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Chen Changming, Mang shonsong, Liang Ruiren, Van Gelder. CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS[J]. Acta Sedimentologica Sinica, 1986, 4(4): 73-86.
Citation: Chen Changming, Mang shonsong, Liang Ruiren, Van Gelder. CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS[J]. Acta Sedimentologica Sinica, 1986, 4(4): 73-86.

CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS

  • Received Date: 1986-03-01
  • Publish Date: 1986-12-10
  • A series of constructjon pits along the Iower Rhine-Mass rivers revealed the subre- cent deposits in different subenviroaments from tidal dominated systems to fluvial do- miaated systems, This makes it possible to study the properties of these sediments. The sedimentary structures of these deposits are examined and compared by sampling a series of lacquer peels.
  • [1] Allen, J.R.L.,1968, Current ripples, Their relation to patterns of water and sediment motion, Amsterdam, North-Holland Publ, Comp.
    [2] Boersma, J.R.,1967, Geol, Mijnb.,V, 46, P. 217-135.
    [3] Boersma, J.R.,1969,I Gaol. Mijnb.,V, 48, P. 409-414.
    [4] Guy, H.H._,Simons, D.B.and Richardson, E.V.,1966, U.S, Geo}sSurv·,Pro-fess, Papers 462-1.
    [5] Klein, G, deV.,1977, Clastic tidal facies, CEPCO, Champaign, Illinois.
    [6] Reading, H.G.,1982, Sedimentary environments and facies, Blackwell Scienti-fic publication, Oxford.
    [7] Reineck, H.E.,1963, Abhandl, Senckn. Nat Gesell.,V, 505, N, 1,P.138.
    [8] Reineck, H.E.et al.,1968, Sedimentology, V, 11, P, 99-104,
    [9] Reineck, H.E.and Singly I.B.,1980, Depositional sedimenfary environments,2ed, Sprin$er-Verlag Berlin, Heidelberg.
    [10] Simons, D.B.and Richardson E.V.,1962, Am, Soc. Civ. Eugrs. Trans.,V,127, P. 923-953.
    [11] Simonsy D_.B.,Richardson, E.V.and Nordin, C.F.,1965, SEPM Spec, Publ., V, 12, P. 34-52,
    [12] Terwindt,J.H.J.,1981,Origin and sequenees of sedimentary structures in in-shore mesotidal deposits of the North Sea, In: Holocene Sedi-meat.,5, Blackwell Scientific Publication,Oxford.
    [13] Yisser,M.J.,1980,Geology,V. 8,P, 543-b46.
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  • Received:  1986-03-01
  • Published:  1986-12-10

CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS

Abstract: A series of constructjon pits along the Iower Rhine-Mass rivers revealed the subre- cent deposits in different subenviroaments from tidal dominated systems to fluvial do- miaated systems, This makes it possible to study the properties of these sediments. The sedimentary structures of these deposits are examined and compared by sampling a series of lacquer peels.

Chen Changming, Mang shonsong, Liang Ruiren, Van Gelder. CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS[J]. Acta Sedimentologica Sinica, 1986, 4(4): 73-86.
Citation: Chen Changming, Mang shonsong, Liang Ruiren, Van Gelder. CHARACTERISTICS OF SEDIMENTARY STRUCTURES IN DIFFERENT SUBENVIRONMENTS FROM FLUVIAL DOMINATED SYSTEMS TO TIDAL DOMINATED SYSTEMS ALONG THE LOELOWER OLD RHINE-MASS RIVERS[J]. Acta Sedimentologica Sinica, 1986, 4(4): 73-86.
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