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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Arctic Ocean
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Norwegian Sea
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Haltenbanken (1)
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-
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Atlantic Ocean
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Mid-Atlantic Ridge (1)
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North Atlantic
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English Channel (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Spain (1)
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Western Europe
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France
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Burgundy (1)
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Hauts-de-Seine France (1)
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Normandy (1)
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Oise France (1)
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Paris Basin (16)
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Paris France (17)
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Poitou (1)
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Seine (2)
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Seine River (3)
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Seine-et-Marne France (2)
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Seine-et-Oise (5)
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Seine-Maritime France
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Rouen France (1)
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Seine-Saint-Denis France (3)
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Val-de-Marne France (1)
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Val-d'Oise France (1)
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Yvelines France
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Versailles France (3)
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Scandinavia
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Norway (1)
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United Kingdom
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Great Britain
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England
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Hampshire Basin (1)
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Scotland
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Edinburgh Scotland (1)
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United States
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Alaska (1)
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commodities
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chalk deposits (1)
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construction materials
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building stone (1)
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geothermal energy (1)
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limestone deposits (1)
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oil and gas fields (1)
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petroleum (3)
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sodium sulfate (1)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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halogens
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bromine
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bromide ion (3)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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oxygen
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O-18/O-16 (1)
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fossils
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bacteria (1)
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Chordata
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Vertebrata
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Pisces (1)
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Invertebrata
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Mollusca
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Bivalvia (1)
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Cephalopoda
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Ammonoidea
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Ammonites (1)
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Nautiloidea
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Nautilus (1)
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Gastropoda
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Turritellidae
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Turritella (1)
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microfossils (3)
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palynomorphs
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Dinoflagellata (1)
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Plantae
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algae
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Chlorophyta
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Chlorophyceae
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Dasycladaceae (1)
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Coccolithophoraceae (1)
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nannofossils
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Nannoconus (1)
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Spermatophyta
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Gymnospermae
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Coniferales
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Cupressaceae (1)
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thallophytes (1)
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geochronology methods
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K/Ar (1)
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geologic age
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Cenozoic
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Quaternary (6)
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Tertiary
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Neogene
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Pliocene (2)
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Paleogene
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Eocene
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lower Eocene
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Sparnacian (2)
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middle Eocene
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Lutetian (5)
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upper Eocene
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Ludian (1)
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Ilerdian (1)
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Oligocene
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Fontainebleau Sandstone (4)
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lower Oligocene
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upper Oligocene
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Chattian (2)
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Paleocene
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upper Paleocene (1)
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Paleocene-Eocene Thermal Maximum (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Jurassic
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igneous rocks
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igneous rocks
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volcanic rocks (1)
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minerals
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carbonates
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calcite (1)
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dolomite (1)
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oxides
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silicates
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framework silicates
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silica minerals
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cristobalite (1)
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opal
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opal-CT (1)
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zeolite group
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clinoptilolite (1)
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sheet silicates
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clay minerals
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smectite (2)
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illite (2)
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serpentine group
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berthierine (1)
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-
-
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sulfates
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gypsum (1)
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Primary terms
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absolute age (1)
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Arctic Ocean
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Norwegian Sea
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Haltenbanken (1)
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Atlantic Ocean
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Mid-Atlantic Ridge (1)
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North Atlantic
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English Channel (1)
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-
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bacteria (1)
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biography (1)
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carbon
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C-13/C-12 (1)
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Cenozoic
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Quaternary (6)
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Tertiary
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Neogene
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Pliocene (2)
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-
Paleogene
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Eocene
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lower Eocene
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Sparnacian (2)
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-
middle Eocene
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Lutetian (5)
-
-
upper Eocene
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Ludian (1)
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-
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Ilerdian (1)
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Oligocene
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Fontainebleau Sandstone (4)
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lower Oligocene
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Rupelian (1)
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Sannoisian (1)
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Stampian (1)
-
-
upper Oligocene
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Chattian (2)
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-
-
Paleocene
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upper Paleocene (1)
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-
Paleocene-Eocene Thermal Maximum (1)
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-
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Chordata
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Vertebrata
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Pisces (1)
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clay mineralogy (1)
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conservation (2)
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construction materials
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building stone (1)
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crystal growth (1)
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deformation (1)
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diagenesis (4)
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epeirogeny (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Spain (1)
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Western Europe
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France
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Burgundy (1)
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Essonne France (1)
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Hauts-de-Seine France (1)
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Normandy (1)
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Oise France (1)
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Paris Basin (16)
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Paris France (17)
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Poitou (1)
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Seine (2)
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Seine River (3)
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Seine-et-Marne France (2)
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Seine-et-Oise (5)
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Seine-Maritime France
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Rouen France (1)
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Seine-Saint-Denis France (3)
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Val-de-Marne France (1)
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Val-d'Oise France (1)
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Yvelines France
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Versailles France (3)
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Scandinavia
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Norway (1)
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United Kingdom
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Great Britain
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England
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Hampshire Basin (1)
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Scotland
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Edinburgh Scotland (1)
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faults (1)
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foundations (3)
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geochemistry (2)
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geochronology (1)
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geology (1)
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geomorphology (3)
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geophysical methods (1)
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geothermal energy (1)
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ground water (2)
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hydrogeology (1)
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igneous rocks
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volcanic rocks (1)
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inclusions (1)
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Invertebrata
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Mollusca
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Bivalvia (1)
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Cephalopoda
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Ammonoidea
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Ammonites (1)
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Nautiloidea
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Nautilus (1)
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-
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Gastropoda
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Turritellidae
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Turritella (1)
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-
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isostasy (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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limestone deposits (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Wealden (1)
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Upper Cretaceous
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Campanian (1)
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Cenomanian (1)
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Turonian (1)
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-
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Jurassic
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Middle Jurassic
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Bathonian (1)
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Callovian (1)
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metasomatism (1)
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oxygen
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paleoclimatology (1)
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paleoecology (1)
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paleontology (3)
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palynomorphs
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paragenesis (1)
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petroleum (3)
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petrology (2)
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Plantae
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algae
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Chlorophyta
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Chlorophyceae
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Dasycladaceae (1)
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-
-
Coccolithophoraceae (1)
-
nannofossils
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Nannoconus (1)
-
-
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Spermatophyta
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Gymnospermae
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Coniferales
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Cupressaceae (1)
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pollution (4)
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rock mechanics (2)
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clastic rocks
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slope stability (3)
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sodium sulfate (1)
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waste disposal (2)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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beachrock (1)
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chalk (3)
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limestone
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oolitic limestone (1)
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clastic rocks
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marl (1)
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sandstone (6)
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coal (1)
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sediments
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oolite (1)
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sediments
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clastic sediments
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alluvium (1)
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loess (1)
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sand (4)
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silt (1)
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soils
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paleosols (1)
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soils
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Cambisols (1)
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Clay soils (1)
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-
Authigenic berthierine and incipient chloritization in shallowly buried sandstone reservoirs: Key role of the source-to-sink context
New insights on the Late Paleocene − Early Eocene dinoflagellate cyst zonation for the Paris and Dieppe basins
THE FRENCH FOUNDATIONS OF HUTTON’S THEORY OF THE EARTH , PART ONE: HUTTON AS A STUDENT OF GUILLAUME-FRANÇOIS ROUELLE
Exhibiting life history at the Paris Muséum d’Histoire Naturelle (nineteenth–twenty-first centuries)
ABSTRACT The notion of a history of life has been the subject of extensive debates in France, from the turn of the nineteenth century to the dawn of the twentieth century and beyond. In this paper, I analyze how the organization of buildings and collections within the Paris National Museum of Natural History (MNHN), and their successive transformations up to the present, have reflected concepts and controversies over this history. After a brief overview of the constitution of the Museum, this chapter studies the organization of the Museum’s paleontological, zoological, and comparative anatomy collections, and the devices through which scientific ideas and debates about evolution have been displayed and presented to the public. This paper will focus more particularly on the settings of three major collections of zoological specimens: (1) Georges Cuvier’s “Museum of Comparative Anatomy,” which was opened to the public in 1806; (2) the Palaeontology and Comparative Anatomy Gallery, which was founded by Albert Gaudry in 1898; and (3) the Great Gallery of Evolution, which was inaugurated in 1994. I will argue that organizing these exhibits involved theoretical choices, taxonomic methods, scientific practices and rhetoric of displays, as well as ideological choices that connected natural history to its intellectual and sociopolitical background. Through the examination of these different settings over a period of more than two centuries and their present use, I will question today’s choices of the Paris Museum regarding the meaning and roles of these galleries, involving patrimonial conservation, public entertainment, and diffusion of scientific knowledge in the public.
New regulatory tool for the conservation of the geological heritage in France: the Prefectural Decree of the Protection of the Geotope (APPG). Application and feedback in the Yvelines department (Paris basin, Île-de-France)
Age of the Fontainebleau sandstones: a tectonic point of view
Comparison between petrophysical properties, durability and use of two limestones of the Paris region
Abstract Most buildings of architectural heritage in Paris and its surroundings are built with Lutetian limestone. Several historic buildings of the ‘Vexin Normand’ region show Lutetian limestone in the upper parts of their walls, while the lower parts are built with a chalk known as ‘Pierre de Vernon’. The ‘Pierre de Vernon’ appears up to the first metre, although in exceptional cases it can reach the middle height of a building. Commonly, chalks exhibit low durability due to their high porosity. However, ‘Pierre de Vernon’ is supposed to have greater durability than other chalks because of its historic use for basement construction. The objective of this research was to understand the use of the ‘Pierre de Vernon’ in the lower part of the constructions. A petrophysical characterization of Vernon chalk and Lutetian limestone was carried out, focusing mainly on the differences in porosity and water uptake. Salt crystallization tests were done to contrast their response to decay. Colour and roughness measurements and scanning electron microscope observations were performed. Results show that the different porous networks of these two limestones lead to a high contrast in their hydric properties and responses to decay, and the use of Vernon chalk in the lower sections of buildings has been found to be appropriate.