Energetics of the Earth: Mountain Building. Theresa Zajac, Haiyan Fu. Mountain Building model.
Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.
Energetics of the Earth:Mountain Building
Theresa Zajac, Haiyan Fu
Mountain Building model
The Solar System began to form about 6 billion years ago and the Earth and other planetsabout 4.5 billion years ago. mountain building events expend energy on time scales of several hundred million years. whereas others, like earthquakes, expend energy on time scales of a few seconds
First, is mountain building resulting primarily from heat. The uplift comes because heat from inside the earth heats the overlying lithosphere, causing it to expand, lifting and swelling the surface upward.
Second is mechanical mountain building. tension (pulling apart) and compression (squeezing together). The relief (differences in elevation) come primarily because different blocks of earth move relative to each other, either falling or rising vertically, or one block being shoved (thrust) horizontally over another.
The overall balance of energy in a steady state FTB:
The static equilibrium equation:
Schematic cross -section of a critically tapered steady state fold-and-thrust belt(DahlenF.A,1988)
WB: the rate of work on the base and front of the FTB
WD: the rate energy is dissipated against friction on the decollement fault
WS: the rate energy is dissipated by internal frictional processes within the deforming brittle wedge
WG: the rate of work against gravitational body forces
Schematic cross section of a steady state FTB and underlying subducting plate(Barr T.D,1989 )
QT: total rate at which heat is conducted out of the top of the Wedge
QB: the total rate at which heat is conducted into the base of the wedge from the top of the basal decollement fault
QA: the total rate which heat is advected into the wedge across all the boundaries
HR: total rate of radiogenic heating
HS:thetotal rate of internal strain heatin