarineGeology,2010,276:30-41.
[33]Christeson G L,McIntosh K D,Shipley T H.Seismic attenuationin the Costa Rica margin wedge:Amplitude modeling of oceanbottom hydrophone data[J].Earth and Planetary Science Letters,2000,179:391-405.