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NARROW
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Mozambique (1)
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Zambia (1)
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Madagascar (2)
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North Africa
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Egypt
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Eastern Desert (1)
-
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Tunisia (1)
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Southern Africa
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Botswana (1)
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Lesotho (1)
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South Africa
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Murchison greenstone belt (1)
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Transvaal region (1)
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Zimbabwe (1)
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West Africa
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Nigeria (1)
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Asia
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Arabian Peninsula
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Oman (1)
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Central Asia
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Far East
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Burma (2)
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Indonesia
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Middle East
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Turkey
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Atlantic Ocean
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North Atlantic
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North Sea
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South Atlantic
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Australasia
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Australia
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Ukraine
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Europe
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Alps
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Central Europe
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Germany
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Hungary
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Inn Valley (1)
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Molasse Basin
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North Austrian Molasse (4)
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Northern Limestone Alps (13)
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Poland
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Polish Carpathians (1)
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Slovakia (4)
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Switzerland
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Vienna Basin
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Georgian Republic
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Pannonian Basin
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Southern Europe
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Italy
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Romania
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Transylvania
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Slovenia (4)
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Tauern Window (16)
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Ukraine
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Variscides (5)
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Western Europe
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Belgium (3)
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France
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Armorican Massif (1)
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Central Massif
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Montagne Noire (1)
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Corsica (1)
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French Alps (1)
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Haute-Savoie France
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Savoy Alps (1)
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Vosges France (1)
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Maritime Alps (1)
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Netherlands (4)
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Scandinavia
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Finland (1)
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Norway (2)
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Sweden (3)
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United Kingdom
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Great Britain
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England
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Wales (3)
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Indian Ocean Islands
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Madagascar (2)
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Kura Lowland (1)
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Malay Archipelago
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Borneo (1)
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North America
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Rocky Mountains
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U. S. Rocky Mountains
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Wind River Range (1)
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North Island (1)
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Northern Hemisphere (1)
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South America
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Andes
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Eastern Cordillera (1)
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Argentina
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Paganzo Basin (1)
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Brazil (2)
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Chile (1)
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Peru (1)
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Southern Alps (1)
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United States
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Alaska (1)
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California
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Florida (1)
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Nevada
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North Carolina (2)
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Oklahoma (2)
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Oregon
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Texas (1)
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U. S. Rocky Mountains
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Wyoming
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USSR (2)
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commodities
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metal ores
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gold ores (2)
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iron ores (3)
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lead ores (3)
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lead-zinc deposits (4)
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manganese ores (1)
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tin ores (1)
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zinc ores (4)
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mineral deposits, genesis (10)
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mineral exploration (3)
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mineral resources (1)
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oil and gas fields (6)
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ornamental materials (1)
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petroleum
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talc deposits (1)
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elements, isotopes
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boron
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B-11/B-10 (1)
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carbon
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C-13/C-12 (10)
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C-14 (1)
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organic carbon (5)
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chemical ratios (1)
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halogens
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bromine
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bromide ion (2)
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fluorine (1)
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hydrogen
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D/H (3)
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deuterium (1)
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isotope ratios (24)
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isotopes
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radioactive isotopes
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Be-10 (1)
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Be-10/Be-9 (1)
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C-14 (1)
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Pb-210 (1)
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Po-210 (1)
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Ra-226 (1)
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Ra-228 (1)
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Re-187/Os-188 (1)
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Rn-222 (1)
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Th-232 (1)
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U-238 (1)
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stable isotopes
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B-11/B-10 (1)
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Be-10/Be-9 (1)
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C-13/C-12 (10)
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D/H (3)
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deuterium (1)
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He-4/He-3 (1)
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Hf-177/Hf-176 (1)
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N-15/N-14 (1)
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Nd-144/Nd-143 (1)
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O-18 (2)
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O-18/O-16 (14)
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Os-188/Os-187 (1)
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Re-187/Os-188 (1)
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S-34/S-32 (4)
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Sr-87/Sr-86 (2)
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metals
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actinides
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thorium
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Th-232 (1)
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uranium
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U-238 (1)
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alkali metals
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lithium (4)
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potassium (2)
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sodium (1)
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alkaline earth metals
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beryllium
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Be-10 (1)
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Be-10/Be-9 (1)
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calcium (2)
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magnesium (4)
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radium
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Ra-226 (1)
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Ra-228 (1)
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strontium
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Sr-87/Sr-86 (2)
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aluminum (4)
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antimony (1)
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arsenic (1)
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bismuth (5)
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chromium (2)
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copper (5)
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iron
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lead
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manganese (6)
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mercury (2)
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nickel (3)
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platinum group
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osmium
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Os-188/Os-187 (1)
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Re-187/Os-188 (1)
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polonium
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Po-210 (1)
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rare earths
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neodymium
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O-18/O-16 (14)
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Vertebrata
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Mammalia
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Theria
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Proboscidea
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Reptilia
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Archosauria
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cyanobacteria (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Podocopida
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Bairdiidae
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Insecta (1)
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Brachiopoda
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Articulata
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Bryozoa (1)
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Cnidaria
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Anthozoa
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Scleractinia (2)
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-
-
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Echinodermata
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Crinozoa
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Crinoidea (2)
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Mollusca
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Bivalvia (6)
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Cephalopoda
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Ammonoidea (4)
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Gastropoda (4)
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Protista
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Foraminifera
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Fusulinina
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Fusulinidae (1)
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Rotaliina
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Buliminacea
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Uvigerinidae
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Uvigerina
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Uvigerina peregrina (1)
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Globigerinacea
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Hantkenina (1)
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Nodosariacea (1)
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Radiolaria (3)
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microfossils
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Conodonta
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Fusulinina
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palynomorphs
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Chitinozoa (1)
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Dinoflagellata (5)
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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 (2)
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nannofossils (1)
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Rhodophyta
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Corallinaceae (2)
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-
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Spermatophyta
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Pleistocene
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Tertiary
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lower Miocene
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middle Miocene
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upper Miocene
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Pliocene (3)
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Paleogene
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lower Eocene (2)
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middle Eocene
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upper Eocene (1)
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Oligocene
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lower Oligocene
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Paleocene
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lower Paleocene
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upper Paleocene (2)
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Mesozoic
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Gosau Formation (4)
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Upper Cretaceous
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Upper Jurassic (5)
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Permian-Triassic boundary (5)
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Middle Triassic
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Upper Triassic
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Triassic-Jurassic boundary (1)
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Wetterstein Limestone (1)
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Moldanubian (10)
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Paleozoic
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Cambrian
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Upper Permian
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Permian-Triassic boundary (5)
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Precambrian
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upper Precambrian
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Rhenohercynian (1)
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Primary terms
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chemical analysis (2)
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Mammalia
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Reptilia
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Globigerinacea
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
The Unusual Seismic Activity from 2021 to 2024 in Eastern Austria: Insights from Seismic Sequences Relocation and Moment Tensor Inversion Available to Purchase
PREPARATION TECHNIQUES: FROM SINGLE BONE FRAGMENTS TO MOUNTED SKELETONS—MODELS, HYBRID EPISTEMIC OBJECTS, AND THE QUESTION OF EVIDENCE IN THE CONTEXT OF 19TH-CENTURY MOA FINDS Available to Purchase
A review of the Mesozoic – Cenozoic acritarch genus Cyclopsiella Drugg & Loeblich Jr. 1967 emend. nov. Available to Purchase
Spectrometric borehole logging in mineral exploration and mining Available to Purchase
Subglacial tills: a process model based on microsedimentological clues Open Access
A window into development of a complex ice-marginal lake prior to the Late Glacial Maximum (LGM) in Austria Available to Purchase
Geochemical characterization, U–Pb apatite geochronology, and geodynamic significance of olivine minette dykes from the Julian Alps, NE Italy Available to Purchase
Permian to Triassic protolith ages of type locality eclogites in the Eastern Alps: Implications for the opening of the Meliata back-arc basin Available to Purchase
Human-induced reactivation of a dormant earthflow? A geomorphological interpretation of historical mining maps of the Ischl salt mine (Austria) Available to Purchase
Seismoacoustic Study of Thunder and Lightning Using the AlpArray Available to Purchase
Nineteenth-century paleontological art in the Natural History Museum Vienna, Austria: Between demystification and mythologization Available to Purchase
ABSTRACT The nineteenth century was the dawn of scientific and systematic paleontology. The foundation of Natural History Museums—built as microcosmic “Books of Nature”—not only contributed to the establishment of this new discipline but also to its visual dissemination. This paper will take the metaphor of the “book” as a starting point for an examination of the paleontological exhibition at the Natural History Museum in Vienna. In keeping with “Natural Theology,” the earliest natural science museums in Britain were designed as expressions of the medieval idea of the “Holy Book of Nature.” Contrary to this, the Natural History Museum Vienna, opened in 1889, wanted to be a nonreligious museum of evolution. Nevertheless, the idea of the “book” was also influential for its design. According to the architects and the first director, it should be a modern “walk-in textbook” instructive for everyone. The most prominent exhibition hall in the museum is dedicated to paleontology. The hall’s decorative scheme forms a unique “Paleo-Gesamtkunstwerk” (Gesamtkunstwerk: total piece of art). The use of grotesque and mythological elements is a particularly striking feature of the hall’s decoration and raises the question of how this relates to the museum’s claim to be a hard-core science institution. As it was paleontology’s task to demystify the monsters and riddles of Earth history systematically, it seems odd that the decorative program connected explicitly to this world. This chapter sheds light on the cultural traditions that led to the creation of this ambiguous program that oscillates between science and imagination. Looking at the results of the research on the nature of the earth, one looks into a book that contains the oldest history we humans know. With amazement, we see the wonders of the first epochs of the earth arising before our mind’s eyes, and what until recently have been incomprehensible hieroglyphs is now almost completely clear to us. How many fables may have been created by the sudden appearance of prehistoric structures in the form of animals and plants? No fairy tales, no fantasies, tangible reality now stands before us and yet no less wonderful, even more wonderful, and this miracle has been achieved by science, the restless seeker. —J. Hoffmann (undated, ca. 1885, p. 1; translation from German)
Alumino-oxy-rossmanite from pegmatites in Variscan metamorphic rocks from Eibenstein an der Thaya, Lower Austria, Austria: A new tourmaline that represents the most Al-rich end-member composition Open Access
Structural and chemical characterization of dienerite, Ni 3 As, and its revalidation as a mineral species Available to Purchase
Isotopic and time series investigations of recent stalagmites (1945–2018), Schlossberg tunnels, Graz, Austria: implications for climate change in Central Europe Available to Purchase
Abstract For the first time, we present a decadal-scale stable isotope record (δ 18 O, δ 13 C) of 67 speleothem calcite samples coming from an artificial tunnel network located in Graz, Austria. Stable isotope data are interpreted with the help of time series (TS) analysis of mean air temperatures (MAT) and mean annual precipitations (MAP) that have been monitored and recorded in a neighbouring meteorological station. Speleothem records have proved to be very useful in reconstructing changes of environmental conditions. For studied stalagmites, which grew between 1945 and 2018, the δ 18 O values average −18.64‰ and range from −23‰ to −17‰ (VPDB, Vienna Pee Dee Belemnite), suggesting variable climatic conditions. The δ 18 O values of calcite increase along the growth axis and are correlated with high temporal resolution MAT, MAP and weighted mean annual δ 18 O of precipitations. For the same time interval, while the temperature TS show an increasing trend, with a steeper gradient since the 1980s, the precipitation TS presents a weak decreasing tendency. Increase in the δ 13 C values of speleothems from −33‰ to −24‰ (VPDB) is correlated with increasing temperature and drought, associated CO 2 degassing and soil erosion over the tunnel system.