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

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Chapter

Title:: Geological analysis of the satellite lineaments of the Vistula Delta Plain, Zulawy Wislane, Poland. Barbara Daniel Danielska & Stanislaw Kibitlewski, Andrzej Sadurski

Document type:: Multivolume work

Structure type:: Chapter

Figure 2. Geologioal structure of basement. A - orystalline basement: a -oontours of a top surfaoe /in meters, after Kubioki,Ryka 1982/, b -faults, o - llthologioal boundaries. Lithology /after Karaczun, Kubicki,Ryka 1982/: 1 -granitoids, 2 -unsubdivided gneisses, 3 -unsubdivided gneisses and eunphlbolites, 4 -pyroxene gneisses and eunphlbolites, 5 -unsubdivi- ded migmatites, 6 -pyroxene migmatites, 7 -anateotio and palingenetio granitoids, 8 - rapakivi like grani toids. B - Zeohstein-Mesozoio series /after Dadlez 1980/; a -oontours of basal surfaoe of series /in m/, b -oon tours of the base of Upper Cretaceous, o -faults pene trating lower part of the series /mainly Zeohsteln or Zeohstein and Triassic/, d -faults outting the whole series. Both structural surfaces inclined southwards. 3 GEOLOGICAL SETTING In the Vistula Delta Plain area the orystalline base ment of the peri-Baltio syneollze lies at depth of about 3500m /in the east/ and more than 4000m /in the west of the area/ - Karaczun,Kubioki,Ryka 1982. The faulting character and wide-radius downwarps and uplifts of the top surface of the basement seem to in fluence the development of the later sedimentary oover of the platform. The top surfaoe of Lower Palaeozolo oover ooours at the depth of about 1500m /in the northern part/ to about 2000m /in the southern part of the area/ - Fig.2A. The Zeohstein-Mesozoio series represents the follo wing part of the geologioal seotion, the lower part of whioh displays some big faults /Dadlez 1980/ - Fig.2B. The upper part of the series is built up of oaloareous and oaloareous- silloeous deposits of Upper Cretaceous /Turonian to Maestrichtian in age/. These brittle se diments underlie, in turn, the loose and soft Caino- zoio sedimentary oover the thickness of whioh varies from 50m /in Gdansk vicinity/ up to 200m /east- and southwards from Gdansk - in Tozew and Malbork region/. Top surfaoe of the Upper Cretaceous series occurs at the depth of approximately 90m dipping gradually eastwards and westwards reaohing the morainio plate aux. It displays a dlstlnot relief due to an intensi ve erosion, possibly facilitated by the faults -Fig.3. The looal small faults are indentlfied in the numerous geoteohnioal works basing, however, only on analysis of denivelations of Cretaoeous strata observed in boreholes /dojskl 1976/, In the area of Zulawy Wiálane /Vistula Delta Plain/ the Tertiary series overlies the Upper Cretaoeous se diments. This series has been looally strongly eroded too, due to the erosion and exaration whioh aoted at Tertiary/Quaternary boundary as well as in Pleistoce ne, affooting - in the distlnot area - even the young est Upper Cretaoeous strata /Fig.4/. The sediments of three glaoiation and the deltaio Holooene ones build the Quaternary oover. Pleistooene series seems to have very oomplioated inner struoture what results from a combined influenoe of the diffe rent prooesses varlated in time and spaoe, as: different kinds of accumulation /glaoial, marginal, marine, fluvial/, erosion and exaration, glaciteoto- nlos and possibly - tectonics. The thiokness of the Pleistooene sediments equals in the 2ulawy area approx. 70m. Their top inclines slightly northwards. In fculawy area the relief of sub-Holocene series is in details insufficiently recognized. Pleistooene sedi ments surfaoe is eroded and buried with Holooene depo sits of thiokness from 0 to 20m /increasing north- and eastwards/. These deposits compose the deltaio plain at the altitudes from about lm b.s.l. to lm a.s.l. Figure 3. Top surface of Cretaoeous series; 1 -bounda ry of morainio plateaux, 2 -oontours of top surfaoe of Cretaoeous series /in m b.s.l./, 3 -boreholes and cross-seotion lines. Figure 4. of morain ce /in m b -Tertia The pre the Holoc /Mojski i peats and Its dev two stage Tertiary, ting the 1 ones a wi has survi the devel tion/ of The depre: ne - desp that last eroded an glaoiatioi glaoiisos level of i oession o of the er uplift of period/, - - due to i The las vial acoui of sedimei ness of tl were acoui goon form from the i sediments It resu sion on ol ned such 1 Cretaoeoui nature of -Quaternai the Quatei 4 ANALYSIS The foil« of top sui of lower i as well a: occurence

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