Differential denudation and flexural isostasy in formation of rifted-margin upwarps
- 1 August 1990
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 346 (6286) , 739-742
- https://doi.org/10.1038/346739a0
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- The role of mantle plumes in the development of continental drainage patternsNature, 1989
- Flexural uplift of rift flanks due to mechanical unloading of the lithosphere during extensionJournal of Geophysical Research, 1989
- Magmatism at rift zones: The generation of volcanic continental margins and flood basaltsJournal of Geophysical Research, 1989
- The timing of uplift, volcanism, and rifting peripheral to the Red Sea: A case for passive rifting?Journal of Geophysical Research, 1989
- A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental marginsGeology, 1989
- Thermal consequences of lithospheric extension: Pure and simpleTectonics, 1988
- Formation of the "steer's head" geometry of sedimentary basins by differential stretching of the crust and mantleGeology, 1988
- Small-scale convection induced by passive rifting: the cause for uplift of rift shouldersEarth and Planetary Science Letters, 1986
- A possible mechanism for epeirogenic upliftNature, 1984
- Rifting process and thermal evolution of the continental margin of Eastern Canada determined from subsidence curvesEarth and Planetary Science Letters, 1980