The source is a flat 1-km-thick layer at 4 km depth. Save this search. I go on to outline a basin evolution history that involves its formation in Mesozoic times and that is consistent with the majority of those data. Double lines: Divergent plate boundaries, based on magnetic lineations. Dashed purple lines: abandoned transfer zones. Together with the Sandwich Plate, the Scotia Plate joins the southern-most Andes to the Antarctic Peninsula, just like the The northern edge of the Scotia plate is bounded by the South American plate, forming the North Scotia Ridge. Someone who either doesn't like Ghostbusters or didn't get the reference left him a note under his wiper on Wednesday. Benjamin Hebb has a Nova Scotia plate on the back of his vehicle, but a plate on the front says "ECTO-1 NEW YORK" and is a replica of the one found on the ambulance/hearse in the film. Instead, the available data almost unanimously invite the conclusion that the central Scotia Sea is at least 80 Myr old and probably hosts part of just one flank of an oceanic spreading system. The magnetic anomaly profiles sample the whole western corridor and part of the central corridor. Mantle flow drives the subsidence of oceanic platesDredged rocks from Powell Basin and the South Orkney MicrocontinentScotia Sea regional tectonic evolution: implications for mantle flow and palaeocirculationThe influence upon Southern Ocean circulation, sedimentation, and climate of the opening of Drake PassageAnomalous temperatures in central Scotia Sea sediments-bottom water variation or pore water circulation in old ocean crustAn early Miocene ridge-crest–trench collision on the South Scotia Ridge near 36°WReappraising elastic thickness variation at oceanic trenchesElastic layer thickening with age of the oceanic lithosphere: a tool for the prediction of the ages of volcanoes or oceanic crustLate Jurassic bimodal magmatism in the northern seafloor remnant of the Rocas Verdes Basin, southern Patagonian AndesMesozoic magnetic lineations in the Bering Sea marginal basinEvidence for Cenozoic crustal extension in the Bering Sea regionRapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific OceanThe correction for sediment loading on the seafloorSouthernmost South America-Antarctic Peninsula relative plate motions since 84 Ma: implications for the tectonic evolution of the Scotia Arc regionTectonics and sedimentary environment of the North Scotia Ridge region revealed by side-scan sonarBack-arc extension in the Southern Andes: a review and critical reappraisalTectonic relations of South Georgia island to the southernmost AndesRegional heat flow variations across the sedimented Juan de Fuca eastern flank: constraints on lithospheric cooling and lateral hydrothermal heat transportRapid Cenozoic glaciation of Antarctica induced by declining atmospheric COTranspressional deformation along the margin of Larsen Basin: new data from Pedersen Nunatak, Antarctic PeninsulaThe evolution of the Scotia Arc as a key to the reconstruction of southwest GondwanalandSummary of paleomagnetic results from West Antarctica: implications for the tectonic evolution of the Pacific margin of Gondwana during the MesozoicSouth Georgia and Gondwana's Pacific margin: lost in translation?Opening history of Powell Basin, Antarctic PeninsulaGondwana breakup and plate kinematics: Business as usualSmall basins in the Scotia Sea: the Eocene Drake Passage gatewayPaleogene volcaniclastic rocks on Seymour Island, northern Antarctic PeninsulaHydrothermal recharge and discharge across 50 km guided by seamounts on a young ridge flankFault plane solutions and tectonics of the South Atlantic and Scotia SeaPropagating rift during the opening of a small oceanic basin: the Protector Basin (Scotia Arc, Antarctica)Continental stretching preceding the opening of the Drake Passage: evidence from Tierra del FuegoHydrocarbon basins in SE Asia: understanding why they are thereThe geology of Cape Dubouzet, northern Antarctic Peninsula: continental basement to the Trinity Peninsula Group?Evidence for Miocene back-arc spreading in the central Scotia SeaEocene circulation of the Southern Ocean: was Antarctica kept warm by subtropical waters?Cenozoic paleoceanography in the southwest Pacific Ocean, Antarctic glaciation and the development of the Circum-Antarctic CurrentInternal structure of a contourite drift generated by the Antarctic Circumpolar CurrentMetamorphic P-T paths from Cordillera Darwin, a core complex in Tierra del Fuego, ChileGeophysical evidence for the East Antarctic plate boundary in the Weddell SeaEarly Cenozoic decoupling of the global carbon and sulfur cyclesThe tectonic history of Drake Passage and its possible impacts on global climateStructure and tectonic evolution of the South Sandwich arcOpening of Drake Passage and its impact on Cenozoic ocean circulationEvolution of Cenozoic seaways in the circum-Antarctic regionMesozoic seafloor spreading in the Southern Weddell SeaScotia Sea tectonics from high-resolution satellite gravityShackleton Fracture Zone: no barrier to early circumpolar circulationDrake Passage and Cenozoic climate: an open and shut case?Possible evidence for Late Cretaceous off-axis volcanism in the outer James Ross BasinContourite deposits in the central Scotia Sea: the importance of the Antarctic Circumpolar Current and the Weddell Gyre flowsEvolution of the deep and bottom waters of the Scotia Sea, Southern Ocean during 1995–2005Evidence for late Oligocene establishment of the Antarctic Circumpolar CurrentImproved seismic stratigraphy of the Mesozoic Weddell SeaMarine gravity anomaly from Geosat and ERS 1 satellite altimetryTiming and climatic consequences of the opening of the Drake PassageEffect of the Drake Passage through flow on global climateAtmospheric moisture transport determines climatic response to the opening of the Drake PassageEffect of ocean gateway changes under greenhouse warmthGlobal seafloor topography from satellite altimetry and ship depth soundingsA model for the global variation in oceanic depth and heat flow with lithospheric ageRocas Verdes ophiolites, southernmost South America: remnants of progressive stages of development of oceanic-type crust in a continental margin back-arc basinProcesses of formation and filling of a Mesozoic back-arc basin on the island of South GeorgiaTiming of events in an Early Cretaceous island arc-marginal basin system on South GeorgiaA mid-Cretaceous age for the Palmer Land event, Antarctic Peninsula: implications for terrane accretion timing and Gondwana palaeolatitudesGroup velocity tomography in the subantarctic Scotia Sea regionGlobal gravity, bathymetry and the distribution of submarine volcanism through space and timeHeat flow through the floor of the Scotia, far south Atlantic and Weddell seas© 2010 The Authors Geophysical Journal International © 2010 RAS

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