2018
DOI: 10.1016/j.jafrearsci.2017.12.018
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Sequence stratigraphic interpretation of parts of Anambra Basin, Nigeria using geophysical well logs and biostratigraphic data

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Cited by 11 publications
(7 citation statements)
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“…Sistem traktus diklasifikasikan menjadi tiga, yaitu Lowstand System Tract (LST), Transgressive System Tract (TST) dan Highstand System Tract (HST) (Catuneanu, 2002). Model analisis urutan stratigrafi sederhana didasarkan pada karakteristik log GR dalam menentukan permukaan stratigrafi (Anakwuba et al, 2018). Pola log GR memiliki konsep dasar yang mencirikan perubahan energi pengendapan sedimen yang memengaruhi ukuran butir dan rangkaian parasekuen.…”
Section: Penentuan Tanda Permukaan Stratigrafiunclassified
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“…Sistem traktus diklasifikasikan menjadi tiga, yaitu Lowstand System Tract (LST), Transgressive System Tract (TST) dan Highstand System Tract (HST) (Catuneanu, 2002). Model analisis urutan stratigrafi sederhana didasarkan pada karakteristik log GR dalam menentukan permukaan stratigrafi (Anakwuba et al, 2018). Pola log GR memiliki konsep dasar yang mencirikan perubahan energi pengendapan sedimen yang memengaruhi ukuran butir dan rangkaian parasekuen.…”
Section: Penentuan Tanda Permukaan Stratigrafiunclassified
“…Gambar 4. Identifikasi penanda permukaan stratigrafi berdasarkan pola log GR (Anakwuba et al, 2018).…”
Section: Penentuan Tanda Permukaan Stratigrafiunclassified
“…The Anambra Basin covers an area of about 40,000 km 2 with a sedimentary sequence of 9 km in thickness (Akaegbobi, 2005). Previous studies classified the Anambra Basin by eight geologic formations that include the Benin (Ogwashi-Asaba) formation, Nkporo/Enugu shale, Mamu formation, Ajali sandstone, Nsukka formation, Imo formation, Ameki formation/Nanka sand and Alluvium (e.g., Reyment, 1965;Obi et al, 2001;Igwe et al, 2013;Nwajide, 2013;Anakwuba et al, 2018). The Ameki formation consists of fossiliferous greyish-green sandy clay with calcareous concretions and white clayey sandstones.…”
Section: Geological and Statistical Analysismentioning
confidence: 99%
“…Symmetrical shape is formed as gradual cleaning upward trend which changes from its maximum value with dirtying uptrend of similar grain size without sharp breaks. Serrated/ irregular shape is characterized as fluctuated GR reading with high and low values over very short vertical interval of well profile, which indicates laminated beds of sand and shale [10].…”
Section: Identification Of Stratigraphic Surface Markersmentioning
confidence: 99%