Date of Award
Master of Science
Geological and Environmental Sciences
Dr. Michelle A. Kominz
Dr. Mohamed Sultan
Dr. David Barnes
Masters Thesis-Open Access
Continental crust extension is a precursor to the formation of a new ocean. The overall crustal extension causes change in the volume of global oceans hence change in sea level. The break-up of Gondwana that began during Late Triassic to Early Jurassic time caused continental crustal extension prior to forming the Indian Ocean. Extension started 184 Ma with rifting between SE Africa, Madagascar and Antarctica. This was followed by rifting between Greater India, Australia and Antarctica beginning about 160 Ma. The most recent episode of extension occurred 34 Ma involving separation between Arabia and Horn of Africa. Gridded data sets including the age of oceanic crust, the current thickness of oceanic sediment and water depth coupled with a compilation of deep sea sediment porosity from Ocean Drilling Project data allows us to quantitatively determine the change in volume of the ocean displaced by extension of continental crust and its impact on global sea level. Analysis of this data is divided into Spatial analysis and Tectonic subsidence analysis. A large amount of extension is observed in Australia, NE Antarctica, South Africa and India; We also see a small amount of extension in East Africa, the Horn of Africa, Arabia, and North and NW Antarctica. Our results from the margin of the Indian Ocean demonstrate that continental extension (0-184 Ma) generated a 6.3 m rise in global sea level, of which 5.9 m occurred between 184 Ma and 90 Ma.
Mwakanyamale, Kisa, "Estimating Sea Level Due to Crustal Stretching in the Margin of the Indian Ocean" (2007). Master's Theses. 4409.