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published "The SFZ separates tectonic plates and oceans, to the east the Scotia Plate and to the west the
Antarctic Plate (which includes the former Phoenix Plate), and to the east the Pacific Ocean and to the west the Atlantic Ocean."
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posits that: "the
Shackleton Fracture Zone could have blocked the gateway until the early Miocene. Geophysical and geochemical evidence presented here suggests that the Shackleton Fracture Zone is an oceanic transverse ridge".
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55:. It extends between 59° and 60°40' south latitude and between 56°30' and 61° west longitude and runs in a northwest to southeast direction from the South American continental shelf to the
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Map showing the proposal presented by the thesis entitled "Natural delimitation between the
Pacific and South Atlantic Oceans by the Shackleton Fracture Zone".
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oceans "could be confirmed from the so-called
Shackleton Fracture Zone (...) the boundary is then located east of the so-called Cape Horn Meridian".
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The researchers Juan
Ignacio Ipinza Mayor and Cedomir Marangunic Damianovic put forward the scientific theory that the separation of the
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Natural delimitation between the
Pacific and South Atlantic oceans by the Scotia Arc
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Roy
Livermore; Graeme Eagles; Peter Morris; Andrés Maldonado (September 2004).
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Shackleton
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In 2004 The
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and other countries postulated that the boundary between the southeastern
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This article about a specific oceanic location or ocean current is a
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Natural delimitation between the Pacific and South Atlantic oceans
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Juan Ignacio Ipinza Mayor; Cedomir Marangunic Damianovic (2021).
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This article about a regional geological feature is a
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59:. Chile claims the area as part of its
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272:. National Geographic. 8 June 2021
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567:Geology of the Southern Ocean
317:(in Spanish). March 27, 2019.
258:(in Spanish). March 27, 2019.
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23:The Shackleton Fracture Zone.
520:. You can help Knowledge by
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210:Bibcode
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
