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VERSION:2.0
PRODID:icalendar-ruby
CALSCALE:GREGORIAN
X-WR-CALNAME:KU Geology Colloquium - Dr. Kevin Evans
X-WR-TIMEZONE:Central Time (US & Canada)
BEGIN:VEVENT
DTSTAMP:20261007T195639Z
UID:tag:localist.com\,2008:EventInstance_51993195817649
DTSTART:20260205T210000Z
DTEND:20260205T220000Z
DESCRIPTION:“Warp and Weft of the Ozarks Uplift\, Phantom Sequences\, and
  Origins of Carbonate Mud Mounds in Southwestern Missouri” Missouri’s 
 Ozarks plateaus region is a product of subtle deformation and epeirogenic 
 uplift that likely began during the middle Devonian\, spanning late Devoni
 an and Mississippian time\, and culminating in the Pennsylvanian. Previous
  investigators have shown that much of southern Missouri and northern Arka
 nsas was dissected by a series of right-lateral (NW-SE) and left-lateral (
 SW-NE) strike-slip faults. Stratigraphic successions in southwestern Misso
 uri are intertwined with structures\, hence a warp and weft analogy. Lower
  Mississippian strata of southwestern Missouri include carbonate mud mound
 s\, mostly in the Compton Limestone. These have been interpreted as bioher
 ms (reef mounds)\, displaced reef mounds\, anomalous accumulations produce
 d by baffling or mud-trapping organisms or microbial agents\, or in recent
  interpretation\, slide or slump masses associated with fault movements. A
 n effort to compare southwestern Missouri’s mounds with former and curre
 nt type-mounds of Waulsort\, Anseremme\, and Celles-Gendron rail tunnel is
  only partly complete and an ongoing international aspect of this study.
LOCATION:Beren Center Auditorium\, Slawson Hall Room G192\, 1420 Naismith D
 R\, Lawrence\, KS
SUMMARY:KU Geology Colloquium - Dr. Kevin Evans
URL;VALUE=URI:https://calendar.ku.edu/event/ku-geology-colloquium-dr-kevin-
 evans
CATEGORIES:Lectures & Presentations
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