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Tectonic evolution of the Transantarctic Mountains information


The tectonic evolution of the Transantarctic Mountains appears to have begun when Antarctica broke away from Australia during the late Cretaceous and is ongoing, creating along the way some of the longest mountain ranges (at 3500 kilometers) formed by rift flank uplift and associated continental rifting.[1] The Transantarctic Mountains (TAM) separate East and West Antarctica. The rift system that formed them is caused by a reactivation of crust along the East Antarctic Craton. This rifting or seafloor spreading causes plate movement that results in a nearby convergent boundary which then forms the mountain range.[2][3] The exact processes responsible for making the Transantarctic Mountains are still debated today. This results in a large variety of proposed theories that attempt to decipher the tectonic history of these mountains.[4]

Front range of the Transantarctic Mountains
  1. ^ Cite error: The named reference arizona was invoked but never defined (see the help page).
  2. ^ Lawrence, J.F.; van Wijk, J.W.; Driscoll, N.W. (2007). "Tectonic implications for uplift of the Transantarctic Mountains" (PDF). USGS (10th International Symposium on Antarctic Earth Sciences).
  3. ^ McAdoo, David; Laxon, Seymour (April 1997). "Antarctic Tectonics: Constraints From an ERS-1 Satellite Marine Gravity Field". Science. 276 (5312): 556–560. doi:10.1126/science.276.5312.556. JSTOR 2892434. PMID 9110969.
  4. ^ Cite error: The named reference fitzgerald was invoked but never defined (see the help page).

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