Permian Formation Characteristics and Petroleum Geological Significance of Well MSD1 in Suhongtu Depression, Yin’e Basin
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摘要:
长久以来,由于银额盆地覆盖区二叠系地层特征认识不清,致使盆地内钻井揭示的油气产层地质时代存在争议。本次研究利用银额盆地苏红图坳陷MSD1井下部井段岩心样品开展了孢粉学、矿物学、锆石年代学等研究工作,结合盆地内钻井、地震测线及地表露头资料开展地层对比,取得了以下认识:①苏红图坳陷MSD1井
2669.00 ~2726.00 m井段内发现的Florinites,Vesicaspora,Striatoabieites,Vittatina和Hamiapollenites等孢粉分子,且碎屑岩薄片显微镜下见腕足、海百合、苔藓虫等零散生物碎屑分布,均指示该段地层为上二叠统哈尔苏海组,时代为二叠纪晚期。②结合钻井时井深标定及地震层位追踪,明确银额盆地二叠系在盆地覆盖区广泛分布,二叠系地震反射呈现弱反射–空白反射、中–弱振幅、层内连续性差、底界偶见强振幅连续界线的特征,反映二叠系沉积后经历了多期构造改造作用。③盆地内多口钻井发现白垩系、二叠系的两套含油气系统,钻井烃源岩地球化学特征显示银额盆地二叠系具有丰富的油气勘探潜力。综合研究认为,银额盆地二叠系原型盆地分布范围广、油气资源潜力丰富,后期构造改造分区性强,局部地区构造破坏严重,MSD1井二叠系古生物地层学、锆石年代学、岩石矿物学及地球物理学地层特征的发现,实现了盆地露头区与覆盖区二叠系特征对比统一,明确了银额盆地二叠系的油气勘探前景。Abstract:For a long time, due to the unclear understanding of the characteristics of Permian residual strata in the coverage area of yin'e basin, the geological age of oil and gas production layers revealed by drilling in the basin is controversial. In this study, palynology, mineralogy, zircon chronology and other research work were carried out by using the core samples of the lower well section of well msd1 in Suhongtu depression of yine basin, and stratigraphic correlation was carried out in combination with the drilling, seismic survey line and surface outcrop data in the basin. The following understandings were obtained: ① sporopollen molecules such as florinites, vesicaspora, stratoabieites, vittatina and hamiapollenites found in the
2669.00 ~2726.00 m well section of well msd1 in Suhongtu depression, The scattered bioclastic distribution of brachiopods, crinoids and bryozoans can be seen under the thin section microscope of clastic rock, indicating that the stratum of this section is the upper Permian halsuhai formation, which is in the Late Permian. ② Combined with drilling time depth calibration and seismic horizon tracking, it is clear that the Permian in yine basin is widely distributed in the coverage area of the basin. The seismic reflection of the Permian presents the characteristics of weak reflection blank reflection, medium weak amplitude, poor continuity in the layer and occasional strong amplitude continuous boundary at the bottom, reflecting that the Permian has experienced multi-stage structural transformation after sedimentation. ③ Two sets of oil and gas systems of Cretaceous and Permian have been found in many wells in the basin. The geochemical characteristics of drilling source rocks show that the Permian in yine basin has rich oil and gas exploration potential. It is comprehensively considered that the Permian prototype basin in yine basin has a wide distribution range, rich oil and gas resource potential, strong zoning of late structural transformation, and serious structural damage in some areas. The discovery of Permian paleontostratigraphic evidence in well msd1 further strengthens the exploration prospect of Permian.-
Keywords:
- Upper Permian /
- Haersuhai Formation /
- palynological paleontology /
- zircon dating /
- Yin’e basin
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图 1 银额盆地及周缘地质简图(a)、银额盆地研究区亚洲主要基底地块位置图(Zhang et al., 2022)(b)、银额盆地周缘中亚造山带南部构造轮廓图(Chen et al., 2019)(c)
Figure 1. (a) The tectonic sketch of Yin’e Basin, (b) major Asian cratons and smaller basement blocks location of Yin’e Basin study region, (c) Tectonic outlines of the southwestern CAOB in Northwest China
图 3 银额盆地MSD1井二叠系岩性特征
a、b.杂色凝灰质角砾岩(取样井段为2 389.18~2 389.34 m);c. 砾质不等粒砂状结构(−)20×;d.砂质砾状结构(−)20×;e、f.绿灰色凝灰岩(取样井段为2 756.72~2 756.79 m);g. 含砾粗粒砂状结构(+)20×;h. 砂质砾状结构(−)20×;i. 砂质砾状结构(−)20×;j. 砂质砾状结构(−)20×;Qm.单晶石英;Qp.多晶石英;Lv.火成岩岩屑;Lm.变质岩岩屑;Ls.沉积岩岩屑;P.斜长石
Figure 3. Lithology characteristics of Permian in well MSD1 in Yin’e Basin
图 4 银额盆地二叠系哈尔苏海组MSD1井孢粉化石
1. 中大光面单缝孢Laevigatosporites medius Kosanke,1950(井深:
2720.00 m);2~4、7. 弗氏粉(未定种)Florinites sp.(2、3. 井深2697.00 m;4、7. 井深2719.00 m);5. 苍白开通粉Vitreisporites pallidus(Reissinger)Nilsson,1958(井深2695.00 m);6. 四方十字粉.Crucisaccites quadratoides(Zhou)Hou and Song,1995(井深2719.00 m);8、9、13. 聚囊粉(未定种)Vesicaspora sp.(8、9. 井深2725.00 m;13. 井深2697.00 m);10. 冷杉型多肋粉(未定种)Striatoabieites sp.(井深2697.00 m);11. 叉肋粉(未定种)Vittatina sp.(井深2725.00 m);12. 葵鳞羊齿粉(未定种)Pteruchipollenites sp.(井深2697.00 m);14、16. 松型粉(未定种)Pityosporites sp.(井深2697.00 m);15. 蝶囊粉(未定种)Platysaccus sp.(井深2697.00 m);17. 逆沟粉(未定种)?Anticapipollis sp.(井深2697.00 m);18. 单束多肋粉(未定种)Protohaploxypinus sp.(井深2697.00 m);19~25. 不能鉴定的类型(19、 20. 井深2720.00 m;21、22. 井深2697.00 m;23~25. 井深2719.00 m)Figure 4. Sporopollen fossils of Well MSD1 in Haersuhai Formation, Yin’e Basin
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