Abstract
Subsurface mapping includes various types of data, and thickness maps are one of the essential tools for the subsurface exploration geoscientist. Vertical thickness (isochore) maps are compiled in using different geostatistical methods for interpolation between input data points, which are in this case based on irregularly-spaced boreholes which have drilled the Lake Pannon sediments. Of the four used methods, Kriging produces the most sound map, whereas Triangulation with linear interpolation is practically useless when plotting irregular spatial data. Additional visualization tools were derived from the kriging map for cross-correlation, and supported the interpretation that the highest-thickness area is the depocenter in the North of the map, while the low-thickness zone is a basement ridge where older sediments can be found on the surface.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Zbornik radova Departmana za geografiju, turizam i hotelijerstvo
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
