References of "Da Silva, Anne-Christine"
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See detailMagnetic susceptibility evolution on Paleozoic sedimentary settings, a clue for past paleoenvironments
Da Silva, Anne-Christine ULg; Pas, Damien ULg; Mabille, Cédric et al

in Suttner; Kido; Piller (Eds.) et al Mid Paleozoic climate and biodiversity. IGCP-596 opening meeting. Abstract Volume (2011)

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See detailSedimentology of a continuous Givetian-Frasnian carbonate succession in Sauerland (Germany) and MS comparison with the time-equivalent ones of Ardennes (Belgium) and Moravia (Czech Republic).
Pas, Damien ULg; Da Silva, Anne-Christine ULg; Boulvain, Frédéric ULg et al

in Suttner, Thomas; Kido, Erika; Piller, W. E. (Eds.) et al IGCP-596 Mid-Paleozoic climate and biodiversity, 19-24 septembre, Graz, Austria, Abstract book (2011)

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See detailSedimentology of a mid-late Ordovician carbonate mud-mound complex from the Katmandu Nappe in Central Nepal.
Pas, Damien ULg; Da Silva, Anne-Christine ULg; Raj Dhital, M. et al

in 13ème congrès Français de Sédimentologie, Dijon. Livre des résumés, 2011, Publ. ASF, Paris, n°68, p270-271. (2011)

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See detailSedimentary and diagenetic processes related to mid-Paleocene exposure surface, effects on the carbonate reservoir properties: Southeastern Pyrenean carbonate platform, Spain
Loisy, Corinne; Cerepi, Adrian; Da Silva, Anne-Christine ULg et al

in 13ème congrès Français de Sédimentologie, Dijon. Livre des résumés, 2011 (2011)

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See detailMagnetic susceptibility evolution in the Eifelian-Givetian Baileux section (Baileux section): complex origin of the magnetic susceptibility signal
Da Silva, Anne-Christine ULg; Dekkers, Mark; Mabille, Cédric et al

in Koptikova, Leona; Hladil, Jindrich; Adamovic, Jiri (Eds.) Miroslav Krs conference: time, magnetism, records, systems and solution. The 2011 Annual IGCP-580 Meeting. Abstract volume (2011)

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See detailPrecessional and half-precessional climate forcing of Mid-Devonian monsoon-like dynamics
De Vleeschouwer, David; Da Silva, Anne-Christine ULg; Boulvain, Frédéric ULg et al

in Suttner; Kido; Piller (Eds.) et al Mid Paleozoic climate and biodiversity. IGCP-596 opening meeting. Abstract Volume (2011)

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See detailSedimentology and magnetic susceptibility of Mobarak Formation (Lower Carboniferous in central and eastern Albroz Mountains, North of Iran)
sardar Abadi, Mehrdad; Da Silva, Anne-Christine ULg; Boulvain, Frédéric ULg et al

in Koptikova, Leona; Hladil, Jindrich; Adamovic, Jiri (Eds.) Miroslav Krs conference: time, magnetism, records, systems and solution. The 2011 Annual IGCP-580 Meeting. Abstract Volume (2011)

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See detailSedimentology and magnetic susceptibility on a continuous Middle Givetian to Lower Famennian fore-reef succession (Sauerland, Germany): a new example of MS study for long-distance correlations (Germany, Belgium, and Moravia)
Pas, Damien ULg; Da Silva, Anne-Christine ULg; Boulvain, Frédéric ULg et al

in Koptikova, Leona; Hladil, Jindrich; Adamovic, Jiri (Eds.) Miroslav Krs conference: time, magnetism, records, systems and solution. The 2011 Annual IGCP-580 Meeting. Abstract Volume (2011)

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See detailPreliminary study of MS-facies relationship in Bajocian-Bathonian carbonates from eastern and north-eastern Paris Basin
Dechamps, Sylvain; Boulvain, Frédéric ULg; Da Silva, Anne-Christine ULg

in Koptikova, Leona; Hladil, Jindrich; Adamovic, Jiri (Eds.) Miroslav Krs conference: time, magnetism, records, systems and solution. The 2011 Annual IGCP-580 Meeting. Abstract Volume (2011)

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See detailSedimentology and magnetic susceptibility on a continuous Lower Givetian to Lower Famennian fore-reef succession (Sauerland, Germany) : A new example which reinforce the use of MS for long-distance correlations (Germany, Belgium and Moravia).
Pas, Damien ULg; Da Silva, Anne-Christine ULg; Boulvain, Frédéric ULg et al

Poster (2011)

This study focuses on the continuous Givetian-Frasnian section of the abandoned Burgberg quarry (Messinghausen Anticline, northern margin of the Rhenish Mountains). The exposed section (102 m thick ... [more ▼]

This study focuses on the continuous Givetian-Frasnian section of the abandoned Burgberg quarry (Messinghausen Anticline, northern margin of the Rhenish Mountains). The exposed section (102 m thick) covers a well constraint stratigraphic interval starting at the base of the Givetian (Stritzke 1991;Aboussalam et al., 2003) and according to Stritzke (1991) and our new datations ending within the Lower Famennian. The Middle-Upper Devonian shelf-edge within the Rheinisches Schiefergebirge can be traced from the supposed position along the southern rim of the Dinant Syncline and the Eifel Synclines, northwards along a line connecting the southern margin of the Devonian reefal outcrops of Attendorn and Brilon (Krebs 1967, 1974). The depositional setting of the investigated section corresponds to complex slope and basinal environments where reworked material from the proximal Brilon platform (located to the north) and basin deposits coexist. Thus, this section allows to follow the evolution of the Givetian-Frasnian Brilon platform (e.g., Machel 1990; Stritze 1990, 1991) in a deeper setting. Petrographic analysis of more than 330 thin-sections leads to the identification of 7 microfacies which are integrated into a palaeoenvironmental model. Microfacies curve evolution shows two main trends. A shallowing upward trend ending within a typical proximal slope setting (dismantling of the platform) followed by a deepening upward trend which is characterized by several meter of pelagic mudstone within the upper part of the studied section. Magnetic susceptibility variations in sedimentary rocks, have commonly been interpreted as related to variations of detritic inputs through climatic or sea level changes (Crick et al., 1994). The magnetic susceptibility (MS) study of more than 330 samples from this long-time fore-reef carbonated succession is an opportunity to better constraint our sedimentological interpretations. To do so, we propose a comparison between general MS trends and some parameters such as microfacies and relative sea level fluctuations interpreted on the basis of the sedimentological study. The relatively long stratigraphic interval covered by the Burgberg section offers a good opportunity to compare our data with the time equivalent Devonian sections of the Ardennes (Belgium) and Moravian karst area (Czech Republic) (Boulvain et al., 2010). And thus to test the magnetic susceptibility tool for long-distance correlation between stratigraphically well constraint sections. [less ▲]

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See detailField trip 1: Givetian and Frasnian of Southern Belgium
Boulvain, Frédéric ULg; Coen-Aubert, Marie; Da Silva, Anne-Christine ULg et al

in Kölner Forum für Geologie und Paläontologie (2011), 20

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See detailStructural and environmental influence on the Causses dolomitized body (south-east France) and reservoir properties
Da Silva, Anne-Christine ULg; Cerepi, Adrian; Loisy, Corinne et al

in 14th Bathurst meeting, Bristol University, Abstract book (2011)

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See detailFrom shallow water to deep mound - sedimentology and stromatoporoids paleoecology from the Frasnian (Upper Devonian) of Belgium
Da Silva, Anne-Christine ULg; Kershaw, Stephen; Boulvain, Frédéric ULg

in Kölner Forum für Geologie und Paläontologie (2011), 19

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See detailLong-expected! - First record of demosponge-type spicules in a Devonian stromatoporoid (Frasnian, Belgium).
Da Silva, Anne-Christine ULg; Kershaw, Stephen; Boulvain, Frédéric ULg et al

in Kölner Forum für Geologie und Paläontologie (2011), 19

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See detailMixed Middle Jurassic sedimentation from North East of Iran: sedimentological model and carbonate production versus detrital inputs influence
Sardar Abadi, Mehrdad; Da Silva, Anne-Christine ULg; Zamanzadeh

in 14th Bathurst meeting, Bristol University, Abstract Book (2011)

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See detailApplication of magnetic susceptibility on different carbonate platforms
Da Silva, Anne-Christine ULg

Scientific conference (2010, December 13)

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See detailDetailed sedimentological study and magnetic susceptibility of and Eifelian mixed ramp-related system in the Eifel area
Pas, Damien ULg; Mabille, Cédric; Aretz, Markus et al

in Geologica Belgica (2010, December), 13(4),

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