Mercury enrichments of the Pyrenean foreland basins sediments support enhanced volcanism during the Paleocene-Eocene thermal maximum (PETM)

Author:

Tremblin Maxime,Khozyem Hassan,Adatte Thierry,Spangenberg Jorge E.,Fillon Charlotte,Grauls Arnaud,Hunger Teodoro,Nowak Andres,Läuchli Charlotte,Lasseur Eric,Roig Jean-Yves,Serrano Olivier,Calassou Sylvain,Guillocheau François,Castelltort Sébastien

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference159 articles.

1. How contact metamorphism can trigger global climate changes: modeling gas generation around igneous sills in sedimentary basins;Aarnes;Geochim. Cosmochim. Acta,2010

2. Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene Thermal Maximum;Aarnes;J. Geol. Soc. Lond.,2015

3. Pre-breakup magmatism on the Vøring margin: Insight from new sub-basalt imaging and results from Ocean Drilling Program Hole 642E;Abdelmalak;Tectonophysics,2016

4. Breakup volcanism and plate tectonics in the NW Atlantic;Abdelmalak;Tectonophysics,2019

5. Lithostratigraphic and mineralogic correlations of near K/T boundary clastic sediments in northeastern Mexico: implications for origin and nature of deposition;Adatte,1996

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