A tool for reconstructing paleobathymetry on oceanic and continental crust.
PyBacktrack is a Python package that backtracks the paleo-water depth of ocean drill sites through time by combining a model of tectonic subsidence with decompaction of the site stratigraphic lithologies. PyBacktrack can also include the effects of mantle-convection driven dynamic topography on paleo-water depth, as well as sea-level variations. PyBacktrack provides a model of tectonic subsidence on both oceanic and continental crust. Ocean crust subsidence is based on a user-selected lithospheric age-depth model and the present-day unloaded basement depth. Continental crust subsidence is based on syn-rift and post-rift subsidence that is modelled using the total sediment thickness at the site and the timing of the transition from rifting to thermal subsidence. On sites that did not penetrate to basement, the age-coded stratigraphy is supplemented with a synthetic stratigraphic section that represents the undrilled section, whose thickness is estimated using a global sediment thickness map. This is essential for estimating the decompacted thickness of the total sedimentary section, and thus bathymetry, through time.
The documentation covers the pyBacktrack Python package. It includes installation, examples and an API reference.
master branch.The following paper covers the theory and algorithms of pyBacktrack:
It can be downloaded either at Geochemistry, Geophysics, Geosystems or ResearchGate.
PyBacktrack 1.4 is now available, and adds support for generating paleobathymetry grids from submerged present-day crust. PyBacktrack is available as a Python package and a Docker image. Installation instructions can be found online in the pyBacktrack documentation. Changes since version 1.3: Can now generate paleobathymetry grids: Submerged oceanic and continental present-day crust is backtracked and … Read more…
PyBacktrack 1.3 is now available as a Python package and a Docker image. The documentation is available at: https://pybacktrack.readthedocs.io/en/latest/ Changes since version 1.2: Supports Python 3: please also use the recent pyGPlates Python 3 release. Added the following output columns: dynamic_topography: change in dynamic topography elevation since present day decompacted_depth: depth from fully decompacted layers (using surface porosity only) … Read more…
PyBacktrack is a Python package that backtracks the paleo-water depth of ocean drill sites through time by combining a model of tectonic subsidence with decompaction of the site stratigraphic lithologies. PyBacktrack can also include the effects of mantle-convection driven dynamic topography on paleo-water depth, as well as sea-level variations. PyBacktrack provides a model of tectonic … Read more…
The pyBacktrack software package allows the backtracking of the paleo-water depth of ocean drill sites, providing a framework for reconstructing the accumulation history of sediment components through time. The software incorporates the effects of decompaction of common marine lithologies and allows backtracking of sites on both oceanic and continental crust. Backtracking on ocean crust is based on … Read more…