Model:Cyclopath: Difference between revisions

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{{Modeler information
|First name=Peter
|Last name=Burgess
|Type of contact=Model developer
|Institute / Organization=Royal Holloway University of London
|Town / City=Egham
|Postal code=TW20 0EX
|State=NO STATE
|Country=United Kingdom
|Email address=p.burgess@es.rhul.ac.uk
}}
{{Model identity
{{Model identity
|Model type=Single
|Model type=Single
|Categories=Carbonate
}}
{{Start models incorporated}}
{{End a table}}
{{Model identity2
|ModelDomain=Marine
|Spatial dimensions=2D, 3D
|Spatial dimensions=2D, 3D
|One-line model description=A 2D/3D model of carbonate cyclicity
|One-line model description=A 2D/3D model of carbonate cyclicity
|Extended model description=A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry  
|Extended model description=A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry
}}
{{Start model keyword table}}
{{Model keywords
|Model keywords=stratigraphy
}}
{{End a table}}
{{Modeler information
|First name=Peter
|Last name=Burgess
|Type of contact=Model developer
|Institute / Organization=Shell International E&P
|Town / City=Rijswijk
|Postal code=2288 GS
|Country=Netherlands
|Email address=p.burgess@es.rhul.ac.uk
|Phone=+(31) 610 97 3376
}}
}}
{{Model technical information
{{Model technical information
Line 23: Line 32:
|Does model development still take place?=No
|Does model development still take place?=No
|End year development=2005
|End year development=2005
|DevelopmentCode=As is, no updates are provided
|DevelopmentCodeYearChecked=2020
|Model availability=As code
|Model availability=As code
|Source code availability=Through owner
|Source code availability=Through CSDMS repository
|Source csdms web address=https://github.com/csdms-contrib/cyclopath
|Program license type=Other
|Program license type=Other
|Program license type other=--
|Program license type other=--
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|Memory requirements=Variable
|Memory requirements=Variable
|Typical run time=Minutes to hours
|Typical run time=Minutes to hours
}}
}}
{{Input - Output description
{{Input - Output description
|Describe input parameters=Various text files defining initial conditions and parameter values  
|Describe input parameters=Various text files defining initial conditions and parameter values
|Input format=ASCII
|Input format=ASCII
|Describe output parameters=A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step  
|Describe output parameters=A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step
|Output format=ASCII
|Output format=ASCII
|Pre-processing software needed?=No
|Pre-processing software needed?=No
|Post-processing software needed?=Yes
|Post-processing software needed?=Yes
|Describe post-processing software=GMT routines or Matlab  
|Describe post-processing software=GMT routines or Matlab
|Visualization software needed?=Yes
|Visualization software needed?=Yes
|If above answer is yes=Matlab
|If above answer is yes=Matlab
Line 52: Line 61:
Depth dependent sediment transport
Depth dependent sediment transport
Diffusional sediment transport
Diffusional sediment transport
|Describe key physical parameters and equations=See Burgess et al. (2001), Basin Research  
|Describe key physical parameters and equations=See Burgess et al. (2001), Basin Research
|Describe length scale and resolution constraints=10s to 100s km length scale  
|Describe length scale and resolution constraints=10s to 100s km length scale
|Describe time scale and resolution constraints=Internal time step years to decades
|Describe time scale and resolution constraints=Internal time step years to decades
Model chron resolution 1000 years
Model chron resolution 1000 years
Total run time 1-10 My
Total run time 1-10 My
|Describe any numerical limitations and issues=Diffusion and other sediment transport routines require short time steps  
|Describe any numerical limitations and issues=Diffusion and other sediment transport routines require short time steps
}}
}}
{{Model testing
{{Model testing
|Describe available calibration data sets=Any outcrop data showing (or purporting to show) cyclical platform interior strata  
|Describe available calibration data sets=Any outcrop data showing (or purporting to show) cyclical platform interior strata
|Describe available test data sets=--
|Describe ideal data for testing=--
}}
}}
{{Users groups model
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=No, but open to suggestions  
|Do you have current or future plans for collaborating with other researchers?=No, but open to suggestions
}}
}}
{{Documentation model
{{Documentation model
|Provide key papers on model if any=Papers:
* Burgess, P.M., Wright, V.P. & Emery, D. (2001) Numerical forward modelling of a peritidal carbonate parasequence development: implications for outcrop interpretation. Basin Research, 13, p.1-16.
* Burgess, P.M. (2001) Modelling Carbonate Sequence Development without Relative Sea Level Oscillations, Geology, vol. 29, p. 1127-1130.
* Barnett, A.J., Burgess, P.M., and Wright, V.P. (2002), Icehouse world sea-level behaviour and resulting stratal patterns in late Visean (Mississippian) carbonate platforms: integration of numerical forward modelling and outcrop studies, Basin Research, v.14, p.417-438.
* Burgess, P.M., and Wright, V.P, (2003) Numerical forward modelling of carbonate platform dynamics: An evaluation of complexity and completeness, Journal of Sedimentary research, v.73, p.637-652.
* Burgess, P.M., and Emery, D. (2005), Sensitive dependence, divergence and unpredictable behaviour in a stratigraphic forward model of a carbonate system, in Curtis, A., and Wood, R. (eds.) Geological prior information: informing science and engineering, Geological Society, London, Special Publication 239, p.77-94.
* Burgess, P.M., 2006, The signal and the noise: forward modeling of allocyclic and autocyclic processes influencing peritidal carbonate stacking patterns, Journal of Sedimentary Research; v. 76; no. 7; p. 962-977.
|Manual model available=No
|Manual model available=No
}}
}}
{{Additional comments model}}
{{Additional comments model}}
{{Infobox Model
{{CSDMS staff part
|model name              = Cyclopath
|OpenMI compliant=No but possible
|developer                = '''Burgess''', Peter
|IRF interface=No but possible
|one-line-description    = A 2D/3D model of carbonate cyclicity   
|CMT component=No but possible
|type                    = Model
|CCA component=No but possible
|source                  = [[image:Red1.png]]
}}
}}
{{DOI information
|DOI model=10.1594/IEDA/100106
|DOI assigned to model version=0.1
|DOI-year assigned to model version=2011
|DOI-filelink=https://csdms.colorado.edu/pub/models/doi-source-code/cyclopath-10.1594.IEDA.100106-0.1.tar.gz
}}
{{Start coupled table}}
{{End a table}}
{{End headertab}}
{{{{PAGENAME}}_autokeywords}}
<!-- Edit the part above to update info on other papers -->
<!-- Edit the part above to update info on other papers -->


== Cyclopath ==
__TOC__
===Introduction===
=== History ===
=== Papers ===
=== Cyclopath Questionnaire ===
==== Contact Information ====
{| class="wikitable"
| class="model_col1"| Model:
| class="model_col2"| Cyclopath
|-
| class="model_col1"| Contact person:
| class="model_col2"| Peter Burgess (Model developer)
|-
| class="model_col1"| Institute:
| class="model_col2"| Royal Holloway University of London
|-
| class="model_col1"| City:
| class="model_col2"|
|-
| class="model_col1"| Country:
| class="model_col2"|
|-
| class="model_col1"| Email:
| class="model_col2"| p.burgess@es.rhul.ac.uk
|-
| class="model_col1"| 2nd person involved:
| class="model_col2"| --
|-
| class="model_col1"| 3rd person involved:
| class="model_col2"| --
|}
==== Model description ====
{| class="wikitable" 
| class="model_col1"| Model type:
| class="model_col2"| Single model for the carbonate domain.
|-
| class="model_col1"| Description:
| class="model_col2"| A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry
|}
==== Technical information ====
{| class="wikitable" 
| class="model_col1"| Supported platforms:
| class="model_col2"| Unix, Linux
|-
| class="model_col1"| Programming language:
| class="model_col2"| C
|-
| class="model_col1"| Model was developed started from:
| class="model_col2"| 1998 and ended in 2005
|-
| class="model_col1"| To what degree will the model become available:
| class="model_col2"| As code
|-
| class="model_col1"| Current license type:
| class="model_col2"| --
|-
| class="model_col1"| Memory requirements:
| class="model_col2"| variable
|-
| class="model_col1"| Typical run time:
| class="model_col2"| minutes to hours
|}
==== Input / Output description ====
{| class="wikitable" 
| class="model_col1"| Input parameters:
| class="model_col2"| Various text files defining initial conditions and parameter values
|-
| class="model_col1"| Input format:
| class="model_col2"| ASCII
|-
| class="model_col1"| Output parameters:
| class="model_col2"| A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step   
|-
| class="model_col1"| Output format:
| class="model_col2"| ASCII
|-
| class="model_col1"| Post-processing software (if needed):
| class="model_col2"| Yes, GMT routines or Matlab
|-
| class="model_col1"| Visualization software (if needed):
| class="model_col2"| Yes, Matlab, GMT.
|}
==== Process description ====
{| class="wikitable" 
| class="model_col1"| Processes represented by model:
| class="model_col2"| Subsidence and uplift
Eustatic oscillations<br>
Water depth dependent in-situ carbonate production<br>
Spatial variations in sediment production rate<br>
Depth dependent sediment transport<br>
Diffusional sediment transport<br>
|-
| class="model_col1"| Key physical parameters & equations:
| class="model_col2"| See Burgess et al. (2001), Basin Research
|-
| class="model_col1"| Length scale & resolution constraints:
| class="model_col2"| 10s to 100s km length scale
|-
| class="model_col1"| Time scale & resolution constraints:
| class="model_col2"| Internal time step years to decades<br>
Model chron resolution 1000 years<br>
Total run time 1-10 My<br>
|-
| class="model_col1"| Numerical limitations and issues :
| class="model_col2"| Diffusion and other sediment transport routines require short time steps
|}
==== Testing ====
{| class="wikitable" 
| class="model_col1"| Available calibration data sets:
| class="model_col2"| Any outcrop data showing (or purporting to show) cyclical platform interior strata
|-
| class="model_col1"| Available test data sets:
| class="model_col2"| --
|-
| class="model_col1"| Ideal data for testing:
| class="model_col2"| --
|}
====User groups ====
{| class="wikitable" 
| class="model_col1"| Currently or plans for collaborating with:
| class="model_col2"| No, but open to suggestions
|}
==== Documentation ====
{| class="wikitable" 
| class="model_col1"| Key papers of the model:
| class="model_col2"|
*Burgess, P.M., Wright, V.P. & Emery, D. (2001) Numerical forward modelling of a peritidal carbonate parasequence development: implications for outcrop interpretation. Basin Research, 13, p.1-16.
Burgess, P.M. (2001) Modelling Carbonate Sequence Development without Relative Sea Level Oscillations, Geology, vol. 29, p. 1127-1130.
*Barnett, A.J., Burgess, P.M., and Wright, V.P. (2002), Icehouse world sea-level behaviour and resulting stratal patterns in late Visean (Mississippian) carbonate platforms: integration of numerical forward modelling and outcrop studies, Basin Research, v.14, p.417-438.
*Burgess, P.M., and Wright, V.P, (2003) Numerical forward modelling of carbonate platform dynamics: An evaluation of complexity and completeness, Journal of Sedimentary research, v.73, p.637-652.
*Burgess, P.M., and Emery, D. (2005), Sensitive dependence, divergence and unpredictable behaviour in a stratigraphic forward model of a carbonate system, in Curtis, A., and Wood, R. (eds.) Geological prior information: informing science and engineering, Geological Society, London, Special Publication 239, p.77-94.
*Burgess, P.M., 2006, The signal and the noise: forward modeling of allocyclic and autocyclic processes influencing peritidal carbonate stacking patterns, Journal of Sedimentary Research; v. 76; no. 7; p. 962-977.
|-
| class="model_col1"| Is there a manual available:
| class="model_col2"| No
|-
| class="model_col1"| Model website if any:
| class="model_col2"| --
|}
==== Additional comments ====
{| class="wikitable" 
| class="model_col1"| Comments:
| class="model_col2"| --
|}


=== Issues ===


=== Help ===
==Introduction==


=== Input Files ===
== History ==


=== Output Files ===
== References  ==
<br>{{AddReferenceUploadButtons}}<br><br>
{{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br>
{{Include_featured_references_models_cargo}}<br>


=== Download ===
== Issues ==


=== Source ===
== Help ==
{{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}


== Input Files ==


[[Category:Carbonate]]
== Output Files ==

Latest revision as of 16:13, 21 April 2021



Cyclopath


Metadata

Also known as
Model type Single
Model part of larger framework
Note on status model
Date note status model
Incorporated models or components:
Spatial dimensions 2D, 3D
Spatial extent
Model domain Marine
One-line model description A 2D/3D model of carbonate cyclicity
Extended model description A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry
Keywords:

stratigraphy,

Name Peter Burgess
Type of contact Model developer
Institute / Organization Shell International E&P
Postal address 1
Postal address 2
Town / City Rijswijk
Postal code 2288 GS
State
Country Netherlands
Email address p.burgess@es.rhul.ac.uk
Phone +(31) 610 97 3376
Fax


Supported platforms
Unix, Linux
Other platform
Programming language

C

Other program language
Code optimized
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 1998
Does model development still take place? No
If above answer is no, provide end year model development 2005
Code development status As is, no updates are provided
When did you indicate the 'code development status'? 2020
Model availability As code
Source code availability
(Or provide future intension)
Through CSDMS repository
Source web address
Source csdms web address https://github.com/csdms-contrib/cyclopath
Program license type Other
Program license type other --
Memory requirements Variable
Typical run time Minutes to hours


Describe input parameters Various text files defining initial conditions and parameter values
Input format ASCII
Other input format
Describe output parameters A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step
Output format ASCII
Other output format
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? Yes
Describe post-processing software GMT routines or Matlab
Visualization software needed? Yes
If above answer is yes Matlab
Other visualization software GMT


Describe processes represented by the model Subsidence and uplift

Eustatic oscillations Water depth dependent in-situ carbonate production Spatial variations in sediment production rate Depth dependent sediment transport Diffusional sediment transport

Describe key physical parameters and equations See Burgess et al. (2001), Basin Research
Describe length scale and resolution constraints 10s to 100s km length scale
Describe time scale and resolution constraints Internal time step years to decades

Model chron resolution 1000 years Total run time 1-10 My

Describe any numerical limitations and issues Diffusion and other sediment transport routines require short time steps


Describe available calibration data sets Any outcrop data showing (or purporting to show) cyclical platform interior strata
Upload calibration data sets if available:
Describe available test data sets
Upload test data sets if available:
Describe ideal data for testing


Do you have current or future plans for collaborating with other researchers? No, but open to suggestions
Is there a manual available? No
Upload manual if available:
Model website if any
Model forum / discussion board
Comments


This part will be filled out by CSDMS staff

OpenMI compliant No but possible
BMI compliant No but possible
WMT component No but possible
PyMT component
Is this a data component
DOI model 10.1594/IEDA/100106
For model version 0.1
Year version submitted 2011
Link to file https://csdms.colorado.edu/pub/models/doi-source-code/cyclopath-10.1594.IEDA.100106-0.1.tar.gz
Can be coupled with:
Model info

Nr. of publications: 7
Total citations: 467
h-index: 6
m-quotient: 0.19
Qrcode Cyclopath.png
Link to this page




Introduction

History

References




Nr. of publications: 7
Total citations: 467
h-index: 6
m-quotient: 0.19



Featured publication(s)YearModel describedType of ReferenceCitations
Burgess, P.M.; Wright, V.P.; Emery, D. 2001. Numerical forward modelling of peritidal carbonate parasequence development: implications for outcrop interpretation. Basin Research, 13, 1–16. 10.1046/j.1365-2117.2001.00130.x
(View/edit entry)
2001 Cyclopath

Model overview

86
Burgess, P.M.; 2011. Cyclopath, version 0.1.. , , https://csdms.colorado.edu/pub/models/doi-source-code/cyclopath-10.1594.IEDA.100106-0.1.tar.gz. 10.1594/IEDA/100106
(View/edit entry)
2011 Cyclopath
Source code ref. 0
See more publications of Cyclopath


Issues

Help

Input Files

Output Files