Geodynamics and Geofluids modelling laboratory
In the geodynamics and geofluids modelling laboratory (GGM), we tackle a range of different problems relating to the earth’s surface and subsurface evolution, including crustal deformation, topographic evolution, hydrogeological and temperature responses to tectonics and other forcings and the advanced use of thermochronology in tectonic and groundwater models.
Our lab uses both commercially available software as well as in house codes and solutions. We use a set of 4 multi-core desktop servers that run linux and windows operating systems. For an overview of the available hardware and model software and access to these machines for your own modelling projects, please see here
We highlight a couple of main research interests here:
1) Mechanical simulation and inversion of balanced cross sections
cross sections are geological profiles constructed according to
certain geometric conservation rules (line lengths of bedding
surfaces, total area of layers) between the deformed (present day)
and undeformed (i.e. beds layed out flat, folds “ironed” out, and
fault displacement removed) states. Hence, where geologists have
often little or no information, in the subsurface, they “fill in
the gap” with these rules, and assume the geometric consistency of
the section makes it a reasonable guess (likely better at least than
one not conforming to the same rules).
With the huge advances in computing, it is now possible to simulate the evolution of a geological cross section, and hence, the entire geohistory contained within it, using forward mechanical models. It is then interesting to see how, starting with the undeformed state given by a balanced section, the mechanical model evolves when the total amount of shortening from the section is applied to it. The core of our model is a discrete element code (PFC5, Itasca consultants) which models solids as an aggregate of large numbers of “grains” with specific elastic and frictional properties.
Here at GGM, we have developed codes and methods to include the effects of erosion and development of topography along the section. We can then vary a number of boundary conditions (e.g. basal friction, overall geometry, material parameters of layers, number of layers and erosion history) to and test for optimal fit between a forward mechanical model and an actual balanced section (Hindle and Kley, 2016a) We are now working on a more advanced system for correlating model results with final state cross sections, giving a numerical, error estimate (Hindle and Kley, 2016b)
2) Quantifying the thermal and exhumation history of sedimentary basins
We use a new code PyBasin to simulate burial and thermal history of 1D (borehole) sections in sedimentary basins to see how much information we can extract on the thermal and geological history of these basins from low-temperature thermochronology (apatite fission track and (U-Th)/He data) and vitrinite reflectance data. Initial model experiments to quantify intraplate deformation and exhumation of a basin in the southern Netherlands have been published in Luijendijk et al. (2011). The code has since been parallelized and can be used to run large (10,000-100,000) model runs automatically to explore parameter space or to model thermal history at large spatial scales. We use this currently to quantify the still enigmatic exhumation histories of the Molasse Basin (von Hagke et al., 2015) and a large part of the European plate (in preparation).
3) Numerical modelling of groundwater flow, heat flow and solute transport at large spatial scales
We use an in-house developed parallel model code (Grompy) to simulate groundwater flow in a large series of 2D cross sections that cover the variability of groundwater flow systems globally. An application of this method to quantify groundwater flux to the oceans at a global scale is currently in review.
Hindle, D., & Kley, J. (2016a). Mechanical forward modeling of balanced cross sections. In Applied Numerical Modeling in Geomechanics – 2016 – Gómez, Detournay, Hart & Nelson (eds.) Paper: 07-03 ©2016 Itasca International Inc., Minneapolis, ISBN 978-0-9767577-4-0 (pdf)
Hindle, D., & Kley, J. (2016b). Modelling" reality" in tectonics: Simulation of the mechanical evolution of the Jura Mountains-Molasse Basin system, and routes to forward-inverse modelling of fold thrust belts. In EGU General Assembly Conference Abstracts (Vol. 18, p. 10470) (pdf)
E., R. T. Van Balen, M. Ter Voorde, and P. A. M. Andriessen (2011),
Reconstructing the Late Cretaceous inversion of the Roer Valley
Graben (southern Netherlands) using a new model that integrates
burial and provenance history with fission track thermochronology, J.
Geophys. Res., 116(B06402), 1–19, doi:10.1029/2010JB008071. (link)
Hagke, C., E. Luijendijk, R. Ondrak, and J. Lindow (2015),
Quantifying erosion rates in the Molasse basin using a high
resolution data set and a new thermal model, Geotectonic
94–97, doi:10.1127/1864-5658/2015-36. (link)