CORDIS Project
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This project investigates the alteration processes of ocean crust, focusing on molybdenum as a tracer to understand chemical changes during high-temperature and low-temperature alterations. By studying specific oceanic crust sections, it aims to clarify how these processes affect the isotopic signals of molybdenum in t…
Alteration of ocean crust is a fundamental on-going geological process.
High-temperature alteration of the ocean crust occurs at the ridge, while diffusive, low temperature alteration is present off-ridge.
Both alteration processes produce secondary minerals and change the primary chemical and isotopic signal of the oceanic crust.
These signals can be brought into the mantle as altered oceanic crust enters a subduction zone and produces mantle inhomogeneities.
As molybdenum is low in abundance i…
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