Publications
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Assessment of undiscovered oil and gas resources of the Sud Province, north-central Africa
The Sud Province located in north-central Africa recently was assessed for undiscovered, technically recoverable oil, natural gas, and natural gas liquids resources as part of the U.S. Geological Survey's (USGS) World Oil and Gas Assessment. Using a geology-based assessment methodology, the USGS estimated mean volumes of 7.31 billion barrels of oil, 13.42 trillion cubic feet of natural gas, and 35
Authors
Michael E. Brownfield, T. R. Klett, Christopher J. Schenk, Ronald R. Charpentier, T. A. Cook, R. M. Pollastro, Marilyn E. Tennyson
Provenance and tectonic significance of the Palaeoproterozoic metasedimentary successions of central and nothern Madagascar
New detrital zircon U–Pb age data obtained from various quartzite units of three spatially separated supracrustal packages in central and northern Madagascar, show that these units were deposited between 1.8 and 0.8 Ga and have similar aged provenances. The distribution of detrital zircon ages indicates an overwhelming contribution of sources with ages between 2.5 and 1.8 Ga. Possible source rocks
Authors
B. De Waele, Ronald J. Thomas, P. H. Macey, M. S. A. Horstwood, R. D. Tucker, P. E. J. Pitfield, D. I. Schofield, K. M. Goodenough, W. Bauer, R. M. Key, C. J. Potter, R. A. Armstrong, J. A. Miller, T. Randriamananjara, V. Ralison, J. M. Rafahatelo, M. Rabarimanana, M. Bejoma
New U.S. Geological Survey method for the assessment of reserve growth
Reserve growth is defined as the estimated increases in quantities of crude oil, natural gas, and natural gas liquids that have the potential to be added to remaining reserves in discovered accumulations through extension, revision, improved recovery efficiency, and additions of new pools or reservoirs. A new U.S. Geological Survey method was developed to assess the reserve-growth potential of tec
Authors
Timothy R. Klett, Emil D. Attanasi, Ronald R. Charpentier, Troy A. Cook, Philip A. Freeman, Donald L. Gautier, Phuong A. Le, Robert T. Ryder, Christopher J. Schenk, Marilyn E. Tennyson, Mahendra K. Verma
Pore-throat sizes in sandstones, siltstones, and shales: Reply
In his discussion of my article (Nelson, 2009), W. K. Camp takes issue with the concept that buoyancy is not the dominant force in forming and maintaining the distribution of gas in tight-gas accumulations (Camp, 2011). I will restrict my response to the issues he raised regarding buoyant versus nonbuoyant drive and to a few comments regarding water saturation and production. I claim that the pres
Authors
Philip H. Nelson
Quantifying Lateral Migration of Sequestered Carbon Dioxide Based on Rock Properties and Permeability Classifications
No abstract available.
Authors
Lauri A. Burke
In-place oil shale resources underlying Federal lands in the Green River and Washakie Basins, southwestern Wyoming
Using a geologic-based assessment methodology, the U.S. Geological Survey estimated an in-place oil shale resource of 906 billion barrels under Federal mineral rights, or 62 percent of the total oil shale in place, in the Green River and Washakie Basins, Wyoming. More than 67 percent of the total oil shale in-place resource, or 969 billion barrels, is under Federal surface management.
Authors
Tracey J. Mercier, Ronald C. Johnson, Michael E. Brownfield
Undiscovered hydrocarbon resources in the U.S. Gulf Coast Jurassic Norphlet and Smackover Formations
The U.S. Geological Survey has completed assessments of undiscovered technically recoverable oil and gas resources in the Jurassic Norphlet and Smackover formations of the onshore coastal plain and State waters of the U.S. Gulf Coast. The Norphlet Formation consists of sandstones and interbedded shales and siltstones deposited during a marine transgression. Along its northeast margin, deposition o
Authors
Ofori N. Pearson
Assessment of in-place oil shale resources of the Eocene Green River Formation, a foundation for calculating recoverable resources
The recently completed assessment of in-place resources of the Eocene Green River Formation in the Piceance Basin, Colorado; the Uinta Basin, Utah and Colorado; and the Greater Green River Basin Wyoming, Colorado, and Utah and their accompanying ArcGIS projects will form the foundation for estimating technically-recoverable resources in those areas. Different estimates will be made for each of the
Authors
Ronald C. Johnson, Tracy J. Mercier
Dealing with zeros
No abstract available.
Authors
Josep Antoni Martin-Fernandez, Javier Palarea-Albaladejo, Ricardo A. Olea
Digital archive of drilling mud weight pressures and wellbore temperatures from 49 regional cross sections of 967 well logs in Louisiana and Texas, onshore Gulf of Mexico basin
This document provides the digital archive of in-situ temperature and drilling mud weight pressure data that were compiled from several historical sources. The data coverage includes the states of Texas and Louisiana in the Gulf of Mexico basin. Data are also provided graphically, for both Texas and Louisiana, as plots of temperature as a function of depth and pressure as a function of depth. The
Authors
Lauri A. Burke, Scott A. Kinney, Temidayo B. Kola-Kehinde
Undiscovered petroleum resources for the Woodford Shale and Thirteen Finger Limestone-Atoka Shale assessment units, Anadarko Basin
In 2010 the U.S. Geological Survey assessed undiscovered oil and gas resources for the Anadarko Basin Province of Colorado, Kansas, Oklahoma, and Texas. The assessment included three continuous (unconventional) assessment units (AU). Mean undiscovered resources for the (1) Devonian Woodford Shale Gas AU are about 16 trillion cubic feet of gas (TCFG) and 192 million barrels of natural gas liquids (
Authors
Debra K. Higley
Evolution of overpressured and underpressured oil and gas reservoirs, Anadarko Basin of Oklahoma, Texas, and Kansas
Departures of resistivity logs from a normal compaction gradient indicate that overpressure previously extended north of the present-day overpressured zone. These indicators of paleopressure, which are strongest in the deep basin, are mapped to the Kansas-Oklahoma border in shales of Desmoinesian age. The broad area of paleopressure has contracted to the deep basin, and today the overpressured dee
Authors
Phillip H. Nelson, Nicholas J. Gianoutsos