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We have 29 Marine Geology PhD Projects, Programmes & Scholarships for Self-funded Students

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Marine Geology PhD Projects, Programmes & Scholarships for Self-funded Students

We have 29 Marine Geology PhD Projects, Programmes & Scholarships for Self-funded Students

Tracking ocean circulation in the Cretaceous ‘Chalk Sea’

Ocean circulation is a fundamental component of the modern climate system but may have operated very differently in the geological past, especially when palaeogeography was different, climates were much warmer and sea-levels were considerably higher. Read more

Towards a holistic understanding of carbonate mineralisation controls

Calcium-carbonates (CaCO. 3. ) are climate-controlling minerals, acting as long-term sinks in the biogeochemical carbon cycle, and playing the role of stable carbon stores in many carbon capture, utilisation and storage (CCUS) technologies. Read more

Tectonics, sea-level change, and submarine landsliding in the South Caspian Basin

This project aims to determine the tectonic and sea-level history within and at the margins of the South Caspian Basin, in Azerbaijan and Turkmenistan, and the timings of major shelf collapse within the basin interior. Read more

Fate of past submarine volcanic input to the ocean

Large Igneous Provinces (LIPs) are extremely large volumes of extrusive igneous rock, created during relatively short-lived volcanic events during the Phanerozoic, often coinciding with major environmental (e.g., Cenozoic hyperthermals and Mesozoic oceanic anoxic events or OAEs) and biotic change (e.g., mass extinctions). Read more

Re-evaluating BOEM's Guidelines for Identifying Submerged Pre-Contact Archaeological Sites in the Gulf of Mexico: an Extensive Geoarchaeological Approach

  Research Group: Archaeological and Forensic Sciences
The Submerged Landscapes Research Centre at the University of Bradford is recruiting a talented, enthusiastic, and motivated PhD candidate to undertake research on the submerged archaeological landscapes of the Gulf of Mexico, U.S.A. Read more

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