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DTSTART;TZID=America/Halifax:20230524T083000
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DTSTAMP:20260422T172222
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UID:10800-1684917000-1684953000@www.apegs.ca
SUMMARY:30 by 30 Employer Leadership Summit
DESCRIPTION:Join engineering employers from across Canada for a full-day event on making change through employer leadership. The summit\, organized by Engineers Canada in partnership with Engineers Nova Scotia\, will include discussions on allyship and championing equity\, diversity\, and inclusion\, particularly within engineering firms and companies. \nBe part of a national movement that is making engineering more inclusive. \nRegister today: https://engineerscanada.ca/event/30-by-30-conference-2023-employer-leadership-summit \n30 by 30 Employer Leadership Summit Invitation
URL:https://www.apegs.ca/event/30-by-30-employer-leadership-summit
LOCATION:Halifax\, Halifax\, Nova Scotia\, Canada
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DTSTART;TZID=America/Regina:20230524T120000
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DTSTAMP:20260422T172222
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LAST-MODIFIED:20230523T155517Z
UID:11472-1684929600-1684933200@www.apegs.ca
SUMMARY:SGS - Upside Potential of the Basal Mississippian Souris Valley Beds/Lodgepole Formation in Southeast Saskatchewan
DESCRIPTION:Abstract \nProspecting for hydrocarbons along the Souris Valley Beds subcrop edge in Southeast Saskatchewan has met with very disappointing results (save for the Parkman Pool). This core display suggests an alternative model for future exploration activity. Klassen (1996) mapped Lodgepole shelf\, slope and basin facies in Southwestern Manitoba and suggested that Southeast Saskatchewan represents deposition in a deeper non-reservoir facies. \nThis core presentation suggests erosion removed the reservoir in Southeast Saskatchewan and northwestern North Dakota. Stratigraphic cross-sections through the Daly and Virden Lodgepole Pools in southwestern Manitoba were studied as an analogue for exploring elsewhere in the basin and revealed Sequence Boundaries and ravinement surfaces/sea cliffs which show rapid sea level changes affecting preservation of the section. \nThe two cores on display are a composite of the Lodgepole Formation from Bakken/Lodgepole contact to top of the Lower Daly Member reservoir (Cruickshank Member in the Daly Pool (100/01-30-009-28W1/00; Cal. Stan. Daly)\, which represents the lower portion of the Lodgepole Formation\, and Lower Daly Member reservoir facies at the top of the Lodgepole Formation (100/11-04-010-28W1/00; Daly Unit No. 1) in southwestern Manitoba). Erosion of the reservoir was likely initiated by reactivation of sinistral faults along the Churchill/Superior Boundary. \nSpeaker Biography \nJohn Lake\nLake Geological Services Inc. \nJohn received an Honours B.Sc in Earth Sciences from the University of Waterloo in 1973 and M.Sc in Earth and Atmospheric Sciences from McGill in 1977. Worked for Mobil Oil Canada in Calgary from 1979-1989 (Production Geology in Saskatchewan from 1983). Worked for Saskoil in Regina and Swift Current from 1990-1995\, and has been a Consulting Geologist from 1995 – present. Experience includes Wellsite Geology and describing cores. \nRSVP by noon\, Tuesday\, May 23. \nSGS_Talk Notice_23-05-24_Lake
URL:https://www.apegs.ca/event/sgs-upside-potential-of-the-basal-mississippian-souris-valley-beds-lodgepole-formation-in-southeast-saskatchewan
LOCATION:Saskatchewan Geological Subsurface Laboratory\, 201 Dewdney Ave\, Regina\, Saskatchewan\, S4N 4G3\, Canada
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