Two dimensional joint inversion of direct current resistivity and radiomagnetotelluric data based on unstructured mesh

Ozyildirim O., DEMİRCİ İ., GÜNDOĞDU N. Y., CANDANSAYAR M. E.

JOURNAL OF APPLIED GEOPHYSICS, cilt.172, 2020 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 172
  • Basım Tarihi: 2020
  • Doi Numarası: 10.1016/j.jappgeo.2019.103885
  • Dergi Adı: JOURNAL OF APPLIED GEOPHYSICS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, Aerospace Database, Aquatic Science & Fisheries Abstracts (ASFA), Compendex, Geobase, INSPEC
  • Anahtar Kelimeler: Direct current resistivity, Radiomagnetotelluric, Joint Inversion, Mineral Exploration, Unstructured mesh, Modelling, DATA INCORPORATING TOPOGRAPHY, FINITE-ELEMENT, GROUNDWATER CONTAMINATION, DC RESISTIVITY, 3D INVERSION, ERT DATA, ELECTROMAGNETIC METHODS, MAGNETOTELLURIC DATA, 2D, SURFACE
  • Ankara Üniversitesi Adresli: Evet

Özet

Using the unstructured mesh, a new two-dimensional joint inversion algorithm has been developed for Radiomagnetotelluric and Direct current resistivity data. The unstructured mesh is generated with triangular cells, whose vertical and lateral lengths increase towards the depths. The Finite Element Method (FEM) has been used in the forward modelling part of the developed joint inversion algorithm. In the previous studies, structured grid-based joint inversion algorithms have been developed using the Finite Difference Method (FDM). In the structured grid-based algorithms, when the mesh is being generated with rectangular cells, the vertical lengths of the cells get bigger towards the depths while the lateral lengths remain constant. With the structured mesh, the undulated surface topography cannot be represented well enough. Also, because of the incompatible aspect ratio of model cell sizes in deeper model sections, the resolution of the model parameters will get smaller and cannot be resolved well with the structured grids. Imaging of surface topography and underground resistivity structures by the new algorithm requires fewer elements than those using structured grids. Therefore, the developed algorithm is faster than traditional 2D inversion algorithms. Furthermore, the resolution of the deeper model parameters has been increased by using the definition of the unstructured grid. A regularized inversion scheme with a smoothness-constrained stabilizer has been employed to invert the data. First, we have tested the developed joint inversion algorithm using synthetic data simplified from archaeological and mine site scenario and the results have been compared with the conventional algorithms using structured grids. We have also tested our algorithm with the real data which were collected from mineral investigation site at approximately 10 km east of the Elbistan district of Kahramanmara province, in the west of the Taurus Mountains, Turkey. The results show that the developed joint inversion algorithm is a powerful tool to detect both resistive and conductive targets. (C) 2019 Elsevier B.V. All rights reserved.