... Triassic Charlie Lake Formation and the Baldonnel Formation in northeastern British Columbia is diachronous. The trace of the Siphon unconformity demonstrates this diachroneity most clearly: in the type section well of the Charlie Lake and Baldonnel formations near Fort St. John in British Columbia...

...George T. Norgard ABSTRACT The Monias Field is the largest Halfway Formation gas field in northeast British Columbia. The field was discovered in 1975 by the re-entry of the 14-15-82-21W6M well. Monias is located 22 kilometres southwest of the city of Fort Saint John. The field is made up...

... formations of the Fort Saint John Group. The Dunvegan Formation in this area is very light gray and poorly sorted, and it consists of conglomerate and medium- and coarse-grained sandstone. In places the sandstone is segregated in lenses that have different size fractions within the sequence. The pebbles...

... Stratigraphy, Volume 4, Western Canada, Including Eastern British Columbia, Alberta, Saskatchewan and Southern Manitoba. D. J. Glass (ed,). Canadian Society of Petroleum Geologists, Calgary, Alberta, p. 220. Stelck, C. R. 1990g. Harmon Member (Peace River Formation, Fort St. John Group). In: Lexicon...

... application “from personal knowledge” was William Henry Fitton (1780–1861), to whom the Austins later dedicated a Cretaceous species in their 1843–1849 monograph. 13 His other supporters were the zoologist John Edward Gray (1800–1875) of the British Museum and geologist William Buckland (1784–1856...

...:00, Saturday (Foreshock? Mainshock reported at 22:00 here.) 1872/12/15 04:30, Sunday. Fort Simcoe, Washington Almost every hour until 5 a.m. Henry House, Alberta Another not so heavy, half an hour after the mainshock with little or no rumbling. Hope, British Columbia 1873/02/27 09:15...

... Peace River area, western Canada . Research Council of Alberta, Geological Division, Bulletin 2 , 35 p. Stott , D.F. 1961 . Type sections of some formations of the Lower Cretaceous Fort Saint John Group near Pine River, British Columbia . Geological Survey of Canada, Paper 61–11 , 66 p...

... of northeastern British Columbia, as well as conventional reservoirs in the Fort Saint John graben ( Berger, 1994 ). Conventional traps also exist in coquina beds within the Triassic section ( Gibson, 1993 ). The base of the Jurassic–Cretaceous section reflects the first pulse of deformation to the west...

... 2006. Cassiani is associate professor of applied geophysics at the Department of Geosciences at the University of Padua in Italy. His research interests are in environmental and engineering geophysics. David Chapman received a B.S. and M.S. in physics from the University of British Columbia...

... Paniconi, C., Univ. of Quebec, Sainte-Foy, QC, Canada Parkin, G.W., Univ. of Guelph, Guelph, ON, Canada Parlange, M.B., Johns Hopkins Univ. Nichol, C., Univ. of British Columbia Nicholl, M., Univ. of Idaho Nicholl, M., Univ. of Nevada Nieber, J., Univ. of Minnesota Ochsner, T...

...: journal quotidien ou hebdomadaire avec date de parution. Outre leur faible dénivelé et leur inclinaison relativement forte, les pentes avalancheuses de la vallée du Saint-Laurent partagent une même caractéristique qui s’avère déterminante, soit la présence au sommet du versant d’une surface...

..., 01-B 16-J 16-G 16-B 01-A 16-1 O0 16-H O I-- C O0 m ~> 16-A 124 ° 122" \ r S tudy Area ~ ¢~ \ Fort St.J ~, John : _ JPeace <~ ' " /R iver , Da"wson -Oo.\Creek. Grande . . . . "~ ' \ l Prairie r u rmsn ~ }' 0 100 Columbia / \ , . , 12o ° 11e- 1!e4~0 56 ° __154 ° 0 8 km I I Study area Oil pools Gas...

... Washington. Correlative strata also extend north into British Columbia where they are called the Huntingdon Formation ( Mustard and Rouse, 1994 ). Mustoe and Gannaway (1997) suggested that this map pattern is evidence of a large depositional basin that was dissected by strike-slip faulting. Johnson (1984a...

... ). The Peejay field is located 113 km north of Fort St. John, British Columbia. The study area covers 320 km2, encompassing map sheets 94-A-15 and 94-A-16 ( Figure 3 ). The examination of over 345 well logs, 132 cored intervals (4700 m of described core) through the Middle Triassic, and good well control...

... A. . . . . . . . . . . Diamond Instrument Co., Wakefield, Mass., 1946. Hobbs, R. D . . . . . . . . . . . . . . . . P.O. Box 1089, Chicago 90, Ill., 1937. Hodgson, E. A . . . . . . . . . . . . . . . Dominion Observatory, Ottawa, Canada, 1919. Hodgson, John H . . . . . . . . . . . . 49 Saint George St., Toronto, Ontario, Canada...

... p. 756 - 775 . Lapen , T.J. , 1998 , Structure and metamorphism of the southern Lillooet River–Northern Breakenridge area, southern Coast Mountains, British Columbia : [M.S. thesis]: Bellingham, Western Washington University . 135 p. Le Fort , P. , Cuney , M. , Deniel...

... Columbia, 2020-2207 Main Mall, Vancouver, British Columbia V6T 1Z4, Canada ROGER J.A. WILSON Department of Ancient Mediterranean and Near Eastern Studies, University of British Columbia, BUCH C 227, 1866 Main Mall, Vancouver, British Columbia V6T 1Z1, Canada RHIANA E. HENRY, AARON C. PALKE, AND MATTHEW F...

... terrain intelligence for Allied forces in both Europe and the Far East from a base in England, within the University of Oxford. John Leonard Farrington (1906–1982), an undergraduate student from 1923 to 1928 of Brock and/or Phemister at the University of British Columbia, co-founded the Section and soon...

.... Insurance Co. of North America . . . . . . . . . . . 1600 Arch St., Philadelphia, Penn., 1926. Inter-Ocean Reinsurance Co . . . . . . . . . . . . . . . Cedar Rapids, Iowa, 1927. Itten, H. E Box 1410, Fort Worth, Tex., 1947. Ivy, John S 1124 Niels Esperson Bldg., Houston, Tex., 1941. Jackson, James G., Jr...

.... and Silberling , N.J. 1990 . New data on the Upper Triassic bivalve Monotis in North America and the new subgenus Pacimonotis . Journal of Paleontology , v. 64 , p. 240 – 254 . Hage , C.O. 1944 . Geology adjacent to the Alaska Highway between Fort Saint John and Fort Nelson , British...