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Isostatic Rebound In The Lake Agassiz Basin Since The Late Wisconsinan, Eric C. Brevik

Theses and Dissertations

This study addressed three main questions: I) how thick was the ice that covered the southern Lake Agassiz basin during the Wisconsinan and how much that ice depressed the crust, 2) how much rebound has occurred since deglaciation and whether or not rebound is complete, and 3) what were the effects of this rebound on the basin.

The most direct method of measuring rebound in the Lake Agassiz basin is from strandlines left by glacial Lake Agassiz. The oldest complete strandline, the Herman, presumably rebounded, with the northern end rebounding more because the ice was thicker there and had melted …

Evaluation Of A Possible Subsurface Impact Crater: The Newporte Structure, Northwestern Renville County, North Dakota, Timothy R. Gerlach

Theses and Dissertations

The purpose of this study was to determine if enough evidence exists to support an impact origin hypothesis the Newporte structure. Newporte, a petroliferous, subsurface, crater-shaped feature is located one mile south of the North Dakota - Saskatchewan border in Renville County. It is evident in Precambrian through Ordovician strata at depths of 9100 to 9600 ft (2774 to 2926 m) structure is approximately 2.0 miles (J.2 km) in diameter. Shell Oil company discovered Newporte field when testing this seismically-defined structure in 1977.

Seismic reflection profiling data and synthetic seismograms were used to generate maps that confirmed the circularity of …

A High Resolution Gravity Survey For The Detection Of Pleistocene Aquifers Underlying The Fort Berthold Indian Reservation, North Dakota, Mark R. Mcdonald

Theses and Dissertations

A high resolution gravity survey was performed over portions of McLean, Mountrail, and Ward Counties in central North Dakota during the fall and winter of 1990-1991. The study was performed to locate and map Pleistocene sand and gravel aquifers. Well data indicate that aquifers beneath the study area range in thickness from 1 to 60 meters. The Bouguer gravity anomalies resulting from these shallow aquifers was estimated to be on the order of 1 to 2 mgals. Previous studies have focused on available well data and by mapping topographic lows. Due to the inferential nature of these studies, the detailed …

A Comparison Of Wellhead Protection Area Delineation Methods At Larimore, North Dakota, Barbara L. Sahl

Theses and Dissertations

Many communities in North Dakota rely on water from shallow, unconfined aquifers that are vulnerable to contamination. A strategy to protect public groundwater supplies is the delineation of wellhead protection areas (WHPAs) around the area which contributes water to a well. Several delineation methods are available, all of which have simplifying assumptions which affect the size or shape of a predicted WHPA.

Five WHPA delineation methods were compared to determine which simplified the aquifer/well system while preserving essential hydrogeologic features. A simple system may not require a complex model to predict an accurate WHPA. Sensitivity of each to changes in …

Preferential Flow Mechanisms : Their Interaction And Effect On Dye Movement In Till And Glaciolacustrine Sediment, Calvin D. Taylor

Theses and Dissertations

Contamination of groundwater by agricultural chemicals is of concern to the population of the Northern Great Plains. Preferential flow (macropore, finger, and funnel) allows such chemicals to move relatively rapidly through materials considered to be aquitards. Preferential flow mechanisms at two sites in North Dakota, one in till, the other in glaciolacustrine sediments were determined by application of blue dye (FD&C No 1) solution to framed sites (9m2 & 4m2) with the topsoil removed. The sites were then cored and blocks hand-excavated to depths of 1.5 and 2.5-meters. The three types of preferential flow (macropore, finger, and funnel) were analyzed …

Diagenetic Controls Of Reservoir Quality In The Mississippian Wayne Beds In The Williston Basin, Bottineau County, North Dakota, Michael M. Wetmore

Theses and Dissertations

The carbonate Wayne beds of the Frobisher-Alida interval (Mississippian Mission Canyon Formation) in the Williston Basin, North Dakota, are capable of producing as much as 400,000 barrels of oil per well at depths of only 3,100 feet. Wayne production is from structural traps in the intertidal packstone-wackestone lithofacies; however, the ultimate recoverable reserves of oil per well is controlled neither by structure, nor by depositional environments.

The Wayne beds underwent cementation and micritization in the marine phreatic diagenetic environment. Hypersaline diagenesis caused minor dolomitization and anhydritization. Dissolution and minor cementation occurred in the freshwater vadose zone. Freshwater phreatic diagenesis resulted …