石油与天然气地质 ›› 2025, Vol. 46 ›› Issue (1): 136-150.doi: 10.11743/ogg20250110
鲍李银1,2(
), 庞雄奇1,2(
), 崔新璇1,2, 陈宏飞1,2, 高军3, 邹亮3, 赵振丞1,2, 王琛茜4, 王雷1,2, 李闻东3, 刘利5
收稿日期:2024-07-31
修回日期:2024-12-18
出版日期:2025-02-28
发布日期:2025-03-03
通讯作者:
庞雄奇
E-mail:995959069@qq.com;pangxq@cup.edu.cn
第一作者简介:鲍李银(1998—),男,博士研究生,油气藏形成机制与分布规律。E‑mail: 995959069@qq.com。
Liyin BAO1,2(
), Xiongqi PANG1,2(
), Xinxuan CUI1,2, Hongfei CHEN1,2, Jun GAO3, Liang ZOU3, Zhencheng ZHAO1,2, Chenxi WANG4, Lei WANG1,2, Wendong LI3, Li LIU5
Received:2024-07-31
Revised:2024-12-18
Online:2025-02-28
Published:2025-03-03
Contact:
Xiongqi PANG
E-mail:995959069@qq.com;pangxq@cup.edu.cn
摘要:
为解决准噶尔盆地金龙油田二叠系佳木河组火山岩岩相类型及优势储层展布特征不清、油气资源开发难度较大问题。基于岩心观察、测井分析及实验化验数据,系统分析了研究区火山岩的岩相类型、储层物性与储集空间特征,建立了岩相组合模型,提出了对产能的控制因素。研究结果表明:①准噶尔盆地金龙油田火山岩具有爆发相、溢流相和火山沉积相三大类。爆发相以熔结火山碎屑岩和安山质火山角砾岩为主,平均孔隙度大于10 %,为主要储层;溢流相以熔岩为主,平均孔隙度小于6 %,火山沉积相物性差。②研究区火山岩储层以气孔、杏仁体内孔及溶蚀孔为主,原生粒间孔较少,爆发相与溢流相顶部溶蚀孔洞发育最为显著。裂缝主要为构造缝和溶蚀缝,发育程度与到断裂距离紧密相关,中-酸性溢流相以斜交缝、网状缝为主,基性溢流相以高角度直劈缝为主。③研究区有中-酸性热碎屑流亚相与中-酸性溢流相互层、基性热碎屑流亚相与基性溢流亚相频繁互层、中性空落亚相与中性溢流亚相互层、中性空落亚相与中-酸性热碎屑流亚相互层等4种岩相组合。产能最高的为中性空落亚相与中-酸性热碎屑流亚相互层组合,其次为中-酸性热碎屑流亚相与中-酸性溢流相互层组合、中性空落亚相与中性溢流亚相互层组合,基性热碎屑流亚相与基性溢流亚相频繁互层组合组合日产量最低。④储层有效厚度与含油饱和度对产能的影响最大,其次为孔隙度和地层压力。
中图分类号:
表1
金龙油田火山岩储层孔、渗特征"
| 火山储集岩类型 | 孔隙度/% | 渗透率/(10-3μm2) | ||||
|---|---|---|---|---|---|---|
| 最大值 | 最小值 | 平均值 | 最大值 | 最小值 | 平均值 | |
| 流纹岩 | 10.14 | 0.81 | 4.42 | 0.11 | 0.01 | 0.06 |
| 英安岩 | 5.84 | 0.15 | 2.49 | 0.27 | 0.01 | 0.16 |
| 安山岩 | 10.01 | 0.66 | 6.64 | 0.27 | 0.01 | 0.08 |
| 玄武岩 | 13.08 | 1.19 | 6.59 | 0.67 | 0.01 | 0.22 |
| 流纹质熔结角砾岩 | 14.47 | 5.21 | 8.89 | 1.63 | 0.73 | 1.21 |
| 安山质熔结角砾岩 | 14.35 | 5.40 | 11.07 | 6.20 | 0.09 | 0.27 |
| 玄武质熔结角砾岩 | 19.85 | 8.21 | 12.87 | 17.42 | 0.13 | 3.12 |
| 安山质火山角砾岩 | 19.05 | 4.50 | 9.11 | 8.64 | 0.01 | 0.88 |
表3
金龙油田佳木河组储层岩相组合及产能"
| 井号 | 试油段深度/m | 岩相组合 | 爆发相有效 储层厚度/m | 有效储层测井解释平均孔隙度/% | 有效储层测井解释平均含油饱和度/% | 地层压力/MPa | 平均日产 当量/(t/d) |
|---|---|---|---|---|---|---|---|
| JL2008 | 4 242~4 268 | D | 23.4 | 14.76 | 67.9 | 52.96 | 64.10 |
| JL2011 | 4 151~4 174 | D | 14.7 | 13.88 | 65.7 | 50.56 | 36.20 |
| 金214 | 4 128~4 144 | A | 10.4 | 12.80 | 52.3 | 51.00 | 16.80 |
| 金208 | 4 206~4 242 | A | 15.3 | 12.85 | 56.3 | 50.79 | 18.38 |
| JL2107 | 4 121~4 151 | B | 17.1 | 12.42 | 34.8 | 49.95 | 2.41 |
| JL2106 | 4 095~4 146 | B | 33.9 | 14.19 | 47.2 | 49.95 | 14.19 |
| 金209 | 4 234~4 247 | C | 9.0 | 13.53 | 55.1 | 52.11 | 14.10 |
| 金213 | 4 232~4 248 | C | 13.2 | 12.58 | 55.6 | 52.39 | 18.50 |
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