Geological Survey of Denmark and Greenland Bulletin 19 ... - Geus
Geological Survey of Denmark and Greenland Bulletin 19 ... - Geus
Geological Survey of Denmark and Greenland Bulletin 19 ... - Geus
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
In the Kuuk area, the sediments overlying the coarsegrained,<br />
basal deposits consist <strong>of</strong> three facies associations:<br />
A, B <strong>and</strong> C (Figs 24, 27, 28). Association A is<br />
dominant <strong>and</strong> consists mainly <strong>of</strong> trough cross-bedded,<br />
erosionally based s<strong>and</strong>stones in shoe-string or irregular<br />
tabular bodies up to 5 m thick (Figs 24, 28). The s<strong>and</strong>stones<br />
are coarse-grained, <strong>of</strong>ten gravelly, with angular<br />
clasts, <strong>and</strong> is poorly sorted. It contains slightly to moderately<br />
kaolinised feldspars <strong>and</strong> kaolinite cement.<br />
Fragments <strong>of</strong> coalified wood <strong>and</strong> fine-grained plant debris<br />
are common. The orientation <strong>of</strong> shoe-string bodies <strong>and</strong><br />
dip direction <strong>of</strong> foresets indicates transport from the<br />
south-east. The s<strong>and</strong>stones alternate with dark laminated<br />
silty mudstones containing much coalified plant debris,<br />
thin lenses <strong>of</strong> lustrous, coalified, woody tissue <strong>and</strong> thin<br />
coal seams (Fig. 24; Pulvertaft <strong>19</strong>79). Association B consists<br />
<strong>of</strong> distinctive coarsening-upward successions <strong>of</strong> mudstones,<br />
cross-laminated siltstones, s<strong>and</strong>stones <strong>and</strong> locally<br />
thin layers <strong>of</strong> gravelly s<strong>and</strong>stones (Figs 24, 27). Association<br />
C is dominated by tabular cross-bedded, medium-grained,<br />
moderately well-sorted subarkosic s<strong>and</strong>stones with pebble<br />
lags <strong>of</strong> quartz or chert. Comminuted coalified plant<br />
debris <strong>and</strong> mica are common in the s<strong>and</strong>stones. Foresets<br />
dips are to the north-west. Cross-laminated, fine-grained<br />
53°00’<br />
52°45’<br />
2 km<br />
30<br />
25<br />
Ikorfat<br />
25<br />
Kussinikassaq<br />
Angiarsuit<br />
Nipitartukassaat<br />
Ujarattoorsuup Killia<br />
Ujarattoorsuaq<br />
Ujarattoorsuup Kangilia<br />
Siorartartarfik<br />
30<br />
D<br />
20<br />
B<br />
Talerua<br />
A<br />
C<br />
70°45’<br />
J.P.J. Ravn Kløft<br />
Slibestensfjeldet<br />
Ikorfat<br />
Qaqqarsui<br />
Aarrusap<br />
Kussinersua<br />
Airport<br />
28<br />
Qaarsut<br />
Vesterfjeld<br />
Qaarsut Kussinersuat<br />
Østerfjeld<br />
Quaternary cover<br />
Vaigat Formation<br />
Vaigat Formation<br />
Tunoqqu Member<br />
Intrusion<br />
Eqalulik Formation<br />
Itilli Formation<br />
Atane Formation<br />
Kingittoq Member<br />
Atane Formation<br />
Ravn Kløft Member<br />
Atane Formation<br />
Undivided, west <strong>of</strong> Ikorfat<br />
Slibestensfjeldet Formation<br />
Umiivik Member<br />
Kome Formation<br />
Precambrian<br />
Ice<br />
Sea/lake<br />
Fault<br />
Strike <strong>and</strong> dip <strong>of</strong> strata<br />
Fig. 22. Detailed geological map <strong>of</strong> the north coast <strong>of</strong> Nuussuaq, from Qaarsut to Ikorfat. The locations <strong>of</strong> the four sedimentological logs<br />
(A–D) in Fig. 25 are indicated. Contour interval 200 m. Modified from Rosenkrantz et al. (<strong>19</strong>74) <strong>and</strong> Midtgaard (<strong>19</strong>96b). For location, see<br />
Fig. 2.<br />
39