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Articles 1 - 11 of 11
Full-Text Articles in Physical Sciences and Mathematics
Nebraska Groundwater Level Map (Decline & Rise), Fall 1963
Nebraska Groundwater Level Map (Decline & Rise), Fall 1963
Conservation and Survey Division
No abstract provided.
Stratigraphic Analysis Of The Queen And Grayburg Formations, Southeastern Chaves County, New Mexico, James L. Mcswain
Stratigraphic Analysis Of The Queen And Grayburg Formations, Southeastern Chaves County, New Mexico, James L. Mcswain
Earth and Planetary Sciences ETDs
The area of study lies in southeastern Chaves County, New Mexico, and is a part of the northwest shelf or backreef province of the Permian Basin. The area encompasses all or parts of Tps. 10 through 15 S., Rs. 24 through 31 E.
The Queen and Grayburg formations comprise the lower part of the Artesia group, an upper Guadalupian sequence of Permian shelf rocks above the San Andres formation and below the Ochoan series. The Queen-Grayburg sequence has an average thickness of about 600 feet and is correlative with the Goat Seep reef at the margin of the Delaware Basin, …
Lithostratigraphy And Correlation Of The Mississippian System In Nebraska, Marvin P. Carlson
Lithostratigraphy And Correlation Of The Mississippian System In Nebraska, Marvin P. Carlson
Conservation and Survey Division
The purpose of this study is to describe and correlate rocks of Mississippian age within the state of Nebraska. Shales, generally classified as "Chattanooga" and commonly referred to as Devonian or Mississippian in the northern Mid-Continent, have been included in this study, although these shales are more generally believed to be Devonian and not Mississippian by most stratigraphers and paleontologists at the present time. Since rocks of Mississippian age are present only in the subsurface of Nebraska, the basic information for this report is derived from the microscopic study of cuttings and cores from test wells drilled within the state.
Water Levels In Observation Wells In Nebraska, 1962, Philip A. Emery, Mildred M. Malhot
Water Levels In Observation Wells In Nebraska, 1962, Philip A. Emery, Mildred M. Malhot
Conservation and Survey Division
No abstract provided.
Beitraege Zur Geologie Der Kelki̇tlinie Und Zur Stratigraphie Des Jura Im Gebiet Kelki̇t-Bayburt (Gümüşane), Hartmann Wedding
Beitraege Zur Geologie Der Kelki̇tlinie Und Zur Stratigraphie Des Jura Im Gebiet Kelki̇t-Bayburt (Gümüşane), Hartmann Wedding
Bulletin of the Mineral Research and Exploration
No abstract provided.
Allgemeine Stratigraphie Des Karbons In Der Umgebung Von İstanbul, Fuat Baykal, Orhan Kaya
Allgemeine Stratigraphie Des Karbons In Der Umgebung Von İstanbul, Fuat Baykal, Orhan Kaya
Bulletin of the Mineral Research and Exploration
No abstract provided.
Relationship Of Igneous Activity To Mineral Deposits In Arkansas, Charles G. Stone, Philip J. Sterling
Relationship Of Igneous Activity To Mineral Deposits In Arkansas, Charles G. Stone, Philip J. Sterling
Journal of the Arkansas Academy of Science
No abstract provided.
Nouvelles Observations Stratigraphiques Et Paleontologiques Sur Les Terrains Paleozoiques Affleurant A L'Est Du Bosphore, Şakir Abdüsselamoğlu
Nouvelles Observations Stratigraphiques Et Paleontologiques Sur Les Terrains Paleozoiques Affleurant A L'Est Du Bosphore, Şakir Abdüsselamoğlu
Bulletin of the Mineral Research and Exploration
No abstract provided.
Hypogene Clay And Mica Minerals Associated With Fault Zones In The Ouachita Mountains-Arkoma Basin Area, Arkansas, Charles G. Stone
Hypogene Clay And Mica Minerals Associated With Fault Zones In The Ouachita Mountains-Arkoma Basin Area, Arkansas, Charles G. Stone
Journal of the Arkansas Academy of Science
No abstract provided.
Geology Along A Portion Of Highway 23, Madison County, Arkansas, J. A. Mcentire Iii
Geology Along A Portion Of Highway 23, Madison County, Arkansas, J. A. Mcentire Iii
Journal of the Arkansas Academy of Science
No abstract provided.
Topographic Regions Maps, J. A. Elder, V. H. Dreeszen, E. C. Weakly
Topographic Regions Maps, J. A. Elder, V. H. Dreeszen, E. C. Weakly
Conservation and Survey Division
No abstract provided.