Remote sensing for resources development and environmental management: Remote sensing for resources development and environmental management

damen, m. c. j.

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Multivolume work

Persistent identifier:: 856342815

Title:: Remote sensing for resources development and environmental management

Sub title:: proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986

Year of publication:: 1986

Place of publication:: Rotterdam; Boston

Publisher of the original:: A. A. Balkema

Identifier (digital):: 856342815

Language:: English

Additional Notes:: Volume 1-3 erschienen von 1986-1988

Editor:: Damen, M. C. J.

Document type:: Multivolume work

Volume

Persistent identifier:: 856641294

Title:: Remote sensing for resources development and environmental management

Sub title:: proceedings of the 7th international Symposium, Enschede, 25 - 29 August 1986

Scope:: IX Seiten, Seiten 551-956

Year of publication:: 1986

Place of publication:: Rotterdam; Boston

Publisher of the original:: A,. A. Balkema

Identifier (digital):: 856641294

Illustration:: Illustrationen, Diagramme

Signature of the source:: ZS 312(26,7,2)

Language:: English

Usage licence:: Attribution 4.0 International (CC BY 4.0)

Editor:: Damen, M. C. J.

Editor:: International Society for Photogrammetry and Remote Sensing, Commission of Photographic and Remote Sensing Data

Publisher of the digital copy:: Technische Informationsbibliothek Hannover

Place of publication of the digital copy:: Hannover

Year of publication of the original:: 2016

Document type:: Volume

Collection:: Earth sciences

Chapter

Title:: 5 Non-renewable resources: Geology, geomorphology and engineering projects. Chairman: J. V. Taranik, Liaison: B. N. Koopmans

Write comment:: Wegen zu enger Bindung kommt es teilweise im Original zu Textverlust.

Document type:: Multivolume work

Structure type:: Chapter

Chapter

Title:: Remote sensing methods in geological research of the Lublin coal basin, SE Poland. Stanislaw Kibitlewski & Barbara Daniel Danielska

Document type:: Multivolume work

Structure type:: Chapter

Figure 6. Landsat lineament pattern in relation to faults: 1 -lineaments, 2 -faults in the top of Pala- eozoio /after ¿eliohowski 1972/. Figure 7. Landsat lineament pattern in relation to faults: 1 -lineaments, 2 -faults in the top of Pala eozoic /kindly was made available by Zdanowski and Porzyoki in 1983/. Figure 9.-1 /In km/km , n - 1,0*0,: Cainozolo fault pattern /Fig.5,8/, It is difficult, however, to prove a direot coincidence of these linea ments with the elements of even deeper structural horizons. They might be, however, indirectly related if the Meso-Cainozoio fault pattern corresponds to the main dislocations / faults / in Palaeozolo /Fig. lia, lio/. . In the area examined it seems to be true at least in a case of Kock horst antioline. Its general struc tural pattern, as well as that of a system of dislo cations parallel, transversal and/or oblique to this unit, have - to some extent - their homologues in the Meso-Cainozoio faulting pattern. It is to be stated that the most important faotor influencing the radar lineaments pattern /with varia- ted intensity in different morphogenetic units/ seems to be the teotonios of the Upper Cretaoeous brittle rooks i.e. direotly - by simple projection of the faults on surfaoe, or indireotly - by the influence of sub-Quatemary relief on later sedimentation. This first oase of influence seems to be the most distinot i.e. easily observable in the remote sensing images in the areas of the lithologloally homogeneous surfa oe cover /e.g. loess/, less distinot in the lithologi cally differentiated surface deposits /e.g. glaoial sediments /Fig,10, 11a/. 6.2 Geologioal interpretation of the Landsat data The pattern of Landsat lineaments displays regular unoomplioated distribution in the region in question /Fig.12/. The maximum density of the lineaments occurs in the following areas: the south-western part of Kook horst anticline and north-eastern region adjaoent to it - the area corresponding to the axial part of Stoozek - Dorohucza syncline /Pig.l2,2B/. The sate] whioh exter ly form th( of NW-SE /1 ENE-WSW /7< vail. The firsl /MW-SE ori* ral direct] i.e. in thi rzyn-Abrank huoza depr« sponds to \ perpendloui well devel< to this hoi Basing ot terpretati« reoognitiot C Figure 10. a -for the for the art with lake ¡

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