Search
Skip to Search Results- 1Black shale
- 1Canol Formation
- 1Devonian
- 1Diastasis cracks
- 1Horn River Group
- 1Microbial mat related structures
-
Microbial Mat-Related Structures: Laboratory Experiments and Observations from the Mesoproterozoic Belt Supergroup, Southwestern Montana, U.S.A.
DownloadSpring 2017
Siliciclastic sediments become biostabilized when benthic bacteria penetrate into the pore spaces and secure grains with filaments and extracellular polymeric substances, forming a microbial mat. The cohesive microbial cover changes typical sedimentary dynamics and leads to formation of diverse...
-
Petrographic and X-ray Microtomographic Analysis of the Upper Montney Formation, Northeastern British Columbia, Canada
DownloadSpring 2013
Utilizing electron microprobe (EMP), scanning electron microscope (SEM) and petrographic analysis, 14 thin sections from the Upper Montney Formation were analyzed. Five microfacies were identified. Rock types observed include: dolomitic lithic arkos, dolomitic litharenite, dolomitic feldspathic...
-
Sequence Stratigraphy, Porosity, and Primary Producers of the Middle to Late Devonian Canol Formation, Northwest Territories, Canada
DownloadFall 2022
The Devonian Canol Formation of the Northwest Territories (NWT) is an organic-rich mudstone interval deposited in a tropical marine setting along the west coast of Ancestral North America. This unit preserves a record of local marine conditions in the Middle to Late Devonian, a time characterized...
-
The Sedimentology, Stratigraphy and Reservoir Characteristics of the Montney D1 and D2 Horizons, Greater Pouce Coupe Area, Alberta and British Columbia
DownloadFall 2016
The Middle Montney D1 and D2 Horizons in the Greater Pouce Coupe Area are important exploration targets. These moderate porosity and low permeability siltstone units have been referred to as distal shelf deposits in the past, based primarily on their restricted grain size. The D1 and D2 Horizons...