35 2 2016 6 GLOBAL GEOLOGY Vol. 35 No. 2 Jun. 2016 1004 5589 2016 02 0487 08 1 2 3 1 2 3 1 2 3 1 2 3 1 2 3 1. 130061 2. 130061 3. 130061 - TOC 4. 87% ~ 19. 90% 7. 88% Ⅰ Ⅱ T max 437 ~ 449-2 3 ZK0809 ZK3201 SY9 P534. 53 P618. 12 A doi 10. 3969 /j. issn. 1004-5589. 2016. 02. 020 Oil shale characteristics of Upper Cretaceous Qiangshankou Formation in Fuyu -Changchunling area of Songliao Basin and its significance SONG Qing-lei 1 2 3 LIU Zhao-jun 1 2 3 HU Fei 1 2 3 XIE Wen-quan 1 2 3 SONG Shuo 1 3 1. College of Earth Sciences Jilin University Changchun 130061 China 2. Key Laboratory Oil Shale and Coexisting Minerals of Jilin Province Changchun 130061 China 3. Key Laboratory for Mineralization Exploration and Exploitation of Oil Shale and Paragenetic Energy Minerals Changchun 130061 China Abstract Oil shale layers found in Fuyu -Changchunling area are popularly developed in the Upper Cretaceous Qingshankou Formation of Songliao Basin. Most of them present brown and dark grey color with the development of horizontal bedding and massive bedding which indicates their semi-deep to deep lake sedimentary environment. Systemic test and analysis results show that oil shale layers here have the charactertics of moderate calorific value high ash content and low sulfur content with medium oil yields. The TOC content is 4. 87% to 19. 90% with the average value of 7. 88% which reflects the high organic matter content in the oil shale. The rock-eval analysis 2 2015-12-04 2016-03-14 201211051-04. 1951 -. E-mail liuzj @ jlu. edu. cn
488 35 results show that the oil shale layers are mainly dominated by type I organic matter and type II organic matter dominated secondly. The T max value of 437 to 449 indicates the immature to low-mature stage of the organic matter in oil shale. The distribution of thickness and oil yield of oil shale layers indicate that the 2nd and 3rd oil shale layers of the target strata both have the maximum thickness and the best continuity. Besides the oil shale layers in boreholes ZK0809 and ZK3201 both have the relatively higher total thickness while in the borehole SY9 the oil shale layers have the highest oil yield. Key words Songliao Basin Fuyu -Changchunling area Qingshankou Formation oil shale quality of oil shale 0 > 3. 5% < 4. 18 MJ /kg 1 2 5 7 8 2014 500 ~ 9 000 m 9 10 9 4 1 7 ~ 18 m 2 1-6 2 3-5 - 6
2 489 Fig. 1 1 Regional geological map of Songliao Basin and location of studied area Fig. 2 2 SY9 Oil shale bearing layer column of Well SY9 of Late Cretaceous Qiangshankou Formation in Fuyu -Changchunling Songliao Basin
490 35 47. 06% 5. 8% 3a - 3 3. 1 3 a S g Q b Fig. 3 Distribution histogram of oil yield a and distribution histogram of total sulfur S g Q b 2006 ω > 3. 5% 3. 5% < ω 5% 5% < ω 3. 2 TOC 1 10% ω > 10% 11 < 3. 5% TOC 3. 59% ~ 16. 37% 5. 72% 0. 96 y = 47. 06% 0. 8013 x - 0. 2332 4 a Fig. 4 4 TOC a b c Cross-plots of oil yield and TOC a cross-plots of oil yield and calorie b and cross-plots of oil yield and ash c
2 491 3. 5% TOC 4. 67% Ⅰ Ⅱ 3. 5% ~ 5. 0% TOC 4. 67% ~ 6. 53% 5% ~ 10% - TOC 4. 67% ~ 12. 77% ROCK EVAL6 12. 77% 3. 3 437 ~ 449 2. 55 ~ 10. 174 kj /g 4. 013 kj /g 1 y = 1. 577 8x - 0. 326 8 0. 960 5 4b 3. 4 800 ± 10 1 67. 57% ~ 86. 41% 81. 60% y = - 0. 765 2x + 67. 875 0 0. 893 7 4c 3. 5 S g Q 5 S g Q 1. 0% 1. 0% < S g Q 1. 5% 1. 5% < S g Q 2. 5% 2. 5% < S g Q 4. 0% S g Q > 4. 0% 1 5 T max a S 2 20. 5% 35. 29% TOC b 44. 12% 3b Fig. 5 Organic matter type diagram of hydrogen index 0. 53% ~ 2. 03% vs. T max a and And organic matter type crossplot of S 2 vs. TOC 1. 39% b 3. 6 T max 5a I H S 2 TOC 5b T max - 12 13 Ⅰ Ⅱ
492 35 - ZK2409 ZK0801 SY09 4 5 ZK1601 4 4. 1 1 ZK2409 ZK1601 ZK0801 1 6 ZK2409 ZK0801 7 8 9 9 5 ZK2409 2345 6 2 23 3 Fig. 6 6 ZK2409 -SY09 -ZK1601 -ZK0801 Cross-sectional comparison drawing of oil shale layers among ZK2409 -SY09 -ZK1601 -ZK0801 in Fuyu -Changchunling of southeastern uplifted area Songliao Basin 4. 2 SY09 7 m 5 2345 7 8 SY09 1 7. 2% SY09 - ZK0809 ZK3201 2
2 493 Fig. 7 7 Distribution of oil yield contour map of oil shale in Qingshankou Formation of studied area Fig. 8 8 2345 Distribution of total thickness contour map of oil shale layers 2345 in Qingshankou Formation of studied area
494 35 TOC 29 3 282-292. 7. 3 Ⅰ J. 2011 18 4 171-180. Ⅱ - 4 2 3 Distinguishing features and their genetic interpretation of- ZK0809 ZK3201 stratigraphic sequences in continental deep water setting a case from Qingshankou Formation in Songliao Basin SY9 J. Earth Science Frontiers 2011 18 4 171-180. 1. M. 2009 1-290. LIU Zhao-jun YANG Hu-lin DONG Qing-shui et al. Qil shale in China M. Beijing Petroleum Industry Press 2009 1-290. 2. ple J. Acta Sedimentologica Sinica 2014 32 3 J. 594-595. 2012 31 4 779-783. LI Bao-yi WANG Jian-peng XU Yin-bo et al. Testing parameters of organic-rich mudstone in faulted basin and depressed basin and their significance J. Global Geology 2012 31 4 779-783. 3 Petroleum Institute 2010. D. 2013. SUN Ping-chang. Environmental dynamics of organic accumulation in the oil shale bearing layers in the Upper Cretaceous southeast Songliao Basin doctor s degree thesis D. Changchun Jilin University 2013. 4 - Daqing Daqing Petroleum Institute 2010. D. 2012. JIA Jian-liang. Research on the recognition and resource evaluation of the Upper Cretaceous oil shale based on geochemistry-geophysics technique in the Songliao Basin doctor s degree thesis D. Changchun Jilin University 2012. 5. NGN1 J. 2015 34 3 736-737. WANG Yi-meng LIU Zhao-jun SUN Ping-chang. Organic matter evolution in the Qingshankou Formation first member of Well NGN1 in the Upper Cretaceous Songliao Basin J. Global Geology 2015 34 3 736-737. 6. Characteristics of the oil shale of the Low Cretaceous J. 2004 29 Dalazi Formation in the Songjiang Basin Jilin Province 3 283-292. XIAO Long WANG Fang-zheng WANG Hua et al. Mantle plume tectonics constraints on the formation of Songliao and Bohaiwan basin J. Earth Science 2004 LIU Zhao-jun SUN Ping-chang JIA Jian-liang et al. 8. J. 2014 32 3 594-595. LIU Zhao-jun SUN Ping-chang LIU Rong et al. Research on geological conditions of shale coexistent energy mineralization accumulation take the Qingshankou Formation in Upper Cretaceous Songliao Basin for exam- 9 D. 2010. GUO Wei. Research on sequence characteristics of Qingshankou Group in southeastern uplifted area Songliao Basin master s degree thesis D. Daqing Daqing 10 D. 2009. JIA Bao-zeng. Research on reservoir-forming rule in wangfu depression middle-shallow layer of Songliao Basin southeast uplift area master s degree thesis D. 11 Sun P C Liu Z J Reinhard G et al. Oil yield and bulk geochemical parameters in the Songliao and Huadian Basins China a grade classification approach J. Oil Shale 2013 30 3 402-418. 12. M. 1986 1-198. WU Li-yan GU Xin-zhang SHENG Zhi-wei et al. Fast quantitative evaluation method for source rock on Rock-Eval analysis M. Beijing Science Press 1986 1-198. 13. J. 2006 36 6 996-1000. ZHANG Lei LIU Zhao-jun DU Jiang-feng et al. J. Journal of Jilin University Earth Science Edition 2006 36 6 996-1000.