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Turnbull, R. E., Allibone, A. H., Matheys, F., Fanning, C. M., Kasereka, E., Kabete, J., McMaughton, N. J., Mwandale, E., & Holliday, J. (2021). Geology and Geochronology of the Archean Plutonic Rocks in the Northeast Democratic Republic of Congo. Precambrian Research, 358, Article ID: 106133.
https://doi.org/10.1016/j.precamres.2021.106133

has been cited by the following article:

• TITLE: Structural Study of the Kakobola Area and Its Surroundings by Detecting the Edges of Gravity Anomaly Sources

  AUTHORS: Albert Mbata Muliwavyo, Jonathan Musitu Muliwavyo, Jean-Marie Tshitenge Mbuebue, Lumière Musitu, Clément N’Zau Umba-Di-Mbudi

  KEYWORDS: First Total Horizontal Derivative, Tilt Angle, Analytical Signal, Dips, Depths

  JOURNAL NAME: Journal of Geoscience and Environment Protection, Vol.11 No.7, July 18, 2023

  ABSTRACT: The area covered by this study is the county of Kakobola and its surroundings. Previous studies show that those related to the study of depths by the gravity method, using other techniques, are not always carried out until now. The main goal of this article is the gravimetric characterization of our area by other approach. The interest is not only to map the lineaments and to know their dip, but also to estimate the depths of these different anomalies. The methods used for this study are the first total horizontal derivative (FTHDT), tilt angle (TA), analytical signal (AS) and horizontal gradient magnitude (HGM). The processing of the complete Bouguer anomalies (CBA) data was done mainly through software. Data analysis using the semi-finished body depth method shows depths ranging from 7.49 m to 224.6 m. Data analysis using the AS method shows values ranging from 41.7 mGal/m to 510 mGal/m. The fractures and/or geological contacts in our study area show dips ranging from -73.73°to 68.16° and North-South orientation according to the tilt angle method. The FTHDT shows several lineaments, a NE oriented fracture of Kakobola and low dip values which suggest a tabular structure of the subsurface in our study area. According to the HGM, the study area shows several preferential directions of fractures and/or geological contacts whose the most frequent directions are the NNE-SSW and WNW.