Petrophysical characteristics of Huoshiling Formation from CCSD SK-2 in the Songliao Basin of Northeast China
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摘要:
松辽盆地资源与环境深部钻探工程是针对白垩纪古气候与古环境研究、地球深部资源调查以及基础地质研究等一系列科学问题而实施的科学钻探。松科二井是松辽盆地科学钻探工程的主体钻孔，设计的测井项目齐全，采集了丰富、连续、原位的地球物理测井资料。本文主要利用该孔的测井资料研究深部火石岭组地层岩石物理学特征；结合实验室岩心核磁共振测试结果，分析不同岩性储层的孔隙结构特征。研究表明，火石岭组地层主要发育安山岩、凝灰岩、复成分砾岩和凝灰质泥岩，其中火成岩岩相以爆发相和喷溢相为主，安山岩和复成分砾岩表现为高电阻率、低声波时差特征，凝灰岩为低电阻率、高声波时差特征，凝灰质泥岩电阻率最低；储层整体上具有低孔低渗的特点，但凝灰岩储层小孔和中孔发育，物性相对较好，是较为有利的储层。研究结果为进一步评价松辽盆地深部油气资源和地层结构提供了有力支持。
Abstract:The Continental Scientific Drilling Project in the Songliao Basin was aimed at solving a series of scientific problems involved in Cretaceous paleoclimate and paleoenvironmental research, the development of deep exploration techniques, and the earth's deep resource survey. As the main borehole of the scientific drilling project of Songliao Basin, SK-2 has collected continuous and in-situ geophysical log data. In this paper, geophysical log data were used to reveal the range of petrophysical parameters of rocks in Huoshiling Formation. Combined with laboratory core NMR test analysis, the authors studied the pore structure characteristics of different igneous reservoirs. The results show that the Huoshiling Formation mainly consists of andesite, tuff, complex conglomerate and tuff mudstone. The igneous facies are dominated by the explosive facies and the effusion facies. The andesite and complex conglomerate are characterized by high resistivity and low acoustic wave time difference. The characteristics of the tuff are low resistivity and high acoustic time difference, and the tuff mudstone has the lowest resistivity. The reservoir has the characteristics of low porosity and low permeability, but the tuff reservoir has developed small and medium pores and has relatively good physical properties, and hence it is a favorable reservoir. The research results provide strong support for further evaluation of deep oil and gas resources and stratigraphic structure in the Songliao Basin.
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1. 研究目的（Objective）
尼玛盆地构造上位于班公湖—怒江缝合带中部，是发育在侏罗系—白垩系海相地层之上的古近系陆相裂谷盆地，北接羌塘地块，南邻冈底斯地块，近东西向展布，面积约3000 km2。本次研究目的是初步查明尼玛盆地东部冻土发育特征，调查盆地东部古近系地层层序，获取古近系烃源岩、储盖层等关键评价参数，进一步评价盆地油气资源潜力。
结合新获取的大地电磁测深、地表地质调查及藏尼地1井资料，通过对盆地东部石油地质条件的进一步论证，中国地质调查局油气资源调查中心在盆地东部赛布错坳陷部署实施了藏双地1井，该井的实施对于西藏高原陆相盆地的油气勘探具有重要意义。
2. 研究方法（Methods）
通过资料的收集和重新处理解释，建立了尼玛盆地基础资料数据库，结合之前在尼玛盆地东部发现的油气显示带及最新的大地电磁测深和藏尼地1井资料，优选井位。藏双地1井完钻井深1206.78 m，全井段进行了取心、录井和测井，共有岩心407箱，岩心总长1108.88 m，收获率95.9%。在古近系牛堡组选取烃源岩样品进行地球化学分析测试，通过分析有机质丰度、有机质类型、热演化成熟度来评价烃源岩生烃潜力；使用荧光分析仪对岩石进行荧光分析，主要进行干照和滴照实验，来检测岩石、岩屑中的沥青、烃类等有机物质。
3. 结果（Results）
藏双地1井从上到下钻遇地层依次为第四系+ 新近系—牛堡组三段—牛堡组二段（未穿），气测录井有3处气测异常段，总烃最高为0.159%，岩性为棕红色粉砂岩、灰色细砂岩。含气量解析取样井段527.90~1206.78 m，共取样54个，现场解析在标准大气压下最高含气量为0.213 m3/t；共做浸水试验20个，拍摄视频20个，其中井深744.40 m、752.08 m、767.30 m、774.66 m、797.20 m、832.43 m均有气泡冒出，以井深752.08 m最为明显。
荧光录井井段0~1206.78 m，对全井岩心按设计逐包进行荧光直照、拍照、氯仿浸泡，定级；全井共录取荧光资料421个点，其中井深1024.23~1026.23 m牛二段灰绿色泥岩断面处，可见黑色薄膜状干沥青，具荧光显示，干照下呈黄色、淡黄色，产状为星点状、带状，用氯仿滴照可呈片状；井深1077.46~1077.76 m牛二段见油迹；井深1078.16~1078.76 m牛二段见点状干沥青；井深1078.76~1079.16 m牛二段层理间见油斑；井深1079.16~1080.16 m牛二段顶部断面处见油迹，都具有荧光显示，呈黄色、淡黄色，产状为星点状、带状（图 1）。
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图 1 藏双地1井牛堡组二段录井柱状图及1079.16~1080.16 m油气显示Figure 1. Logging histogram and the oil and gas display in 1079.16-1080.16m of the second member of Niubao formation in Well Zangshuangdi 14. 结论（Conclusions）
（1）藏双地1井全井取心，获得了尼玛盆地东部古近系地层层序、烃源岩及储层等相关参数，分别在牛三段418.43~422.00 m、牛二段890.00~898.00 m及1068.16~1087.00 m发现3处气测异常段，总烃最高为0.159%，现场解析含气量值最大为0.213 m3/t，并在牛二段1077~1080 m处发现不同级别的油气显示，首次实现了尼玛盆地地下油气的重要发现，对盆地下一步的勘探部署具有重要意义。
（2）本井是继藏尼地1井后在西藏尼玛盆地部署实施的第2口地质调查井，通过对藏双地1井的钻井技术攻关，进一步总结出了适合高寒缺氧、地表及地下地质条件复杂的高原钻井施工工艺和设备参数，为下一步在该区钻井施工提供了重要的技术支撑。
尼玛盆地平均海拔近4800 m，由于其高海拔的特殊性，具有高寒缺氧、气候恶劣、生态脆弱等特征，在野外施工过程中与其他地区有着很大的不同，通过藏尼地1井、藏双地1井的钻探，克服了高寒条件下冻土发育钻井技术难题和高原缺氧条件下深井取心难题，基本形成了一套安全、环保、高效的作业技术体系，为高原地区的钻探施工工程积累了丰富的经验。
5. 致谢（Acknowledgement）
感谢李韬、李显亮等同志的交流和启发。
致谢: 本文工作得到了松辽盆地资源与环境深部钻探工程首席科学家王成善院士、总地质师王璞珺教授以及副总指挥冉恒谦教授的大力支持；中国石油集团测井有限公司天津分公司测井队成员参加了测井数据采集工作，在此一并表示衷心的感谢。 -
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图 1 “松辽盆地大陆深部科学钻探”井位及松辽盆地纵剖面图（据Wang et al., 2013a）
松科二井中的黄色层段为取心层段，红色条带代表油层, T02-5表示地震反射层位
Figure 1. Borehole distribution of deep continental scientific drilling engineering and structural cross section across the central part of the Songliao Basin based on regional seismic analyses (after Wang et al., 2013a)
The yellow bar in SK-2 borehole is coring interval. The red regions indicate oil reservoirs. T02-5 is seismic horizons
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图 2 火石岭组地层典型岩心照片
a—黑色凝灰质泥岩（顶面）；b—黑色凝灰质泥岩（侧面）；c—杂色火山角砾岩（顶面）；d—杂色火山角砾岩（侧面）；e—杂色安山质角砾岩（顶面）；f—杂色安山质角砾岩（侧面）
Figure 2. Typical core photographs in Huoshiling Formation
a-Black tuff mudstone (top); b-Black tuff mudstone (lateral); c-Variegated volcanic breccia (top); d- Variegated volcanic breccia (lateral); e-Variegated andesite breccia (top); f-Variegated andesite breccia (lateral)
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图 3 松科二井火石岭组测井响应特征图
Figure 3. Logging response characteristics in the Huoshiling Formation
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图 4 不同岩性地层测井响应统计结果图
a—岩性与自然伽马的关系；b—岩性与电阻率的关系；c—岩性与声波时差的关系；d—岩性与密度的关系
Figure 4. Statistical results of log response in different lithologic formations
a-Relationship between lithology and GR; b-Relationship between lithology and Rd; c-Relationship between lithology and AC; d-Relationship between lithology and DEN
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图 5 火石岭组地层岩性识别交会图
Figure 5. Lithologic identification cross plot in the Huoshiling Formation
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图 6 松科二井沙河子组底部至基底地震响应
Figure 6. Seismic response characteristics through the bottom of Shahezi Formation to the basement in SK-2e
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图 7 火石岭组地层各岩石物性参数之间的关系
Figure 7. Relationship between physical parameters of rocks in the Huoshiling Formation
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图 8 饱水状态下各岩类的核磁共振T2谱分布图
Figure 8. Nuclear magnetic resonance T2 distribution of different lithologic types in saturated state
表 2 火石岭组地层各岩性储层物性参数平均值分布范围
Table 2 Distribution of physical parameters of various reservoirs in the Huoshiling Formation
下载: 导出CSV
表 3 火石岭组地层各类岩性孔喉分布平均值
Table 3 Average distribution of pore throat of different lithologic types in the Huoshiling Formation
下载: 导出CSV
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