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Monday, May 11, 2020 | History

2 edition of Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area found in the catalog.

Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area

Robert W. Baumgardner

Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area

by Robert W. Baumgardner

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  • 7 Currently reading

Published by University of Texas at Austin in Austin, TX .
Written in English

    Subjects:
  • Geology -- Texas -- East Texas Basin -- Remote sensing,
  • Geology -- Louisiana -- Remote sensing,
  • Landsat satellites.,
  • Remote sensing.

  • Edition Notes

    StatementRobert W. Baumgardner, Jr.
    SeriesReport of investigations (University of Texas at Austin. Bureau of Economic Geology) -- no. 167.
    Classifications
    LC ClassificationsTEXASRI#167 1987
    The Physical Object
    Paginationiv, 26 p. :
    Number of Pages26
    ID Numbers
    Open LibraryOL22073121M
    LC Control Number88-623612

    Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area. Report of investigations no. Austin: The University of Texas at Austin, Bureau of Economic Geology. 26 pp. Bernard, H. A. Landsat-based lineament analysis, east Texas basin and Sabine Uplift area. The University of Texas at Austin, Bureau of Economic Geology, Berg, R. R.

    Effects of Hydrostratigraphy and Basin Development on Hydrodynamics of the Palo Duro Basin, Texas: RI Origin and Evolution of Deep-Basin Brines, Palo Duro Basin, Texas: RI Landsat-Based Lineament Analysis, East Texas Basin and Sabine Uplift Area. Comprehensive, peer-reviewed reports of Bureau research on energy and the environment in Texas, the U.S., and internationally, from to the present.

    PS Basin Modeling and Petroleum System Analysis in the Easternmost Hammerfest Basin – Barents Sea, Anindito Satrio Baskoro, Dicky Harishidayat, and Stephen John Lippard, # (). Analyzing Reservoir Architecture of Isolated Carbonate Platforms, by Phillip Bassant and Paul M. (Mitch) Harris, # (). River Basin Regional Studies; STATEMAP Project Maps; Thematic Maps; Digital Data. Disks with Text; CD-ROMs or CD-ROM Sets; Teachers & the Public. Down To Earth (DE) Educational Materials (EM) Guidebooks (GB) Color, Poster-sized Maps (BX, MM) Color Posters (EM) Color, Wall-sized Texas Maps (SM) Postcards (MM) Mineral Resource Circular (MC.


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Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area by Robert W. Baumgardner Download PDF EPUB FB2

Baumgardner, R. W.,Landsat-Based Lineament Analysis, East Texas Basin and Sabine Uplift Area: The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations No.26 p.

RI Landsat-Based Lineament Analysis, East Texas Basin and Sabine Uplift Area, by R. Baumgardner, Jr. 26 p., 18 figs., 5 tables, ISSN: X: Print Price: $4.

Get this from a library. Landsat-based lineament analysis, East Texas Basin and Sabine Uplift area. [Robert W Baumgardner].

Straightness morphological pattern of spread and intensity level of tectonic deformation by the force in the research area is obtained by calculating the count lineament. The eastern Gulf of Mexico province (GOM) contains the following elements: Sabine uplift, East Texas Salt Basin, San Marcos arch, south Texas area, Sabinas Basin, Burgos Basin, Burro-Salado arch, Tamaulipas arch, Magiscatzin Basin, Tampico-Misantla Basin, Coahuila block, the eastern Sierra Madre Oriental (SMO), Valles-San Luis Potosí and.

Loei area, the major province of NE Thailand close to Laos (Fig. 1), has been a focus of interest for several ScienceAsia 30 (): Lineaments Analysis Determined from Landsat Data Implication for Tectonic Features and Mineral Occurrences in Northern Loei Area, NE Thailand Kachentra Neawsuparp1,2* and Punya Charusiri1*.

ted by the information yielded by this lineament den-Fig. Lineament density contour map based upon lineament network labelled B in Fig. Isoline intervals are 1,2,3 and 4%. sity contour map (bearing in mind field Geology data) may be easily interpreted in terms of the pre­ senee of a NE trending sheared area close to.

Geology Mapping and Lineament Visualization using Image Enhancement Techniques: Comparison of Landsat 8 (OLI) and Landsat 7 (ETM+) M. Mwaniki a* aDepartment of Geomatics Engineering and. The Impact of Heat Flow Variations in Shale Gas Evaluation: A Haynesville Shale Case Study Uplift area, East Texas and every uplift event over the Sabine Uplift area.

Laboratory analysis. analysis the data from the lineament map. DISCUSSION OF RESULTS LENGTH OF LINEAMENT IN THE STUDY AREA Table 1 reveals that the length of the lineament ranges from km to km (Figure 3). Figure 4 shows the distribution of lineament in the study area. The total area of the lineament on the imagery is km, while the total area.

The EROS Architecture Study Team (EAST) strategy for assessing user needs and requirements has certainly considered the typical categories of user classification, but has also paid special attention to current and future uses in terms of data volume, types of science data or information products used, and access/distribution requirements.

Visual Interpretation of LANDSAT imagery of Eastern Ghats-Godavari delta area on scaleon spectral bands 5 and 7 was attempted.

A neotectonic and geomorphic map was prepared from these images showing among other features major and minor lineaments. The importance of some of these lineaments for sedimentation, oil migration and localisation Author: D.

Rao. area containing semi arid and highland characteristics. Therefore, Landsat 7 (ETM+, ) and Landsat 8 (OLI, ) were compared in determining suitable bands suited for geological mapping in the. Subsurface fractures and their relationship to stress history in East Texas basin sandstone.

Tectonophysics, Subsurface fractures were sampled with more than m of core from the Lower Cretaceous Travis Peak Formation, a tabular sandstone and shale unit approximately m thick that was deposited in the gradually subsiding Gulf Cited by: Lineament Analysis of Qatar Peninsula Based on Landsat Imagery The synoptic view of the Landsat satellite images (Km x Km) facilitates delineating the lineaments of regional extent that cannot be recognized by field observation work or it.

Geology of the Lower Cretaceous Travis Peak Formation, East Texas. Depositional history, diagenesis, structure, and reservoir-engineering implications. Topical report, November February Baumgardner, R. W., Jr.,Landsat based lineament analysis, East Texas Basin and Sabine Uplift area: The University of Texas at Austin, Bureau of Economic Geology Report of Investigations No.

26 p. Landsat-Based Lineament Analysis, East Texas Basin and Sabine Uplift Area, Robert W Baumgardner X Re a Phukalla: Gr 9: Teacher's Guide, S. Motibe, M. Modibedi, D.

Mafatle Broadway showstoppers, Carol Cuellar, David C. Olsen. GCD. Lineament Analysis Based on Landsat Imagery, Texas Panhandle - Downloadable PDF. Part Number GCD. Lineament analysis based on Landsat imagery, Texas Panhandle. Austin, Tex.: Bureau of Economic Geology, University of Texas at Austin.

Chicago / Turabian - Author Date Citation (style guide) Finley, Robert J and Thomas C. Gustavson. Lineament Analysis Based On Landsat Imagery, Texas Panhandle. Geological interpretation of the area northwes tof Poona was carried out with the help of Multiband LANDSAT-1 imagery. An area of about sq.

km which is exclusively covered by the Deccan Trap basalts was selected to study the lineament pattern. The interpretation was mainly carried out on a scale ofIt has been observed that N50°E Author: V. V. Peshwa, A. G. Desai.Landsat Based Lineament Analysis East Texas Basin and Structural History of the Sabine Uplift Area East Texas and North Louisiana: Baumgardner, R.

W., Jr., Jackson, M. L. W. Hydrogeologic Characterization of the Saline Aquifers, East Texas Basin-Implications to Nuclear Waste Storage in East Texas Salt Domes: Texas: The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, no.89 p. Baumgardner, R. W., Jr.,Landsat based lineament analysis, East Texas Basin and Sabine Uplift area: The University of Texas at Austin, Bureau of Economic Geology Report of Investigations No.26 p.