Citation: | ZHANG Tao, LI Yongfei, SUN Shouliang, GAO Xiaoyong, ZHOU Tiesuo, SUN Peng. Saturated hydrocarbon geochemical characteristics of the oil sand from YD1 well in Jinyang Basin and its significance for oil and gas exploration[J]. Geological Bulletin of China, 2017, 36(4): 582-590. |
Recently researchers from Shenyang Geological Survey of CGS made several new discoveries in geological well YD1 in Jinglingsi-Yangshan basin (Jinyang Basin). During the drilling of YD1 the authors detected several oil and gas showings in the fractures of the drilling core in Mid-Jurassic Tiaojishan Formation (J2t) which was mainly composed of intermediate igneous rocks. The characteristics of biomarkers from YD1 oil sand were analyzed by the method of gas chromatography and gas chromatography mass spectrometry (GC, GC-MS). The results show that the two oil sand samples have similar geochemical characteristics:the n-alkane distribution exhibits one sole peak pattern, and the dominant peaks are nC21 and nC22 separately; there is no clear odd or even carbon number predominance for the n-alkanes, and thus the carbon preference index (CPI) is only slightly higher than 1; the samples have low Pr/Ph ratios. The terpene is characterized by the normal distribution of C23 tricyclic terpene and similar abundance of C24 tetracy-clic terpene and C26 tricyclic terpene, with a relatively abundant value of gammacerane. The regular steranes are dominated by the C27-steranes, and their relative abundance is in the order of C27 > C29 > C28, exhibiting the "V" distribution pattern. These biomarkers' characteristics indicate that the source rocks are matured and predominated mainly by planktonic/algal organic matter. The source rocks were deposited in a lacustrine environment with a high-salinity stratified water column and anoxic conditions. The oil-source correlation results showed that the crude oil from the samples was possibly derived from the source rock in Early Jurassic Beipiao Formation (J1b). The results indicate that the source rock from Beipiao Formation is widely spread in Jinyang Basin and has good oil and gas potential, and hence Jinyang Basin is a petroliferous basin with good potential for oil and gas exploration.
[1] | 何保, 李茂丰, 刘颖鑫.金岭寺-羊山盆地北票组烃源岩特征[J].中国煤炭地质, 2008, 120(3):25-27. |
[2] | 樊新杰. 金岭寺-羊山盆地石油地质条件分析与评价[D]. 辽宁工程技术大学硕士学位论文, 2003. |
[3] | 李永飞, 郜晓勇, 孙守亮, 等.辽西金羊盆地北票组泥页岩有机地球化学特征——以SZK01钻孔岩心为例[J].地质论评, 2015, 61(S):673-674. |
[4] | 何保, 付秋萍, 张亚明.辽西金羊盆地北票组烃源岩分布及有机质丰度[J].辽宁工程技术大学学报, 2006, 25(1):24-27. |
[5] | 张坤, 李永飞, 唐友军, 等.辽西金羊盆地北票组油砂饱和烃地球化学特征——以SZK02井为例[J].地质通报, 2015, 34(10):1929-1937. doi: 10.3969/j.issn.1671-2552.2015.10.017 |
[6] | 张坤. 辽西金羊盆地北部北票组烃源岩地球化学特征及油砂成因研究[D]. 长江大学硕士学位论文, 2016. |
[7] | 李永飞, 陈树旺.辽西地区金岭寺-羊山盆地油气资源调查新发现[J].地质通报, 2014, 33(9):1463-1464. |
[8] | 甄甄, 李永飞, 郜晓勇, 等.金羊盆地SZK01井下侏罗统北票组沉积相及其有机质特征[J].世界地质, 2016, 35(1):207-215. |
[9] | 唐友军, 陈践发.内蒙古西部额济纳旗苦水沟地区下石炭统白山组烃源岩分子化石的特征[J].地质通报, 2011, 30(6):888-894. |
[10] | 蒋兴超, 陈树旺, 唐友军, 等.内蒙古突泉盆地ZK-WJT钻井下侏罗统红旗组生烃潜力[J].地质通报, 2013, 32(8):1236-1242. |
[11] | 卢双舫, 张敏.油气地球化学[M].北京:石油工业出版社, 2008. |
[12] | Peters K E, Walters C C, Moldowan J M. The biomarker guide, Volume 2, Biomarkers and isotopes in petroleum exploration and earth history[M]. Cambridge:Cambridge University Press, 2005:475-1155. |
[13] | 梅博文, 刘希江.我国原油中异戊间二烯烷烃的分布及其与地质环境的关系[J].石油与天然气地质, 1980, 1(2):99-115. doi: 10.11743/ogg19800203 |
[14] | Ten Haven H L, De Leeuw J W, Schenck P A. Organic geo-chemical studies of a Messinian evaporitic basin, northern Apen-nines (Italy) Ⅰ:Hydrocarbon biological markers for a hypersaline environment[J]. Geochimica et Cosmochimica Acta, 1985, 49(10):2181-2191. doi: 10.1016/0016-7037(85)90075-4 |
[15] | Damsté J S S, Kenig F, Koopmans M P, et al. Evidence for gam-macerane as an indicator of water column stratification[J]. Geochim-ica et Cosmochimica Acta, 1995, 59(9):1895-1900. doi: 10.1016/0016-7037(95)00073-9 |
[16] | Schwark L, Vliex M, Schaeffer P. Geochemical characterization of Malm Zeta laminated carbonates from the Franconian Alb, SWGermany (Ⅱ)[J]. Organic Geochemistry, 1998, 29(8):1921-1952. doi: 10.1016/S0146-6380(98)00192-2 |
[17] | 陈义才, 沈忠民, 罗小平.石油与天然气有机地球化学[M].北京:科学出版社, 2007:1-275. |
[18] | Riboulleau A, Schnyder J, Riquier L, et al. Environmental change during the Early Cretaceous in the Purbeck-type Durlston Bay sec-tion (Dorset, Southern England):a biomarker approach[J]. Organic Geochemistry, 2007, 38(11):1804-1823. doi: 10.1016/j.orggeochem.2007.07.006 |
Geological sketch map of Jinyang Basin and lithological column of YD1
Oil spot in the drilling core of YD1 at the footage of 1273.21m, 1273.71m and its fluorescent photo, with the core composed of andesite
The distribution of n-alkanes of oil sand from Tiaojishan Formation in YD1 well, Jinyang Basin
Terpanes series distribution of oil sand from Tiaojishan Formation in YD1 well, Jinyang Basin
The distribution of steranes of oil sand from Tiaojishan Formation in YD1 well, Jinyang Basin
Comparison for the characteristics of biomarker from oil sand of YD1 well and source rock of Beipiao Formation in Jinyang Basin
Correlation between Pr/Ph and G/C30H, sterane C27/C29 and C24TT/C26TE for the three groups of samples