THE LOWER CRETACEOUS SOURCE ROCKS FROM EASTERN BASIN GROUP IN THE PERIPHERY OF SONGLIAO BASIN: Sedimentary Characteristics and Hydrocarbon Generation Potential
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摘要:
松辽外围东部盆地群位于中国东北地区的东部，研究区内共有39个中小规模沉积盆地，总面积约52×104 km2.在总结东部盆地群烃源岩沉积特征的基础上，通过对三江、勃利、通化及红庙子等盆地下白垩统烃源岩有机地球化学综合分析，查明了研究区下白垩统主力烃源岩有机质丰度、有机质成熟度以及有机质类型等指标特征、分布规律，并分析了影响这些指标在区域上规律变化的地质因素，以提升研究区的油气基础地质认识，为东北地区油气资源调查与勘探部署提供科学依据.
Abstract:The eastern basin group in the periphery of Songliao Basin, located in the east of Northeast China, includes 39 small- and medium-scale sedimentary basins, covering an area about 52×104 km2. Based on the sedimentary characteristics of source rocks in the eastern basin group, through comprehensive analysis of organic geochemistry of the Lower Cretaceous source rocks in Sanjiang, Boli, Tonghua and Hongmiaozi basins, the paper identifies the characteristics and distribution rule of organic matter abundance, maturity and types in the Lower Cretaceous source rocks of the study area, and analyzes the geological factors that affect regular changes of the above indexes regionally, to improve the basic geological understanding of oil-gas resources in the area and provide scientific basis for the oil-gas survey and exploration in Northeast China.
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表 1 松辽外围东部盆地群南、北地层区主要特征
Table 1. Characteristics of south and north stratigraphic subareas in the eastern periphery of Songliao Basin
地层分区名称 构造位置 地层发育状况 一般厚度/m 主要沉积盆地 黑龙江东部地层分区 新华夏系第二隆起带 海相、海陆交互相地层及早白垩世早中期及古近纪和新近纪地层较发育 E+N：800~1500
K：1500~3000
J：1000
T：1500~3000三江盆地、勃利盆地、虎林盆地、鸡西盆地、鹤岗盆地、宁安盆地、佳木斯盆地 吉林东部地层分区 新华夏系第二隆起带 白垩系、古近系和新近系较发育 E+N：1400~4800
K：500~2200
J：500
T: 1000~2000依兰-伊通地堑、延吉盆地、敦化盆地、蛟河盆地、柳河盆地、通化盆地、红庙子盆地、果松盆地、马鞍山盆地 
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表 2 松辽外围东部盆地群下白垩统烃源岩有机质丰度统计表
Table 2. Organic matter abundance of Lower Cretaceous source rocks in the eastern periphery of Songliao Basin
盆地 地层 烃源岩 TOC/% (S1+S2)/10-3 氯仿沥青“A”/% 总烃HC/10-6 综合评价 三江盆地 穆棱组 煤系泥岩 $\frac{0.25 \sim 3.80}{1.22(106)}$ $\frac{ 0.09 \sim 2.27 }{ 0.89(70) }$ $\frac{ 0.003 \sim 0.044 }{ 0.018(32) }$ $\frac{ 36 \sim 268 }{ 121(15) }$ 差-中 暗色泥岩 $\frac{6.73 \sim 13.58}{ 9.07(3) }$ $\frac{11.36 \sim 93.81}{ 36.08(4) }$ $\frac{0.108 \sim 0.317}{ 0.213(2) }$ $\frac{509 \sim 2163}{ 1336(2) }$ 城子河组 煤系泥岩 $\frac{0.14 \sim 4.30}{ 1.47(77) }$ $\frac{0.02 \sim 5.80}{ 1.04(60) }$ $\frac{0.003 \sim 0.105}{ 0.033(33) }$ $\frac{47 \sim 488}{ 207(18) }$ 暗色泥岩 9.55 11.88 鸡西盆地 穆棱组 煤系泥岩 $\frac{0.12 \sim 5.02}{ 1.36(112) }$ $\frac{0.06 \sim 17.04}{ 1.04(96) }$ $\frac{0.003 \sim 0.116}{ 0.022(56) }$ $\frac{79 \sim 606}{ 543(2) }$ 差-中 碳质泥岩 $\frac{8.15 \sim 36.80}{ 21.06(6) }$ $\frac{1.62 \sim 96.19}{ 43.25(6) }$ $\frac{0.015 \sim 0.340}{ 0.105(4) }$ $\frac{164 \sim 1274}{ 719(2) }$ 城子河组 煤系泥岩 $\frac{0.30 \sim 5.96}{ 1.84(75) }$ $\frac{0.07 \sim 13.54}{ 1.73(64) }$ $\frac{0.003 \sim 0.156}{ 0.034(62) }$ $\frac{133 \sim 917}{ 385(11) }$ 碳质泥岩 $\frac{6.50 \sim 39.57}{ 22.76(21) }$ $\frac{0.54 \sim 105.78}{ 35.09(21) }$ $\frac{0.013 \sim 0.709}{ 0.218(12) }$ $\frac{327 \sim 3001}{ 939(10) }$ 双阳盆地 长安组 煤系泥岩 $\frac{1.54 \sim 4.10}{ 2.68(6) }$ $\frac{0.19 \sim 9.34}{ 3.33(6) }$ 0.039 341 中-好 金家屯组 煤系泥岩 $\frac{3.06 \sim 3.41}{ 3.24(2) }$ $\frac{0.30 \sim 5.53}{ 2.92(2) }$ 0.328 1375 通化盆地 亨通山组 暗色泥岩 $\frac{0.25 \sim 2.79}{ 1.08(36) }$ $\frac{0.08 \sim 10.33}{ 2.57(36) }$ $\frac{0.107 \sim 0.159}{ 0.133(2) }$ $\frac{762 \sim 976}{ 869 (2) }$ 中等-好 下桦皮甸子组 暗色泥岩 $\frac{1.02 \sim 3.08}{ 1.85(8) }$ $\frac{1.19 \sim 9.65}{ 4.42(8) }$ $\frac{0.052 \sim 0.087}{ 0.064(3) }$ $\frac{195 \sim 576}{ 334(3) }$ 虎林盆地 云山组 煤系泥岩 $\frac{0.39 \sim 5.90}{ 1.97(40) }$ $\frac{0.08 \sim 20.80}{ 3.29(34) }$ 碳质泥岩 $\frac{6.89 \sim 36.33}{ 14.50(5) }$ $\frac{27.43 \sim 73.05}{ 44.85(5)}$ 勃利盆地 穆棱组 暗色泥岩 $\frac{0.40 \sim 0.53}{ 0.48(3) }$ $\frac{0.06 \sim 0.28}{ 0.1767(3) }$ $\frac{0.007 \sim 0.259}{ 0.091(3) }$ 1135 下云山组 暗色泥岩 $\frac{0.15 \sim 3.52}{ 0.78(14) }$ $\frac{0.04 \sim 2.41}{ 0.31(14) }$ $\frac{0.002 \sim 0.038}{ 0.010(14) }$ 珠山组 暗色泥岩 $\frac{0.11 \sim 4.37}{ 1.12(30) }$ $\frac{0.04 \sim 16.93}{ 1.45(28) }$ $\frac{0.002 \sim 0.422}{ 0.039(17) }$ $\frac{204 \sim 1046}{ 625(2) }$ 宁安盆地 穆棱组 煤系泥岩 $\frac{0.22 \sim 5.93}{ 1.63(19) }$ $\frac{0.24 \sim 41.06}{ 5.34(22) }$ 碳质泥岩 $\frac{6.30 \sim 33.75}{ 14.87(7) }$ $\frac{0.58 \sim 112.36}{ 41.47(6) }$ 延吉盆地 铜佛寺组 暗色泥岩 $\frac{0.31 \sim 4.57}{ 1.94(42) }$ $\frac{0.08 \sim 33.77}{ 3.69(51) }$ $\frac{0.008 \sim 0.225}{ 0.057(25) }$ $\frac{306 \sim 583}{ 444(2) }$ 大砬子组 暗色泥岩 $\frac{0.16 \sim 4.81}{ 1.57(56) }$ $\frac{0.04 \sim 34.01}{ 4.39(68) }$ $\frac{0.005 \sim 0.220}{ 0.053(38) }$ $\frac{70 \sim 960}{ 357(5) }$ 安民组 煤系泥岩、碳质泥岩 $\frac{1.48 \sim 8.38}{ 4.62(6) }$ $\frac{0.04 \sim 4.75}{ 2.38(6) }$ $\frac{0.010 \sim 0.080}{ 0.030(5) }$ 久大组 煤系泥岩 $\frac{2.55 \sim 5.54}{ 3.54(11) }$ $\frac{0.34 \sim 46.80}{ 16.13(11) }$ $\frac{0.010 \sim 0.690}{ 0.390(4) }$
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表 3 松辽外围东部盆地群下白垩统烃源岩有机质显微组分统计表
Table 3. Characteristics of organic maceral in Lower Cretaceous source rocks in the eastern periphery of Songliao Basin
盆地 地层 烃源岩 腐泥组/% 壳质组/% 镜质组/% 惰性组/% 类型指数 干酪根类型 三江盆地 穆棱组 煤系泥岩 $\frac{42.0 \sim 84.7 }{ 67.7(24) }$ $\frac{0.3 \sim 2.0 }{ 0.8(8) }$ $\frac{12.3 \sim 48.0 }{ 29.8(24) }$ $\frac{0.3 \sim 17.0 }{ 4.5(13) }$ $\frac{-2.8 \sim 73.2 }{ 43.2(24) }$ Ⅱ1-Ⅲ 城子河组 煤系泥岩 $\frac{28.3 \sim 74.0 }{ 62.6(22) }$ $\frac{0.3 \sim 0.7 }{ 0.5(2) }$ $\frac{24.0 \sim 64.3 }{ 36.3(23) }$ $\frac{0.3 \sim 7.3 }{ 2.4(9) }$ $\frac{-27.3 \sim 54.5 }{ 34.4(22) }$ 鸡西盆地 穆棱组 煤系泥岩 $\frac{24.0 \sim 46.7 }{ 39.5(24) }$ $\frac{0.7 \sim 6.7 }{ 6.4(21) }$ $\frac{30.0 \sim 66.0 }{ 40.9(24) }$ $\frac{6.7 \sim 16.7 }{ 14.8(23) }$ $\frac{-35.5 \sim 10.8 }{ -2.7(24) }$ Ⅱ2-Ⅲ 双阳盆地 长安组 煤系泥岩 35.2 64.8 -31.0 Ⅲ 金家屯组 煤系泥岩 9.3 90.7 -63.4 炭质泥岩 6.3 93.7 -67.1 柳河盆地 亨通山组 暗色泥岩 $\frac{35.0 \sim 78.0 }{ 51.8(5) }$ $\frac{20.0 \sim 60.0 }{ 43.8(5) }$ $\frac{1.0 \sim 8.0 }{ 4.4(5) }$ $\frac{-32.5 \sim 22.0 }{ -11.4(5) }$ Ⅱ2-Ⅲ 通化盆地 亨通山组 暗色泥岩 $\frac{78.7 \sim 80.7 }{ 79.7(2) }$ $\frac{19.3 \sim 21.3 }{ 20.3(2) }$ $\frac{23.4 \sim 25.92 }{ 4.65(2) }$ Ⅱ1-Ⅲ 下桦皮甸子组 暗色泥岩 $\frac{68.0 \sim 81.0 }{ 74.7(3) }$ $\frac{15.0 \sim 24.0 }{ 19.3(3) }$ $\frac{4.0 \sim 8.0 }{6.0(3) }$ $\frac{8.0 \sim 25.01 }{ 6.7(3) }$ 鹰嘴砬子组 暗色泥岩 $\frac{16.0 \sim 25.0 }{ 19.7(3) }$ $\frac{68.0 \sim 76.0 }{ 51.7(7) }$ $\frac{14.0 \sim 65.0 }{ 34.5(6) }$ $\frac{1.0 \sim 9.0 }{ 4.3(4) }$ $\frac{-43.0 \sim 41.5 }{ 3.7(7) }$ 红庙子盆地 亨通山组 暗色泥岩 $\frac{60.0 \sim 75.0 }{ 66.2(5) }$ $\frac{18.0 \sim 30.0 }{ 24.2(5) }$ $\frac{7.0 \sim 11.0 }{ 9.6(5) }$ $\frac{-3.0 \sim 17.0 }{ 5.2(5) }$ Ⅱ2-Ⅲ 油页岩 $\frac{60.0 \sim 70.0 }{ 65.0(2) }$ $\frac{22.0 \sim 30.0 }{ 26.0(2) }$ $\frac{8.0 \sim 10.0 }{ 9.0(2) }$ $\frac{-3.0 \sim 11.0 }{ 4.0(2) }$ 下桦皮甸子组 暗色泥岩 $\frac{83.0 \sim 85.0 }{ 84.0(2) }$ $\frac{10.0 \sim 12.0 }{ 11.0(2) }$ 5.0 $\frac{28.0 \sim 30.0 }{ 39.0(2) }$ 鹰嘴砬子组 暗色泥岩 22.0 $\frac{55.0 \sim 73.0 }{ 66.0(3) }$ $\frac{20.0 \sim 23.0 }{ 21.7(3) }$ $\frac{7.0 \sim 8.0 }{ 7.5(2) }$ $\frac{11.0 \sim 32.3 }{ 19.4(3) }$
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