Using Mg Isotopes to Estimate Natural Calcite Compositions and Precipitation Rates During the 2010 Eyjafjallajökull Eruption

Chemical weathering of silicate rocks is a key control on the long-term climate, via drawdown of atmospheric CO2. Magnesium isotopes are increasingly being used to trace weathering, but are often complicated by several coincident fractionating processes. Here we examine Mg isotope ratios of waters s...

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Xehetasun bibliografikoak
Egile Nagusiak: Philip A. E. Pogge von Strandmann, Jonas Olsson, Tu-Han Luu, Sigurður R. Gislason, Kevin W. Burton
Formatua: Artikulua
Hizkuntza:English
Argitaratua: Frontiers Media S.A. 2019-02-01
Saila:Frontiers in Earth Science
Gaiak:
Sarrera elektronikoa:https://www.frontiersin.org/article/10.3389/feart.2019.00006/full