Source Rock Evaluation Pdf The result shows good correlation using decker (toc) model and mallick raju (ro vitrinite reflectance) model. two source rocks potential zones were detected by these log models. In this paper, the authors established four toc (total organic carbon content) logging calculation models; passey, schmoker hester, meyer nederloff, and decker density model by considering the geology of ngimbang.
Pdf Source Rock Formation Evaluation Using Toc Ro Log Model Based In this paper, the authors established four toc (total organic carbon content) logging calculation models; passey, schmoker hester, meyer nederloff, and decker density model by considering the geology of ngimbang. In this study, four wells was used to observe the characteristics of distribution of toc in the ngimbang formation. these wells are sh 1, sh 2, sh 3, and afa 1. however well afa 1 is the only well where no toc core data is available. In this paper, the authors established four toc (total organic carbon content) logging calculation models; passey (1990), schmoker hester (1983), meyer nederloff (1984), and decker density cross plot model (1993) by considering the geology of ngimbang in north eastern java basin. Three wells data along with its available core data was used to determine the most suitable model to be applied in the ngimbang formation, as well as to compare the accuracy of these toc model values.
Pdf Source Rock Formation Evaluation Using Toc Ro Log Model Based In this paper, the authors established four toc (total organic carbon content) logging calculation models; passey (1990), schmoker hester (1983), meyer nederloff (1984), and decker density cross plot model (1993) by considering the geology of ngimbang in north eastern java basin. Three wells data along with its available core data was used to determine the most suitable model to be applied in the ngimbang formation, as well as to compare the accuracy of these toc model values. Bon (toc) value. in this study there were 5 wells, namely wells a1, a2, a3, a4 and a5 with toc calculation results. well a1 contained 35 layers of source rock, obtaining toc values between 0.56% 1.38%, well a2 contained 6 layers of source rock, obtaining toc values between 0.67. % 0.81%, well a3 has 21 layers of source rock with toc values. Optimum well log based approaches to better predict the toc content in an organic matter are presented. sembar formation of cretaceous encountered in khajari 01 and miran 01 wells, which are located in the southern indus basin (sib), pakistan. In this paper, the authors established four toc (total organic carbon content) logging calculation models; passey (1990), schmoker hester (1983), meyer nederloff (1984), and decker density cross plot model (1993) by considering the geology of ngimbang in north eastern java basin.
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