PPT-Question from Monday (3/2/15): Can the 1-degree mantle convection that may have formed

Keller and Tackley 2009 Towards selfconsistent modeling of the martian dichotomy The influence of oneridge convection on crustal thickness distribution Icarus 202 429443 The dominant feature of the crustal thickness distribution obtained from oneridge convection in the mantle is a characteristic roughly elliptical shape that shows a striking first order similarity to the shape of the . Steps involved in Crustal deformationstudies using GPS geodesy Brian . Mapes. RSMAS. , University of Miami. Harvard, Oct 17 2009. (personal) historical moment. Two very old ideas. , . fiiinally. coming to fruition?. 1995: study convection sensitivities. inhibition vs. bulk instability (CAPE) controls. Transfer of Energy as Heat. Energy moves as heat in three ways. Heat is always a transfer of energy from objects at a higher temperature to a lower temperature. There are 3 different ways this transfer of energy can happen. The process which heat or electricity is . directly. transferred through a substance when there is a difference in temperature or electrical potential. . Conduction = TOUCHING . Conduction. Convection. Part 2 – Modes of Isolated Organization. AOS 453 – Spring 2014. 4/3/. 2014. Structure Of DMC Lectures This Week. Tuesday. DMC (Convective/Convection) Initiation. Chapter 7 in MR09. Isolated DMC Organization (Part 1). 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, . a Mantle Anchor Structure. Adam Dziewonski, . Ved. . Lekic. and Barbara Romanowicz . Two main points:. A very large structure at the bottom of the mantle imposes a permanent imprint on the tectonics at the surface. It determines the band in which subduction can occur and regions of high hot-spot activity.. To Make Foldable:. 1. On the short side of the paper, fold it down an inch.. 2. Now fold it in half, hamburger style.. 3. Now fold it in 1/3.. Conduction. Convection . Radiation. Heat Transfer. Examples. . 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. 1 TWTT0 s 10 s -wave reflection profile over ~1,000 km p. otential hotspot. p. otential hotspot. Based on illustration by . Lidunka. . Vočadlo. , University College London. We propose this scenario: . Layered Mantle Convection. Location of the boundary can be adjusted to suit different needs.. Goals: . Review isotopic and geophysical data, discuss elements of crustal structure. build a composite picture of the crust . compare results to mineral trends and tectonic features of successively younger events. reconstructions and tectonic implications. Randell . Stephenson et al.. A sub-crustal piercing point for North Atlantic . reconstructions and tectonic implications. Randell . Stephenson et al.. a . “tie” from one conjugate margin to . Kielman. -Schmitt, Ellen . Kooijman. , Anders . Scherstén. , . Jaana. . Halla. , . Wouter. Bleeker, J. Elis Hoffmann, Om Prakash Pandey, . Arathy. Ravindran, Alessandro Maltese, Klaus . Mezger. Secular change in the age of TTG sources during the Archean from in-situ Sr and Hf isotope analysis by LA-MC-ICPMS .