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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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Karoo Basin (1)
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South Africa (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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Australasia
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Australia (1)
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United States
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Potomac River (1)
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Virginia (1)
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Wyoming
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Teapot Dome (1)
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-
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commodities
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bitumens (1)
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metal ores
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uranium ores (1)
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petroleum (1)
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fossils
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Invertebrata
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Protista
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Foraminifera
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Rotaliina
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Globigerinacea
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Globigerinidae
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Globigerinoides
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Globigerinoides sacculifer (1)
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Orbulina
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Orbulina universa (1)
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microfossils (1)
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geologic age
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Cenozoic
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Tertiary
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Paleogene
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Oligocene
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Fontainebleau Sandstone (2)
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-
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Mesozoic
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Cretaceous
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Lower Cretaceous (1)
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Upper Cretaceous
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Castlegate Sandstone (1)
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Paleozoic
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Permian
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Ecca Group (1)
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-
-
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igneous rocks
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igneous rocks
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plutonic rocks
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diabase (1)
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granites (1)
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-
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metamorphic rocks
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turbidite (1)
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minerals
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carbonates (1)
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silicates
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sheet silicates
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clay minerals
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montmorillonite (1)
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illite (1)
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-
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sulfates
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gypsum (1)
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-
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Primary terms
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Africa
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Southern Africa
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Karoo Basin (1)
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South Africa (1)
-
-
-
Antarctica
-
Victoria Land
-
McMurdo dry valleys (1)
-
-
-
Australasia
-
Australia (1)
-
-
bitumens (1)
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Cenozoic
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Tertiary
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Paleogene
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Oligocene
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Fontainebleau Sandstone (2)
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-
-
-
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data processing (1)
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fractures (2)
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geochemistry (1)
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geophysical methods (1)
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ground water (2)
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igneous rocks
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plutonic rocks
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diabase (1)
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granites (1)
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-
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intrusions (4)
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Invertebrata
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Protista
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Foraminifera
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Rotaliina
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Globigerinacea
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Globigerinidae
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Globigerinoides
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Globigerinoides sacculifer (1)
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-
Orbulina
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Orbulina universa (1)
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-
-
-
-
-
-
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magmas (5)
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Mesozoic
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Cretaceous
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Lower Cretaceous (1)
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Upper Cretaceous
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Castlegate Sandstone (1)
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-
-
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metal ores
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uranium ores (1)
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metasomatism (1)
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Paleozoic
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Permian
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Ecca Group (1)
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-
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petroleum (1)
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rock mechanics (1)
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sea water (1)
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sedimentary rocks
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carbonate rocks
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limestone
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micrite (1)
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-
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clastic rocks
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mudstone (1)
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sandstone (3)
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oil sands (1)
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sedimentary structures
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soft sediment deformation
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clastic dikes (1)
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-
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sedimentation (3)
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sediments
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clastic sediments
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mud (1)
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sand (1)
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-
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United States
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Potomac River (1)
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Virginia (1)
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Wyoming
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Teapot Dome (1)
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-
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone
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micrite (1)
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-
-
clastic rocks
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mudstone (1)
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sandstone (3)
-
-
oil sands (1)
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-
turbidite (1)
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sedimentary structures
-
sedimentary structures
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soft sediment deformation
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clastic dikes (1)
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-
-
-
sediments
-
sediments
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clastic sediments
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mud (1)
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sand (1)
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-
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turbidite (1)
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Reynolds number
Comparison of gas, Klinkenberg, and liquid permeability of sandstone: Flow regime and pore size
Reactive Transport in Evolving Porous Media
Flow diagnostics for naturally fractured reservoirs
Laboratory investigation of nonlinear flow characteristics through natural rock fractures
Tracking Diverse Minerals, Hungry Organisms, and Dangerous Contaminants Using Reactive Transport Models
The clay minerals present in the oil-sands ore are responsible for some of the most challenging (and intriguing) processing behavior experienced on a routine basis in oil-sands surface mining. In previous chapters, significant details have been provided on how specific clay properties can give rise to changes in slurry rheology and interface phenomena. Because the bitumen extraction process relies heavily on manipulation of interfacial effects to enhance separation, changes in clay content in the ore, not surprisingly, can have a dramatic impact on the ability to process the material. This chapter provides an overview of the extraction process, the influence of clay minerals on bitumen recovery, and the challenges in reacting to changes in the ore clay content in a typical operation. The chapters that follow focus on the larger issue of tailings treatment to create a reclaimed landscape at the end of mine life.
Indicators of propagation direction and relative depth in clastic injectites: Implications for laminar versus turbulent flow processes
Magmatic life at low Reynolds number: REPLY
Magmatic life at low Reynolds number: COMMENT
Sticky issues arising from high-viscosity magma: Settling arguments on magmatic structures
Magmatic life at low Reynolds number
Implications of pore microgeometry heterogeneity for the movement and chemical reactivity of CO 2 in carbonates
Investigation of flow and flow noise around a seismic streamer cable
Which effective viscosity?
Determination of Drag Coefficients in Measuring Particle Diameters: Reply
A Preliminary Experimental Study of Turbidite Fan Deposits: Discussion
Determination of Drag Coefficients in Measuring Particle Diameters
Hydrodynamic strategies in the morphological evolution of spinose planktonic foraminifera
Possible hydraulic significance of two kinds of potholes: Examples from the paleo-Potomac River
Abstract The purpose in writing these notes has been to present a discussion of a few topics central to a physical understanding of the mechanics of sediment movement. Discussion has been confined to unidirectional flows (excluding waves) of relatively small scale (excluding Coriolis effects). A large number of topics have been not considered at all or only in passing, including one of the most important problems in sediment mechanics: theories for the prediction of bed-load and suspended-load discharge. It seemed more important to try to develop some physical insight about the elementary processes of sediment movement than to attempt to elaborate any comprehensive quantitative theories of sediment movement.