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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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Kenya
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Kenya Rift valley (1)
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Tanzania (1)
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Zambia (1)
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North Africa
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Southern Africa
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Namibia (1)
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Antarctica
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Victoria Land
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McMurdo dry valleys (1)
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Arctic Ocean
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Svalbard
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Asia
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Indian Peninsula
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Urals (1)
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stable isotopes
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oxygen
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fossils
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Reptilia
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Invertebrata
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geochronology methods
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Cenozoic
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Tertiary
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Neogene
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Paleogene
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Mesozoic
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Comanchean
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Upper Cretaceous
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Jurassic
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Navajo Sandstone (1)
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Triassic
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Lower Triassic
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Bunter (2)
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Middle Triassic (1)
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Sherwood Sandstone (1)
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Upper Triassic
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Rhaetian
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Paleozoic
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Cambrian
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Upper Cambrian
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Potsdam Sandstone (1)
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Carboniferous
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Lower Carboniferous
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Dinantian (1)
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Mississippian
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Lower Mississippian
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Tournaisian (1)
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Deadwood Formation (1)
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Devonian
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Lower Devonian
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Old Red Sandstone (1)
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Upper Devonian
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Famennian
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Wabamun Group (1)
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Nisku Formation (1)
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lower Paleozoic
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Rose Run Sandstone (2)
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Ordovician
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Lower Ordovician
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Ellenburger Group (1)
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Utica Shale (1)
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Permian
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Upper Permian
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Zechstein (3)
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Silurian
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Precambrian
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upper Precambrian
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Proterozoic
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igneous rocks
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pyroxene group
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framework silicates
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sorosilicates
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epidote group
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ring silicates
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tourmaline group (1)
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sheet silicates
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chlorite group
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chlorite (2)
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clay minerals
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illite (3)
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sulfates
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sulfides
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coloradoite (1)
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sylvanite (1)
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Primary terms
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absolute age (4)
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Africa
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East Africa
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Kenya
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Kenya Rift valley (1)
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Tanzania (1)
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Zambia (1)
-
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North Africa
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Algeria (1)
-
-
Southern Africa
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Namibia (1)
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-
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Antarctica
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Victoria Land
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McMurdo dry valleys (1)
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-
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Arctic Ocean
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Beaufort Sea (1)
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Arctic region
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Svalbard
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Spitsbergen (1)
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Asia
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Altai Russian Federation (1)
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Baikal rift zone (1)
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Buryat Russian Federation (1)
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Far East
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China
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Liaoning China (1)
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Qaidam Basin (1)
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Qinghai China (1)
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Shandong China
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Shandong Peninsula (1)
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Xiaoqinling Mountains (1)
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Xinjiang China
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Junggar Basin (1)
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-
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Indian Peninsula
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Afghanistan (1)
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Irkutsk Russian Federation (1)
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Krasnoyarsk Russian Federation
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Taymyr Dolgan-Nenets Russian Federation
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Middle East
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Israel (1)
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Jordan (2)
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Atlantic Ocean
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Gulf of Mexico (2)
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atmosphere (1)
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Australasia
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Australia
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brines (16)
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Canada
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Eastern Canada
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Maritime Provinces
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Ontario
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Rainy River District Ontario
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Quebec (1)
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Western Canada
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Manitoba
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carbon
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C-13/C-12 (2)
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Cenozoic
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Quaternary
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Holocene (2)
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upper Pleistocene (1)
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Tertiary
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Neogene
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Miocene (1)
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Paleogene
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Oligocene (1)
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Chordata
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Vertebrata
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Tetrapoda
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Reptilia
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Archosauria
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clay mineralogy (5)
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Poland
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Sowie Mountains (1)
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Slovakian Pannonian Basin (1)
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Sudeten Mountains
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Sowie Mountains (1)
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Switzerland
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Bern Switzerland
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Grimsel Test Site (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
saline composition
In-situ and ex-situ experimental investigation on the chalcopyrite replacement in saline solution at 310–365 °C and 15–25 MPa
Site characterization of the Endurance CO 2 store, Southern North Sea, UK
Subsurface maturation in a saline aquifer CCS project development. Experience from the Northern Lights project, offshore Norway
A process-led approach to framing uncertainty and risk in CO 2 storage in the subsurface
Field tests of geological storage of CO 2 at the Otway International Test Centre, Australia: trapping and monitoring the migrating plumes
Geoelectric evidence for a wide spatial footprint of active extension in central Colorado
Two discrete gold mineralization events recorded by hydrothermal xenotime and monazite, Xiaoqinling gold district, central China
Origin of heavy shale oil in saline lacustrine basins: Insights from the Permian Lucaogou Formation, Junggar Basin
Pressure-derived storage efficiency for open saline aquifer CO 2 storage
The NaCl-CaCO 3 and NaCl-MgCO 3 systems at 6 GPa: Link between saline and carbonatitic diamond forming melts
3D reservoir simulation of CO 2 injection in a deep saline aquifer of the Lower Paleozoic Potsdam Sandstone of the St Lawrence Platform, Gentilly Block, Quebec
Experimental measurement of the exclusion-diffusion potential in sandstone and shaly sand samples at full and partial water saturation
Geophysical Assessment of Freshwater Intrusion into Saline Aquifers Beneath Plain Reservoirs
Authigenic Phyllosilicates in Sand Layers from the Mudflats of Saline Lakes in the Northern Great Prairies, Saskatchewan
ABSTRACT The deposits of Pleistocene Lake Tecopa include lacustrine, alluvial, eolian, and groundwater discharge deposits of the Tecopa basin in southeastern California. Stratigraphic sections measured in the Tecopa basin and detailed sedimentary facies analysis were used to interpret the depositional settings and track the evolution of sedimentary processes in the basin during the Pleistocene. The early Pleistocene (ca. 2.4–1.0 Ma) deposits of the Lake Tecopa beds record deposition in small saline, alkaline lakes and playas with surrounding mudflats and sandflats and adjacent alluvial fans. Ancestral Amargosa River gravels are first observed in fluvial deposits in the northern part of the basin at ca. 1.0 Ma and correspond with lake expansions (Glass Mountain [GM] lakes) during deposition of the uppermost Glass Mountain ash beds. Several oscillations in lake level followed the post-GM lake decline, culminating in the basin-filling Lava Creek (LC) lake, which reached its acme during deposition of the 0.63 Ma Lava Creek B ash bed. The post–Lava Creek B strata reflect primarily alluvial, fluvial, eolian, and groundwater discharge depositional processes, punctuated in the youngest part of the section by basin-filling lakes (high lake 1 and 2). The Lava Creek B ash bed and older lacustrine strata exhibit extensive zeolitization and clay authigenesis, characteristic of saline, alkaline lake deposits, but the post–Lava Creek B ash bed lacustrine strata have only minor zeolite and clay alteration, suggesting fresher water conditions and a change in the hydrologic state of the basin. Sedimentological observations along with shoreline elevation data provide evidence for intermittent spillover of basin-filling lakes after ca. 0.63 Ma. Subtle tectonic deformation influenced sedimentary processes in the Tecopa basin throughout its history. Episodes of uplift and tilting of Lake Tecopa strata during the middle Pleistocene in the southern part of the basin along the Tecopa Hump likely controlled the sill elevation for spillover of the lake, creating accommodation space for late Pleistocene basin-filling lakes. Ultimately, decreased uplift could not keep pace with increased discharge resulting from high effective moisture during latest middle Pleistocene pluvial periods, and Lake Tecopa drained, most likely during or immediately after marine oxygen isotope stage (MIS) 10 (ca. 0.3 Ma). The deposits of Lake Tecopa provide a detailed record of Pleistocene paleoclimate from ca. 2.4 to 0.3 Ma that demonstrates Milankovitch-scale tuning and clarifies the amplitude of Pleistocene climate change in the southern Great Basin of North America.
Beginning with the nineteenth-century territorial surveys, the lakes and lacustrine deposits in what is now the western United States were recognized for their economic value to the expanding nation. In the latter half of the twentieth century, these systems have been acknowledged as outstanding examples of depositional systems serving as models for energy exploration and environmental analysis, many with global applications in the twenty-first century. The localities presented in this volume extend from exposures of the Eocene Green River Formation in Utah and Florissant Formation in Colorado, through the Pleistocene and Holocene lakes of the Great Basin to lakes along the California and Oregon coast. The chapters explore environmental variability, sedimentary processes, fire history, the impact of lakes on crustal flexure, and abrupt climate events in arid regions, often through the application of new tools and proxies.