Incorporating the spatial positions of the major formation boundaries, including the effects of faulting, folding, and erosion (unconformities). The major stratigraphic divisions are further subdivided into layers of cells with differing geometries with relation to the bounding surfaces (parallel to top, parallel to base, proportional). Maximum cell dimensions are dictated by the minimum sizes of the features to be resolved (everyday example: On a digital map of a city, the location of a city park might be adequately resolved by one big green pixel, but to define the locations of the basketball court, the baseball field, and the pool, much smaller pixels – higher resolution – need to be used).
Each cell in the model is assigned a rock type. In a coastal clastic environment, these might be beach sand, high water energy marine upper shoreface sand, intermediate water energy marine lower shoreface sand, and deeper low energy marine silt and shale. The distribution of these rock types within the model is controlled by several methods, including map boundary polygons, rock type probability maps, or statistically emplaced based on sufficiently closely spaced well data.
Reservoir quality parameters almost always include porosity and permeability, but may include measures of clay content, cementation factors, and other factors that affect the storage and deliverability of fluids contained in the pores of those rocks. Geostatistical techniques are most often used to populate the cells with porosity and permeability values that are appropriate for the rock type of each cell.
Most rock is completely saturated with groundwater. Sometimes, under the right conditions, some of the pore space in the rock is occupied by other liquids or gases. In the energy industry, oil and natural gas are the fluids most commonly being modelled. The preferred methods for calculating hydrocarbon saturations in a geological model incorporate an estimate of pore throat size, the densities of the fluids, and the height of the cell above the water contact, since these factors exert the strongest influence on capillary action, which ultimately controls fluid saturations.
An important part of geological modelling is related to geostatistics. In order to represent the observed data, often not on regular grids, we have to use certain interpolation techniques. The most widely used technique is kriging which uses the spatial correlation among data and intends to construct the interpolation via semi-variograms. To reproduce more realistic spatial variability and help assess spatial uncertainty between data, geostatistical simulation based on variograms, training images, or parametric geological objects is often used, e.g.5
Geologists involved in mining and mineral exploration use geological modelling to determine the geometry and placement of mineral deposits in the subsurface of the earth. Geological models help define the volume and concentration of minerals, to which economic constraints are applied to determine the economic value of the mineralization. Mineral deposits that are deemed to be economic may be developed into a mine.
Geomodelling and CAD share a lot of common technologies. Software is usually implemented using object-oriented programming technologies in C++, Java or C# on one or multiple computer platforms. The graphical user interface generally consists of one or several 3D and 2D graphics windows to visualize spatial data, interpretations and modelling output. Such visualization is generally achieved by exploiting graphics hardware. User interaction is mostly performed through mouse and keyboard, although 3D pointing devices and immersive environments may be used in some specific cases. GIS (Geographic Information System) is also a widely used tool to manipulate geological data.
Geometric objects are represented with parametric curves and surfaces or discrete models such as polygonal meshes.67
Problems pertaining to Geomodelling cover:89
In the 70's, geomodelling mainly consisted of automatic 2D cartographic techniques such as contouring, implemented as FORTRAN routines communicating directly with plotting hardware. The advent of workstations with 3D graphics capabilities during the 80's gave birth to a new generation of geomodelling software with graphical user interface which became mature during the 90's.121314
Since its inception, geomodelling has been mainly motivated and supported by oil and gas industry.
Software developers have built several packages for geological modelling purposes. Such software can display, edit, digitise and automatically calculate the parameters required by engineers, geologists and surveyors. Current software is mainly developed and commercialized by oil and gas or mining industry software vendors:
Moreover, industry Consortia or companies are specifically working at improving standardization and interoperability of earth science databases and geomodelling software:
Mallet, J. L. (2008). Numerical Earth Models. European Association of Geoscientists and Engineers (EAGE Publications bv). ISBN 978-90-73781-63-4. Archived from the original on 2016-03-04. Retrieved 2013-08-20. 978-90-73781-63-4 ↩
Fanchi, John R. (August 2002). Shared Earth Modeling : Methodologies for Integrated Reservoir Simulations. Gulf Professional Publishing (Elsevier imprint). pp. xi–306. ISBN 978-0-7506-7522-2. 978-0-7506-7522-2 ↩
Chen, Shang-Ying; Hsieh, Bieng-Zih; Hsu, Kuo-Chin; Chang, Yi-Fei; Liu, Jia-Wei; Fan, Kai-Chun; Chiang, Li-Wei; Han, Yin-Lung (January 2021). "Well spacing of the doublet at the Huangtsuishan geothermal site, Taiwan". Geothermics. 89: 101968. Bibcode:2021Geoth..8901968C. doi:10.1016/j.geothermics.2020.101968. S2CID 224972986. https://www.sciencedirect.com/science/article/pii/S0375650520302601 ↩
Caumon, G., Collon-Drouaillet, P., Le Carlier de Veslud, C., Sausse, J. and Viseur, S. (2009), Surface-based 3D modeling of geological structures, Mathematical Geosciences, 41(9):927–945 ↩
Cardenas, IC (2023). "A two-dimensional approach to quantify stratigraphic uncertainty from borehole data using non-homogeneous random fields". Engineering Geology. 314: 107001. Bibcode:2023EngGe.31407001C. doi:10.1016/j.enggeo.2023.107001. S2CID 255634245. https://doi.org/10.1016%2Fj.enggeo.2023.107001 ↩
Mallet, J.-L., Geomodeling, Applied Geostatistics Series. Oxford University Press. ISBN 978-0-19-514460-4 /wiki/ISBN_(identifier) ↩
Caumon, G., Towards stochastic time-varying geological modeling (2010), Mathematical Geosciences, 42(5):(555-569) ↩
Perrin, M., Zhu, B., Rainaud, J.F. and Schneider, S. (2005), Knowledge-driven applications for geological modeling, "Journal of Petroleum Science and Engineering", 47(1–2):89–104 ↩
Tahmasebi, P., Hezarkhani, A., Sahimi, M., 2012, Multiple-point geostatistical modeling based on the cross-correlation functions, Computational Geosciences, 16(3):779-79742 https://doi.org/10.1007%2Fs10596-012-9287-1 ↩
M.R. Alvers, H.J. Götze, B. Lahmeyer, C. Plonka and S. Schmidt, 2013, Advances in 3D Potential Field Modeling EarthDoc, 75th EAGE Conference & Exhibition incorporating SPE EUROPEC 2013 http://www.earthdoc.org/publication/publicationdetails/?publication=68364 ↩
Dynamic Graphics History Archived 2011-07-25 at the Wayback Machine http://www.dgi.com/dynamicgraphics/dgimain.html ↩
Origin of the Gocad software http://www.gocad.org/w4/index.php/gocad/origin ↩
J. L. Mallet, P. Jacquemin, and N. Cheimanoff (1989). GOCAD project: Geometric modeling of complex geological surfaces, SEG Expanded Abstracts 8, 126, doi:10.1190/1.1889515 /wiki/Doi_(identifier) ↩