Zobrazeno 1 - 10
of 36
pro vyhledávání: '"O H Ardakani"'
The Lower Triassic Montney Formation is a major siltstone dominated unconventional tight gas play in the Western Canadian Sedimentary Basin (WCSB). In the Peace River region, the Montney Formation contains a regionally variable amount of hydrogen sul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::052deb2f7ebfa75b2bd041a4962ea0df
https://doi.org/10.4095/329785
https://doi.org/10.4095/329785
Induced (anthropogenic) earthquakes are caused by reactivation of pre-existing faults due to human activities, including hydraulic fracturing and saltwater disposal. The Montney play, the pre-eminent shale gas play in Canada, contains localized regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3ab5c43f318c2d31967b20046005b1a
https://doi.org/10.4095/329795
https://doi.org/10.4095/329795
The Montney Formation is a highly productive hydrocarbon reservoir with significant reserves of hydrocarbon gases and liquids making it of great economic importance to Canada. However, high concentrations of hydrogen sulfide (H2S) have been encounter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ccfff634501057f6c9968b1fbf7040e6
https://doi.org/10.4095/329797
https://doi.org/10.4095/329797
The link between organic matter and gold in sediment-hosted Carlin-type deposits is controversial. This study aims to tackle this potential link by documenting the occurrence of organic matter in a single borehole from a Carlin-type gold deposit in Y
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d2db69388028910d22cac1da559b267
https://doi.org/10.4095/330086
https://doi.org/10.4095/330086
Autor:
D Lavoie, N Pinet, S Zhang, J Reyes, C Jiang, O H Ardakani, M M Savard, R S Dhillon, Z Chen, J R Dietrich, K Hu, J A Craven, B Roberts, M J Duchesne, V I Brake, G Huot-Vézina, J M Galloway, A D McCracken, E Asselin, V Decker, M Beauchemin, M P B Nicolas, D K Armstrong, K E Hahn
As part of its Geo-mapping for Energy and Minerals program, the Geological Survey of Canada included the Hudson Bay Basin in its research portfolio with the goal of generating a modern understanding of its geological framework and a precise knowledge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e721c256bb7904c38780947f95bd7f1
https://doi.org/10.4095/326090
https://doi.org/10.4095/326090
In the last decade, the Lower Triassic Montney Formation of the Western Canada Sedimentary Basin (WCSB) has undergone significant development, providing a rich dataset to study structural, stratigraphic, and facies control on the variations in hydrog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a162bbbcb4be8b95f35f6563cc450164
https://doi.org/10.4095/329796
https://doi.org/10.4095/329796
Hydraulic fracturing is a reservoir stimulation technique that involves the injection of high-pressure fluids to enhance recovery from unconventional hydrocarbon reservoirs. Often this involves the injection of surface waters (along with additives su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4689b859b7e87a15d564fcb46fe7cc48
https://doi.org/10.4095/330712
https://doi.org/10.4095/330712
Hydrogen sulfide (H2S) is a toxic and corrosive gas that commonly occurs in deeply buried sedimentary systems. Understanding its distribution is paramount to creating safe and effective models of H2S occurrence aiding in the identification of high-ri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e178f9da32e8d8ec05b5dbaf2cc805f0
https://doi.org/10.4095/329789
https://doi.org/10.4095/329789
The Western Canada Sedimentary Basin (WCSB) is a mature oil and gas basin with an extraordinary endowment of publicly accessible data. It contains structural elements of varying age, expressed as folding, faulting, and fracturing, which provide a rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cec055434fcde7074687d84b1e937b68
https://doi.org/10.4095/328850
https://doi.org/10.4095/328850