石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (5): 891-902.doi: 10.11743/ogg20200501
薛永安1(), 王奇2, 牛成民1, 苗全芸3, 刘梦醒2, 殷杰4
收稿日期:
2020-05-05
出版日期:
2020-10-28
发布日期:
2020-10-22
第一作者简介:
薛永安(1963-),男,博士,教授级高级工程师,海上油气勘探与管理。E-mail:基金项目:
Yong'an Xue1(), Qi Wang2, Chengmin Niu1, Quanyun Miao3, Mengxing Liu2, Jie Yin4
Received:
2020-05-05
Online:
2020-10-28
Published:
2020-10-22
摘要:
综合凝析油的地球化学特征、周缘洼槽烃源岩生烃史、流体包裹体岩相学观察、均一化温度及含油包裹体的石英颗粒的频数(GOI),分析了渤中19-6地区深层凝析气的来源及充注成藏过程。研究表明:潜山凝析油气的热成熟度高,对应的烃源岩Ro约1.3%。轻烃、碳同位素组成与生物标志物参数分析表明凝析油气来源于油型母质,即沙河街组烃源岩。烃类包裹体主要分布于石英微裂隙,少量分布于加大边。液态烃类包裹体呈黄绿色及蓝白色荧光,GOI值高达80%,揭示高的原油充满度。渤中19-6深层潜山凝析气藏表现为近源、早油晚气连续充注,其中原油充注在明化镇组下段时期(12~5.1 Ma),天然气大量充注时间为明化镇组下段沉积末期甚至更晚的时期(5.1~0 Ma)。尽管新构造运动期油气垂向调整显著,但烃源岩快速熟化与近源强充注是构造活化区深层潜山动态富集的重要物质基础。
中图分类号:
表1
渤中凹陷渤中19-6潜山构造带原油物性特征"
井号 | 层位 | 深度/m | 密度/(g·cm-3) | 相对密度/° (API) | 粘度/(mPa·s) | 蜡含量/% | 沥青质含量/% | 胶质含量/% | 硫含量/% |
BZ19-6-A | E1-2k | 3 566.8~3 634 | 0.79 | 45.60 | 1.41 | 14.13 | 0.31 | 0.79 | 0.02 |
BZ19-6-A | E1-2k | 3 521.1 | 0.86 | 31.80 | 8.13 | 18.73 | 3.52 | 8.97 | — |
BZ19-6-A | Ar | 4 043.4~4 142 | 0.79 | 46.04 | 1.24 | 11.80 | 0.15 | 0.84 | 0.02 |
BZ19-6-B | Ar | 3 873.7~3 923.5 | 0.80 | 44.11 | 1.65 | 14.64 | 0.15 | 0.28 | 0.13 |
BZ19-6-B | Ar | 3 879~3 998.66 | 0.81 | 42.34 | 2.29 | 15.82 | 0.20 | 1.34 | 0.02 |
BZ19-6-C | E1-2k | 4 079.18 | 0.79 | 47.39 | 2.06 | 7.32 | 0.02 | 0.57 | 0.01 |
BZ19-6-D | Ar | 4 411~4 499.80 | 0.80 | 44.71 | 1.72 | 17.62 | 0.16 | 0.69 | 0.01 |
BZ19-6-E | E1-2k | 3 500~3 566 | 0.79 | 46.26 | — | 10.11 | 0.72 | 0.91 | 0.02 |
BZ19-6-E | E1-2k | 3 901.5 | 0.82 | 40.85 | 2.50 | 20.52 | 0.26 | 2.30 | 0.04 |
图8
渤中凹陷渤中19-6潜山储层流体包裹体单偏光和荧光照片 a,b.黄绿色荧光烃包裹体沿石英颗粒微裂隙串珠状分布,BZ19-6-C井,埋深4 049.56 m;c,d.黄绿色与蓝白色荧光烃包裹体呈群体状分布,BZ19-6-C井,埋深3 818 m;e,f.蓝白色荧光烃包裹体沿石英颗粒微裂隙呈串珠状分布,BZ19-6-G井,埋深4 678.43 m;g,h.甲烷气烃包裹体与蓝白色荧光烃包裹体沿石英颗粒微裂隙呈串珠状分布,BZ19-6-C井,埋深3 818 m;i,j.含甲烷气盐水包裹体与蓝白色荧光烃包裹体伴生,BZ19-6-C井,埋深3 851.77 m;k. CO2三相包裹体沿石英颗粒微裂隙呈串珠状分布,BZ19-6-G井,埋深4 686.1 m;l. CO2气包裹体沿石英颗粒微裂隙分布,BZ19-6-G井,埋深4 494.1 m AI.盐水包裹体;CH4 FI.甲烷气包裹体;含CH4 AI.含甲烷气盐水包裹体"
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