2017
DOI: 10.18393/ejss.297245
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Depositional environments signatures, maturity and source weathering of Niger Delta sediments from an oil well in southeastern Delta State, Nigeria

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Cited by 11 publications
(10 citation statements)
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“…CIA is also much affected by grain size. It increases as grain size decreases (Oni and Olatunji, 2017).…”
Section: Chemical Weatheringmentioning
confidence: 96%
“…CIA is also much affected by grain size. It increases as grain size decreases (Oni and Olatunji, 2017).…”
Section: Chemical Weatheringmentioning
confidence: 96%
“…An increase in cia values is generally attributed to climatic fluctuations from cold to warm and humid [40]- [41]. For the Marriaga Swamp, the cia is in a medium range for the lower sedimentary sequence (220-162 cm) and high over 162 cm to near-surface (Fig.…”
Section: Chemical Index Of Alteration (Cia)mentioning
confidence: 98%
“…The cia increases within the medium range from bottom to upper sequences, indicating climatic changes from 1,130 ± 90 a to present, from more arid and maybe colder conditions in late Holocene to humid and warmer conditions nowadays. The cia ranges hint at low weathering from 0 to 40, moderate from 40 to 70, and high from 70 to 100 [40]. The Marriaga Swamp cia values range from 65 to 82, with an average of 72, which means the Marriaga Swamp sediments are highly weathered.…”
Section: Chemical Index Of Alteration (Cia)mentioning
confidence: 99%
“…Geochemical fingerprints can predict where petroleum, water and other valuable minerals can be found [2]. The use of inorganic geochemical fingerprints for the classification of siliciclastic sediments, provenance, tectonic setting and depositional environment have been carried out by different workers [2][3][4][5][6][7][8][9]. The geochemical study using X-ray fluorescence analysis for the reservoir rocks of Surma Basin in Bangladesh showed that the reservoir rocks are mainly greywacke to lithic arenite and are from quartzose sedimentary provenance which was deposited under active continental margin setting [2].…”
Section: Introductionmentioning
confidence: 99%
“…Trace and rare earth element ratios were used to determine the geochemical signatures of some sediment from the Niger Delta Basin and the conclusion was that felsic source rock is the provenance for the sediment from the Agbada Formation [8]. The silicate weathering index of some sediment from southeastern Delta suggested a low to moderate weathering of the source area during transportation [9].…”
Section: Introductionmentioning
confidence: 99%