Comparison Between Second Vertical Derivative and Tilt Angle Methods in Detecting Edges of Gravity Anomaly

References

[1] Aku, M. O. ( 2014). Application of second vertical derivative analytical method to bouguer data for the purpose of delineation of lithological boundaries. . science world journal vol 9 (No 3), , 27-32.

[2] DOĞRU Fikret, Oya PAMUKÇUb and İlkin ÖZSÖZc. (2017). Application 0f Tilt Angle Method to the Bouguer Gravity Data Of Western Anatolia. Bulletin of the Mineral Research and Exploration155, 213-222.

[3] Elkins, T. A. (1951). The Second Derivative Method of Gravity Interpretation. Geophysics, 16-29.

[4] Eshaghzadeh. (2017). Depth Estimation Using the Tilt Angle of Gravity Field due to the Semi-Infinite Vertical Cylindrical Source. . Journal of Geological research.

[5] Essa, k. S. (2012). A Fast InterpretationMethod for InverseModeling of Residual Gravity Anomalies Caused by Simple Geometry. Journal of Geological Research, Article ID 327037, 10 pages.

[6] Essa, k. S. (2012). A Fast InterpretationMethod for InverseModeling of Residual Gravity Anomalies Caused by Simple Geometry. Journal of Geological Research, Article ID 327037, 10 pages.

[7] Fikret Dogru, Oya Ankaya Pamukçu, İlkin Özsöz. (2017). Application of tilt angle method to the bouguer gravity data of Western Anatolia. Bulletin of The Mineral Research and Exploration, 1-16.

[8] Geodesy, I. A. (2016). Journal of Geodesy, the geodesist hand book.

[9] Hinson George; Aboagye Menyeh & David Dotse Wemegah. (2015). Qualitative interpretation of Aerogravity and Aeromagnetic survey Data over the sourth western part of the volta River basin of Ghana. International Journal off scientific and technology research.

[10] Ibe, S. O and Iduma, U. . (**2018). Structural Interpretation of Northern Sokoto Basin, UsingAirborne Magnetic Data. International Journal of Innovative Research in Science, Engineering and Technology, 7(7), 8041-8048. doi:10.15680/IJIRSET.2018.70707070

[11] Ismail M Ibraheem, Menna Haggag, Bullent Tezkan. (2019). Edge Detectors as Structural Imaging Tools Using Aeromagnetic Data: A case study of Sohag Area, Egypt. Geosciences vol 9(5), 211.

[12] Justia, Marsellei; Muhammad Fikri H Hiola, Nur Baiti Febryana S. ( 2018). Gravity anomaly to identify Walanae fault using second vertical derivative. Journal of Physics: Theories and Applications, vol2, , 36-42.

[13] Ofoha C. C., Emujakporue G and Ekine A. S. (2018). Structural Evaluation of Bouguer Gravity Data Covering Parts of Southern Niger Delta, Nigeria. Archives of Current Research International, 13(3), 1-18.

[14] Okonkwo Churchill Chukwunonso , Onwuemesi Ajana Godwin , Anakwuba Emmanuel Kenechukwu , Chinwuko Augustine Ifeanyi , Ikumbur Bemsen Emmanuel and Usman Ayatu Ojonugwa. (2012). Aeromagnetic Interpretation over Maiduguri and Environs of Southern Chad Basin, Nigeria. Journal of Earth Sciences and Geotechnical Engineering, vol.2, no. 3, 77-93 .

[15] Prihadi Sumintadireja, Darharta Dahrin, & Hendra Grandis. . (2018). A Note on the Use of the Second Vertical Derivative (SVD) of Gravity Data with Reference to Indonesian Cases. J. Eng. Technol. Sci., Vol. 50, No. 1, 127-139.

[16] Putra M I, Hidayah A N, Septiana L A E S and Supriyana E . (2019). Gravity analysis to estimate the mud stream direction in porong by applying the delaunay approach. IOP Conference Series: Earth and Environmental Science,, 311.

[17] Putri D.R, Nanda M, Rizal S, Idroes R and Ismail N. (2019). Interpretation of gravity satellite data to delineate structural features connected to geothermal resources at Bur Ni Geureudong geothermal field. IOP Conf. Series: Earth and Environmental Science 364 , 1-14.

[18] Richard W. Saltus, Richard J. Blakely. . (2011). Unique geologic insights from “non-unique” gravity and magnetic interpretation. . GSA TODAY vol 21 issue 12, 4-10.

[19] Wahyudi, E J; Kynantoro, Y; Alawiyah, S. (2016). Second Vertical Derivative Using 3-D Gravity Data for Fault Structure Interpretation. . International Conference on Energy Sciences (p. 877). IOP Publishing IOP Conf. Series: Journal of Physics: Conf. Series .

[20] Yanis Muhammad,, Marwan and Nazli Ismail. ( 2019). Efficient Use of Satellite Gravity Anomalies for mapping the Great Sumatran Fault in Aceh province. . Indonesian Journal of Applied Physics Vol.9 No.2, 61.

[21] Yunus & Yigitbas. (2015). interpretation of gravity anomalies to delineate some structural features of Biga and Gelibolu peninsulas and their surroundings (north-west Turkey). Geodinamica Acta 27 (4), 300-319.

@article{1703006,
      author = {Ahmad Alhassan, Auwal Aliyu, Yusuf Abdulhameed, Nasiru Bala, Abdullahi Hussaini},
      title = {Comparison Between Second Vertical Derivative and Tilt Angle Methods in Detecting Edges of Gravity Anomaly},
      journal = {Iconic Research And Engineering Journals},
      year = {2021},
      volume = {5},
      number = {6},
      pages = {83-87},
      issn = {2456-8880},
      url = {https://www.irejournals.com/formatedpaper/1703006.pdf},
      abstract = {Edge detection is very important in description of subsurface structures. Interest is usually placed on boundaries or edges especially during exploration minerals. Second vertical derivative and tilt angle methods are among the most commonly used methods in detection of lithological boundaries. The choice of which method to select in edge/boundary detection is very vital and that is why this paper addresses the two methods. Satellite gravity data of Hadejia segment of chad basin Nigeria acquired from Bureau Gravimetric International (BGI)was used as case study. The area is a contact region between Chad sedimentary formation and cretaceous northern basement complex. Second vertical derivative and tilt angle maps were plotted on surfer software to produce maps that shows boundaries between the two formations. Comparison was made between the two results pointing out some similarities and differences between the two results. This will guide an individual researcher while making choice of which among the two methods will suit his research based on his interest.},
      keywords = {Second vertical derivative, Tilt angle, Edge detection, Gravity anomaly.},
      month = {December},
  }