Subsurface correlations of the Cretaceous Greenhorn-Lakota interval in North Dakota. by Dan E. Hansen Download PDF EPUB FB2
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects Subsurface correlations of the cretaceous Greenhorn-Lakota interval in North Dakota: a study in facies Dan E.
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Find more information about: OCLC Number: Title: Subsurface correlations of the Cretaceous Greenhorn - Lakota interval in North Dakota; Author(s): Hansen, D.E. Publishing Organization: North Dakota Geological Survey; Series and Number: Bulletin 29; Publication Date: ; Map Scale: ,; Cross Section: Yes; North Latitude: 49° 0' 0" N () South Latitude: 45° 56' 5" N ().
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#29 Hansen D. SUBSURFACE CORRELATIONS OF THE CRETACEOUS GREENHORN-LAKOTA INTERVAL IN NORTH DAKOTA wps, ex-lib, vg 46 pp., 2 plts, 10 figs. Price: $ (stock#NDB) #30 Laird W. GUIDE FOR GEOLOGIC FIELD TRIP IN NORTHEASTERN NORTH DAKOTA wps, ex-lib, vg 20 pp.
Price: $ (stock#NDB). Subsurface correlations of the cretaceous Greenhorn-Lakota interval in North Dakota: a study in facies, Dan E. Hansen. PDF. Stream piracy and glacial diversion of Little Missouri River, North Dakota, Emmett R.
Schmitz. Theses/Dissertations from PDF. The geology of Bomi Hill, Liberia, Africa, Roland I. Erickson. Subsurface Stratigraphic Cross Sections Showing Correlation of Cretaceous and.
Lower Tertiary Rocks in the Bighorn Basin, Wyoming and Montana. By Thomas M. Finn. Chapter 6 of. Petroleum Systems and Geologic Assessment of Oil and Gas in the Bighorn Basin Province, Wyoming and Montana.
By U.S. Geological Survey Bighorn Basin Province Assessment Team. Subsurface Stratigraphic Cross Sections of Cretaceous and Lower Tertiary Rocks in the Southwestern Wyoming Province 5 Depositional Setting All but the uppermost Cretaceous rocks in the SWWP were deposited in or adjacent to a broad epicontinental seaway that periodically covered much of the Western Interior of the United States (ﬁg.
PDF | On Jan 1,Thomas M. Finn and others published Subsurface Stratigraphic Cross Sections of Cretaceous and Lower Tertiary Rocks in the Southwestern Wyoming Province, Wyoming, Colorado. Stratigraphy of the Danek Bonebed (Upper Cretaceous Horseshoe Canyon Formation, central Alberta) and correlations with strata in the Drumheller and Grande Prairie regions November Canadian.
To the north and east, a distinctive geophysical log response in the subsurface represents the contact. The top of the uppermost Cretaceous-Tertiary prism is a regional unconformity resulting from the removal of between one and three kilometres of sediment during post-Laramide erosion in the middle to late Tertiary (Nurkowski, ; Bustin, ).
Hansen, D.E.,Subsurface correlations of the Cretaceous Greenhorn-Lakota interval in North Dakota: North Dakota Geological Survey Bulletin, no. Summary: Benton shale restricted from Williston basin, North Dakota. subsurface, despite differences in burial and diagenetic histories.
The Fall River sandstone is exposed in outcrop in South Dakota and Wyoming around the Black Hills Uplift, and it passes into the subsurface westward in the Powder River Basin (Fig. 1), where it produces. (table 2),pl.
Greenhorn formation of Colorado group. In subsurface of North Dakota consists of dark-gray, calcareous, soft shale with thin beds of very shaly limestone. Thickness to feet. Overlies Belle Fourche formation of Colorado group. Fossiliferous (GLOBIGERINA, INOCERAMUS).
Age is Late Cretaceous. The surface geology of NE Thailand consists almost entirely of Jurassic to Mid-Cretaceous Khorat Group red-beds. During the last 30 years, however, hydrocarbon exploration has resulted in 40 deep wells being drilled through the Khorat Group cover into an extensive system of Late Triassic (Kuchinarai Group) and Mid–Carboniferous to earliest Late Permian (Saraburi Group) basins.
Subsurface information obtained during a recent investigation has been combined with information from previous investigations to establish a stratigraphic framework for the Cretaceous rocks of southwestern Minnesota.
This new framework makes possible the reconstruction of Late Cretaceous (Cenomanian to Campanian) paleogeography. Subsurface correlations of upper Cretaceous and Tertiary rocks, southern Washakie Basin, Wyoming to northern Sand Wash Basin, Colorado.
Browse related items Start at call number: U58O B. Publication: Hansen, D.E.,Subsurface correlations of the Cretaceous Greenhorn-Lakota interval in North Dakota: North Dakota Geological Survey Bulletin, no.
29 Usage in. Correlation of these Cretaceous formations, mem-bers and beds to equivalent units in other provinces and states in North America has resulted in numerous changes to Manitoba's stratigraphic.
The paper by Clayton and Moran () focuses on the North Dakota, Minnesota, Manitoba, and Saskatchewan regions. The stratigraphic nomenclature for southern and central Saskatchewan is undergoing significant revision (Christiansen, pers.
comm., ), with the definition of a number of new units being considered. Hansen, D.E.,Subsurface correlations of the Cretaceous Greenhorn-Lakota interval in North Dakota: North Dakota Geological Survey Bulletin, no.
Summary: Extends name into the subsurface of the Williston basin in North Dakota in a series of correlation diagrams. Subsurface stratigraphic analysis of Upper Cretaceous rocks, southeastern flank of the Williston Basin, North and South Dakota Open-File Report By: J.K. Baird and T.S. Dyman.
The Basal Colorado Sandstone, in southeastern Alberta, southern Saskatchewan, northern Montana and North Dakota, is a thin (less than m thick), sheet-like unit underlying the Joli Fou marine shales and overlying the non-marine Mannville Group (Banerjee, ). Correlation of nonmarine lower cretaceous deposits of the south European part of the former USSR on the basis of charophyta I.
Shaikin, F. Kisielevsky, L. Vacula Pages A portable x-ray fluorescence (XRF) device was in this study used to identify geochemical markers associated with the Cretaceous–Paleogene boundary in North Dakota, USA. At the time of the K–Pg boundary, an asteroid struck the Earth which resulted in one of the five big mass extinctions.
The event left behind a globally distributed clay layer consisting of material derived from the. Lower Cretaceous interval in the North Dakota portion of the Willis ton Basin and adjacent areas hereto fore has generally been interpreted to be at a major unconformity.
This in terpretation as applied in the sub surface of North Dakota is herewith substantially refuted. Instead, the. Hansen, D. E.,Subsurface correlations of the Cretaceous Greenhorn-Lakota interval in North Dakota: North Dakota Geol.
Survey, Bull. 29, 46 p. Hatch, F. H., Rastall, R. H., and Black, Maurice,The petrology of the sedimentary rocks: London, Thomas Murby, p. The D and J sandstone of the Cretaceous Dakota Group are considered as the major oil and gas producing units within in the Denver Basin.
The distribution of these units in the Denver Basin is a sub-basin of the Early Cretaceous Western Interior units are well understood within the northern Denver Basin and the linkage between the subsurface units and their equivalents in outcrop.
Merriam () has suggested possible correlations of surface and subsurface units, although much additional work, especially on surface outcrops, is necessary before correlations can be verified.
The main difference is in the use of Dakota, which is used to designate a formation on the surface (Plummer and Romary, ), whereas in the subsurface approximately the same unit is here designated by.
Cretaceous–Tertiary (K–T) mass extinction and the rise of pla- cental mammals (e.g., Alroy, ; Wilson, ), and for devel- oping a Late Cretaceous biochronology of North America (Cifelli. Karl R. Newman, "Biostratigraphic correlation of Cretaceous-Tertiary boundary rocks, Colorado to San Juan Basin, New Mexico", The Cretaceous-Tertiary Boundary in the San Juan and Raton Basins, New Mexico and Colorado, James E.
Fassett, J. Keith Rigby, Jr.North Dakota and South Dakota contain strata in the Cretaceous, Jurassic, Permian, Pennsylvanian, Mississippian, and Siluro-Devonian that have produced oil in near-by regions. The well on the Camp Crook anticline, Sec. 35, T. 18 N., R. 1 E., South Dakota, had a good showing of live oil in strata of Cambrian or Ordovician age according to scout.Detailed north-south cross section of interval from the Dakota Sandstone to the lower part of the Upper Cretaceous Mesaverde Group, Douglas Creek arch and western part of Piceance Basin.
Depositional Framework of the Upper Cretaceous Mancos Shale and the Lower Part of the 3.