Lithostratigraphy of the Cretaceous–Paleocene Nuussuaq Group, Nuussuaq Basin, West Greenland
G Dam, GK Pedersen, M Sønderholm… - GEUS …, 2009 - geusbulletin.org
The authors have contributed to various extents in the completion of the manuscript. Gregers
Dam, Gunver Krarup Pedersen and Martin Sønderholm have had dual roles as authors and …
Dam, Gunver Krarup Pedersen and Martin Sønderholm have had dual roles as authors and …
[HTML][HTML] Fagaceae pollen from the early Cenozoic of West Greenland: revisiting Engler's and Chaney's Arcto-Tertiary hypotheses
In this paper we document Fagaceae pollen from the Eocene of western Greenland. The
pollen record suggests a remarkable diversity of the family in the early Cenozoic of …
pollen record suggests a remarkable diversity of the family in the early Cenozoic of …
Landslide and tsunami 21 November 2000 in Paatuut, west Greenland
T Dahl-Jensen, LM Larsen, SAS Pedersen, J Pedersen… - Natural Hazards, 2004 - Springer
A large landslide occurred November 21, 2000 at Paatuut, facing the Vaigat Strait onthe
west coast of Greenland. 90 million m 3 (260 million tons) of mainly basalticmaterial slid very …
west coast of Greenland. 90 million m 3 (260 million tons) of mainly basalticmaterial slid very …
Basaltic glass with high-temperature equilibrated immiscible sulphide bodies with native iron from Disko, central West Greenland
AK Pedersen - Contributions to Mineralogy and Petrology, 1979 - Springer
Immiscible sulphide bodies show eutectic quench textures in a basaltic glass rock (mg= 66)
from a native iron-bearing dyke chilled at T= 1,200° C and P= 250 bars. The sulphide bodies …
from a native iron-bearing dyke chilled at T= 1,200° C and P= 250 bars. The sulphide bodies …
Cenozoic uplift of Nuussuaq and Disko, West Greenland—elevated erosion surfaces as uplift markers of a passive margin
Remnants of a high plateau have been identified on Nuussuaq and Disko, central West
Greenland. We interpret the plateau as an erosion surface (the summit erosion surface) …
Greenland. We interpret the plateau as an erosion surface (the summit erosion surface) …
Palynostratigraphy of the lower Tertiary volcanics and marine clastic sediments in the southern part of the West Greenland Basin: implications for the timing and …
S Piasecki, LM Larsen, AK Pedersen… - Rapport Grønlands …, 1992 - geusbulletin.org
Volcanic rocks, forming hyaloclastites and subaqueous lava flows, were deposited
intercalated with clastic sediments in a water-filled basin in West Greenland in the Early …
intercalated with clastic sediments in a water-filled basin in West Greenland in the Early …
Paleomagnetism of large igneous provinces: case-study from West Greenland, North Atlantic igneous province
J Riisager, P Riisager, AK Pedersen - Earth and Planetary Science Letters, 2003 - Elsevier
We present new paleomagnetic and multi-model stereo photogrammetry data from lava
sequences in the West Greenland part of the North Atlantic igneous province (NAIP). The …
sequences in the West Greenland part of the North Atlantic igneous province (NAIP). The …
[PDF][PDF] Reaetion between pierite magma and continental ernst: early Tertiary silicie basalts and magnesian andesites from Di ko, West Greenland
AK Pedersen - 1985 - scholar.archive.org
Abstract The Kiiganguaq Member is a lava and tuff sequence comprising about 7. S km'of
magnesian silicic basalts (92%), magnesian andesites (7%) and feldspar-phyric silicic …
magnesian silicic basalts (92%), magnesian andesites (7%) and feldspar-phyric silicic …
Multi-model photogrammetric analysis of the 1990s surge of Sortebræ, East Greenland
Sortebræ is a surge-type tidewater glacier complex draining southeastward from the Geikie
Plateau, East Greenland. Sortebræ's main flow unit surged around 1950 and again between …
Plateau, East Greenland. Sortebræ's main flow unit surged around 1950 and again between …
The syn-volcanic Naajaat lake, Paleocene of West Greenland
GK Pedersen, LM Larsen, AK Pedersen… - Palaeogeography …, 1998 - Elsevier
The Naajaat lake in the Nuussuaq Basin on Disko and Nuussuaq formed in a geological
setting between cratonic crystalline Precambrian rocks overlain by Cretaceous sediments …
setting between cratonic crystalline Precambrian rocks overlain by Cretaceous sediments …