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

damen, m. c. j.

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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

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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

geological map /Pig,7/ the parallel displacement of the lineaments corresponding faults might be observed. The faot itself can be explained in a different way, namelyj 1 - only a part of the really existing faults has been reoognized and drawn on the geologioal map, 2 - the faults could have displayed different chara cter i.e. an interpreted fault might be only an idea lized image of the wider zone of parallel fault pla nes, only one of which reaches the surface, 3 -several parallel faults oould accompany the main one on the surface as the traces of the seoond order faults, an tithetic faults etc., 4 -in the interval from the deep horizon up to the present surfaoe there oould have oocured a refraction of the fault surfaoe due to the ohanges in lithology what has affeoted an inclination of the fault plane and finally resulted in different location of the traces of this plane in the different stratigraphic horizons and recent surface as well. In the NE side of the Kock horst anticline there occurs a distinct trend of the Landsat lineaments pa rallel to the main fault of the structure under dis- oussion and their shifting north-eastwards /Pig.7/. Since the seismic data interpretation /Zeliohowski 1972/ suggests possibility of NE inclination of the whole Kook horst anticline it is not to be excluded that the parallel "shifting" might reflect this asym metry. Discussion ooncerns the faults seen beneath 800m below the present surface. Taking such an inter pretation into acoount the fault surface under discus sion would be Inclined /dipped 60°SW/. It must be repeated here that the coincidence bet ween geological recognition of the interpreted area in the different regions and Landsat lineament pat terns increases with the better geological recogni tion. That is why the remote sensing Landsat linea ments pattern in the region south-westwards from the Kock horst anticline /i.e. in Stoozek-Dorohuoza de pression distinctly worse recognized/ does not corre spond to the hitherto proposed Palaeozoic fault model. It seems to be possible that in this region Landsat lineaments correspond to the deformations caused by the younger Alpine movements, whioh have not reached Palaeozoic horizon. Still since the geological infor mation might be not complete the disoussion there has rather academic character. The observed fact that the satellite lineaments distinctly correspond to the changes of coal-potential in the discussed depression seems to be, however, one of the most interesting/Fig.13/. Basing on the ooincidenoe of the main satellite li neaments and coal-potential isolines, as well as those transversal ones which reflect the shifting and direc tional ohanges of these isolines it might be suggested that sedimentary Carboniferous trough was already af fected by long-active, synsedimentary movements. Landsat lineaments suggest that also Stoczek-Doro- hucza depression might be stronger faulted them it re sults from the present structural map. The proposed interpretation of the remote sensing data applied to the coal basin recognition demands, however, to be checked in the further geologioal recognition of ooal deposits. 7 PINAL REMARKS As it seen from the faots above a distinct coincidence between Toros radar lineaments, satellite Landsat ones and the geologioal structure of ICB ocours. Radar li neaments seem to be connected with not deep-lying structural horizon /the top surface of brittle Mesozo ic and Lower Tertiary sediments/ and might have some significance for the further geologioal recognition of the oap rocks of the coal-bearing sediments. Prom the other side Landsat lineaments correspond to the geological structure of the Palaeozoic series whioh oontains the coal-bearing sediments. Such the relation is so distinct that basing on the standard geological methods and the remote sensing techniques a creation of a certain model of the structure of the Figure 13. Landsat lineament pattern and coal-poten tial ohanges* 1 -lineaments, 2 -coal-potential isoli nes Aindly was made available by Zdanowski and Porzy- cki in 1983/. area might be postulated. Such the model might be - in particular - in case of Lublin coal basin quickly checked and verified due to the progressive develop ment of the black-coal deposit. In general - the model itself - can be applied to improve the geological recognition of the other coal basins with a comparable geological setting. REFERENCES Bojkowski, K.kJ.Porzycki 1980. Geological problems of coal basins in Poland. Warszawa, Wyd.Geol. Henkiel, A. 1983. Tektonika./Tectonics. In Cainozoio of Lublin Coal Basin.Symposium in Lublin, 9-11.IX/, Kenozoik Lubelskiego Zaglqbia Wqglowego. Lublin, UMCS, p. 41-6*1. - /In Polish only/. Malinowski, J. &J.E.Mojski 1978. Arlcusz Lublin. Mapa Geologiczna Polski 1;200 000 /Sheet Lublin. The Geo logical Map of Poland, 1:200 000/, Warszawa,Inst. Geol. - /Explanation in Polish only/. Mojski, J.E. 1968. Arkusz luk6w. Mapa Geologiczna Pol ski 1:200 000 /Sheet Iuk6w. The Geological Map of Poland, 1; 200 000/. Warszawa Inst.Geol. /Explana tion in Polish only/. Ryka, W. 1983. Map of ore mineralization signs in cry stalline basement rocks 1;500 000. In Atlas of the geological structure and mineral deposits in the Lu blin region, Table 39. Warszawa, Inst.Geol. ¿elichowski, A.M. 1972. Rozw6j budowy geologicznej ob- szaru mi^dzy Gdrami Swiqtokrzyskimi i Bugiem /Eng lish summary; Evolution of the geologioal structure of the area between the G6ry Swiqtokrzyskie and the river Bug/. Bull.IG, 263. Warszawa, Inst.Geol. Zelichowski, A.M. 1983. Tectonic map 1:500 000. In At las of the geological structure and mineral deposits in the Lublin region. Table 34. Warszawa, Inst.Geol.

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