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Booklet Reference Zeezoogdieren in Belgïe in 2014 [Marine mammals in Belgium in 2014]
Located in Library / RBINS Staff Publications 2016
Article Reference Drapetis bruscellensis (Diptera: Hybotidae) a new species for science from the outskirts of Brussels, a not so cryptic species supported by COI barcoding
Located in Library / RBINS Staff Publications 2016
Article Reference A revision of the Thyropygus allevatus group. Part V: Nine new species of the extended opinatus subgroup, based on morphological and DNA sequence data (Diplopoda: Spirostreptida: Harpagophoridae)
Located in Library / RBINS Staff Publications 2016
Article Reference Description d'une nouvelle espèce de lobobunaea Packard, 1901 (Lepidoptera)
Located in Library / RBINS Staff Publications 2016
Article Reference Two new Nogodinidae from Vietnam in the genera orthophana Melichar, 1923 and Goniopsarite's Meng, Wang & Wang, 2014 (Hemiptera: Fulgoromorpha: Nogodinidae)
Located in Library / RBINS Staff Publications 2016
Inproceedings Reference Reservoir capacity assessment and ranking of potential targets for geological storage of CO2 in Austria
Located in Library / RBINS Staff Publications 2016
Inproceedings Reference CO2-enhanced oil recovery in the North Sea region and its importance for Belgium
Located in Library / RBINS Staff Publications 2016
Inproceedings Reference Measuring the amount of CO2 in oversaturated waters by mass balance: an overview of trials and errors
Located in Library / RBINS Staff Publications 2016
Inproceedings Reference Board games as scientific communication tools for black-box methodologies: the principles of the geo-techno-economic PSS III simulator translated into an interactive educational game
Located in Library / RBINS Staff Publications 2016
Article Reference Genesis of the vein-type tungsten mineralization at Nyakabingo (Rwanda) in the Karagwe–Ankole belt, Central Africa
The vein-type tungsten deposit at Nyakabingo in the central Tungsten belt of Rwanda is located in the eastern flank of the complex Bumbogo anticlinal structure. The host rock is composed of alternating sequences of sandstones, quartzites, and black pyritiferous metapelitic rocks. Two types of W-mineralized quartz veins have been observed: bedding-parallel and quartz veins that are at high angle to the bedding, which are termed crosscutting veins. Both vein types have been interpreted to have been formed in a late stage of a compressional deformation event. Both vein types are associated with small alteration zones, comprising silicification, tourmalinization, and muscovitization. Dating of muscovite crystals at the border of the veins resulted in a maximum age of 992.4 ± 1.5 Ma. This age is within error similar to the ages obtained for the specialized G4 granites (i.e., 986 ± 10 Ma). The W-bearing minerals formed during two different phases. The first phase is characterized by scheelite and massive wolframite, while the second phase is formed by ferberite pseudomorphs after scheelite. These minerals occur late in the evolution of the massive quartz veins, sometimes even in fractures that crosscut the veins. The ore minerals precipitated from a H2O–CO2–CH4–N2–NaCl–(KCl) fluid with low to moderate salinity (0.6–13.8 eq. wt% NaCl), and minimal trapping temperatures between 247 and 344 °C. The quartz veins have been crosscut by sulfide-rich veins. Based on the similar setting, mineralogy, stable isotope, and fluid composition, it is considered that both types of W-mineralized quartz veins formed during the same mineralizing event. Given the overlap in age between the G4 granites and the mineralized quartz veins, and the typical association of the W deposits in Rwanda, but also worldwide, with granite intrusions, W originated from the geochemically specialized G4 granites. Intense water–rock interaction and mixing with metamorphic fluids largely overprinted the original magmatic-hydrothermal signature.
Located in Library / RBINS Staff Publications 2016