... and western coast. Also, reservoirs may be present in lime-mud buildups and overlying allochthonous carbonate rocks farther down the slope in Nyeboe through Wulff Lands. In Peary Land, Crinoidal Calcarenite intrashelf buildups and overlying alochthonous carbonate rocks may be present in the subsurface...

...FIG. 13 —(a) Carbonate buildup (R) with long axis aligned perpendicular to carbonate-shelf stepped margin, and interbedded downslope with slope mudstones (SM). C, conglomerates. Buildup height, 300 m (1,000 ft). Eastern Wulff Land immediately north of Apollo Sø ( Fig. 4 ). (b) Ordovician...

...Fig. 7 —Diagrammatic stratigraphic cross section showing lithologic differences in Cambrian beds across Wulff Land arch. ...

.... Late Cambrian and Early Ordovician conodonts from the Franklinian miogeosyncline, Canadian Arctic Islands Journal of Paleontology 1985 59 96 122 Peel J. S. Cambrian and Ordovician geology of Warming Land and southern Wulff Land, central North Greenland Grønlands Geologiske Undersøgelse...

... Hipponicharion skovstedi n. sp. and Beyrichona avannga n. sp. from the Kap Troedsson Formation in southern Wulff Land (GGU sample 298984) and the land area south of Nares Land (GGU samples 315056, 315057, and 315061); (C) location of A and B in North Greenland (rectangle) and samples described by Skovsted...

... interpreted from the literature but not proven by our direct observation of the illustrated specimens (circles): Passage Creek ( Niklas and Smocovitis 1983 ), Wulff Land ( Larsen et al. 1987 ), Port Clinton ( Strother 1988 ), Ludford Lane ( Glasspool et al. 2004 ), Brown Clee Hill ( Glasspool et al...

... and shallow-water nearshore environments ( Surlyk and Ineson 1987 ). In northern Wulff Land, the group passes gradationally upwards into dolostones of the overlying Portfjeld Formation. In NE Peary Land, in contrast, the group is succeeded by basinal carbonates of the Polkorridoren Group (see later...

..., with the appearance of sandstone turbidites. Towards the end of the early Silurian (latest Llandov- ery, C6), basin turbidites and mudstones spread for the first time over the carbonate platform to the E of Wulff Land (Fig. 1). In North Greenland, the platform carbonates and their cover of basin turbidites...

... from Navarana Fjord: an internal mold ( Fig. 5.7 , 5.8 ) of Pagetides ? sp. and a single broken pygidium of Ekwipagetia sp. ( Fig. 5.9 , 5.10 ), the latter also known from the Kap Troedsson Formation (Cambrian Stage 4) in southern Wulff Land (Blaker and Peel, 1997 ; Fig. 1.3 ). Apart from...

... 1995 ). Olenelloidean trilobites collected by Troelsen from the Wulff River Formation in Inglefield Land ( Fig. 1B ) were described by Poulsen (1958) , while Valdemar Poulsen (1964) partially revised the earlier studies of Poulsen (1927 , 1946 ) based on Troelsen’s collections and described some...

... the event were evaluated and digitized in GIS. Based on these studies, land subsidence due to collapse of qanats, local toppling, and sliding of soil blocks were mapped. Instabilities of qanats were evaluated using 2-D and 3-D models, and the results were compared with existing conditions. Good agreement...