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Record #121210:

Scoresby Sund, East Greenland: structure and distribution of sedimentary rocks / Gabriele Uenzelmann-Neben.

Title: Scoresby Sund, East Greenland: structure and distribution of sedimentary rocks / Gabriele Uenzelmann-Neben.
Author(s): Uenzelmann-Neben, Gabriele.
Date: 1992[pub.1993]
In: Polarforschung. (1992[pub.1993]), Vol. 62(1) (1992[pub.1993])
Abstract: Reflection seismic investigation allowed refined interpretation of Mesozoic and Cenozoic sedimentary evolution of area. Synsedimentary subsidence is suggested for western part of Jameson Land basin. Two seismic sequences document strong erosion which took place during Cretaceous/Tertiary. Further erosion resulted from development of several glacial phases in Quaternary, leading to very thin (<12 m, even as little at 5 m) cover of Quaternary sediments. Infers that most recent glaciation, developed during Late Weichselian, built up grounded glacier.
Notes:

Polarforschung. Vol. 62(1) :1-9 (1992[pub.1993]).

Keywords: 551.1/.4 -- Geology.
551.3.051 -- Sedimentation and stratification.
551.33 -- Glacial geology.
551.331.4 -- Glacial erosion, processes.
551.336 -- Ice ages.
551.791 -- Pleistocene.
550.34 -- Seismology.
E7 -- Glaciology: glacial geology and ice ages.
(*38) -- Greenland.
(*381.4) -- Kong Christian den Xs Land.
SPRI record no.: 121210

MARCXML

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001 SPRI-121210
005 20240419054030.0
007 ta
008 240419s1992####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-121210
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aUenzelmann-Neben, Gabriele.
245 10 ‡aScoresby Sund, East Greenland :‡bstructure and distribution of sedimentary rocks /‡cGabriele Uenzelmann-Neben.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992[pub.1993]
300 ## ‡ap. 1-9 :‡bill., diags., maps.
500 ## ‡aPolarforschung. Vol. 62(1) :1-9 (1992[pub.1993]).
520 3# ‡aReflection seismic investigation allowed refined interpretation of Mesozoic and Cenozoic sedimentary evolution of area. Synsedimentary subsidence is suggested for western part of Jameson Land basin. Two seismic sequences document strong erosion which took place during Cretaceous/Tertiary. Further erosion resulted from development of several glacial phases in Quaternary, leading to very thin (<12 m, even as little at 5 m) cover of Quaternary sediments. Infers that most recent glaciation, developed during Late Weichselian, built up grounded glacier.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.331.4 -- Glacial erosion, processes.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a550.34 -- Seismology.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc
773 0# ‡7nnas ‡tPolarforschung. ‡gVol. 62(1) (1992[pub.1993]) ‡wSPRI-14580
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419