Chave A D, Cox C S. 1982. Controlled electromagnetic source for measuring electrical conductivity beneath the oceans 1. Forward problem and model study.Journal of Geophysical Reasearch, 87(B7):5372-5338, doi: 10.1029/JB087iB07p05327.
[2]
Chen G B, Wang H N, Yao J J, et al. 2009.Three-dimensional numerical modeling of marine controlled-source electromagnetic responses in a layered anisotropic seabed using integral equation method. Acta Physica Sinica, 58(06):3848-3857,doi: 10.7498/aps.58.3848.
[3]
Crepaldi J L S, Buonora M P P, Figueiredo I. 2011. Fast marine CSEM inversion in the CMP domain using analytical derivatives.Geophysics,76(5):F303-F313, doi: 10.1190/geo2010-0237.1
[4]
Edwards R N, Chave A D. 1986. A transient electric dipole-dipole method for mapping the conductivity of the sea floor.Geophysics, 51(4):984-987, doi: 10.1190/1.1442156.
[5]
Edwards R N. 1997.On theresource evalution of marine gas hydrate deposits using sea-floor transient electric dipole-dipole methods. Geophysics, 62(1):63-74, doi: 10.1190/1.1444146.
[6]
Eidesmo T, Ellingsurd S, MacGregor L M, et al. 2002. Sea bed Logging(SBL), a new method for remote and direct identification of hydrocarbon filled layers in deepwater areas. First Break, 20(3):144-152, doi: 10.1046/j.1365-2397.2002.00264.x.
[7]
Everett M E, Constable S C. 1999.Electric dipole fields over an anisotropic seafloor: theory and application to the structure of 40 Ma Pacific Ocean lithosphere. Geophysical Journal International, 136:41-56, doi: 10.1046/j.1365-246X.1999.00725.x.
[8]
Freund R W. 1993. A transpose-free quasi-minimal residual algorithm for non-Hermitian linear systems.SIAM J. Sci. Stat. Comput, 14: 470-482, doi: 10.1137/0914029.
[9]
Gellert W, Kuestner H, Hellwich M, et al. 1986. Mathematik, VEB BibliographischesInstitut, Leipzig
[10]
Gribenko A, Zhdanov M S. 2007.Rigorous 3D inversion of marine CSEM databased on the integral equation method.Geophysics, 72(2):WA73-WA84, doi: 10.1190/1.2435712.
[11]
Li Y, Dai S. 2011. Finite element modelling of marine controlled-source electromagnetic responses in two-dimensional dipping anisotropic conductivity structures.Geophysical Journal International, 185:622-636, doi: 10.1111/j.1365-246X.2011.04974.x.
[12]
Lseth L O, Ursin B. 2007.Electromagnetic fields in planarly layered anisotropic media. Geophysical Journal International, 107:44-80, doi: 10.1111/j.1365-246X.200703390.x.
[13]
Yin C C, Liu Y H, Weng A H, et al. 2012.Research on marine controued-source electromagnetic method airwave.Journal of Jilin University (Earth Science Edition), 42(5):1506-1520, doi: 10.6038/j.issn.0001-5733.2012.08.027.
[14]
Zhdanov M S. 2002. Geophysical inverse theory and regularization problems:Elsevier Science Publ. Co., Inc.
[15]
Zhdanov M S, Lee S K, Yoshioka K. 2006.Integral equation method for 3D modeling of electromagnetic fields incomplex structures with inhomogeneous background conductivity.Geophysics, 71(6):G333-G345, doi: 10.1190/1.2358403.
[16]
Constable S C, Cox C S. 1996. Marine controlled source electromagnetic sounding:2.The PEGASUS experiment.Journal of Geophysical Research, 101(B3):5519-5530, doi: 10.1029/95JB03738.
[17]
Constable S C, Srnka L J. 2007. An introduction to marine controlled-source electromagnetic methods for hydrocarbon exploration.Geophysics, 72(2):WA3-WA12, doi: 10.1190/1.2432483.
[18]
Constable S C. 2010. Ten years of marine CSEM for hydrocarbon exploration. Geophysics, 75(5):75A67-75A81,doi: 10.1190/1.3483451.
[19]
Commer M, Newman G A. 2008.New advamces in three-dimensional controlled-source electromagnetic inversion.Geophysical Journal International, 172:513-535, doi: 10.1111/j.1365-246X.2007.03660.x.
[20]
Cox C S. 1980. Electromagnetic induction in the oceans and inferences on the constitution of the earth.Geophysical Surveys. 4(1-2):137-156, doi: 10.1007/BF01452963.
[21]
Cox C S. 1981. On the electrical conductivity of the oceanic lithosphere.Physics of the Earth and Planetary Interiors, 25(3):196-201, doi: 10.1016/0031-9201(81)90061-3.
[22]
Cox C S, Constable S C, Chave A D, et al. 1986. Controlled source electromagnetic sounding of the ocean lithosphere.Nature, 320 (6):52-54, doi: 10.1038/320052a0.
[23]
Hoversten G M, Morrison H F, Constable S C. 1998. Marine magnetotellurics for petroleum exploration, Part II:Numerical analysis of subsalt resolution. Geophysics, 63(3):826-840, doi:10.1190/1.1444394.
[24]
HunzikerJ, Slob E, Mulder W. 2011. Effects of the airwave in time-domain marine controlled-source electromagnetics.Geophysics, 76(4):F251-F261, doi:10.1190/1.3587222.
[25]
Kong F N, Johnstad S E, Rsten T, et al. 2008. A 2.5D finite-element-modeling difference method for marine CSEM modeling in stratified anisotropic media. Geophysics, 73(1):F9-F19, doi: 10.1190/1.2819691.
[26]
Liu C, Zhou F, Lin J. 2012. Simulation and analysis on the prospecting capability of marine controlled-source electromagnetic methods to hydrocarbon reservoirs.Chinese Journal of Radio Science, 27(4):747-772.
[27]
Liu Y, Yin C, Weng A, et al. 2012. Attitude effect for marine CSEM system. Chinese J. Geophys., 55(8):2757-2768. doi: 10.6038/j. issn. 0001-5733. 2012. 08. 027.
[28]
Mittet R, Morten J P. 2013. The marine controlled-source electromagnetic method in shallow water.Geophysics, 78(2):E67-E77, doi: 10.1190geo2012-0112.1.
[29]
Newman G A, Alumbaugh D L. 1995.Frequency-domain modelling of airbone electromagnetic responses using staggered finite differences. Geophysical Prospecting, 43:1021-1042, doi: 10.1111/j.1365-2478.1995.tb00294.x.
[30]
Newman G A, Commer M, Carazzone J J. 2010. Imaging CSEM data in the presence of electrical anisotropy.Geophysics,75(2):F51-F61, doi: 10.1190/1.3295883.
[31]
Um E S, Alumbaugh D L. 2007.On the physics of the marine controlled-source electromagnetic method.Geophysics, 72(2):WA13-WA26, doi: 10.1190/1.2432482.
[32]
Weiss C J, Constable S. 2006. Mapping thin resistors and hydrocarbons with marine EM methods, Part Ⅱ—Modeling and analysis in 3D. Geophysics, 71(6): G321-G332, doi: 10.1190/1.2356908.
[33]
Wiik T, Ursin B, Hokstad K. 2013. 2.5D EM modelling in TIV conductive media and the effect of anisotropy in normalized amplitude responses.Journal of Geophyscis and Engineering, 2013(10):1-10, doi: 10.1088/1742-2132/10/1/015006.
[34]
Sasaki Y. 2013. 3D inversion of marine CSEM and MT data:An approach to shallow-water problem. Geophysics, 78(1):E59-E65, doi: 10.1190/geo2012-0094.1.
[35]
Sinba M C, Patel P D, Unsworth M J, et al. 1990. An active source electromagnetic sounding system for marine use.Marine Geophysical Research, 12(1-2):59-68, doi: 10.1007/BF00310563.
[36]
Yin C. 2006. MMT forward modeling for a layered earth with arbitrary anisotropy. Geophysics, 71(3):G155-G128, doi: 10.1190/1.2197492.
[37]
Yang B, Xu Y X, He Z X, et al. 2012.3D frequency-domain modeling of marine controlled source electromagnetic responses with topography using finite volume method.Chinese J.Geophys.(in China), 55(4):1390-1399. doi: 10. 6038/j. issn. 0001-5733. 2012. 04. 035.
