Tectonics of the triple junction at the southern end of the Shackleton Fracture Zone (Antarctic Peninsula) |
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Authors: | F. Aldaya A. Maldonado |
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Affiliation: | (1) Departamento de Geodinámica, Universidad de Granada, Facultad de Ciencias, 18002 Granada, Spain;(2) Instituto Andaluz de Ciencias de la Tierra, C.S.I.C./Universidad de Granada, Facultad de Ciencias, 18002 Granada, Spain |
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Abstract: | The southern end of the Shackleton Fracture Zone is subducted below the South Shetland forearc, while the basal detachment of the forearc continues eastward of the Shackleton ridge as a thrust fault. The western boundary between the Antarctic/Scotia plates is located at the eastern margin of the Shackleton ridge, where an elongated depositional basin and a morphological trough delineates the contact. The boundary of the Antarctic/Scotia plates and the South Shetland forearc form a triple junction at the intersection of the Shackleton Fracture Zone with the trench, between these two plates, and an independent South Shetland block. |
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