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Andrea Moscariello
Researcher at University of Geneva
Publications - 113
Citations - 1870
Andrea Moscariello is an academic researcher from University of Geneva. The author has contributed to research in topics: Facies & Structural basin. The author has an hindex of 22, co-authored 101 publications receiving 1555 citations. Previous affiliations of Andrea Moscariello include Delft University of Technology & Royal Dutch Shell.
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Sequence Stratigraphy in Lacustrine Basins: A Model for part of the Green River Formation (Eocene), Southwest Uinta Basin, Utah, U.S.A.
TL;DR: In this article, two types of sequence boundary are identified in the middle Green River Formation of central Nine Mile Canyon, Uinta Basin, Utah, several lacustrine-dominated intervals 10 m thick comprise aggradational carbonate parasequence sets and a progradational clastic parsequence, which exhibit a basinward shift in facies across a regionally mappable surface that is an angular or, rarely, parallel unconformity.
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Tunnel valleys: current knowledge and future perspectives
TL;DR: A review of the current knowledge of tunnel valleys can be found in this article, providing an overview of the observations around the world, as well as the wide variety of sedimentary environments found to contribute to the infilling of these features.
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Variable style of transition between Palaeogene fluvial fan and lacustrine systems, southern Pyrenean foreland, NE Spain
TL;DR: Two Palaeogene fluvial fan systems linked to the south-Pyrenean margin are recognized in the eastern Ebro Basin: the Cardona-Su´ ria and Solsona-Sanau.
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Microfacies of detrital event layers deposited in Quaternary varved lake sediments of the Piànico‐Sèllere Basin (northern Italy)
TL;DR: A Quaternary interglacial lake sediment record from the Pianico-Sellere Basin (northern Italy) consists of biochemical calcite varves with intercalated detrital layers.
Chemostratigraphy of the Upper Carboniferous Schooner Formation, southern North Sea
TL;DR: Chemostratigraphy has enabled the Schooner Formation encountered in well 44/21-3 to be divided into three chemostigraphical units (S1, S2 and S3) and eleven sub-units (S 1a-f, S 2a-b and S 3a-c), based on variations in mudstone and sandstone geochemical data acquired from core samples and cuttings as discussed by the authors.