石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (1): 34-45.doi: 10.11743/ogg20230103
李剑1,2(), 杨春龙1,2(), 谢武仁1, 芮宇润3, 王晓波1,2, 张璐1,2, 谢增业1,2, 郭泽清1
收稿日期:
2022-06-06
修回日期:
2022-11-15
出版日期:
2023-01-14
发布日期:
2023-01-13
通讯作者:
杨春龙
E-mail:lijian69@petrochina.com.cn;yangchunlong69@petrochina.com.cn
第一作者简介:
李剑(1966—),男,博士、教授级高级工程师,天然气地球化学与油气成藏。E-mail:基金项目:
Jian LI1,2(), Chunlong YANG1,2(), Wuren XIE1, Yurun RUI3, Xiaobo WANG1,2, Lu ZHANG1,2, Zengye XIE1,2, Zeqing GUO1
Received:
2022-06-06
Revised:
2022-11-15
Online:
2023-01-14
Published:
2023-01-13
Contact:
Chunlong YANG
E-mail:lijian69@petrochina.com.cn;yangchunlong69@petrochina.com.cn
摘要:
四川盆地安岳气田是中国迄今为止发现的最大规模的海相碳酸盐岩气田,探明天然气地质储量1.03×1012 m3,其中震旦系灯影组占56.3 %。目前灯影组勘探开发主要围绕灯影组四段台缘带展开,且台缘带单井产能明显高于台内地区。基于台缘带和台内地区天然气地球化学特征及气藏对比关系,结合成藏条件分析,探讨其成藏差异性。研究表明:①灯影组台缘带较台内地区天然气甲烷氢同位素明显偏重,对应寒武系源岩古水体介质盐度高于震旦系,反映由台缘带到台内地区震旦系烃源岩贡献比例的增加;②台缘带与台内地区储层在岩石类型、储集空间等方面一致,但台缘带储层内部溶蚀孔洞发育程度强于台内地区,主要受控于丘滩发育程度和表生岩溶作用强度;③台缘带和台内地区成藏组合存在差异,台缘带紧邻裂陷内烃源岩,储层侧向对接烃源岩,存在旁生侧储、上生下储等多种成藏组合,而台内地区距裂陷内烃源岩较远,需要通过沟通油、源的断裂输导油气,成藏组合单一;④震旦系-寒武系烃源岩贡献比例的不同和优质储层发育位置及组合类型的差异,是导致台缘带和台内地区产能差异巨大的主要原因。川西北蓬莱—剑阁地区是未来深层灯影组台缘带的有利勘探领域,古隆起围斜部位台地内部构造-岩性气藏是灯影组台内地区主要有利勘探区。
中图分类号:
表1
四川盆地震旦系相关烃源岩地球化学参数对比"
层系 | 岩性 | TOC/% | EqVRo/% | 裂陷槽厚度/m | 台内厚度/m | δ13C干酪根/‰ | 资料来源 | |
---|---|---|---|---|---|---|---|---|
寒武系 | 筇竹寺组 | 泥页岩 | 0.50~8.49(1.95) | 1.84~2.40 | 50~300 | 40~120 | -36.0~-31.0(-33.3) | 文献[ |
震旦系 | 灯三段 | 泥岩 | 0.50~4.73(0.87) | 3.16~3.21 | 5~30 | 5~25 | -33.4~-28.5(-32.0) | 文献[ |
灯影组 | 藻云岩 | 0.20~3.67(0.61) | 1.97~3.46 | 100~300 | 200~300 | -32.8~-23.8(-29.4) | 文献[ | |
陡山沱组 | 泥岩 | 0.50~14.17(2.91) | 2.08~3.82 | 10~30 | 0~10 | -31.5~-30.3(-30.8) | 文献[ |
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