
新疆石油地质 ›› 2025, Vol. 46 ›› Issue (6): 693-702.doi: 10.7657/XJPG20250605
邹阳1a(
), 陈文顺1b, 罗刚1a, 陈绍蓉1a, 陈方文2(
), 何文军1a, 刘新龙1a, 朱涛1a
收稿日期:2025-04-30
修回日期:2025-08-20
出版日期:2025-12-01
发布日期:2025-12-05
通讯作者:
陈方文
E-mail:zou_yang@petrochina.com.cn;chenfw@upc.edu.cn
作者简介:邹阳(1988-),男,湖北荆州人,高级工程师,硕士,油气地质,(Tel)13519901597(Email)基金资助:
ZOU Yang1a(
), CHEN Wenshun1b, LUO Gang1a, CHEN Shaorong1a, CHEN Fangwen2(
), HE Wenjun1a, LIU Xinlong1a, ZHU Tao1a
Received:2025-04-30
Revised:2025-08-20
Online:2025-12-01
Published:2025-12-05
Contact:
CHEN Fangwen
E-mail:zou_yang@petrochina.com.cn;chenfw@upc.edu.cn
摘要: 准噶尔盆地玛湖凹陷二叠系风城组碱湖页岩油富集和高产主控因素不清,其理论认识和勘探开发受到限制。以风城组页岩油储集层岩石学特征、有机地球化学特征和物性特征为基础,分析风城组烃源岩和储集层岩性对页岩油富集的影响,结合重点井产液剖面获得产油量,分析页岩油富集、裂缝和地层超压对页岩油产量的影响。结果表明:风城组页岩油储集层游离烃含量随总有机碳含量的增大而增大,含油饱和度指数随埋深的增加呈增大趋势,有机质丰度、类型和成熟度是决定页岩油富集程度的关键因素;风城组粉砂岩类页岩油储集层储集空间最好,其次为泥岩类和内源岩类储集层,储集层岩性控制储集空间,影响页岩油富集程度;页岩油富集为页岩油高产的基础,风城组页岩油储集层米产油量随总有机碳含量和长英质矿物含量的增大而增大;裂缝走向与现今最大水平主应力方向的关系影响页岩油渗流特征和产量;地层超压具有保孔、增渗、降黏、提高页岩油产量和采收率的作用。研究结果确定了风城组页岩油富集和高产主控因素,为勘探开发部署提供了科学依据。
中图分类号:
邹阳, 陈文顺, 罗刚, 陈绍蓉, 陈方文, 何文军, 刘新龙, 朱涛. 玛湖凹陷风城组碱湖页岩油富集和高产主控因素[J]. 新疆石油地质, 2025, 46(6): 693-702.
ZOU Yang, CHEN Wenshun, LUO Gang, CHEN Shaorong, CHEN Fangwen, HE Wenjun, LIU Xinlong, ZHU Tao. Main Factors Controlling the Enrichment and High Production of Alkaline Lacustrine Shale Oil in Fengcheng Formation, Mahu Sag, Junggar Basin[J]. Xinjiang Petroleum Geology, 2025, 46(6): 693-702.
图2
玛湖凹陷风城组储集层岩性 a—泥质粉砂岩,玛湖286井,4 577.79 m,铸体薄片;b—石灰质粉砂岩,夏203井,4 692.90 m,铸体薄片;c—白云质细砂岩,玛59X井,5 735.85 m,铸体薄片;d—白云质粉砂岩,玛59X井,5 738.12 m,铸体薄片;e—砂质泥岩,金砂1井,6 281.76 m,铸体薄片;f—石灰质泥岩,玛49井,4 503.61 m,铸体薄片;g—白云质泥岩,夏203井,4 695.70 m,铸体薄片;h—白云质泥岩,玛49井,4 663.43 m,铸体薄片;i—中晶石灰岩,夏云1井,5 097.50 m,风三段,铸体薄片;j—粉晶白云岩,风城7井,5 010.71 m,铸体薄片;k—微晶白云岩,玛页1井,4 748.89 m,铸体薄片;l—硅质岩,夏203井,4 679.72 m,铸体薄片。"
表1
玛湖凹陷风城组储集层有机地球化学参数统计结果"
| 岩性 | 总有机碳含量/% | 游离烃含量/(mg·g-1) | 热解烃含量/(mg·g-1) | 氯仿沥青“A”含量/% |
|---|---|---|---|---|
| 粉砂岩类 | 0.97(0.11~3.91) | 2.10(0.02~11.65) | 4.06(0.03~19.12) | 0.258(0.006~1.341) |
| 泥岩类 | 0.81(0.11~2.85) | 1.78(0.05~7.54) | 3.00(0.06~11.49) | 0.201(0.005~1.265) |
| 内源岩类 | 0.78(0.17~2.82) | 1.05(0.08~6.30) | 2.92(0.19~13.58) | 0.277(0.006~0.836) |
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