Magnesium isotope ratios of pore-fluids and dolomites

Magnesium concentrations in deep-sea sediment pore-fluids typically decrease down core due to net precipitation of dolomite or clay minerals in the sediments or underlying crust. To better characterize and differentiate these processes, we have measured magnesium isotopes in pore-fluids and sediment...

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Bibliographic Details
Main Authors: Higgins, J A, Schrag, Daniel P
Format: Dataset
Language:English
Published: PANGAEA 2010
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.783095
https://doi.org/10.1594/PANGAEA.783095