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

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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

619 Symposium on Remote Sensing for Resources Development and Environmental Management / Enschede / August 1986 Remote sensing methods in geological research of the Lublin coal basin, SE Poland Stanislaw Kibitlewski & Barbara Daniel Danielska Photogeological Department, Geological Institute, Warsaw, Poland ABSTRACT! Some connections were found comparing the patterns of lineaments obtained from Landsat images and side' looking radar /Toros/ ones with faults in Lublin coal basin area /LCB/, SE Poland. It concerns the satel lite lineaments pattern and the radar one corresponding to the Upper Palaeozoic- and Meso-Cainozoic faults, respectively. The conclusions suggest possibility of projection onto the reoent surface the deep linear struc tures through the thick sedimentary cover which consists of soft and loose deposits - in LCB region. 1 INTRODUCTION In the papers on photogeo logy there exist many eviden ces of a tectonic character of lineaments observed on the different remote sensing images of the structu rally controlled areas exposed in a geological sense. Many geologists treat sceptically such opinions when they concern the regions covered with a thick layer of soft and loose sediments especially in relation to lineaments in a local or subregional scale. Big linea ments - of regional or transcontinental quality - seem to be, however, accepted as the traces of featu»- res of tectonic origin despite of the nature of their host rock. The great part of territory of Poland has been cove red with soft and loose thiok Cainozoio sediments which bury older structures and render these structu res recognition difficult using standar methods. That is why it seems to be of special significance here to apply the photogeologioal data as possible indicators of tectonic phenomena /i.e. faults/. The paper presents the results of a test done in aim to estimate the significance of an appication of the satellite Landsat images and airborne side-looking ra dar images /of Soviet system Toros/ to examination of the geological structure of coal-bearing region near Lublin, SE Poland. 2 TEST DESCRIPTION To check out a coincidence between remote sensing da ta and the geological ones the test has been done in an entirely small area chosen in respect to geological recognition. The area tested covered all the characte ristic structural units of the Lublin coal basin in aim to extrapolate the testing results to the whole basin - in case of positive resuts of the test. In that very case it would be also possible to introduce photogeological data to the construction and gradual improvement of the structural model still existing. The Lublin coal basin area is oovered by the thick Cainozoic sediments and displays either block-faulting or block-folding character of the inner structure /fteliohowski 1972, Bojkowski and Porzycki I960/. It is geologically well recognized at the several depths due to a black-coal mines development. 3 GEOLOGICAL CHARACTER OP THE AREA Lublin coal basin is situated in the south-west margi nal part of East—Europeon platform in the region bet ween Vistula and Bug rivers /Fig.l/. The terrigenic sediments of Upper Proterozoic platform /zonally pre served/ lie on the crystalline complex of Lower Prote rozoic, top of whioh plunges from about 1000m b.s.l.— in NE part, to 7000m-in SW part, Pig.2A/. The following overlying strata of Lower Palaeozoic /of total thick ness of 950-2500m/ are represented by the terrigenic sediments of Lower and Middle Cambrian and/with depo- sitional gaps/ those of Ordovician and Silurian. The sediments are folded only in the zone of Caledonian movements adjacent from 37/ to the platform margin /outside the area tested/ - Fig.3. Figure i. Scene: E-30087-08451 MSS-5,31 May 1978. In vestigated area and image position are marked. The platform conditions occur in the whole territo ry discussed since Devonian. The Lower Devonian sedi ments are terrigenic, while Middle and Upper Devonian ones are suooesively those of lacustrine-marine and terrigenic, partially carbonate /i.e.dotomitic/ as well. The Devonian sediments thickness varies from 1590 to 6300m. Their top surface occurs recently from 800m b.s.l. in the NE part of the studied area down to 2600m b.s.l. in the SW part of it. Due to the Bretonian movements distinct system of horst and grabens with NIV-SE and S'MJE orientation and high amplitude has been developed. The NiV-SE orientation seems to prevail in S’" part of the area under investigation while that SW-NE - in NE part. Those structures have been intensively eroded prior to Carboniferous sedimentation.

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