Title: Strata2.1
1- Strata2.1
-
- Forward Modeling to learn about the controls of
Tectonics, sedimentation and eustasy on
stratigraphic geometry - Strata2.1 is Open Source software was written by
Flemings, Grotzinger, Morris and Nelson, 1996
2Baltimore Canyon Trough
- Movie produced by students Spinelli an Hotsinski
- http//hydro.geosc.psu.edu/Sed_html/movie1.html
Sea-level drops produces major regional
unconformity
3Mixed Carbonate-clastic systemsMiddle to Late
Ordovician, Central Pennsylvania
- The following movie was created by Roberta
Hotsinski and Andrew Hoover http//hydro.geosc.ps
u.edu/Sed_html/movie2.html
4Low heat-flux rift basin
- http//hydro.geosc.psu.edu/Sed_html/movie4.html
Sediment traps heat faster than it can escape
(thermal blanket effect)
5High sediment-flux rift basin
- http//hydro.geosc.psu.edu/Sed_html/movie5.html
A thick thermal blanket traps heat in deeper
parts of the basin
6Near-forebulge stratigraphy
7Near-forebulge stratigraphy
8Near-forebulge stratigraphy
Erosion
9Near-forebulge stratigraphy
10Near-forebulge stratigraphy
11Near-forebulge stratigraphy
Erosion
12Input parameters in Strata
- Sediment types
- Compaction and composition
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
13Input parameters in Strata
- Sediment types
- Compaction and composition
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
14Sediment Types
Clastic sediments
Continental diffusion rate
pelagic
Marine diffusion rate
Sediment flux
Sedimentation rates
15q-volume sediment flux (m2/s) k- diffusion
constant h-elevation x-horizontal distance
Continental diffusion rate
Values can vary across the model and input in
tabular form (x q1 x2 q2 x3 q3 etc.)
Sedimentation rates
16Sediment Types
Carbonate sediments
- Sedimentation rate types simple exponential
decay (epeiric)
- Sedimentation rate types constant and simple
exponential decay below a certain depth
(oceanic)
Sedimentation rates
17Input parameters in Strata
- Sediment types
- Compaction and composition
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
18Compaction and Composition
Porosity versus depth- exponential compaction
relation Sand-shale ratios based on water-depth
or diffusion constants
19Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
20Tectonic styles of subsidence
- Subsidence increases linearly left to right
(foreland) - Subsidence is constant (flat geometry/cratonic)
- Subsidence increases linearly right to left
(passive) - Simple elastic flexure or local isostasy (Te0)
21Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
22Sea-level changes
- As a file (all parameters can be entered as such)
- As a sinusoid
23Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
24Heat Flow
- mW/m2 (e.g., 60 for continents)
- Thermal conductivity is calculated as a funciton
of the sand, shale and fluid content which may be
derived from the sedimentation diffusion
constants and water depths - Thermal maturation indices can then be calculated
- Heat flow is one-dimensional (hot-to-cold
--down-up)
25Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
26Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
27Wheeler Plot
Erosion
sea-level drop
time
distance
28Input parameters in Strata
- Sediment types
- Compaction behavior
- Tectonic styles
- Sea-level changes
- Heat flow
Output data in Strata (versus time)
Depth-sections Time-sections Wheeler
plots Seismic responses
29Seismic Responses
- Seismic velocity is calculated using the ration
of sand, shale and water - Density for sand, shale and fluid is user-input
- Seismic sections are displayed