Baker E T, Edmonds H N, Michael P J, et al. 2004. Hydrothermal venting in magma deserts: The ultraslow-spreading Gakkel and Southwest Indian Ridges. Geochem Geophys Geosyst, 5: Q08002, doi:10.1029/2004GC000712
[3]
Cande S C, Kent D V. 1995. Revised calibration of the geomagnetic polarity timescale for the late cretaceous and cenozoic. J Geophys Res, 100: 6093-6095
[4]
Cannat M, Rommevaux-Jestin C, Sauter D, et al. 1999. Formation of the axial relief at the very slow spreading Southwest Indian Ridge (49° to 69°E). J Geophys Res, 104: 21825-21843
[5]
Cannat M, Sauter D, Mendel V, et al. 2006. Modes of seafloor generation at a melt-poor ultraslow-spreading ridge. Geology, 34: 605-608
[6]
Charvis P, Recq M, Operto S, et al. 1995. Deep structure of the northern Kerguelen Plateau and hotspot related activity. Geophys J Int, 122: 899-924
[7]
Chen Y J, Lin J. 1999. Mechanisms for the formation of ridge-axis topography at slow-spreading ridges: A lithospheric-plate flexural model. Geophys J Int, 136: 8-18
[8]
Curray J R, Munasinghe T. 1991. Origin of the Rajmahal Traps and the 85°E Ridge: Preliminary reconstructions of the trace of the Crozet hotspot. Geology, 19: 1237-1240
[9]
Debayle E, Sambridge M. 2004. Inversion of massive surface wave data sets: model construction and resolution assessment. J Geophys Res, 109: B02316, doi:10.1029/2003JB002652
[10]
Dick H J B, Lin J, Schouten H. 2003. An ultraslow-spreading class of ocean ridge. Nature, 426: 405-412
[11]
Dziewonski A, Anderson D. 1981. Preliminary reference Earth model. Phys Earth Planet Int, 25: 297-356
[12]
Georgen J E, Lin J, Dick H J B. 2001. Evidence from gravity anomalies for interactions of the Marion and Bouvet hotspots with the Southwest Indian Ridge: Effects of transform offsets. Earth Planet Sci Lett, 187: 283-300
[13]
Goslin J, Patriat P. 1984. Absolute and relative plate motions and hypotheses on the origin of five aseismic ridges in the Indian Ocean. Tectonophys, 101: 221-244
[14]
Ito G, Lin J, Graham D. 2003. Observational and theoretical studies of the dynamics of mantle plume-mid-ocean ridge interaction. Rev Geophys, 41: 1017, doi:10.1029/2002RG000117
[15]
Lin J, Zhang C. 2006. The first collaborative China-international cruises to investigate mid-ocean ridge hydrothermal vents. Inter Ridge News, 15: 33-34
[16]
Mendel V, Sauter D, Rommevaux-Jestin C, et al. 2003. Magmatic-tectonic cyclicity at the ultra-slow spreading Southwest Indian Ridge: Evidence from variations of axial volcanic ridge morphology and abyssal hills pattern. Geochem Geophys Geosyst, 4: 9102, doi: 10.1029/ 2002GC000417
[17]
Mendel V, Munschy M, Sauter D, et al. 2005. MODMAG, a MATLAB program to model marine magnetic anomalies. Comput Geosci, 31: 589-597
[18]
Montelli R, Nolet G, Dahlen F, et al. 2004. Finite-frequency tomography reveals a variety of plumes in the mantle. Science, 303: 338-343
[19]
Müller R D, Sdrolias M, Gaina C, et al. 2008. Age, spreading rates, and spreading asymmetry of the world''s ocean crust. Geochem Geophys Geosyst, 9: Q04006, doi: 10.1029/2007GC001743
[20]
Parker R L. 1973. The rapid calculation of potential anomalies. Geophys J Roy Astron Soc, 31: 447-455
[21]
Recq M, Goslin J, Charvis P, et al. 1998. Small-scale crustal variability within an intraplate structure: The Crozet Bank (southern Indian Ocean). Geophys J Int, 134: 145-156
[22]
Sandwell D T, Smith W. 1997. Marine gravity anomaly from Geosat and ERS 1 satellite altimetry. J Geophys Res, 102: 10039-10054
[23]
Sauter D, Carton H, Mendel V, et al. 2004. Ridge segmentation and the magnetic structure of the Southwest Indian Ridge (at 50°30′E, 55°30′E and 66°20′E): Implications for magmatic processes at ultraslow-spreading centers. Geochem Geophys Geosyst, 5: Q05K08, doi: 10.1029/2003GC000581
[24]
Sauter D, Cannat M, Meyzen C, et al. 2009. Propagation of a melting anomaly along the ultraslow Southwest Indian Ridge between 46° E and 52°20′E: Interaction with the Crozet hotspot? Geophys J Int, 179: 687-699
[25]
Smith D K, Cann J, Escartin J. 2006. Widespread active detachment faulting and core complex formation near 13° N on the Mid-Atlantic Ridge. Nature, 442: 440-443
[26]
Smith W H F, Sandwell D T. 1997, Global sea floor topography from satellite altimetry and ship depth soundings. Science, 277: 1956-1962
[27]
Tao C, Lin J, Guo S, et al. 2012. First active hydrothermal vents on an ultraslow-spreading center: Southwest Indian Ridge. Geology, 40: 47-50
[28]
Tucholke B, Behn M, Buck W R, et al. 2008. Role of melt supply in oceanic detachment faulting and formation of megamullions. Geology, 36: 455-458
[29]
Van Ark E, Lin J. 2004. Time variation in igneous volume flux of the Hawaii-Emperor hot spot seamount chain. J Geophys Res, 109: B11401, doi:10.1029/2003JB002949.
[30]
Vidal V, Bonneville A. 2004. Variations of the Hawaiian hot spot activity revealed by variations in the magma production rate. J Geophys Res, 109: B03104, doi: 10.1029/2003JB002559
[31]
Wang T, Lin J, Tucholke B et al. 2011. Crustal thickness anomalies in the North Atlantic Ocean basin from gravity analysis. Geochem Geophys Geosyst, 12: Q0AE02, doi: 10.1029/2010GC003402
[32]
Wessel P, Smith W H F. 1995. New version of the Generic Mapping Tools released. EOS Trans AGU, 76: 329
[33]
Zhao M, Zhang J, Qiu X, et al. 2011. Preliminary results of 3D seismic structure in the Southwest Indian Ocean Ridge (37°50''S). AGU Fall Meeting, Abstract #S41A-2146
[34]
Zhu J, Lin J, Chen Y J, et al. 2010. A reduced crustal magnetization zone near the first observed active hydrothermal vent field on the Southwest Indian Ridge. Geophys Res Lett, 37: L18303, doi: 10.1029/2010GL043542