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Inbook Reference De geologische kaart van België - La carte géologique de Belgique
Located in Library / RBINS Staff Publications 2022
Inbook Reference Verschillen tussen "museumgeologen" en "vrije geologen" - Différences entre les "géologues de musée" et les "géologues libres"
Located in Library / RBINS Staff Publications 2022
Inbook Reference Informatisering - Informatisation
Located in Library / RBINS Staff Publications 2022
Inbook Reference Een dak boven het hoofd voor de BGD - Un toit pour le SGB
Located in Library / RBINS Staff Publications 2022
Inbook Reference Enkele opmerkelijke personen - Quelques personnes remarquables
Located in Library / RBINS Staff Publications 2022
Inbook Reference Gender- en taaldiversiteit aan de BGD: een geschiedenis van vooruitgang - La diversité linguistique et de genre au SGB: une histoire de progrès
Located in Library / RBINS Staff Publications 2022
Inbook Reference Sint-Barbara - Sainte Barbe
Located in Library / RBINS Staff Publications 2022
Inbook Reference Comfort op kantoor: temperatuur in tijden van energieschaarste - Le confort au bureau : la température en période de pénurie d'énergie
Located in Library / RBINS Staff Publications 2022
Article Reference Three new species of Rhaphium Meigen, 1803 from mangroves in Hong Kong (Diptera: Dolichopodidae: Rhaphiinae)
Located in Library / No RBINS Staff publications
Article Reference Unfolding veined fold limbs to deduce a basin’s prefolding stress state
Tectonic structures that developed prior to folding, such as pre- and early-kinematic veins, hold valuable information on the stress state of the paleobasin in which these early structures formed. To derive the parental orientation of these prefolding brittle structures, folds need to be ‘unfold’. A fold restoration methodology is presented in which fold limbs, and structures they contain, are rotated back to their depositional horizontal position by removing the tilt of the fold hinge line and the dip of individual fold limbs. The method is applied on quartz veins emplaced in folded Lower Devonian sandstones from the High-Ardenne slate belt (Belgium, Germany) and allowed deducing NW-SE opening when the Ardenne-Eifel Basin was at maximum burial depth (early Carboniferous). This exercise can be used in structural geology classes to teach how to rotate data using stereonet techniques hereby encouraging students in applying an unfolding strategy to derive information from prefolding structures.
Located in Library / RBINS Staff Publications 2018