Skip to main content
Log in

Edge position detection and depth estimation from gravity data with application to mineral exploration

  • Original Article
  • Published:
Carbonates and Evaporites Aims and scope Submit manuscript

A Correction to this article was published on 19 March 2019

This article has been updated

Abstract

A method is applied to residual gravity data taken from the Ortaklar mine, Turkey to delineate the edge position and to estimate the depth of a buried ore body. The horizontal gradient magnitude (HGM) and tilt angle map (TAM) techniques are applied to the first vertical derivative (FVD) of the residual gravity data. The maxima contours of the HGM data and the zero contours of the TAM correspond to the edges of the ore body. The half distance between ± 45° (± 0.785 rad) TAM contours is used to determine the depths of the body. The obtained results are then compared against the depths retrieved from the Grav2dc inversion program, which inverted two profiles taken across the maximum response of the gravity anomaly map. The depths of the ore body estimated by the two methods are found in good agreement as reveal from drilling information.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2

(Modified after URL-1, 2018)

Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

Change history

  • 19 March 2019

    The original version of this article unfortunately contained a mistake in the Methodology section.

References

  • Arısoy MÖ, Dikmen Ü (2011) Potensoft: MATLAB-based software for potential field data processing, modelling and mapping. Comput Geosci 37:935–942

    Article  Google Scholar 

  • Biswas A (2017) A review on modeling, inversion and interpretation of self-potential in mineral exploration and tracing paleo-shear zones. Ore Geol Rev 91:21–56

    Article  Google Scholar 

  • Biswas A, Parija MP, Kumar S (2017) Global nonlinear optimization for the interpretation of source parameters from total gradient of gravity and magnetic anomalies caused by thin dyke. Ann Geophys 60(2):G0218, 1–17

    Article  Google Scholar 

  • Cordell L, Grauch VJS (1985) Mapping basement magnetization zones from aeromagnetic data in the San Juan basin, New Mexico. In: Hinzc WJ (ed) The utility of regional gravity and magnetic anomaly maps. Society Exploration Geophysics, Houston, pp 181–197

    Chapter  Google Scholar 

  • Essa KS, Elhussein M (2016) A new approach for the interpretation of magnetic data by a 2-D dipping dike. J Appl Geophys. https://doi.org/10.1016/j.jappgeo.2016.11.022

    Google Scholar 

  • Evjen HM (1936) The place of the vertical gradient in gravitational interpretations. Geophysics 1:127–136

    Article  Google Scholar 

  • Gunn PJ (1975) Linear transformations of gravity and magnetic fields. Geophys Prospect 23:300–312

    Article  Google Scholar 

  • Güvenç T (1973) Gaziantep-Kilis bölgesi stratigrafisi: MTA Jeo. Et. Dai. rapor arşivi, Rap. no. 304, 70 s. Ankara

  • Hansen RO, Pawlowski RS, Wang X (1987) Joint use of analytic signal and amplitude of horizontal gradient maxima for three-dimensional gravity data interpretation. In: 57th annual international management. Soc. Expl. Geophys., Expanded Abstracts, pp 100–102

  • Hinze WJ (1990) The role of gravity and magnetic methods in engineering and environmental studies. In: Ward SH (ed) Geotechnical and environmental geophysics, vol I: review and tutorial. Society of Exploration Geophysicists, Tulsa

    Google Scholar 

  • Klingele EE, Marson I, Kahle HG (1991) Automatic interpretation of gravity gradiometric data in two dimensions: downright gradient. Geophys Prospect 39:407–434

    Article  Google Scholar 

  • Mehanee S (2014) Accurate and efficient regularized inversion approach for the interpretation of isolated gravity anomalies. Pure Appl Geophys 171(8):1897–1937

    Article  Google Scholar 

  • Mehanee S (2015) Tracing of paleo-shear zones using self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes. Earth Planets Space 67:14–47

    Article  Google Scholar 

  • Mehanee S, Essa K (2015) A 2.5D regularized inversion scheme for the interpretation of residual gravity data by a dipping thin-sheet like target: numerical examples and case studies with an insight on sensitivity and non-uniqueness. Earth Planets Space 67:130. https://doi.org/10.1186/s40623-015-0283-2

    Article  Google Scholar 

  • Miller HG, Singh V (1994) Potential field tilt-a new concept for location of potential field sources. J Appl Geophys 32:213–217

    Article  Google Scholar 

  • Oruç B (2010) Edging detection and depth estimation using a tilt angle map from gravity gradient data of the Kozaklı-Central Anatolia Region, Turkey. Pure Appl Geophys 45:85. https://doi.org/10.1007/s00024-010-0211-0

    Google Scholar 

  • Oruç B, Keskinsezer A (2008) Structural setting of the northeastern Biga Peninsula (Turkey) from tilt derivatives of gravity gradient tensors and magnitude of horizontal gravity components. Pure Appl Geophys 165:1913–1927

    Article  Google Scholar 

  • Pei J, Li H, Wang H, Si J, Sun Z, Zhou Z (2014) Magnetic properties of the Wenchuan Earthquake Fault Scientific Drilling Project Hole-1 (WFSD-1), Sichuan Province, China. Earth, Planets Space 66:23

    Article  Google Scholar 

  • Saibi H, Nishijima J, Ehara S, Aboud E (2006) Integrated gradient interpretation techniques for 2D and 3D gravity data interpretation. Earth Planets Space 58:815–821

    Article  Google Scholar 

  • Salem A, Williams S, Fairhead JD, Ravat DJ, Smith R (2007) Tilt-depth method: a simple depth estimation method using first-order magnetic derivatives. Lead Edge 26:1502–1505

    Article  Google Scholar 

  • Tontini FC, Blakely RJ, Stagpoole V, Seebeck H (2018) Semi-automatic determination of dips and depths of geologic contacts from magnetic data with application to the Turi Fault System, Taranaki Basin, New Zealand. J Appl Geophys 150:67–73. https://doi.org/10.1016/j.jappgeo.2018.01.001

    Article  Google Scholar 

  • Ulu Ü, Genç Ş, Giray S, Metin Y, Çörekçloglu E, Örçen S, Ercan T, Yaşar T ve Karabıyıkoğlu M (1991) Belveren-Araban-Yavuzeli-Nizip-Birecik dolayının jeolojisi, Senozoyik yaşlı ve volkanik kayaçların petrolojisi ve bölgesel yayılımı: MTA Rap. no. 9226, Ankara

  • URL-1 (2018) http://www.ephesus.us/images/map_ephesus2.jpg. Accessed 8 Aug 2018

  • URL-2 (2018) http://www.geoafrica.co.za/reddog/gc/grav2dc/grav2dc.htm. Accessed 8 Aug 2018

  • Verduzco B, Fairhead JD, Green CM, Mackenzie C (2004) New insights into magnetic derivatives for structural mapping. Lead Edge 23:116–119

    Article  Google Scholar 

  • Yoldemir 0 (1987) Suvarlı-Haydarlı-Narlı Gaziantep arasında kalan alanın jeolojisi, yapısal durumu ve petrol olarakları: TPAO Rap. no. 2257, 60 s. Ankara

  • Zhdanov MS (2002) Geophysical inversion theory and regularization problems. Elsevier, Amsterdam

    Google Scholar 

Download references

Acknowledgements

Thanks to Prof. Dr. Bülent ORUÇ from Kocaeli University due to his contributions and valuable suggestions. I also would like to address my thanks to Rasim Taylan KARA for precious support.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Ali Elmas.

Additional information

Publisher's Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Elmas, A. Edge position detection and depth estimation from gravity data with application to mineral exploration. Carbonates Evaporites 34, 189–196 (2019). https://doi.org/10.1007/s13146-018-0480-8

Download citation

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s13146-018-0480-8

Keywords

Navigation