Alt J C, Shanks W C. 1998. Sulfur in serpentinized oceanic peridotites: Serpentinization processes and microbial sulfate reduction. J Geophys Res, 103: 9917-9929
[2]
Bach W, Banerjee N R, Dick H J B, et al. 2002. Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°-16°E. Geochem Geophys Geosyst, 3: 1-14
[3]
Bach W, Garrido C J, Paulick H, et al. 2004. Seawater-peridotite interactions: First insights from ODP Leg 209, MAR 15°N. Geochem Geophys Geosyst, 5, doi: 10.1029/2004gc000744
[4]
Beard J S, Frost B R, Fryer P, et al. 2009. Onset and progression of serpentinization and magnetite formation in olivine-rich troctolite from IODP Hole U1309D. J Petrol, 50: 387-403
[5]
Bina M M, Henry B. 1990. Magnetic properties, opaque mineralogy and magnetic anisotropies of serpentinized peridotites from ODP Hole 670A near the Mid-Atlantic Ridge. Phys Earth Planet Inter, 65: 88-103
[6]
Boillot G, Beslier M O, Krawczyk C M, et al. 1995. The formation of passive margins: Constraints from the crustal structure and segmentation of the deep Galicia margin, Spain. Geol Soc London Spec Publ, 90: 71-91
[7]
Boillot G, Grimaud S, Mauffret A, et al. 1980. Ocean-continent boundary off the Iberian margin: A serpentinite diapir west of the Galicia Bank. Earth Planet Sci Lett, 48: 23-34
[8]
Boillot G, Recq M, Winterer E L, et al. 1987a. Tectonic denudation of the upper mantle along passive margins: A model based on drilling results (ODP leg 103, western Galicia margin, Spain). Tectonophysics, 132: 335-342
[9]
Boillot G, Winterer E L, Meyer A W. 1987b. Leg 103. Proc ODP. Initial Reports, 103: 663
[10]
Bonatti E, Lawrence J R, Morandi N. 1984. Serpentinization of oceanic peridotites: Temperature dependence of mineralogy and boron content. Earth Planet Sci Lett, 70: 88-94
[11]
Burch S H. 1968. Tectonic emplacement of the Burro Mountain ultramafic body, Santa Lucia Range, California. Geol Soc Am Bull, 79: 527-544.
[12]
Cannat M, Bideau D, Bougault H. 1992. Serpentinized peridotites and gabbros in the Mid-Atlantic Ridge axial valley at 15°37￠N and 16°52￠N. Earth Planet Sci Lett, 109: 87-106
[13]
Cannat M, Mevel C, Maia M, et al. 1995. Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge (22°-24°N). Geology, 23: 49-52
[14]
Cornen G, Beslier M O, Girardeau J. 1996. Petrology of the mafic rocks cored in the Iberia Abyssal Plain. In: Proceeding-Ocean Drilling Program Scientific Results, National Science Foundation. 449-470
[15]
Day R, Fuller M, Schmidt V A. 1977. Hysteresis properties of titanomagnetites: Grain-size and compositional dependence. Phys Earth Planet Inter, 13: 260-267
[16]
Dilek Y, Coulton A, Hurst S D. 1997. Serpentinization and hydrothermal veining in peridotites at site 920 in the Mark area Proc-ODP Sci Res. National Science Foundation. 35-60
[17]
Dunlop D J. 2002. Theory and application of the Day plot (Mrs/Ms versus Hcr/Hc). Theoretical curves and tests using titanomagnetite data. J Geophys Res, 107, doi: 10.1029/2001jb000487
[18]
Dunlop D J, ？zdemir ？. 2001. Rock Magnetism: Fundamentals and Frontiers. Cambridge: Cambridge University Press
[19]
Dunlop D J, Prévot M. 1982. Magnetic properties and opaque mineralogy of drilled submarine intrusive rocks. Geophys J Int, 69: 763-802
[20]
Dyment J, Arkani-Hamed J, Ghods A. 1997. Contribution of serpentinized ultramafics to marine magnetic anomalies at slow and intermediate spreading centres: Insights from the shape of the anomalies. Geophys J Int, 129: 691-701
[21]
刘青松, 邓成龙. 2009. 磁化率及其环境意义. 地球物理学报, 52: 1041-1048
[22]
Afilhado A, Matias L, Shiobara H, et al. 2008. From unthinned continent to ocean: The deep structure of the West Iberia passive continental margin at 38°N. Tectonophysics, 458: 9-50
[23]
Agrinier P, Cannat M. 1997. Oxygen-isotope constrains on serpentinization process in ultramafic rocks from the mid-atlantic ridge (23°N). Notes, 47: 95
[24]
Agrinier P, Cornen G, Beslier M O. 1996. Mineralogical and oxygen isotopic features of serpentinites recovered from the ocean/continent transition in the iberia abyssal plain. In: Proceedings of the Ocean Drilling Program, Scientific Results. 149: 541
[25]
Agrinier P, Mével C, Girardeau J. 1988. Hydrothermal alteration of the peridotites cored at the ocean/continent boundary of the Iberian margin: Petrologic and stable isotope evidence. In: Boillot G, Winterer E L, et al., eds. Proc ODP Sci Results, 103: 225-234
[26]
Allen D E, Seyfried Jr W E. 2003. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars. Geochim Cosmochim Acta, 67: 1531-1542
[27]
Bideau D, Hebert R, Hekinian R, et al. 1991. Metamorphism of deep-seated rocks from the Garrett Ultrafast Transform (East Pacific Rise near 13°25￠S). J Geophys Res, 96: 10079-10099
[28]
Evans B W, Hattori K, Baronnet A. 2013. Serpentinite: What, why, where? Elements, 9: 99-106
[29]
Evans C A, Girardeau J. 1988. Galicia margin peridotites: Undepleted abyssal peridotites from the North Atlantic. In: Boillot G, Winterer E L, et al., eds. Proc ODP Sci Results, 103: 195-207
[30]
Evans M, Heller F. 2003. Environmental Magnetism: Principles and Applications of Enviromagnetics. New York: Academic press
[31]
Féraud G, Beslier M O, Cornen G. 1996. 40Ar/39Ar dating of gabbros from the Ocean/Continent Transition of the west Iberia Margin. Proc ODP Preliminary Results, doi: 10.2973/odp.proc.sr.149.224.1996
[32]
Hébert R, Gueddari K, Lafleche M R, et al. 2001. Petrology and geochemistry of exhumed peridotites and gabbros at non-volcanic margins: ODP Leg 173 West Iberia ocean-continent transition zone. Geol Soc London Spec Publ, 187: 161-189
[33]
Hattori K H, Guillot S. 2003. Volcanic fronts form as a consequence of serpentinite dehydration in the forearc mantle wedge. Geology, 31: 525-528
[34]
Hess H H. 1964. The oceanic crust, the upper mantle and the Mayaguez serpentinized peridotite, in a study of serpentinite: NAS-NRC pub. 1188, 153-169
[35]
Hess H H. 1962. History of ocean basins. Petrologic Studies, 4: 599-620
[36]
IAGA Division V, Working Group 8. 1995. International geomagnetic reference field, 1995 revision. J Geomagn Geoelectricity, 47, 1257-1261.
[37]
Jackson M, Carter-Stiglitz B, Egli R, et al. 2006. Characterizing the superparamagnetic grain distribution f (V, Hk) by thermal fluctuation tomography. J Geophys Res, 111, doi: 10.1029/2006jb004514
[38]
Lienert B R, Wasilewski P J. 1979. A magnetic study of the serpentinization process at Burro Mountain, California. Earth Planet Sci Lett, 43: 406-416
[39]
Liu Q, Deng C, Yu Y, et al. 2005. Temperature dependence of magnetic susceptibility in an argon environment: Implications for pedogenesis of Chinese loess/paleosols. Geophys J Int, 161: 102-112
[40]
Mével C. 2003. Serpentinization of abyssal peridotites at mid-ocean ridges. C R Geosci, 335: 825-852
[41]
Manatschal G, Froitzheim N, Rubenach M, et al. 2001. The role of detachment faulting in the formation of an ocean-continent transition: Insights from the Iberia Abyssal Plain. Geol Soc London Spec Publ, 187: 405-428
[42]
McDougall I, Harrison T M. 1999. Geochronology and Thermochronology by the 40Ar/39Ar Method. Oxford: Oxford University Press
[43]
Michael P J, Thiede J, Dick H J, et al. 2001. The Arctic Mid-Ocean Ridge Expedition-AMORE 2001-Seafloor Spreading at the Top of the World. In: AGU Fall Meeting Abstracts. 1: 0853
[44]
Minshull T A, Dean S M, Whitmarsh R B, et al. 1998. Deep structure in the vicinity of the ocean-continent transition zone under the southern Iberia Abyssal Plain. Geology, 26: 743-746
[45]
Muxworthy A R, McClelland E. 2000. Review of the low-temperature magnetic properties of magnetite from a rock magnetic perspective. Geophys J Int, 140: 101-114
[46]
Nazarova K A. 1994. Serpentinized peridotites as a possible source for oceanic magnetic anomalies. Mar Geophys Res, 16: 455-462
[47]
Niu Y. 1997. Mantle melting and melt extraction processes beneath ocean ridges: Evidence from abyssal peridotites. J Petrol, 38: 1047-1074
[48]
Niu Y. 2004. Bulk-rock major and trace element compositions of abyssal peridotites: Implications for mantle melting, melt extraction and post-melting processes beneath mid-ocean ridges. J Petrol, 45: 2423-2458
[49]
O’Hanley D S. 1992. Solution to the volume problem in serpentinization. Geology, 20: 705-708
[50]
O’reilly W. 1984. Rock and Mineral Magnetism. Glasgow: Blackie
[51]
Ogg J G. 1988. Early cretaceous and tithonianmagnetostratigraphy of the Galicia Margin. In: Ocean Drilling Program Leg 103, doi: 10.2973/odp.proc.sr.103.166.1988
[52]
Oufi O, Cannat M, Horen H. 2002. Magnetic properties of variably serpentinized abyssal peridotites. J Geophys Res, 107, doi: 10.1029/2001jb000549
[53]
Pinheiro L M, Wilson R C L, Pena dos Reis R, et al. 1996. The western Iberia margin: A geophysical and geological overview. In: Proceeding- Ocean Drilling Program Scientific Results, National Science Foundation. 3-26
[54]
Prévot M, Lecaille A, Mankinen E A. 1981. Magnetic effects of maghemitization of oceanic crust. J Geophys Res, 86: 4009-4020
[55]
Raleigh C B, Paterson M S. 1965. Experimental deformation of serpentinite and its tectonic implications. J Geophys Res, 70: 3965-3985
[56]
Sawyer D S, Whitmarsh R B, Klaus A, et al. 1994. Proc. ODP, Init. Repts., 149: College Station. TX (Ocean Drilling Program), doi: 10.2973/odp.proc.ir.149.1994
[57]
Saad A H. 1969. Magnetic properties of ultramafic rocks from Red Mountain, California. Geophysics, 34: 974-987
[58]
Seifert K, Brunotte D. 1996. Geochemistry of serpentinized mantle peridotite from Site 897 in the Iberia Abyssal Plain. In: Proceeding-Ocean Drilling Program Scientific Results, National Science Foundation. 413-424
[59]
Shive P N, Frost B R, Peretti A. 1988. The magnetic properties of metaperidotitic rocks as a function of metamorphic grade: Implications for crustal magnetic anomalies. J Geophys Res, 93: 12187-12195
[60]
Snow J E, Dick H J B. 1995. Pervasive magnesium loss by marine weathering of peridotite. Geochim Cosmochim Acta, 59: 4219-4235
[61]
Tauxe L, Staudigel H. 2004. Strength of the geomagnetic field in the Cretaceous Normal Superchron: New data from submarine basaltic glass of the TroodosOphiolite. Geochem Geophys Geosyst, 5, doi: 10.1029/2003gc000635
[62]
Toft P B, Arkani-Hamed J, Haggerty S E. 1990. The effects of serpentinization on density and magnetic susceptibility: A petrophysical model. Phys Earth Planet Inter, 65: 137-157
[63]
Tucholke B E, Ludwig W J. 1982. Structure and origin of the J anomaly Ridge, western North Atlantic Ocean. J Geophys Res, 87: 9389-9407
[64]
Whitmarsh R B, Beslier M O, Wallace P J, et al. 1998. Proc. ODP, Init. Repts., 173: College Station. TX (Ocean Drilling Program), doi: 10.2973/odp.proc.ir.173.1998
[65]
Whitmarsh R B, Miles P R, Sibuet J C, et al. 1996. Geological and geophysical implications of deep-tow magnetometer observations near sites 897, 898, 899, 900, and 901 on the west Iberia Continental Margin. In: Proceedings of the Ocean Drilling Program, Scientific Results. doi: 10.2973/odp.proc.sr.149.241.1996
[66]
Zhao X. 1996. Magnetic signatures of peridotite rocks from Sites 897 and 899 and their implications. In: Proceeding-Ocean Drilling Program Scientific Results, National Science Foundation. 431-448
[67]
Zhao X. 2001. Paleomagnetic and rock magnetic results from serpentinized peridotites beneath the Iberia Abyssal Plain. Geol Soc London Spec Publ, 187: 209-234
[68]
Zhao X, Riisager P, Antretter M, et al. 2006. Unraveling the magnetic carriers of igneous cores from the Atlantic, Pacific, and the southern Indian oceans with rock magnetic characterization. Phys Earth Planet Inter, 156: 294-328
[69]
Zhao X, Turrin B D, Jackson M, et al. 2001. Paleomagnetic and rock magnetic characterization of rocks recovered from Leg 173 sites. In: Proceedings of the Ocean Drilling Program (ODP). Scientific Results, 173: 1-73
[70]
Zhu R, Hoffman K A, Nomade S, et al. 2004. Geomagnetic paleointensity and direct age determination of the ISEA (M0r?) chron. Earth Planet Sci Lett, 217: 285-295
[71]
Zolotov M Y, Shock E L. 2003. Energy for biologic sulfate reduction in a hydrothermally formed ocean on Europa. J Geophys Res, 108, doi: 10.1029/2002je001966
