[an error occurred while processing this directive] Global Geology 2014, 17(4) 199-205 DOI:     ISSN: 1673-9736 CN: 22-1371/P

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Cryton Phiri
WANG Pujun
G. Roland Nguimbi
and Abdallah- Yousif Ibrahim Hassan
PubMed
Article by Cryton P
Article by Wang P
Article by G. RN
Article by And AYIH
 
 
 
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Interpreting effects of TOC inert organic content on source rock potential using S 2 vs.TOC graph in Maamba Coalfield,southern Zambia
Cryton Phiri , WANG Pujun, G. Roland Nguimbi, and Abdallah- Yousif Ibrahim Hassan
1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. Geology Department,University of Zambia,Lusaka 10101,Zambia; 3. College of Construction Engineering,Jilin University,Changchun 130026,China
Abstract:

The authors present the effects of the total organic carbon (TOC inert ) during pyrolysis and how it overall affects the estimates of the hydrocarbon index (HI) using the cross plot S 2 vs. TOC graph. A total of 21 drillcore samples consisting of the non- carbonaceous mudstones,carbonaceous mudstones,coaly mudstones and coals with S 2 > 0. 35 are selected and used. The average TOC for the sampled population is 10. 36 wt%. TOC inert measured from the S 2 vs. TOC graph is 2. 97 wt% and the average pyrolysable TOC live is 7. 39 wt%. The HI is 102 mg HC/g TOC and the pyrolysable HI is 175 mg HC/g TOC,indicating that the TOC inert or mi- neral matrix adsorbs some of the hydrocarbons liberated during pyrolysis resulting into the low HI values which affects the correct determination of the source rock potential. Other applications of the S 2 vs. TOC cross plot have been used to determine the depositional system tracts. The high stand system tract is also determined through this method.

Keywords: Rock- Eval pyrolysis   S 2 vs. TOC   Maamba Coalfield Basin   Zambia  
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