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DTSTART:20070311T020000
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UID:d65d3cb4-9968-469d-af22-9ab58ff6644e.234509@calendar.missouristate.edu
CREATED:20240229T144712Z
LAST-MODIFIED:20240229T144712Z
LOCATION:Roy Blunt Hall 345
SUMMARY:SEES Seminar: "The Okavango Rift in Botswana"
DESCRIPTION:The Okavango Rift (OR) in Botswana is part of the southwestern
  extension of the more mature East African Rift System. The OR is the you
 ngest part of the East African Rift System and is currently at the beginn
 ing stages of becoming a continental rift. Thus\, there have been numerou
 s questions if the OR is actually a contenental rift. There are no surfac
 e volcanic rocks\, limited evidence of extension and no plateau uplift. T
 o aid in determining if the OR is an active rift\, a series of geophysica
 l experiments have been conducted to study the lithospheric structure of 
 the OR. These studies include active and passive seismic\, gravity\, magn
 etics and magnetotellurics. The studies have shown that underneath the OR
 \, the lithosphere and asthenosphere display the classic signatures of a 
 continental rift including: thinned crust\, lower density and seismic vel
 ocities. Higher electrical conductivities in the lithosphere indicate a r
 ising warm asthenosphere. Additionally\, a magnetic analysis indicated th
 at the Curie Isothermal depths are elevated\, again agreeing with the oth
 er geophysical results. Thus\, the OR is considered to be in the initial 
 stages of continental rift evolution. The future extension will create ri
 ft-related grabens and magmatic activity will reach the surface.\n\n\nDr.
  Kevin Mickus\, distinguished professor of geology at Missouri State Univ
 ersity specializes in geophysical methods. He studies Earth's tectonic en
 vironment to explore for water\, mineral and geothremal resources.
X-ALT-DESC;FMTTYPE=text/html:&lt;html&gt;&lt;head&gt;&lt;title&gt;&lt;/title&gt;&lt;/head&gt;&lt;body&gt;&lt;p&gt;Th
 e Okavango Rift (OR) in Botswana is part of the southwestern extension of
  the more mature East African Rift System. The OR is the youngest part of
  the East African Rift System and is currently at the beginning stages of
  becoming a continental rift. Thus\, there have been numerous questions i
 f the OR is actually a contenental rift. There are no surface volcanic ro
 cks\, limited evidence of extension and no plateau uplift. To aid in dete
 rmining if the OR is an active rift\, a series of geophysical experiments
  have been conducted to study the lithospheric structure of the OR. These
  studies include active and passive seismic\, gravity\, magnetics and mag
 netotellurics. The studies have shown that underneath the OR\, the lithos
 phere and asthenosphere display the classic signatures of a continental r
 ift including: thinned crust\, lower density and seismic velocities. High
 er electrical conductivities in the lithosphere indicate a rising warm as
 thenosphere. Additionally\, a magnetic analysis indicated that the Curie 
 Isothermal depths are elevated\, again agreeing with the other geophysica
 l results. Thus\, the OR is considered to be in the initial stages of con
 tinental rift evolution. The future extension will create rift-related gr
 abens and magmatic activity will reach the surface.&lt;/p&gt;\n&lt;p&gt;&lt;a href="http
 s://people.missouristate.edu/kevinmickus/"&gt;Dr. Kevin Mickus&lt;/a&gt;\, &lt;a href
 ="https://search.missouristate.edu/people/kevinmickus"&gt;distinguished prof
 essor&lt;/a&gt; of geology at Missouri State University specializes in geophysi
 cal methods. He studies Earth's tectonic environment to explore for water
 \, mineral and geothremal resources.&lt;/p&gt;&lt;/body&gt;&lt;/html&gt;
DTSTART;TZID=America/Chicago:20240426T143000
DTEND;TZID=America/Chicago:20240426T153000
SEQUENCE:0
URL:http://www.geosciences.missouristate.edu
CATEGORIES:Public,Alumni,Current Students,Faculty,Future Students
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