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Rudy Swennen

Researcher at Katholieke Universiteit Leuven

Publications -  7
Citations -  271

Rudy Swennen is an academic researcher from Katholieke Universiteit Leuven. The author has contributed to research in topics: Dolomite & Dolomitization. The author has an hindex of 6, co-authored 7 publications receiving 234 citations.

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Hyperspectral image analysis of different carbonate lithologies (limestone, karst and hydrothermal dolomites): the Pozalagua Quarry case study (Cantabria, North-west Spain)

TL;DR: In this paper, ground-based hyperspectral imaging combined with terrestrial lidar scanning is applied to Early and Late Albian carbonates of the Pozalagua Quarry (Cantabrian Mountains, Spain).
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Zinc speciation in mining and smelter contaminated overbank sediments by EXAFS spectroscopy

TL;DR: In this paper, powder Zn K-edge EXAFS spectroscopy was used to identify three main Zn species: Smithsonite (ZnCO3), tetrahedrally coordinated sorbed Zn (sorbed IVZn) and Zn-containing trioctahedral phyllosilicate.
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Reservoir characteristics of fault-controlled hydrothermal dolomite bodies: Ramales Platform case study

TL;DR: In this paper, a geo-statistical investigation of the reservoir characteristics in the Pozalagua body revealed that the HTD types (defined based on their texture) show spatial clustering controlled by the orientation of faults, joints and the platform edge.
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Multiple dolomitization events along the Pozalagua Fault (Pozalagua Quarry, Basque–Cantabrian Basin, Northern Spain)

TL;DR: The Pozalagua Quarry in the Basque-Cantabrian Basin of northern Spain exposes a unique set of fault-associated dolomites that can be studied on a decametre scale as mentioned in this paper.
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Fault-related hydrothermal dolomites in Cretaceous carbonates (Cantabria, northern Spain): Results of petrographic, geochemical and petrophysical studies

TL;DR: In this paper, the authors investigated the relationship between planar and non-planar dolomite structures and reported that the planar structures are variably reworked by subsequent alterations, which resulted in neomorphism and recrystallization, cataclastic deformation and calcite filling of dolostones.