Carbonate dissolution by euendolithe cyanobacterium
Bioerosion is the process of destruction of rocks by living organisms. The bioerosion of biogenic carbonates by so-called "euendolithic" cyanobacteria (which live in rocks) is a major but poorly quantified process, causing, among other things, the disintegration of coral reefs. Euendolitic ...
Raman spectrometry on Carbonaceous Material (RSCM) thermometry - Aiguilles Rouges massif
RSCM analyses on metamorphic rocks from the Servoz syncline.
Geochemical data - Aiguilles Rouges - Mont-Blanc massifs
Contents of major and trace elements and of Rare Earth elements from whole rocks and minerals.
Geochronological data - Aiguilles Rouges - Mont-Blanc massifs
LA-ICPMS U-Th-Pb analyses on zircon and monazite from the Aiguilles Rouges - Mont-Blanc massifs.
Geochronological data - Agly massif
LA-ICPMS U-Th-Pb analyses on zircon and monazite from the Agly massif.
Physicochemical and bacteriological characteristics of water - Arcier watershed - 2020-2022
Physical characteristics, major ions, minor ions, trace elements measured from May 2020 to February 2022 in five sites of the Arcier karst watershed (Doubs, France), as well as at the Arcier spring. These measurements were complemented by the acquisition of extended spectrum beta-lactamase ...
Pressure-Temperature quantification of continental crustal hydration - Colorado Plateau
Data acquired in collaboration with the University of Boulder in Colorado (U.S.A.) for the understanding of the Colorado Plateau elevation. These data sets include mineralogical, petrological, chemical, pressure-temperature modelisation and density evolution.
Suretta nappe shear zones
The database "Suretta nappe shear zones" contains petrological, structural and microtextural data of millimetre-scale shear zones from the Roffna rhyolite (Suretta nappe, Eastern Alps, Switzerland). The data consist of structural orientations, optical and electronic images of the mineralogy of the ...
Clay mineralogical and geochemical expressions of the "Late Campanian Event" in the Aquitaine and Paris basins (France): Palaeoenvironmental implications
Campanian sediments from two French sedimentary basins were studied, using clay mineralogy and stable isotope (δ13C and δ18O) geochemistry, in order to investigate the Late Campanian Event. The clay fraction of the Campanian sediments from the Tercis-les-Bains section (Aquitaine Basin) and from the ...
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