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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 |
LDR 01626naa#a2200000#a#4500 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