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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Algeria (2)
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Libya (1)
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Morocco (1)
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Nubian Shield (1)
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Sahara (1)
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Southern Africa
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South Africa
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Free State South Africa
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Vredefort Dome (1)
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West Africa
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Cameroon (1)
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Taoudenni Basin (1)
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Antarctica
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Lake Vostok (1)
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Transantarctic Mountains
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Arctic region
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Greenland
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East Greenland (1)
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Asia
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Far East
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Cyprus
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Turkey
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Ob River (1)
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Western Canada
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Pacific Coast (2)
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North Pacific
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polar regions (1)
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commodities
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metals
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alkaline earth metals
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beryllium
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Be-10 (4)
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strontium
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Sr-87/Sr-86 (2)
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aluminum
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Al-26 (3)
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lead
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Pb-210 (1)
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platinum group
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osmium
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Os-188/Os-187 (1)
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rare earths
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oxygen
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O-18/O-16 (4)
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fossils
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Graptolithina (1)
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Invertebrata
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Brachiopoda (1)
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Protista
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microfossils
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geologic age
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Paleogene
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upper Cenozoic (3)
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Lake Bonneville (1)
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Mesozoic
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Cretaceous
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Paleozoic
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-
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Ellis Bay Formation (1)
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-
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Precambrian
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Proterozoic
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Paleoproterozoic (1)
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-
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igneous rocks
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igneous rocks
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ophiolite (1)
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orthosilicates
-
nesosilicates
-
zircon group
-
zircon (2)
-
-
-
-
-
-
Primary terms
-
absolute age (22)
-
Africa
-
North Africa
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Algeria (2)
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Libya (1)
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Morocco (1)
-
-
Nubian Shield (1)
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Sahara (1)
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Southern Africa
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South Africa
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Free State South Africa
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Vredefort Dome (1)
-
-
-
-
West Africa
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Cameroon (1)
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Taoudenni Basin (1)
-
-
-
Antarctica
-
Lake Vostok (1)
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Transantarctic Mountains
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Shackleton Range (1)
-
-
-
Arctic region
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Greenland
-
East Greenland (1)
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Greenland ice sheet (2)
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Northern Greenland (1)
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South Greenland (1)
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West Greenland (1)
-
-
-
Asia
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Arabian Peninsula
-
Oman (1)
-
-
Far East
-
China
-
Huang He (1)
-
Xizang China
-
Lhasa Block (1)
-
-
-
-
Himalayas (3)
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Indian Peninsula
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Ganga Basin (1)
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India
-
Uttar Pradesh India (2)
-
-
Indo-Gangetic Plain (1)
-
Nepal (1)
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Pakistan (1)
-
-
Lena River (1)
-
Middle East
-
Cyprus
-
Troodos Massif (1)
-
-
Turkey
-
Anatolia (1)
-
-
-
Ob River (1)
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Siberia (1)
-
Tibetan Plateau (2)
-
Yenisei River (1)
-
-
Atlantic Ocean
-
East Atlantic (1)
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Equatorial Atlantic (1)
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North Atlantic
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Baltic Sea (3)
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Gulf of Maine (1)
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Hudson Strait (1)
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Irish Sea (1)
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Labrador Sea (1)
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atmosphere (1)
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Australasia
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Canada
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Eastern Canada
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Maritime Provinces
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Halifax County Nova Scotia
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-
-
-
Newfoundland and Labrador
-
Newfoundland (1)
-
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Quebec
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Anticosti Island (1)
-
-
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Hudson Bay (2)
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Hudson Bay Lowlands (1)
-
Nunavut
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Baffin Island (1)
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Devon Island (1)
-
Ellesmere Island (1)
-
Sverdrup Islands
-
Amund Ringnes Island (1)
-
Ellef Ringnes Island (1)
-
-
-
Queen Elizabeth Islands
-
Devon Island (1)
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Ellesmere Island (1)
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Sverdrup Islands
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Amund Ringnes Island (1)
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Ellef Ringnes Island (1)
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Western Canada
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Alberta
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Alberta Basin (1)
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Athabasca Oil Sands (1)
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British Columbia
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-
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Manitoba
-
Lake Winnipeg (3)
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Nelson River (1)
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Northwest Territories (2)
-
-
-
carbon
-
C-13/C-12 (4)
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C-14 (14)
-
organic carbon (1)
-
-
Caribbean region
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West Indies
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Antilles
-
Greater Antilles
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Jamaica (1)
-
-
Lesser Antilles
-
Montserrat Island (1)
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Soufriere (1)
-
-
-
Bahamas (1)
-
-
-
Cenozoic
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Quaternary
-
Cordilleran ice sheet (1)
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Holocene
-
lower Holocene (4)
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middle Holocene (1)
-
Preboreal (1)
-
upper Holocene (4)
-
-
Innuitian ice sheet (1)
-
lower Quaternary (1)
-
Mazama Ash (1)
-
Pleistocene
-
Champlain Sea (1)
-
Lake Agassiz (2)
-
Lake Lahontan (1)
-
lower Pleistocene (1)
-
upper Pleistocene
-
Baltic ice lake (1)
-
Devensian (1)
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Eemian (1)
-
Weichselian
-
upper Weichselian
-
Allerod (1)
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Bolling (1)
-
Younger Dryas (1)
-
-
-
Wisconsinan
-
upper Wisconsinan
-
Fraser Glaciation (1)
-
-
-
-
-
upper Quaternary
-
Pinedale Glaciation (1)
-
Scandinavian ice sheet (2)
-
-
-
Tertiary
-
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isostatic rebound
Evidence for a more extensive Greenland Ice Sheet in southwestern Greenland during the Last Glacial Maximum
The influence of glacial isostatic adjustment on continental shelf stratigraphic correlation
Narrow is normal: Exploring the extent and significance of flooded marine shelves in icehouse, transitional, and greenhouse climate settings
Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)–observed uplift due to recent mass loss at Patagonia ice fields
Unconformity development in retroarc foreland basins: implications for the geodynamics of Andean-type margins
Fast Pliocene integration of the Central Anatolian Plateau drainage: Evidence, processes, and driving forces
The ups and downs of the Missouri River from Pleistocene to present: Impact of climatic change and forebulge migration on river profiles, river course, and valley fill complexity
How Climate, Uplift and Erosion Shaped the Alpine Topography
Late Quaternary sea level, isostatic response, and sediment dispersal along the Queen Charlotte fault
The “Passive” Margin of Eastern North America: Rifting and the Influence of Prerift Orogenic Activity on Postrift Development
Processes and deformation rates generating seismicity in metropolitan France and conterminous Western Europe
A Comparison of Site Response Techniques Using Weak-Motion Earthquakes and Microtremors
Postglacial Uplift: Record in the Gravity Field and in Neogene–Quaternary Structures
Late Quaternary sea-level history of Saipan, Commonwealth of the Northern Mariana Islands, USA: A test of tectonic uplift and glacial isostatic adjustment models
The timing of fjord formation and early glaciations in North and Northeast Greenland
Glacial isostatic adjustment in central Cascadia: Insights from three-dimensional Earth modeling
An integrated high-resolution geophysical and geologic visualization of a Lake Bonneville shoreline deposit (Utah, USA)
Glacial isostatic adjustment deflects the path of the ancestral Hudson River
Eemian estuarine record forced by glacio-isostasy (southern Iceland)—link with Greenland and deep sea records
Role of karst denudation on the accurate assessment of glacio-eustasy and tectonic uplift on carbonate coasts
Abstract Quaternary glacio-eustasy has traditionally been determined in part by the examination of fossil coral reefs on carbonate islands and coasts uplifted by tectonics. These studies do not properly account for dissolutional denudation, which is cumulative, making higher and therefore older terraces exist at elevations far below their assumed depositional elevation. Karst pedestals (karrentische) on Guam reveal the extent of the denudation ( c. 50 mm ka −1 ) and demonstrate that theoretical denudation models can be accurately applied to eogenetic carbonates in tropical settings. Aeolian calcarenite islands such as the Bahamas have been used as tectonically stable sea-level calibrations for other islands, which may not be correct. Flank margin caves, forming in the distal margin of the freshwater lens within a carbonate island, are excellent sea-level indicators. Analysis of flank margin cave elevations indicates that the Bahamas have had past sea-level highstands >6 m, perhaps up to 15 m or more, for which no fossil coral data exist. Denudational removal of these older corals has biased the record to younger events and only flank margin caves remain as viable terrestrial signatures of these older sea-level highstands.