Organic carbon and trace metal distribution in the Gokcesu Shale: Eocene basin, Bolu-Turkey

被引:3
|
作者
Aliyev, S. [1 ]
Koralay, B. [1 ]
Sonel, N. [1 ]
Koc, S. [1 ]
Imer, S. [1 ]
机构
[1] Ankara Univ, Fac Engn, Dept Geol Engn, TR-06100 Ankara, Turkey
关键词
bituminous shale; Eocene basin; living organisms; organic carbon; trace metal;
D O I
10.1080/009083190957667
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Samples collected from the bituminous shales in the Eocene Tokmaklar formation are the material of this study. Distribution of organic material and trace metals in the shale samples and their concentration levels and correlations were evaluated. Organic carbon content of the bituminous shales is between 0.59 and 15.89% (averaging as 4.86%). The type of organic material is 100% amorphous material (kerogen type is Type I and Type II) and it has a potential to produce oil. Trace metal enrichment levels were determined on the basis of average shale concentration in the earth crust. These levels are divided into two groups. Mo (1.98-2.64), Cu (1.27), As (1.59-8.83), and Sr (2.58-2.75) in bituminous rocks show enrichment character while Pb, Zn, Ba, and Co metals do not display any enrichment. Moreover, comparison with the average values of these metals in seawater and living organisms yield enrichment coefficients of 86.17-386.000 (with respect to seawater) and 4.59-1,723.5 (with respect to living organisms).
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页码:591 / 605
页数:15
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