3 edition of Sand-body geometry and depositional systems, Ogallala Formation, Texas found in the catalog.
Sand-body geometry and depositional systems, Ogallala Formation, Texas
Steven J. Seni
by Bureau of Economic Geology, University of Texas at Austin in Austin, Tex
Written in English
Bibliography: p. 34-36.
|Statement||by Steven J. Seni ; prepared for the U.S. Department of Energy under contract number DE-AC97-80ET-46615.|
|Series||Report of investigations ;, no. 105, Report of investigations (University of Texas at Austin. Bureau of Economic Geology) ;, no. 105.|
|LC Classifications||QE167 .T42 no. 105, QE571 .T42 no. 105|
|The Physical Object|
|Pagination||iv, 36 p. :|
|Number of Pages||36|
|LC Control Number||81620625|
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Geochemistry of Eagle Ford group source rocks and oils from the first shot field area, Texas. USGS Publications Warehouse. Edman, Janell D.; . Fluctuations in fluvial style in the Wasatch Formation, Piceance Basin, Colorado: Climatic, tectonic, or sediment driven. SciTech Connect. Nadon, G.C.; Lorenz, J.C.
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Seni, S. Sand-Body Geometry and Depositional Systems, Ogallala Formation, Sand-body geometry and depositional systems exas (Univ.
T exas Austin, Bureau of Economic Geology, Report of Investigations No. ). Steven J. Herrup has written: 'Exploring careers in research and information retrieval' -- subject(s): Information retrieval, Information science, Research, Vocational guidance.
Request PDF | On May 1,Don G. Wyckoff and others published Knappable silcrete in the Cretaceous Antlers Formation of Oklahoma and Texas |. Soils and landscape evolution of eolian plains: the Southern High Plains of Texas and New Mexico Bureau of Economic Geology Bulletinpp.
Seni, S.J., Sand-body geometry and depositional systems, Ogallala Formation, Texas. The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations36 pp. Soil Sand-body geometry and depositional systems by: Seni, S.
J.,Sand-body geometry and depositional systems, Ogallala Formation, Texas: The University of Texas at Austin, Bureau of Economic Geology Report of Investigations No. 36 p. Van Rensburg, W. J.,The classification of coal resources and reserves: The University of Texas at Austin, Bureau of Economic Geology Mineral.
The High Plains aquifer, one of the largest freshwater aquifers in the world, is the primary source of potable and irrigation waters in the central Great Plains and underpins much of the region’s economy (Fig. 1).The aquifer provides ~30% of irrigation waters for the United States and drinking water for 82% of the population living within the aquifer boundary (Dennehy, ).
depositional environments or other types of analysis, re quires a great deal of interpretation on the part of the geologist. This book hopefully provides a simplified outline of the major.
It was found that the Coconino could be correlated as a diachronous sand body from southern California to North Dakota, and from Texas to Idaho, an area of approximately million km 2. Formations included the Glorieta Sandstone (New Mexico, Texas, and Oklahoma), the Lyons Sandstone (Colorado), the Wood River Formation (Idaho), the Weber Author: Dr.
John H. Whitmore. The Antevs Library Online Author Title Catalog The catalog includes nearly titles. The following list, arranged alphabetically by first author for dissertations & theses, books and reprints; then by journal, map and media; can be searched using your browser's "FIND" (ctrl-F) utility.
Journal of Hydrology, 59 () Elsevier Scientific Publishing Company, Amsterdam -- Printed in The Netherlands  GEOCHEMISTRY AND HYDRODYNAMICS OF DEEP FORMATION BRINES IN THE PALO DURO AND DALHART BASINS, TEXAS, U.S.A.* R.L.
BASSETT and M.E. BENTLEY Bureau of Economic Geology, The University of Texas at Cited by: Ogallala Formation Depositional History The Ogallala Formation in Texas is the southernmost extension of the major water-bearing unit underlying the Great Plains physiographic province of North America.
It was named by Darton () for the town of File Size: 2MB. The Oakville Formation consists of sediments deposited by several major fluvial systems that traversed the Texas Coastal Plain during the Miocene Epoch. Facies geometry and composition, together with superimposed structure and topography, are important determinants of ground-water flow, aquifer.
The Cenozoic fill of the Gulf of Mexico basin contains a continuous record of sediment supply from the North American continental interior for the past 65 million years. Regional mapping of unit thickness and paleogeography for 18 depositional episodes defines patterns of shifting entry points of continental fluvial systems and quantifies the Cited by: Sand-body geometry and depositional systems, Ogallala Formation, Texas.
Austin (Texas): The University of Texas at Austin; Bureau of Economic Geology. Report of Investigations No. 36 p. Geological Sciences Theses and Dissertations Abstracts: The Theses and Dissertations Abstracts from to are from masters and dissertations completed at the University of Texas at Austin in the field of Geological Sciences.
See the Theses and Dissertations Index: for a more concise listing of authors and titles. Bulletin of the Texas Archaeological Society – Creel, Darrell G.
A Study of Prehistoric Burned Rock Middens in West Central Texas. Ph.D. diss., Department of Anthropology, University of Arizona, Tucson.
Cronin, James G. Ground Water in the Ogallala Formation in the Southern High Plains of Texas and New Mexico. U.S. The barrier-is- land sand body, which is the largest and most significant of the three, is long (usually tens of miles)and narrow (2—6 mi or km), is oriented parallel with the coastline, and attains maximum thicknesses of ft ( m).
An aquifer is an underground layer of water-bearing permeable rock, rock fractures or unconsolidated materials (gravel, sand, or silt).
Groundwater can be extracted using a water study of water flow in aquifers and the characterization of aquifers is called d terms include aquitard, which is a bed of low permeability along an .Ogallala The Ogallala occurs at the surface in most of the Texas Panhandle area.
The Ogallala is composed of clay, silt, fine to coarse sand, gravel and caliche. Generally, individual beds, lenses, sand, or gravel cannot be traced over long distances. The formation ranges in thickness from 0 .Paper/report: Kaiser, W.
R., Johnston, J. E., and Bach, W. N.Sand-body geometry and the occurrence of lignite in the Eocene of Texas: The University of Texas at Austin, Bureau of Economic Geology Geological Circular19 p.