Geophysical characterisation of the ocean–continent transition at magma-poor rifted margins

[1]  C. Beaumont,et al.  Complex rifted continental margins explained by dynamical models of depth-dependent lithospheric extension , 2008 .

[2]  I. Villa,et al.  The rift-to-drift transition in the North Atlantic: A stuttering start of the MORB machine? , 2007 .

[3]  D. Schmitt,et al.  Seismic and magnetic anisotropy of serpentinized ophiolite: Implications for oceanic spreading rate dependent anisotropy , 2007 .

[4]  G. Kent,et al.  Variation in styles of rifting in the Gulf of California , 2007, Nature.

[5]  S. P. Srivastava,et al.  Exhumed mantle-forming transitional crust in the Newfoundland-Iberia rift and associated magnetic anomalies , 2007 .

[6]  R. Hobbs,et al.  Crustal structure of the French Guiana margin, West Equatorial Atlantic , 2007 .

[7]  Jun Korenaga,et al.  Thermal cracking and the deep hydration of oceanic lithosphere: A key to the generation of plate tectonics? , 2007 .

[8]  R. Mjelde,et al.  Continent–ocean-transitions: Review, and a new tectono-magmatic model of the Vøring Plateau, NE Atlantic , 2007 .

[9]  J. Hopper,et al.  Seismic velocity structure of the rifted margin of the eastern Grand Banks of Newfoundland, Canada , 2006 .

[10]  J. Hopper,et al.  Crustal structure across the Grand Banks–Newfoundland Basin Continental Margin – II. Results from a seismic reflection profile , 2006 .

[11]  A. Watts,et al.  Gravity anomalies and segmentation at the East Coast, USA continental margin , 2006 .

[12]  J. Escartín,et al.  Modes of seafloor generation at a melt-poor ultraslow-spreading ridge , 2006 .

[13]  R. White,et al.  Crustal structure of the Southwest Indian Ridge at 66°E: seismic constraints , 2006 .

[14]  T. Minshull,et al.  From continental extension to seafloor spreading: crustal structure of the Goban Spur rifted margin, southwest of the UK , 2005 .

[15]  H. Shimamura,et al.  Continent‐ocean transition on the Vøring Plateau, NE Atlantic, derived from densely sampled ocean bottom seismometer data , 2005 .

[16]  J. Collins,et al.  Spreading-rate dependence of melt extraction at mid-ocean ridges from mantle seismic refraction data , 2004, Nature.

[17]  F. Schilling,et al.  Electrical Resistivity of Dehydrating Serpentinite , 2004 .

[18]  T. Funck,et al.  Crustal structure of the northern Nova Scotia rifted continental margin (eastern Canada) , 2004 .

[19]  L. Matias,et al.  Deep structure of the West African continental margin (Congo, Zaïre, Angola), between 5°S and 8°S, from reflection/refraction seismics and gravity data , 2004 .

[20]  C. Ranero,et al.  Geophysical evidence for hydration of the crust and mantle of the Nazca plate during bending at the north Chile trench , 2004 .

[21]  H. Schouten,et al.  An ultraslow-spreading class of ocean ridge , 2003, Nature.

[22]  J. Hopper,et al.  Crustal structure of the ocean‐continent transition at Flemish Cap: Seismic refraction results , 2003 .

[23]  R. Whitmarsh,et al.  Magmatism at the west Iberia non-volcanic rifted continental margin: evidence from analyses of magnetic anomalies , 2003 .

[24]  W. Jokat,et al.  Geophysical evidence for reduced melt production on the Arctic ultraslow Gakkel mid-ocean ridge , 2003, Nature.

[25]  C. Zelt,et al.  Assessment of crustal velocity models using seismic refraction and reflection tomography , 2003 .

[26]  M. Gutscher,et al.  The crustal structure of the NW Moroccan continental margin from wide-angle and reflection seismic data , 2002 .

[27]  T. Minshull,et al.  Azimuthal seismic anisotropy in a zone of exhumed continental mantle, West Iberia margin , 2002 .

[28]  P. Kelemen,et al.  Methods for resolving the origin of large igneous provinces from crustal seismology , 2002 .

[29]  D. Bernoulli,et al.  Seismic structure and response of ocean-continent transition zones – A comparison of an ancient Tethyan and a present-day Iberian site , 2002 .

[30]  M. Cannat,et al.  Magnetic properties of variably serpentinized abyssal peridotites , 2002 .

[31]  T. Jordan,et al.  On the state of sublithospheric upper mantle beneath a supercontinent , 2002 .

[32]  H. Shiobara,et al.  Lower crustal seismic velocity-anomalies; magmatic underplating or serpentinized peridotite? Evidence from the Vøring Margin, NE Atlantic , 2002 .

[33]  T. Minshull,et al.  Evolution of magma-poor continental margins from rifting to seafloor spreading , 2001, Nature.

[34]  W. Steven Holbrook,et al.  Gravity anomalies and crustal structure at the southeast Greenland margin , 2001 .

[35]  T. Reston,et al.  Rheological evolution during extension at nonvolcanic rifted margins: Onset of serpentinization and development of detachments leading to continental breakup , 2001 .

[36]  R. White,et al.  Crustal structure of the Southwest Indian Ridge at the Atlantis II Fracture Zone , 2000 .

[37]  R. Trumbull,et al.  Deep structure of the Namibia continental margin as derived from integrated geophysical studies , 2000 .

[38]  S. P. Srivastava,et al.  Magnetic evidence for slow seafloor spreading during the formation of the Newfoundland and Iberian margins , 2000 .

[39]  H. C. Larsen,et al.  Crustal structure of the southeast Greenland margin from joint refraction and reflection seismic tomography , 2000 .

[40]  L. Matias,et al.  Crustal structure of a super‐slow spreading centre:a seismic refraction study of Mohns Ridge, 72° N , 2000 .

[41]  T. Minshull,et al.  Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles : The IAM-9 transect at 40^° 20^' N , 2000 .

[42]  R. White,et al.  Segmentation and melt supply at the Southwest Indian Ridge , 1999 .

[43]  T. Minshull,et al.  Deep structure of the ocean-continent transition in the southern Iberia Abyssal plain from seismic refraction profiles : Ocean Drilling Program (Legs 149 and 173) transect , 1999 .

[44]  S. Constable,et al.  Magmatic processes at slow spreading ridges: implications of the RAMESSES experiment at 57° 45′N on the Mid-Atlantic Ridge , 1998 .

[45]  Colin A. Zelt,et al.  Three‐dimensional seismic refraction tomography: A comparison of two methods applied to data from the Faeroe Basin , 1998 .

[46]  D. Miller,et al.  A new assessment of the abundance of serpentinite in the oceanic crust , 1997 .

[47]  R. Whitmarsh,et al.  Insight into the nature of the ocean-continent transition off West Iberia from a deep multichannel seismic reflection profile , 1996 .

[48]  Walter D. Mooney,et al.  Seismic velocity structure and composition of the continental crust: A global view , 1995 .

[49]  C. Keen,et al.  The transition from a volcanic to a nonvolcanic rifted margin off eastern Canada , 1995 .

[50]  R. Whitmarsh,et al.  Models of the development of the West Iberia rifted continental margin at 40°30′N deduced from surface and deep‐tow magnetic anomalies , 1995 .

[51]  D. Hutchinson,et al.  Seismic structure of the U.S. Mid‐Atlantic continental margin , 1994 .

[52]  T. Minshull.  Poisson's ratio of a seaward‐dipping reflector series, Hatton Bank , 1993 .

[53]  P. Kelemen,et al.  Large igneous province on the US Atlantic margin and implications for magmatism during continental breakup , 1993, Nature.

[54]  R. White,et al.  Oceanic crustal thickness from seismic measurements and rare earth element inversions , 1992 .

[55]  G. Boillot,et al.  Undercrusting by serpentinite beneath rifted margins , 1989, Nature.

[56]  R. White,et al.  Magmatism at rift zones: The generation of volcanic continental margins and flood basalts , 1989 .

[57]  R. White,et al.  The Hatton Bank continental margin—II. Deep structure from two-ship expanding spread seismic profiles , 1989 .

[58]  K. Hinz.  A Hypothesis on Terrestrial Catastrophes. , 1981 .

[59]  X. Pichon,et al.  Passive margins: A model of formation , 1981 .

[60]  R. White,et al.  Compressional to shear wave conversion in oceanic crust , 1980 .

[61]  P. Spudich,et al.  A New Look at the Seismic Velocity Structure of the Oceanic Crust (Paper 80R0584) , 1980 .

[62]  J. Sibuet,et al.  Breakup of the Newfoundland–Iberia rift , 2007 .

[63]  R. G. Pratt,et al.  Full waveform tomography for lithospheric imaging: results from a blind test in a realistic crustal model , 2007 .

[64]  E. Morris,et al.  Active Source Electromagnetic Survey of Hydrothermal Venting Areas at the Saldanha Massif, Mid-Atlantic Ridge, the CD176/2004 Cruise , 2005 .

[65]  F. Klingelhöfera,et al.  Crustal structure of a super-slow spreading centre : a seismic refraction study of Mohns Ridge , 72 ° , 2005 .

[66]  T. Minshull,et al.  Three-dimensional tomographic inversion of combined reflection and refraction seismic traveltime data , 2003 .

[67]  M. Bickle,et al.  Is the oceanic Moho a serpentinization front? , 1998, Geological Society, London, Special Publications.

[68]  D. Miller,et al.  Seismic velocities of lower crustal and upper mantle rocks from the slow-spreading Mid-Atlantic Ridge, south of the Kane Transform Zone (MARK) , 1997 .

[69]  Robert B. Smith,et al.  Seismic traveltime inversion for 2-D crustal velocity structure , 1992 .