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Wednesday, July 29, 2020 | History

3 edition of Geology of the eastern part of the Marathon Basin, Texas found in the catalog.

Geology of the eastern part of the Marathon Basin, Texas

Philip Burke King

Geology of the eastern part of the Marathon Basin, Texas

by Philip Burke King

  • 279 Want to read
  • 16 Currently reading

Published by U.S. Govt. Print. Off., for sale by the Supt. of Docs., GPO in Washington .
Written in English

    Places:
  • Texas,
  • Marathon Basin.
    • Subjects:
    • Geology -- Texas -- Marathon Basin.

    • Edition Notes

      Bibliography: p. 39-40.

      Statementby Philip B. King.
      SeriesGeological Survey professional paper ;, 1157, Geological Survey professional paper ;, 1157.
      Classifications
      LC ClassificationsQE168.M36 K49
      The Physical Object
      Paginationiii, 40 p. :
      Number of Pages40
      ID Numbers
      Open LibraryOL4239787M
      LC Control Number80607171

      Marathon Basin, Texas R.M. Flores and D.H. Hanselman TEXAS POCKET OF BOOK Plate I Geology of the Finlay Mountains Samples and Core Library Listings of Wells Drilled in the Midland Basin and Eastern Shelf Texas Bureau of Economic Geology POCKET Field Conference Route Map R. Laury(Plate 1); Geology of the Type Area, Canyon Group, North File Size: KB. AAPG Datapages/Archives. Welcome Guest. Login as a different user Home > Browse Collections > Abilene Geological Society > Book/Publication Combined Publications Database Abilene Geological Society. Abstract Geological Contributions , Pages Eastern Shelf of the Permian Basin. Jack E. Mergele. View the First Page. A text.

      A boulder bed unit in the upper Haymond Formation (Pennsylvanian), generally believed to be olistostromes, is exposed in the eastern Marathon Basin, west Texas. Two localities of this unit (Housetop Mountain and Clark Butte) contain clasts derived from several formations found within the basin, as well as exotic Devonian metamorphic and. West Texas and New Mexico, the ancestral basin that developed was called the Tobosa Basin. While the shelf deposits of limestone, dolomite and shale were robust, the deep ocean basin, called the “Marathon Basin”, that formed between the opening gulf between South America and N.A. was starved of Size: 2MB.

      Diagrammatic sketch of the slope beds of Stops showing carbonate textures and fabrics encountered along this part of the trail and location of stops relative to elevation markers and geographic features. S trail and thin-section photographs. S trail and thin-section photographs. S basal reef. Stop @article{osti_, title = {Structural geology of the Sunset Lake slice, Taconic fold thrust belt, western Vermont}, author = {Carpenter, D. and Day, K.}, abstractNote = {The Sunset Lake slice is purported to be the lowest thrust sheet in the Taconics. Only a small area is underlain by this thrust sheet and the region has remained unmapped since the regional compilation by Zen.


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Geology of the eastern part of the Marathon Basin, Texas by Philip Burke King Download PDF EPUB FB2

Additional Physical Format: Online version: King, Philip B., Geology of the eastern part of the Marathon Basin, Texas (OCoLC) Geology of the eastern part of the Marathon Basin, Texas (DLC) (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Philip B King; Geological Survey (U.S.).

Geology of the eastern part of the Marathon Basin, Texas. Geology of the eastern part of the Marathon Basin, Texas: Series title: Professional Paper: Series number: DOI: /pp Edition-Year Published: Language: ENGLISH: Description: 40 p.; 1 plate in pocket: Part or all of this report is presented in Portable Document.

Geology of the eastern part of the Marathon Basin, Texas (Geological Survey professional paper) [King, Philip Burke] on *FREE* shipping on qualifying offers. Geology of the eastern part of the Marathon Basin, Texas (Geological Survey professional paper)Author: Philip Burke King.

The Marathon Uplift is a Paleogene-age domal uplift, approximately 78 miles ( km) in diameter, in southwest Texas. The Marathon Basin was created by erosion of Cretaceous and younger strata from the crest of the uplift.

Northeast trending ridges of pre-Permian Paleozoic strata in the basin were formed by the Ouachita orogeny, which also formed the Ouachita District: Brewster County. Hydrogeology of the Marathon Basin Brewster County, Texas Richard Smith1 Introduction The Marathon Basin lies in the northeastern part of Brewster County in western Texas (fig.

The region, referred to as Trans-Pecos Texas in the literature, is in the westward-projecting part of the state that lies along the Rio Grande west of the Pecos. Mountains, Marathon Basin, Solitario, and at Persimmon Gap. These rocks represent a transgressive, then regressive, marine sequence that was caught between the North American continent and another unidentified continent during the Pennsylvanian and intensely deformed and thrust onto North America forming the Marathon-Ouachita Size: 1MB.

MAIN LIBRARY. Perry-Castañeda Library East 21st St. Austin, TX. Phone: () Preliminary Report on Observations on the Sacramento Mountains of New Mexico Made During the Latter Part of Confidential Study: No: Marathon Basin Area, Brewster, Co., Texas, May Guidebook: Hueco and Franklin Mountains, Texas, April Guidebook: Eastern Edge of Permian Basin, Texas, May Guidebook: 2 Texas The Geology of Texas Section Texas.1 Summary Learning about the geology of Texas provides local examples of the main themes of physical geology, espe-cially the theory of plate tectonics.

Texas has abundant geologic resources, including petroleum, coal, minerals, groundwater, and fertile soils. 9/8/06 PM Page 2File Size: 3MB. The geology of the DFW Metroplex consists of gently tilted sediments of mostly Cretaceous age, which also obscures a much older geologic record.

Sediments older than Cretaceous can only be found at the surface in the extreme western part of the DFW Metroplex, in the area around Weatherford, Texas.

Pub. Id: A () First Page: Last Page: Book Title: SP Habitat of Oil Article/Chapter: Oil and Geology in the Permian Basin of Texas and New Mexico: North America Subject Group: Basin or Areal Analysis or Evaluation Spec.

Pub. Type: Special Volume Pub. Year: Author(s): John E. Galley (2) Abstract: Pre-Mississippian strata in the Permian. McBride, E. F., Ed. / A GUIDBOOK TO THE STRATIGRAPHY, SEDIMENTARY STRUCTURES AND ORIGIN OF FLYSCH AND PRE-FLYSCH ROCKS OF THE MARATHON BASIN, TEXAS, Dallas,pb, pages, 50 figs., - 3 - $ 10 [This is.

Geology of the Marathon region, Texas: Series title: Professional Paper: Series number: DOI: /pp Edition-Year Published: Language: ENGLISH: Description: p. Google Analytic Metrics: Metrics page: Part or all of this report is presented in Portable Document Format (PDF).

For best results viewing and printing PDF. Buy Sedimentary petrology and history of the Haymond formation (Pennsylvanian), Marathon Basin, Texas on FREE SHIPPING on qualified orders. Alexander Deussen, Geology of the Coastal Plain of Texas (Washington: U.S.

Department of the Interior, ). Ross A. Maxwell, Geologic and Historic Guide to the State Parks of Texas (Bureau of Economic Geology, University of Texas at Austin, ).

Samuel D. Myres, The Permian Basin: Petroleum Empire of the Southwest (2 vols., El Paso: Permian,). Senior Geologist, Shell Oil Company. The author wishes to acknowledge his gratitude for the interest and encouragement of Thomas A. Hendricks and the late John G. Bartram, who first suggested to him the presentation of this paper, and of the late E.

Russell Lloyd, whose kindly criticisms and friendly advice were a constant aid during its preparation. Marathon Basin.—Marathon, Texas, is a small village on the Southern Pacific Railway and U.

Highway The town is near the center of a large topographic depression, the Marathon Basin, which is crossed by U. Highway 90 from east to west and U. Highwayfrom Marathon to the Park, on the south. Flood Geology Challenge #7: The East Texas Basin is one of the three interior basins of the greater Gulf Coast Basin.

It covers the majority of the eastern third of the state of Texas. The history of the basin rightly starts in the early Mesozoic. In the Triassic the basin began rifting with the axis of extension trending NNE-SSW. Subscribe to our Newsletter Give to the Libraries © The University of Texas at Austin.

Rapid basin subsidence and sedimentary filling took place during this phase. Broad carbonate shelves became established on the western, northern, and eastern margins of the Permian Basin and Central Basin Platform as a result of its equatorial location during this phase.

Clastics meanwhile dominated in the basins. By Late Paleozoic time the original .RID. Geology of the Solitario Dome, Trans-Pecos Texas: Paleozoic, Mesozoic, and Cenozoic Sedimentation, Tectonism, and Magmatism.

The Solitario lies in the eastern part of the Basin and Range province. It occupies a relatively unfaulted block surrounded by Basin and Range normal and strike-slip faults. W. R., editors,Geology.outcropping rocks present in the Marathon Basin, a topographic basin located on the Marathon uplift.

I would like to acknowledge the assistance of the Texas Bureau of Economic Geology as well as that of wide in the eastern part to more than 25 mi wide in the western part.

The northern play boundary is.