Geological Survey of Denmark and Greenland Bulletin 19 ... - Geus

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Svartenhuk Halvø Upernivik Næs, Qeqertarsuaq North coast Nuussuaq Western Nuussuaq Central Nuussuaq Thanetian Umiivik Itsaku Sv Up. E of Ikorfat W of Ikorfat 17 Aaffarsuaq 19 17 Paleocene Selandian Danian Maastrichtian Campanian Kangilia 4 ? Kangilia Vaigat Vaigat 12 E t 15 Itilli Umiivik 1 6 1 7 Kangilia O Na AC Itilli Kangilia Agatdal Vaigat E t Anariartorfik O Na An Vaigat E Itilli t Aaffarsuaq O Na It Upper Cretaceous Santonian Coniacian Itilli Umiivik 3 14 Atane 8 13 Qilakitsoq Turonian 1.5 km undated deep marine sediments Lower Cretaceous Cenomanian Albian Upernivik Næs 4 12 4 9 Contact to basement Upernivik Næs Slibestensfjeldet Atane Kome 2 Contact to basement Kingittoq Ravn Kløft t Volcanic rocks Subaerial lava flow Hyaloclastic breccia Coal Mudstone Sandstone Conglomerate Macrofossils Tuff 3 Key reference 30
Central Nuussuaq Agatdalen South coast Nuussuaq Ataata Kuua Paatuut North coast Disko South coast Nuussuaq Eastern Disko South coast Disko Asuk Kingittoq Pingu Skansen, Atanikerluk Assoq Vaigat E t O Na M Vaigat At E t N RDM O M Vaigat 16 19 RDM O Na M At t 17 A U N RDM M At 17 A U P Ak RDM M At A 17 18 RDM Agatdal Quikavsak Pa NQ Tu Quikavsak Tu Kangilia 13 14 OAC Kangilia 5 Atane Itilli Aaffarsuaq 8 13 Qilakitsoq Atane Qilakitsoq Alluvial fan Lake Fluvial channel Flood plain Delta plain 2 15 16 Itilli Atane Kingittoq Kussinerujuk Atane Kingittoq Atane Skansen Atane Skansen Delta front Estuary Marine shoreface Contact to basement 11 10 10 Marine shelf Marine slope Marine slope channel 31
Page 1 and 2: GEOLOGICAL SURVEY OF DENMARK AND GR
Page 4 and 5: Contents Abstract . . . . . . . . .
Page 7 and 8: Preface The onshore Cretaceous-Pale
Page 9 and 10: Introduction The Nuussuaq Basin bel
Page 11 and 12: chemistry of the Nuussuaq Basin hav
Page 13 and 14: Fig. 5. Plant fossils from the Atan
Page 15 and 16: Peak 2010 m Peak 1900 m Peak 1760 m
Page 17 and 18: A lithostratigraphy for the marine
Page 19 and 20: to provide further funding for stud
Page 21 and 22: DGR Geological setting As a result
Page 23 and 24: TSS 8 Agatdal Fm Eqalulik Fm Kangil
Page 25 and 26: A Svartenhuk Halvø 50 km B Hinterl
Page 27 and 28: Nuussuaq Group new group History. T
Page 29: ley (Figs 2, 40, 65). The section a
Page 33 and 34: 3 10 4 6 5 Qorlortorssuaq Slibesten
Page 35 and 36: volcanic sediments are referred to
Page 37 and 38: Fig. 20. View from Uummannaq toward
Page 39 and 40: In the Kuuk area, the sediments ove
Page 41 and 42: m m 15 14 14 13 12 11 10 9 8 7 6 5
Page 43 and 44: Kome Formation m 40 30 20 D tial re
Page 45 and 46: Fig. 28. Reference locality of the
Page 47 and 48: Vaigat Fm Vesterfjeld Slibestensfje
Page 49 and 50: Gilbert delta in the Ikorfat area (
Page 51 and 52: 150 300 450 100 250 400 m 550 50 20
Page 53 and 54: Fig. 36. Outcrop of the Upernivik N
Page 55 and 56: Correlation. The Upernivik Næs flo
Page 57 and 58: 12’ 09’ 15’ 06’ 03’ Saqqa
Page 59 and 60: m 0 GGU 247801 200 400 247815 ★
Page 61 and 62: wave-rippled sand streaked mudstone
Page 63 and 64: the formation in the marine mudston
Page 65 and 66: d d Fig. 47. Type locality of the S
Page 67 and 68: Fig. 49. Cross-bedded medium- to co
Page 69 and 70: and Qaarsut (Fig. 22). Its wider di
Page 71 and 72: Fig. 52. Two closely spaced section
Page 73 and 74: Type section. The type section of t
Page 75 and 76: Fig. 56. Delta front succession of
Page 77 and 78: Fig. 59. The Kingittoq Member at Ki
Page 79 and 80: sh L sh ch delta front Vaigat Forma
Page 81 and 82:
Fig. 63. Type locality of the Itivn
Page 83 and 84:
782 Quaternary cover 54° 888 Malig
Page 85 and 86:
Kuugannguaq-Qunnilik Fault and is o
Page 87 and 88:
and include clasts of intraformatio
Page 89 and 90:
deposited in a base-of-slope and ba
Page 91 and 92:
VK 53°30’ 53°15’ Niaqornat Tu
Page 93 and 94:
Umiivik-1 m Overburden ★ ★ No p
Page 95 and 96:
76). Heavily bioturbated interbedde
Page 97 and 98:
Fig. 78. Type locality of the Kussi
Page 99 and 100:
A B Itilli Formation Kussinerujuk M
Page 101 and 102:
160 140 120 100 Vaigat Formation Eq
Page 103 and 104:
Fig. 85. Mudstones and conglomerati
Page 105 and 106:
Fig. 87. Type section of the Kangil
Page 107 and 108:
m 150 140 130 120 110 100 90 Kangil
Page 109 and 110:
channellised, high-density currents
Page 111 and 112:
Thickness. The Annertuneq Conglomer
Page 113 and 114:
Fig. 96. A: Type locality of the Oy
Page 115 and 116:
On Svartenhuk Halvø, on the east s
Page 117 and 118:
Fig. 100. Reference locality of the
Page 119 and 120:
Tupaasat Member Atane Formation Fig
Page 121 and 122:
ever, have a fluvio-lacustrine orig
Page 123 and 124:
etween Tupaasat and Nuuk Qiterleq a
Page 125 and 126:
Vaigat Formation sill Quikavsak For
Page 127 and 128:
Fig. 112. The sharp boundary betwee
Page 129 and 130:
Agatdal Formation Eqalulik Formatio
Page 131 and 132:
Fig. 116. Basal conglomerate unit o
Page 133 and 134:
heterolithic deposits of the Kangil
Page 135 and 136:
GANE#1 Vaigat Fm Anaanaa Mb m Hyalo
Page 137 and 138:
Fig. 121. Well reference section of
Page 139 and 140:
Pedersen 1978). The beds are usuall
Page 141 and 142:
In detail, however, the boundary be
Page 143 and 144:
Fig. 126. Composite type section of
Page 145 and 146:
m m 240 340 m Pingu Member 230 230
Page 147 and 148:
Naujât Member Atane Formation, Kin
Page 149 and 150:
The TOC [Total Organic Carbon] cont
Page 151 and 152:
Fig. 133. Correlation of the member
Page 153 and 154:
Fig. 135. Type locality of the Ping
Page 155 and 156:
Fig. 137. Lower, sharp boundary of
Page 157 and 158:
m 130 125 110 t t invasive lava low
Page 159 and 160:
Fig. 141. Upper part of the Assoq M
Page 161 and 162:
Brown, R. 1875: Geological notes on
Page 163 and 164:
a rosetted spreite trace fossil: Da
Page 165 and 166:
ing bark from the Nûgssuaq peninsu
Page 167 and 168:
1998: The syn-volcanic Naajaat lake
Page 169 and 170:
Appendix: Place names and localitie
Page 171:
Place name Place name P Paatuut sou
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Geological Survey of Denmark and Greenland Bulletin 19 ... - Geus

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