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  • Recent extension driven by mantle upwelling beneath the

     · Importantly, the observation that extension between East and West Antarctica is still at work in recent time and interacts with dextral wrenching [Rossetti et al., 2006 Storti et al., 2007] may have implication for the global plate-reconstruction circuit [e.g., Steinberger et al., 2004]. 6. Conclusion

  • Sea Ice Index National Snow and Ice Data Center

     · The monthly Sea Ice Index provides a quick look at Antarctic-wide changes in sea ice. It is a source for consistently processed ice extent and concentration images and data values since 1979. Monthly images show sea ice extent with an outline of the 30-year () median extent for that month (magenta line).

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  • Evaluating Extension in the Ross Sea vs. Vertical Axis

    Evaluating Extension in the Ross Sea vs. Vertical Axis Rotation in West Antarctica as the Cause of the Offset of West and East Antarctic ca. 100 Ma Paleomagnetic Poles

  • Extension of Antarctic ozone hole to lower latitudes in

     · Vol. 135, 1991 Extension of Antarctic Ozone Hole 613 values for South Pole (Amundsen-Scott Base). The dashed curve immediately below shows Syowa values for October only. The following may be noted (1) There is a large month-to-month change, in the range of D.U. However, the maxima seem to occur in November or December and the minima in

  • Recent extension driven by mantle upwelling beneath

    [1] Northern Victoria Land is located at the boundary between an extended, presumably hot, region (West Antarctic Rift System) and the thick, possibly cold, East Antarctic craton. The style and timing of Tertiary deformation along with relationships with the magmatic activity are still unclear, and contrasting models have been proposed. We performed structural and morphotectonic analyses at

  • Antarctic Sea Ice Reaches New Record Maximum NASA

     · Editor’s note Antarctica and the Arctic are two very different environments the former is a continent surrounded by ocean, the latter is ocean enclosed by land. As a result, sea ice behaves very differently in the two regions. While the Antarctic sea ice yearly wintertime maximum extent hit record highs from 2012 to 2014 before returning to average levels in 2015, both the Arctic

  • Cenozoic motion between East and West Antarctica Nature

     · The West Antarctic rift system is the result of late Mesozoic and Cenozoic extension between East and West Antarctica, and represents one of the largest active continental rift systems on Earth.

  • (PDF) Cretaceous and Tertiary extension throughout the

    Antarctica. Extension in the rift is believed to have . occurred in two main episodes in the Cretaceous and in the . Cenozoic(Davey and Brancolini, 1995). Cenozoic extension .

  • Magmatism of the Weddell Sea rift system in Antarctica

     · Two separate episodes of Weddell Sea extension and magmatism have been identified by several authors (e.g. König and Jokat, 2006 Jordan et al., 2017) an early stage east-west rifting episode potentially linked to back-arc extension and a later stage north-south rifting episode associated with the separation of Antarctica and Africa.

  • The Geology of AntarcticaUNESCO

     · and West Antarctica reflects a marked set of geological distinctions. The major geological units and features of East Antarctica largely formed and developed in the Precambrian or Palaeozoic to early Mesozoic (largely pre-170 Ma). In contrast, West Antarctica is dominated by a Mesozoic and Cenozoic geological evolution related to the

  • Recent extension driven by mantle upwelling beneath the

     · Recent extension driven by mantle upwelling beneath the Admiralty Mountains (East Antarctica) Claudio Faccenna,1 Federico Rossetti,1 Thorsten W. Becker,2 Stefania Danesi,3 and Andrea Morelli3 Received 10 August 2007 revised 4 April 2008 accepted 17

  • Antarctic temperature variability and change from station

     · Variability and change in near-surface air temperature at 17 Antarctic stations is examined using data from the SCAR READER database. We consider the relationships between temperature, and atmospheric circulation, sea ice concentration and forcing by the tropical oceans.

  • The transition from diffuse to focused extension

    Two distinct stages of extension are recognized in the West Antarctic Rift system (WARS). During the first stage, beginning in the Late Cretaceous, extension was broadly distributed throughout much of West Antarctica. A second stage of extension in the late Paleogene was focused primarily in the Victoria Land Basin, near the boundary with the East Antarctic craton. The transition to focused

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  • Cenozoic geodynamics of the Ross Sea region, Antarctica

    Cenozoic geodynamics of the Ross Sea region, Antarctica Crustal extension, intraplate strike-slip faulting, and tectonic inheritance Francesco Salvini, 1'2 Giuliano Brancolini, 3 Martina Busetti, 3 Fabrizio Storti, 4 Francesco Mazzarini, 5 and Franco Coren 3 Abstract. An integrated study of onshore and offshore geology of the Ross Sea region

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  • Cretaceous and Tertiary extension throughout the Ross

     · the West Antarctic Rift System between East and West Antarctica. Extension in the rift is believed to have occurred in two main episodes in the Cretaceous and in the Cenozoic(Davey and Brancolini, 995). Cenozoic extension can be related to sea floor spreading on the Adare spreading system located northwest of the Ross Sea.

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  • SpOT-Light Lightweight Private Set Intersection from

     · SpOT-Light Lightweight Private Set Intersection from Sparse OT Extension Benny Pinkas Mike Rosulek yNi Trieu Avishay Yanai June 2, 2019 Abstract We describe a novel approach for two-party private set intersection (PSI) with semi-honest security. Compared to existing PSI protocols, ours has a more favorable balance between communication and

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  • Flat Earth Supporters Now Plan An Antarctica Expedition To

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  • Ross Sea mylonites and the timing of

    There are few direct constraints on the timing and style of faulting in the Ross Sea sector of the West Antarctic rift system, although Cretaceous plate reconstructions indicate that Ross Sea extension between East and West Antarctica occurred prior to breakup of the Gondwana margin ca. 80 Ma. Mylonitic gneisses dredged from the eastern Ross Sea indicate shear-zone deformation considerably

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