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John R. Dyni

Publications and source records attributed to John R. Dyni.

30 records · Page 2Linked to original sources

Survey of geologic research on Green River oil shale

In the last decade, geologic research on oil-shale deposits and associated rocks of the Green River Formation in Colorado, Utah, and Wyoming has mushroomed largely in response to the Department of the Interior's oil-shale leasing program and to the active interest of private and governmental groups concerned with environmental aspects of an oil-shale industry. Geologic studies, however, are only a small part of the total research effort on Green River oil shale. Investigations covering such diverse topics as archaeology, plant and wildlife, mining and processing, oil-shale law, sociology, and "baseline" studies of soils, water, and air are currently being pursued by researchers from the United States and from as far away as England. Probably noother mineral deposit in the world is being so intensively studied by so many, but it has yet to yield a single barrel of oil commercially.

Colorado, Utah, Wyoming↗

Nahcolite analyses of seven drill cores from the saline facies of the Green River Formation in Northwest Colorado

This report presents the results of about 3,060 quantitative analyses for nahcolite in cores from seven holes drilled in the saline facies of the Green River Formation (Eocene) in Rio Blanco County, Colorado. Nahcolite analyses of three additional drill cores from the same area were reported earlier by Dyni, Beck, and Mountjoy (1971). The analyses of these 10 drill cores were made during a detailed stratigraphic and resource study of the nahcolite that is found in association with the oil-shale deposits of the Green River Formation in the Piceance Creek basin (Dyni, 1973). The locations of the drill holes are shown on figure 1 and are described in the table headings.

Colorado↗

Stratigraphy and nahcolite resources of the saline facies of the Green River Formation, Rio Blanco County, Colorado

Based on a study of 10 drill cores, a sequence of oil shale and associated nahcolite, nearly 2,000 feet thick, in the lacustrine Green River Formation (Eocene) in the Piceance Creek basin, Rio Blanco County, Colo., was divided in ascending order into zones 1 to 13, B-groove, Mahogany zone (with lower, middle, and upper parts), and A-groove at the top. The odd-numbered zones and the Mahogany zone are mappable subsurface units of relatively thick oil shale and are distinguished from the even-numbered zones and A- and B-grooves which are thinner units of oil shale of lower grade. Large amounts of nahcolite found in zones 5 to 12 occur in (1) coarse-grained crystalline aggregates scattered through oil shale, (2) laterally continuous units of fine-grained crystals disseminated in oil shale, (3) brown microcrystalline beds, and (4) white coarse-grained beds that grade laterally into halitic rocks toward basin center. The original .upper limit of the nahcolite and halitic rocks is not yet completely known, but the present top is marked by a dissolution surface. Above this surface the rocks, extending from zones 11 or 12 upward into the Mahogany zone, form a water-saturated 'leached zone,' a geohydrologic unit in which large amounts of water-soluble minerals probably mostly nahcolite, and halite, were removed by ground-water dissolution. Rocks in the leached zone, mostly oil shale, are commonly broken and fractured and contain crystal cavities and solution breccias. Several solution breccias can be traced laterally into unleached beds of nahcolite and halite. Although evidence of salines is found in rocks above A-groove, the original saline facies that includes most of the bedded deposits extends from zone 5 upward into A-groove. Potentially ruinable beds of white nahcolite as much as 12 feet thick are found at depths of 1,560 or more feet below the surface. Some thicker beds of high-grade nahcolite are believed to be too close to the dissolution surface for safe room-and-pillar mining. Probably the most economical method of mining nahcolite would be as a coproduct of a shale-oil industry. Removal of nahcolite prior to retorting increases significantly the grade of oil shale by as much as 1.6 times, Several zones are more than 300 feet thick and average 30 or more weight percent nahcolite. Resources of nahcolite per square mile range as high as 489 million short tons. The total nahcolite resource in the basin is conservatively estimated at 32 billion short tons, which makes it the secondlargest deposit of sodium carbonate known .in the world.

Open-File Report↗

Trioctahedral smectite in the Green River Formation, Duchesne County, Utah

Abundant trioctahedral smectite and smaller amounts of illite comprise a simple assemblage of clay minerals in a basin-edge sequence of lacustrine claystones and oil shales in the Eocene Green River Formation, southwest Uinta Basin, Duchesne County, Utah. Chlorite and mixed-layer clay are present in a few samples. The smectite is well crystallized and has a high expansible-layer content; its chemical composition is uncertain for lack of pure material, but available data suggest a Mg- and Fe-bearing species in the compositional range between saponite and lembergite. Although no significant differences were noted in the clay-mineral content of the claystones versus the oil shales, it was found that calcite strongly prefers oil shale whereas dolomite strongly favors claystone, suggesting that interstitial waters of the claystones during deposition and lithification were more saline than those of the oil shales. The trioctahedral smectite may be part of a basin edge-to-center series of clay-mineral facies--kaolinite to smectite to mica (illite).

Utah↗