PPT-Geology 6690/7690 Geodesy & Crustal Deformation

15 Sep 2017 AR Lowry 2017 Read for Fri 22 Sep Luttrell et al GRL 2013 GPS Positioning Resection location of intersecting ranges Uses three components i. Steps involved in Crustal deformationstudies using GPS geodesy Selwyn’s career goal #__: What does the . asthenosphere. have to do with earthquakes, crustal motions, and mantle convection?. Upper crust. Lower crust. Upper mantle. Upper crust. Lower crust. Upper mantle. Signal Analysis. 30. . Oct 2015. © A.R. Lowry . 2015. Last time: . Kalman. . Filtering & Example. • As with all methods that rely on information about the. . statistical behavior of signals/observations,. Michael Purucker, Planetary Geodynamics Lab, SGT @ NASA, . 17 May 2012, Moldavian Risks-1. Outline. . Near Earth objects today. NASA’s latest target, and a short personal history of the field. Natural history (origin, life span, size). . plateau. Update from CIDER 2011: Dynamics of Mountain Building. Marianne Karplus. 1,2. , . Warren . Caldwell. 1. , Flora Bajolet. 3. , . Whitney . Behr. 4. , . Jiajun. . Chong. 5,6. 1 . Stanford University, . . is the . measurement . and representation of the . shape of the Earth and its gravity field. Among the most important (& growing!) . a. pplications. of. . . geodesy monitoring/studies . Geodesy & Crustal Deformation. 28 . Oct . 2015. Last time(s): . Dislocation . Green’s . functions (. I) . Mogi. • . Inflation/Deflation of a fluid inclusion point source in an. elastic half-space produces displacements. Introduction. Lecture . 1 . – Spring 2016. 1. What is Structural Geology?. Structural Geology is the branch of geology that deals with the form, arrangement, and internal structure of the rocks, and especially with the description, representation, and analysis of structures, chiefly on a moderate to small scale. “Civilization exists by geologic consent” -Will Durant. Where are the world’s great cities located and why?. Why are Earliest Humans Here?. East African Rift. Water. Animals. Preservation of fossils. 25 Oct 2017. © A.R. Lowry . 2017. Last . time(s):. . Kinematic modeling of GPS velocities. • . Kinematic strain modeling. assumes. . two-. dimensional. . strain compatibility. . (i.e., strain behaves like 2D flow):. -Ge106-. Instructor:. Jean-Philippe Avouac (301NM; . avouac@gps.caltech.edu. ).  . Teaching Assistant:. Dustin Morris . dkmorris. @. caltech.edu.  . Administrative Assistant:. Lisa Christiansen (302NM, <. . from. . geostatistical. . analysis. Wolfgang Szwillus. Geoneutrino . science. . meeting. , Prague . 22. . October. 2019. O, . what. a . tangled. web . we. . weave. ,…. 38 TW. Al. 2. O. 3. Lecture 1: Introduction. Nature of Structural Geology. Study of . Deformation. What was the rock like before deformation?. What forces were required to deform the rock?. How long and in what order did deformation events proceed?. 2. Çanakkale . Onsekiz. Mart University, Engineering Faculty, Geological Engineering Department, . Çanakkale. , Turkey. #shareEGU2020, EGU General Assembly 2020. Deformation history of the Marmara .