The Upper Devonian Grosmont shelf complex is the worlds largest heavy oil deposit hosted in carbonates, with an estimated >50 billion cubic meters (318 to probably 406 bbls) of initial volume in place. At present the Grosmont is not yet under production. This study involves log interpretation, core examination; facies description; strontium, sulphur, carbon, and oxygen isotope analysis. The Grosmont is subdivided into four shallowing-upward cycles. Most Hondo evaporites are part of the Upper Grosmont 3 and Lower Grosmont and were deposited in a series of small, shallow subaqueous brine ponds or in an extensive lagoon. In the eastern part of the area, the Hondo appears to be dissolved resulting in solution-collapse breccias. Other diagenetic processes that were important in shaping the present reservoir characteristics were pervasive dolomitization and dolomite
recrystallization, fracturing, and karstification.
Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:AEU.10048/1568 |
Date | 11 1900 |
Creators | Borrero, Mary |
Contributors | Machel, Hans G. (Earth and Atmospheric Sciences), Pemberton, S. George (Earth and Atmospheric Sciences), Schmitt, Douglas (Physics) |
Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
Language | English |
Detected Language | English |
Type | Thesis |
Format | 9801555 bytes, application/pdf |
Relation | Borrero, Mary (2009). http://www.cspg.org/conventions/abstracts/2009abstracts/139.pdf, Borrero, Mary (2010). http://www.searchanddiscovery.com/abstracts/pdf/2010/intl/abstracts/ndx_borrero.pdf |
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