Vancouver Thermal Structure / Wedges on Venus | ||
This notebook, started by Dahlen in May 1990, is contained in an orange binder
and has both written notes from Dahlen as well as those of Charles A. Williams, who at the time
was a postdoc working at Princeton with Dahlen. In addition, due to the nature of the work
laid out in this notebook, there are myriad graphs detailing the supposed shapes and slopes of
decollements and wedges.
The notebook begins with Dahlen's own notes on the thermal structure of Vancouver, where he employs the heat equation in a moving medium to estimate how temperature varies with depth. However about halfway through the notebook it shifts gears to be more decollement and wedge centric, especially with respects to those on Venus. Helping Dahlen on this was of course Williams, mentioned above. This collection can be found at: Guyot Hall, Princeton, NJ, 08544. Back to Main Page |
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Pages | Sheet Numbers | |
[Notes on internal heating] | 1–6 | 1–2,1–4 |
One-dimensional erosion | 7–14 | 1–4,1–2 |
dq/dt for 1-D (growing rod) | 15 | N/A |
[Computer-generated graphs of Heat Flow as a function of Distance for Wedges] | 16–22 | N/A |
[Letter from Richard Iverson about question at AGU - followed by Dahlen's explanation] | 23–28 | N/A |
Non-Steady State - Narrow taper approximation | 29–44 | 1–16 |
On rereading England and Molnar JGR April '90 | 45–51 | 1–6 |
[Graphs of Heat Flux v. Distance for erosion/heating variation] | 52–56 | N/A |
Temperature field in the subducting plate | 57–77 | 1–10,1–11 |
[Graphs of Vancouver Thermal Structure & Analytical Solution] | 78–96 | N/A |
Zero Taper "Wedge" | 97–100 | 1–4 |
[Annotated Graphs of Taiwan's heat flux in wedge] | 101–112 | N/A |
Consider equation (98) in Dahlen Ann. Rev. Earth Planet Sci. | 113–119 | 1–7 |
[Wedge and Slab sediment velocity with graphs] | 120–126 | N/A |
Growth of a bulldozer wedge / Mass conservation law | 127–152 | 1–2,1–17,1–7 |
Fluid flow along the decollement | 153–162 | 1–8,1–2 |
[Annotated graphs of vedge velocity field and fluid movement] | 163–187 | N/A |
[Excerpt from textbook chapter on Permeability and Flow Rates] | 188–191 | N/A |
[Notes on wedge fluid movement on Venus] | 192–200 | N/A |
[Code for Wedge Height and Slope with accompanying graphs by Evelyn Price] | 201–258 | N/A |
[Notes on calculating slope of wedge] | 259–273 | 1–12 |
[Graphs on Decollement Dip and Elevation] | 274–283 | N/A |
Why the Critical Taper Equation is Second Order for a Compacting Wedge w/ Fluid Expulsion | 284–297 | 1–3,1–8 |
[Iterative Solution for Decollement Elevation] | 298–308 | N/A |
Effects of Non-brittle Behavior on Accretionary Wedge Deformation: Applications to Venus | 309–323 | N/A |
Thin skinned wedge | 324–326 | 1–3 |
Velocity Fields of a Wedge of Arbitrary Porosity, n(x,z) | 327–337 | 1–5,1–3 |
[fwedge2.f code to compute predicted wedge shape - includes ductile forces] | 338–346 | 1–9 |
Derivation of Vorder Bruegge and Fletcher Model with Power-law Flow | 347–352 | 1–6 |
Power-law Flow in a Wedge | 353–354 | 1 |
[Test case graphs for different rheological properties for the decollement] | 355–373 | N/A |
Wedge Synopsis | 374–379 | 1–6 |
[More graphs on decollement shape and slope] | 380–395 | N/A |
Green's Fcns | 396–398 | 1–3 |
Wedges | 399–401 | 1–3 |