Earth Science Frontiers ›› 2025, Vol. 32 ›› Issue (5): 417-431.DOI: 10.13745/j.esf.sf.2025.7.15
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WAN Xiaolong1,2,3(), WU Shenghe1,2,*(
), ZHOU Xinping4, XU Zhenhua1,2, FU Jinhua5, WANG Zifeng1,2, MA Shuwei4, WU Degang1,2, LI Zhen4, LIU Mingcheng1,2
Received:
2025-06-20
Revised:
2025-07-10
Online:
2025-09-25
Published:
2025-10-14
Contact:
WU Shenghe
CLC Number:
WAN Xiaolong, WU Shenghe, ZHOU Xinping, XU Zhenhua, FU Jinhua, WANG Zifeng, MA Shuwei, WU Degang, LI Zhen, LIU Mingcheng. Research on the prediction method of 3D reservoir sweet spots distribution of shale oil in shale intercalated layer: A case from the Yanchang Formation of B15 block, Ordos Basin[J]. Earth Science Frontiers, 2025, 32(5): 417-431.
沉积微相 | 岩性 | 砂体厚度 | 韵律 | 孔隙度 | 泥质含量 | 含油饱和度 | GR曲线响应特征 | ||
---|---|---|---|---|---|---|---|---|---|
水道 | 细砂岩和粗粉砂岩为主 | 1.5~4.0 m | 正韵律 | >10% | <5% | >55% | 高幅度钟型 | ||
朵叶体 | 朵叶主体 | 细砂岩和粗粉砂岩为主 | 1.5~4.0 m | 反韵律或 均质韵律 | 6%~10% | 5%~8% | 45%~55% | 高幅度漏斗型或箱型 | |
朵叶侧缘 | 细粉砂岩 | 0.5~1.5 m | 无明显韵律 | <6% | >8% | 40%~45% | 小幅度漏斗型或指型 |
Table 1 Characteristics of microfaices of B15 Block, Ordos Basin
沉积微相 | 岩性 | 砂体厚度 | 韵律 | 孔隙度 | 泥质含量 | 含油饱和度 | GR曲线响应特征 | ||
---|---|---|---|---|---|---|---|---|---|
水道 | 细砂岩和粗粉砂岩为主 | 1.5~4.0 m | 正韵律 | >10% | <5% | >55% | 高幅度钟型 | ||
朵叶体 | 朵叶主体 | 细砂岩和粗粉砂岩为主 | 1.5~4.0 m | 反韵律或 均质韵律 | 6%~10% | 5%~8% | 45%~55% | 高幅度漏斗型或箱型 | |
朵叶侧缘 | 细粉砂岩 | 0.5~1.5 m | 无明显韵律 | <6% | >8% | 40%~45% | 小幅度漏斗型或指型 |
步骤 | 方法流程 |
---|---|
1 | 输入:待聚类对象点集合P={p1,p2,…,pn} |
2 | 从与优势甜点区域Fi相近的任一对象点pi开始; |
3 | 寻找合并pi直接密度可达的对象,并约束这些对象的簇中心点不远离优势甜点区域Fi; |
4 | 如果pi是一个核心点,则找到了一个聚类,如果pi是一个边界点(即从pi没有密度可达的点)则寻找下一个对象点pi+1; |
5 | 循环进行2、3步骤,直到所有点都被处理。 |
Table 2 Workflow of density clustering method with constrained cluster centers
步骤 | 方法流程 |
---|---|
1 | 输入:待聚类对象点集合P={p1,p2,…,pn} |
2 | 从与优势甜点区域Fi相近的任一对象点pi开始; |
3 | 寻找合并pi直接密度可达的对象,并约束这些对象的簇中心点不远离优势甜点区域Fi; |
4 | 如果pi是一个核心点,则找到了一个聚类,如果pi是一个边界点(即从pi没有密度可达的点)则寻找下一个对象点pi+1; |
5 | 循环进行2、3步骤,直到所有点都被处理。 |
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