Zobrazeno 1 - 10
of 32
pro vyhledávání: '"S.P. Price"'
Autor:
S.P. Price, R. McGarva, M. Grecula, K. Engenes, M. Boya Ferrero, J. Hognestad, K. T. Noraberg, K. van Ojik, P. Mears, G. De Bruijn
Publikováno v:
Geological Society, London, Special Publications. 403:157-183
Akademický článek
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Publikováno v:
Geological Society, London, Special Publications. 177:227-246
Publikováno v:
Geological Society of America Bulletin. 111:1054-1068
Apatite fission-track analyses from the area north of Jameson Land, East Greenland, indicate that the region has undergone at least three phases of cooling during the Mesozoic and Cenozoic. Two major periods of cooling during the Tertiary have been i
Publikováno v:
Geological Society, London, Petroleum Geology Conference Series. 5:325-336
A tectono-sedimentary model is proposed for the Cretaceous (post-Valanginian) succession of NE Greenland which provides insights into the evolution of adjacent margins. Subsequent to a major reorganization of fault blocks during rifting in the Volgia
Publikováno v:
Journal of the Geological Society. 155:993-1008
The finest exposures of Barremian to Santonian sedimentary rocks in the northern North Atlantic region are exposed in Hold with Hope, NE Greenland. These rocks comprise the Hold with Hope Group which, together with its constituent formations and memb
Publikováno v:
Journal of the Geological Society. 154:419-434
A number of planar normal faults displace Tertiary basaltic intrusions in the Traill O region of East Greenland. This 9post-magmatic9 extension occurs over an along-strike length of >350 km and over an across-strike width of >100 km with fault displa
Publikováno v:
All Days.
Hydrodynamic aquifer conditions have been described in many basins around the world since first introduced by Hubbert1 in 1953. The hydrodynamic aquifer concept in Ormen Lange has been assessed using iso-potential mapping1 and dynamic simulation of t
Autor:
Barry C. Scott, S.P. Price
Publikováno v:
Journal of the Geological Society. 148:345-354
The Pliocene Burdur Formation of SW Turkey was deposited in a NE-SW trending half-graben with a major basement fault along its SE margin. Hangingwall-sourced fans were confined proximally by basement topography. Distally, they developed 9ideal9 fan g
Akademický článek
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