Proving the correctness of transient electromagnetic data processing method on theoretical models of horizontally layered earth

https://tapchi.humg.edu.vn/en/archives?article=482
  • Affiliations:

    1 Trường Đại học Mỏ - Địa chất

  • Received: 17th-Aug-2015
  • Revised: 11st-Oct-2015
  • Accepted: 30th-Oct-2015
  • Online: 30th-Oct-2015
Views: 1659
Downloads: 498
Rating: 5.0, Total rating: 49
Yours rating

Abstract:

Conductivity-depth processing is such an effective method to improve resolution and locality for transient electromagnetic (TEM) data. Its applications on theoretical models led to some impressive results. With several 1D models, we derived TEM data from forward problems and then put it into conductivity-depth processing. Anomalies, after the processing, showed precise position of conductive ore-bodies with depth. By changing theoretical models, several parameters affecting k factor in investigation depth fomula has been shown. The results also provided the value range of k factor. This is the base of applying conductivity-depth processing for practical trasient electromagnetic data

How to Cite
Pham, K.Ngoc 2015. Proving the correctness of transient electromagnetic data processing method on theoretical models of horizontally layered earth (in Vietnamese). Journal of Mining and Earth Sciences. 52 (Oct, 2015).

Other articles