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Tania Hildebrand-Habel

Researcher at University of Stavanger

Publications -  19
Citations -  401

Tania Hildebrand-Habel is an academic researcher from University of Stavanger. The author has contributed to research in topics: Genus & Dinophyceae. The author has an hindex of 9, co-authored 19 publications receiving 373 citations. Previous affiliations of Tania Hildebrand-Habel include Norwegian Petroleum Directorate & University of Oslo.

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Chemical Alterations Induced by Rock–Fluid Interactions When Injecting Brines in High Porosity Chalks

TL;DR: In this article, the results from simplified aqueous chemistry using MgCl2 brines, and compare these results with seawater, are presented, showing that the effects of magnesium seem to be governed not only by the differences in mineralogy, but also a time dependency on chalk deformation is additionally observed.
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A proposed classification of archeopyle types in calcareous dinoflagellate cysts

TL;DR: The phylogenetic significance of archeopyles in calcareous dinoflagellates cysts has been evaluated, and a classification model is developed that focuses on the archeopyle categories and types established for organic-walled din oflageLLates by Evitt (1967, 1985).
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Variations in calcareous dinoflagellate associations from the Maastrichtian to Middle Eocene of the western South Atlantic Ocean (São Paulo Plateau, DSDP Leg 39, Site 356)

TL;DR: In contrast to the stable Paleocene associations, Eocene calcareous dinoflagellates show fluctuations in relative abundances, which can possibly be attributed to redeposition related to increased seaward transport of specimens, due to strengthened western boundary currents.
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Evaluation of the compositional changes during flooding of reactive fluids using scanning electron microscopy, nano-secondary ion mass spectrometry, x-ray diffraction, and whole-rock geochemistry

TL;DR: In this article, the first centimeter of the flooded chalk sample showed an increase in MgO by approximately 100, from a weight percent of 0.33% to 33.03% and a corresponding depletion of CaO by more than 70% from 52.22 to 14.43 wt.%.