Finite element analysis of Transantarctic Mountain uplift and coeval subsidence in the Ross Embayment
- 1 January 1992
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 201 (3-4) , 341-356
- https://doi.org/10.1016/0040-1951(92)90241-w
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Earthquakes in continental AntarcticaPublished by Elsevier ,2003
- Formation of sedimentary basins of graben type by extension of the continental crustPublished by Elsevier ,2003
- Stress distribution and plate boundary force associated with collision mountain rangesTectonophysics, 1990
- Plate boundary forces at subduction zones and trench-arc compressionTectonophysics, 1989
- A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental marginsGeology, 1989
- Antarctic earthquakesNature, 1988
- Small-scale convection induced by passive rifting: the cause for uplift of rift shouldersEarth and Planetary Science Letters, 1986
- Episodic Rifting of Phanerozoic Rocks in the Victoria Land Basin, Western Ross Sea, AntarcticaScience, 1985
- Isostasy and the ambient state of stress in the oceanic lithosphereJournal of Geophysical Research, 1981
- Gravity measurements in East AfricaPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1936