Sökning: "IODP"
Visar resultat 1 - 5 av 7 uppsatser innehållade ordet IODP.
1. Anisotropy of Magnetic Susceptibility and Remanent Magnetization studies in sediments from the Ångermanälven River estuary (IODP Expedition 347, site M0061)
Magister-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : .... LÄS MER
2. Cell Size Variation in Fossil Coccolithophores (Haptophyta) : A Study of Pliocene Sediments from Northwestern Australia
Kandidat-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : This report examines the size variations of fossil carbonate-producing haptophyte microalgae, coccolithophores, using sediments deposited during the Pliocene. The sediments were collected by the International Ocean Discovery Program (IODP) in 2015, off the coast of NW Australia (Gallagher et al., 2017). LÄS MER
3. Magmatic Sources and Processes Recorded by the Volcanics from the Izu Bonin Rear Arc
Master-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : The Izu rear-arc volcanism was investigated by IODP EXP350 in spring 2014. A total stratigraphy of1800 m was drilled, and contains volcaniclastic material within tuffaceous mudstone. LÄS MER
4. Size and Abundance of Late Pleistocene Reticulofenestrid Coccoliths from the Eastern Indian Ocean in Relation to Temperature and Aridity
Master-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : Measurements on coccolith abundance and mass can be used as a signal of primary productivity and pelagic calcification in response to environmental change. The Leeuwin Current (LC) is known to transport warm and low-salinity waters from the Indo-Pacific Warm Pool (IPWP) southwards along the coast of West Australia. LÄS MER
5. Cenozoic history of North Atlantic deep sea carbonate preservation
Kandidat-uppsats, Stockholms universitet/Institutionen för geologiska vetenskaperSammanfattning : Carbonate preservation in the oceans occurs at a depth called the carbonate compensation depth (CCD). The CCD is where the input rate of carbonate from the surface of the ocean is balanced by the dissolution rate. LÄS MER