Zobrazeno 1 - 10
of 11
pro vyhledávání: '"N. L. Watts"'
Publikováno v:
Geological Society, London, Special Publications. 65:247-263
Publikováno v:
AAPG Bulletin. 77
The Akaso Field [STOIIP 78 × 106 m3 (401 Million STB)] of The Eastern Niger Delta is separated from the large Cawthorne Channel field [STOIIP 208 × 106 m3 (1307 million STB)] by a major antithetic (counterregional) normal fault. In 1989, three-dime
Autor:
N. L. Watts
Publikováno v:
Earth Surface Processes. 2:63-74
Deformation structures, within some Quaternary calcretes of Botswana and South Africa, have been classified into five types. Type 1 folds are small-scale ( 20 m), but low amplitude (< 1 m), anticlines in hardpan calcrete; structural evidence suggests
Autor:
N. L. Watts
Publikováno v:
Calcretes
The calcretes of the Kalahari are amongst the thickest in the world representing pedogenic episodes in a semi-arid climate during Pliocene to Recent times. The descriptive morphological terminology of Netterberg is used to describe the calcrete types
Autor:
N. L. Watts
Publikováno v:
AAPG Bulletin. 69
Cap-rock seals can be divided genetically into those that fail by capillary leakage (membrane seals) and those that fail due to fracturing or wedging open of faults (hydraulic seals). A given membrane seal can trap a larger column of oil than gas at
Autor:
N. L. Watts
Publikováno v:
AAPG Bulletin. 67
Production data from many North Sea chalk fields have indicated moderate to considerable contribution to production from natural fractures. This paper illustrates a detailed study of natural fracturing in the Albuskjell field, where gas/condensate hy
Autor:
N. L. Watts, V. P. Wright
Publikováno v:
Journal of Sedimentary Research. 48:1360-1361
Publikováno v:
Geology. 8:217
Maastrichtian-Danian chalks of well 1/6-3 (Albuskjell structure, North Sea) contain large-scale allochthonous chalk units that were emplaced by slumping, debris flows, turbidity flows, and other bottom-traction processes in a slope and a base-of-slop
Autor:
N. L. Watts
Publikováno v:
Geology. 7:421