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Médard Thiry

Researcher at PSL Research University

Publications -  80
Citations -  1811

Médard Thiry is an academic researcher from PSL Research University. The author has contributed to research in topics: Sedimentary rock & Massif. The author has an hindex of 20, co-authored 78 publications receiving 1652 citations. Previous affiliations of Médard Thiry include ParisTech & Mines ParisTech.

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Palaeoclimatic interprétation of clay minerals in marine deposits : an outlook from the continental origin.

TL;DR: In this article, a review of the influence of climate on marine clays in the sedimentary record is presented, focusing mainly on the continental origin of the clay minerals and showing the difficulties of retrospective analysis of the impact of climate change on common marine deposits.
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Mineralogical forms of silica and their sequence of formation in silcretes

TL;DR: The paragenesis and the sequence of formation of silica polymorphs have been studied in three examples of silicification in the regolith of the Paris Basin and the Central Massif of France as mentioned in this paper.
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Global δ13C changes across the Paleocene-Eocene boundary: criteria for terrestrial-marine correlations

TL;DR: The early Cenozoic marine carbon isotopic record is marked by a long-term shift from high δ13C values in the late Paleocene to values that are 2 to 3 lower in the early Eocene.
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Assessing the fate of antibiotic contaminants in metal contaminated soils four years after cessation of long-term waste water irrigation

TL;DR: It is suggested that antibiotics may represent a durable contamination of soils, and risks for groundwater contamination, depending on the physicochemical characteristics both of the organic molecules and of soil constituents.
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Interpretation of palaeoweathering features and successive silicifications in the Tertiary regolith of inland Australia

TL;DR: A detailed study of morphological, micromorphological and geochemical characteristics of silcretes in the deep bleached and weathered regolith across a large area of inland Australia have provided a new interpretation of the history of the regolith and its climatic and morphological evolution during the Tertiary as mentioned in this paper.