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NARROW
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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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North America
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Dakota Aquifer (1)
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Williston Basin (1)
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United States
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Anadarko Basin (1)
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Arkansas (1)
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Jefferson County Nebraska (2)
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Lancaster County Nebraska (5)
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North Dakota (1)
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Oklahoma (1)
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metals
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metamorphic rocks
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North America
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Dakota Aquifer (1)
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oil and gas fields (1)
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Paleozoic
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Carboniferous
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Pennsylvanian
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Upper Pennsylvanian
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Missourian
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Stanton Formation (1)
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soils (2)
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stratigraphy (2)
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United States
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Anadarko Basin (1)
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Arkansas (1)
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Arkansas River valley (1)
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Forest City Basin (1)
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Iowa (1)
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Kansas (1)
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Midcontinent (1)
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Midwest (1)
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Missouri (1)
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Nebraska
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Cass County Nebraska (2)
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Jefferson County Nebraska (2)
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Lancaster County Nebraska (5)
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Sarpy County Nebraska (1)
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North Dakota (1)
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Oklahoma (1)
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Ouachita Mountains (1)
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South Dakota (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone (1)
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clastic rocks
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claystone (1)
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mudstone (1)
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sandstone (1)
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siltstone (2)
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sedimentary structures
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soils
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soils (2)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Impact of the Dakota Aquifer on major-ion chemistry of Rock Creek discharge, eastern Nebraska, Midwest region Available to Purchase
Building and decorative stones, and other geological aspects, of the Nebraska Capitol Available to Purchase
Abstract The Nebraska Capitol is a stunning Art Deco structure located in the heart of Lincoln, Nebraska. This monumental Capitol building contains outstanding examples of the exterior and interior use of Indiana limestone , and interior use of Red Verona (Rosso Verona) marble , Ridgway bluestone , Yellow Kasota stone , Napoleon Gray marble , Belgian Black marble , Portoro (Black and Gold) marble , and Verde Antique . Examples of numerous other stone types quarried in the United States and Europe can also be found within the building. This chapter discusses these building and decorative stones as used in the Capitol, as well as the geologic setting of this building, the striking paleontological iconography of its Rotunda, and the stones used for the Lincoln Monument on the Capitol grounds.
EXCEPTIONALLY PRESERVED LATE ALBIAN (CRETACEOUS) ARCELLACEANS (THECAMOEBIANS) FROM THE DAKOTA FORMATION NEAR LINCOLN, NEBRASKA, USA Available to Purchase
Geomorphology of a Pennsylvanian land surface; pedogenesis in the Rock Lake Shale Member, southeastern Nebraska Available to Purchase
Paleogeomorphic significance of two Paleosols in the Dakota Formation (Cretaceous), southeastern Nebraska Available to Purchase
Depositional history of Dakota Formation (Cretaceous) sandstones, southeastern Nebraska Available to Purchase
Mid-Continent Region Available to Purchase
Abstract The outstanding structural feature of the Dakotas is the Williston basin. It is bounded on the east and southeast by gentle, rather featureless dips off the Canadian shield and the Sioux uplift and on the west by the abrupt Black Hills uplift and the lesser Baker-Glendive anticline of eastern Montana. More pronounced local structures are present in South Dakota, but the chief present interest in the petroleum possibilities of North Dakota is related to the regional structure. The combined area of the two states is approximately 100,000 square miles. The thickness of sedimentary rocks ranges from 1,000 to 12,000 feet or more. The average thickness is about 6,000 feet and the sedimentary volume is about 115,000 cubic miles. Subsurface structural information is available from seventy-nine wells, and thirty-two wells have been drilled into pre-Cretaceous beds. Not more than half of these wells were actual tests for oil and gas. The deepest test is The California Company's Kamp No. 1, drilled to 10,281 feet in Williams County, North Dakota. It stopped in either Ordovician or Devonian limestone. The percentages of different lithologic types in the sedimentary rocks vary widely through the area. Rough estimates for North Dakota are 45 per cent shale, 16 per cent sandstone, 37 per cent limestone and dolomite, and 2 per cent such evaporites as anhydrite and salt. For South Dakota, they are 66 per cent shale, 17 per cent sandstone, 16 per cent limestone and dolomite, and 1 per cent evaporites. A basal sand and shale