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HYDROCARBON GENERATIVE POTENTIAL OF CRETACEOUS SEDIMENTS OF KANADI-1 WELL, BORNU BASIN, NIGERIA

The hydrocarbon potential and paleodepositional environment of Cretaceous sediments from the Borno Basin, Nigeria, were assessed by Rock-eval pyrolysis and biomarker geochemistry. The Total Organic Carbon (TOC), soluble organic matter (SOM) and genetic potential (GP) values ranged from 0.52 – 0.82wt...

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Published: 2016
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LEADER 00000njm a2000000a 4500
001 oai:repository.ui.edu.ng:123456789/1364
042 |a dc 
720 |a Nton, M. E.  |e author 
720 |a Ekom, J. C.  |e author 
260 |c 2016 
520 |a The hydrocarbon potential and paleodepositional environment of Cretaceous sediments from the Borno Basin, Nigeria, were assessed by Rock-eval pyrolysis and biomarker geochemistry. The Total Organic Carbon (TOC), soluble organic matter (SOM) and genetic potential (GP) values ranged from 0.52 – 0.82wt%, 455.64 – 1003.04 ppm and 0.23 – 0.63 mg/g, respectively. These values suggested that the sediments were moderately rich in organic matter. The Hydrogen Index (HI) values (19 – 85 mgHC/gTOC) and cross plots of Hydrogen Index (HI) versus Oxygen Index (OI), classified the sediments as types 111 and IV organic matter which had potential oto generate mainly gas. The T and Production Index (PI) values ranged from 339 – 436C and 0.08 – 0.32 max while the Production Index (PI) ranged from 0.08 – 0.32, respectively, suggesting low maturity. Biomarker data revealed the presence of C to C steranes and oleanane which indicated organic matter from mixed sources with 27 29 more terrigenous contribution. The dominance of C over C and C also supported higher terrigenous input. 29 28 27, Various thermal maturity parameters computed from the terpanes and steranes distributions in the sediments indicated low thermal maturity. The C /C – C Homohopane index and Pr/Ph values ranged from 0.06-0.24 35 31 35 and 0.23 – 2.52 respectively. These values suggested organic matter deposited under anoxic to suboxic conditions. The results of this study showed that the sediments had potential to generate mainly gas at appropriate thermal maturity 
024 8 |a Department of Geology, 
024 8 |a ui_art_nton_hydrocarbon_2016 
024 8 |a http://ir.library.ui.edu.ng/handle/123456789/1364 
245 0 0 |a HYDROCARBON GENERATIVE POTENTIAL OF CRETACEOUS SEDIMENTS OF KANADI-1 WELL, BORNU BASIN, NIGERIA