Cenozoic range‐front faulting and development of the Transantarctic Mountains near Cape Surprise, Antarctica: thermochronologic and geomorphologic constraints
The Transantarctic Mountains (TAM) define the western flank of the West Antarctic rift
system. Cape Surprise, near the Shackleton Glacier in the central TAM, is the only location …
system. Cape Surprise, near the Shackleton Glacier in the central TAM, is the only location …
Structure and timing of transpressional deformation in the Shackleton Glacier area, Ross orogen, Antarctica
TS Paulsen, J Encarnación… - Journal of the …, 2004 - pubs.geoscienceworld.org
Abstract Basement of the Transantarctic Mountains comprises the Ross orogenic belt, a
Neoproterozoic to Ordovician mobile belt located along the palaeo-Pacific margin of …
Neoproterozoic to Ordovician mobile belt located along the palaeo-Pacific margin of …
[HTML][HTML] Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana …
Changes in magmatism and sedimentation along the late Neoproterozoic-early Paleozoic
Ross orogenic belt in Antarctica have been linked to the cessation of convergence along the …
Ross orogenic belt in Antarctica have been linked to the cessation of convergence along the …