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机构地区:[1]中国石化石油勘探开发研究院,北京100083
出 处:《石油与天然气地质》2004年第4期400-407,421,共9页Oil & Gas Geology
基 金:中国石化科技项目"中国石化环渤海湾地区前第三系油气资源前景"(P03076)
摘 要:东濮凹陷文留地区石炭-二叠纪煤系分布稳定、含有机质丰富,是文留气藏可靠的气源岩. 煤系在埋藏过程中有两次生烃过程:第一次发生在中、下三叠统沉积后,镜质体反射率(Ro)、磷灰石裂变径迹、古流体包裹体分析证实当时煤系的古埋深约为3500m,古地 温118℃,古演化程度为Ro=0.80%~0.85%. 其后经历了中生代约180Ma以抬升剥蚀为主的历程,煤系生烃中止.早第三纪裂谷发育 期间,煤系因埋深加大而进入二次生烃期,并在东营组沉积后达到生烃峰值阶段.主体烃源 岩主要分布在文东-前梨园洼陷,埋深5290~6360m.文留地区天然气资源探明程度已 达到90%以上,有效供气边界条件清楚.经计算,文留气藏有效供气区石 炭-二叠纪煤系生烃量为3253.3×108m3,排烃量2657.0×108m3,天然气聚集系数为5.92%.The Carboniferous-Permian coal measure strata in Dongpu sag is a fair source rock unit of Wenliu gas pool due to its stable distribution and high organic content. There are two hydrocarbon-generating periods in the burial history of coal measures. The first one occurs when the T1-2 formation is deposited. Vitrinite reflectance, apatite fission track and fluid inclusion analyses indicate that the burial depth of coal measures is about 3500 m, with the palaeotem-perature of 118℃ and Ro of 0.80%-0.85% .Hydrocarbon generation of coal measures was interrupted in the Meso-zoic uplift and erosion period (about 1.8 million years) .During the Paleogene rifting period,the coal measures was entered into its secondary hydrocarbon-generating period as the burial depth increases, reaching its hydrocarbon-generating peak after the deposition of Dongying formation. The gas-prone source rock is mainly distributed in the region of Wendong-Qianliyuan, with the buried depth of 5290-6360m. The discovery maturity (percentage of ultimately proven reserve with respect to total resources) of gas resources in Wenliu area is more than 90% . In the effective gas supply area of Wenliu gas pool, the hydrocarbon-generating volume and hydrocarbon-expelling volume of Carboniferous-Permian coal measures are estimated to be 3253.3 million m3 and 2657.0 million m3 respectively, with a gas accumulation coefficient of 5.92%.
关 键 词:文留气藏 石炭-二叠纪煤系 生烃潜力 一次生烃 二次生烃 聚集系数
分 类 号:TE112.1[石油与天然气工程—油气勘探]
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