TEMPERATURE-STRATIFIED MISSISSIPPIAN CARBONATES AS HYDROCARBON RESERVOIRS—EXAMPLES FROM THE FOOTHILLS OF THE CANADIAN ROCKIES

1997 ◽  
pp. 391-409 ◽  
Author(s):  
WILLIAM MARTINDALE ◽  
THOMAS D. BOREEN
Keyword(s):  
Hydrocarbon Reservoirs ◽  
Canadian Rockies

Continuous hydrocarbon reservoirs

Fact Sheet ◽  
1997 ◽  
Author(s):  
James W. Schmoker
Keyword(s):  
Hydrocarbon Reservoirs

TYPES OF UNCONFORMITY AND PREDICTION OF HYDROCARBON RESERVOIRS IN YANTAI DEPRESSION, SOUTH YELLOW SEA BASIN

2017 ◽  
Author(s):  
Yinguo Zhang ◽  
◽  
Qinghua Chen ◽  
Qinghua Chen ◽  
Qinghua Chen ◽  
...  
Keyword(s):  
Yellow Sea ◽  
Hydrocarbon Reservoirs ◽  
South Yellow Sea ◽  
South Yellow Sea Basin

Faulting, fault sealing and fluid flow in hydrocarbon reservoirs: an introduction

1998 ◽  
Vol 147 (1) ◽  
pp. vii-xxi ◽  
Author(s):  
R. J. Knipe ◽  
G. Jones ◽  
Q. J. Fisher
Keyword(s):  
Fluid Flow ◽  
Hydrocarbon Reservoirs

In the Heart of the Canadian Rockies

1906 ◽  
Vol 38 (2) ◽  
pp. 144
Author(s):  
James Outram
Keyword(s):  
Canadian Rockies

scholarly journals Neoglacial history of Robson Glacier, British Columbia

2017 ◽  
Vol 54 (11) ◽  
pp. 1153-1164 ◽  
Author(s):  
B.H. Luckman ◽  
M.H. Masiokas ◽  
K. Nicolussi
Keyword(s):  
British Columbia ◽  
Little Ice Age ◽  
Ice Age ◽  
Tree Line ◽  
Canadian Rockies ◽  
The Holocene ◽  
Forest Sites ◽  
History Of ◽  
Subfossil Wood ◽  
Glacier Advance

As glaciers in the Canadian Rockies recede, glacier forefields continue to yield subfossil wood from sites overridden by these glaciers during the Holocene. Robson Glacier in British Columbia formerly extended below tree line, and recession over the last century has progressively revealed a number of buried forest sites that are providing one of the more complete records of glacier history in the Canadian Rockies during the latter half of the Holocene. The glacier was advancing ca. 5.5 km upvalley of the Little Ice Age terminus ca. 5.26 cal ka BP, at sites ca. 2 km upvalley ca. 4.02 cal ka BP and ca. 3.55 cal ka BP, and 0.5–1 km upvalley between 1140 and 1350 A.D. There is also limited evidence based on detrital wood of an additional period of glacier advance ca. 3.24 cal ka BP. This record is more similar to glacier histories further west in British Columbia than elsewhere in the Rockies and provides the first evidence for a post-Hypsithermal glacier advance at ca. 5.26 cal ka BP in the Rockies. The utilization of the wiggle-matching approach using multiple 14C dates from sample locations determined by dendrochronological analyses enabled the recognition of 14C outliers and an increase in the precision and accuracy of the dating of glacier advances.

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