Ongoing research: Deep hydrothermal systems
The circulation of seawater through the newly formed seafloor at mid-ocean ridges plays a pivotal role in advecting away the heat released through the formation of the seafloor and allowing it to cool, this process manifest spectacularly at the seafloor through black smoker hydrothermal vents. Hydrothermal circulation is preserved in the rock record by the presence of secondary minerals formed by fluid/rock reaction, the distribution and abundance of these secondary minerals provides insights into the temperature, magnitude and pathways of the circulating fluids. Previous studies using samples from the modern ocean basins indicate that the hydrothermal system must extend deep into the ocean crust in order to cool the ocean crust (). One of the key questions that the Oman Drilling Project drill cores will help address is 'what is the role of deep hydrothermal circulation in cooling the lower oceanic crust?' and is a focus on the ongoing research at the ¶¶Òõ¶ÌÊÓÆµ by Dr Michelle Harris and PhD student Marta Grabowska.
Further information about the Oman drilling project can be found on the project websites: