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DTSTART:20070311T020000
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UID:104aca47-ef2d-424d-9c1c-984e0c3b1de1.194877@calendar.missouristate.edu
CREATED:20190114T193423Z
LAST-MODIFIED:20190114T193423Z
LOCATION:Roy Blunt Hall 345
SUMMARY:GGP Seminar: Jacob O. Thacker - "The what\, where\, when and why o
 f the Laramide orogeny"
DESCRIPTION:"The what\, where\, when and why of Laramide orogeny"\n\n\nEpi
 sodes of deformation thousands of kilometers into continental interiors r
 emains a major topic for furthering our understanding of plate tectonic p
 rocesses. One such event\, the Laramide orogeny\, is responsible for stru
 ctural arches and deep intermontane basins of the U.S. Rocky Mountains th
 at formed 90 to 45 million years ago within the stable cratonic interior.
  This mountain building phase has long perplexed geologists due to an aty
 pical "thick-skinned" deformation style and its far field strain. Signifi
 cant strides have been made to understand the Laramide ("what and where")
 \, though confusion and controversy still persist on its extent\, time fr
 ame\, and mechanisms. These topics will be discussed in this talk\, with 
 a focus on time frame by examining the detailed spatiotemporal distributi
 on ("where and when") of Laramide deformation. Interpretations on the tec
 tonic processes responsible ("why") will also be discussed in light of th
 ese and other data.\n\n\nJacob Thacker is a PhD. candidate at the Univers
 ity of New Mexico studying intraplate deformation in the western U.S. (Sa
 n Andreas-related and Rocky Mountains). He formally began working on Lara
 mide structure and tectonics during his master's degree at Montana State 
 University\, and holds a B.Sc. in Geological Sciences from Cleveland Stat
 e University.
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;&lt;s
 trong&gt;"The what\, where\, when and why of Laramide orogeny"&lt;/strong&gt;&lt;/p&gt;\
 n&lt;p&gt;Episodes of deformation thousands of kilometers into continental inte
 riors remains a major topic for furthering our understanding of plate tec
 tonic processes. One such event\, the Laramide orogeny\, is responsible f
 or structural arches and deep intermontane basins of the U.S. Rocky Mount
 ains that formed 90 to 45 million years ago within the stable cratonic in
 terior. This mountain building phase has long perplexed geologists due to
  an atypical "thick-skinned" deformation style and its far field strain. 
 Significant strides have been made to understand the Laramide ("what and 
 where")\, though confusion and controversy still persist on its extent\, 
 time frame\, and mechanisms. These topics will be discussed in this talk\
 , with a focus on time frame by examining the detailed spatiotemporal dis
 tribution ("where and when") of Laramide deformation. Interpretations on 
 the tectonic processes responsible ("why") will also be discussed in ligh
 t of these and other data.&lt;/p&gt;\n&lt;p&gt;Jacob Thacker is a PhD. candidate at t
 he University of New Mexico studying intraplate deformation in the wester
 n U.S. (San Andreas-related and Rocky Mountains). He formally began worki
 ng on Laramide structure and tectonics during his master's degree at Mont
 ana State University\, and holds a B.Sc. in Geological Sciences from Clev
 eland State University.&lt;/p&gt;&lt;/body&gt;&lt;/html&gt;
DTSTART;TZID=America/Chicago:20190322T143000
DTEND;TZID=America/Chicago:20190322T153000
SEQUENCE:0
URL:http://www.geosciences.missouristate.edu
CATEGORIES:Public,Alumni,Current Students,Faculty,Future Students,Staff
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