新疆石油地质 ›› 2023, Vol. 44 ›› Issue (3): 299-306.doi: 10.7657/XJPG20230305
秦恩鹏1(), 张君莹2, 张生兵1, 刘俊田1, 张小芹1(
), 陈永慧1
收稿日期:
2022-09-13
修回日期:
2022-10-27
出版日期:
2023-06-01
发布日期:
2023-05-19
通讯作者:
张小芹(1969-),女,陕西乾县人,高级工程师,岩石矿物,(Tel)13239735079(E-mail)作者简介:
秦恩鹏(1966-),男,山西平陆人,高级工程师,地层古生物,(Tel)13094023244(E-mail) 基金资助:
QIN Enpeng1(), ZHANG Junying2, ZHANG Shengbing1, LIU Juntian1, ZHANG Xiaoqin1(
), CHEN Yonghui1
Received:
2022-09-13
Revised:
2022-10-27
Online:
2023-06-01
Published:
2023-05-19
摘要:
针对火山活动发育层系细粒岩成分复杂、胶结致密、非均质性强等特点,系统梳理了细粒岩概念和分类方法,结合岩石薄片鉴定、全岩X射线衍射、电镜能谱等实验,开展了三塘湖盆地芦草沟组细粒岩岩石学特征、储集空间类型及储集空间成因分析。结果表明,芦草沟组细粒岩储集层岩石以细粒碳酸盐岩类和细粒火山碎屑岩类为主;储集空间主要为裂缝和孔隙,裂缝以构造缝和层间缝为主,细粒火山碎屑岩类显孔普遍较发育,主要有火山尘溶孔、岩屑溶孔、晶屑溶孔和方解石脉溶孔;细粒碳酸盐岩类显孔不发育,微纳米孔较发育,主要为白云石晶间孔、方解石晶间孔、黏土矿物晶间孔等;火山物质富集是火山活动发育层系细粒岩储集性能好的物质基础,多种细粒岩纹层交互发育有利于微孔—微裂缝储集空间形成。
中图分类号:
秦恩鹏, 张君莹, 张生兵, 刘俊田, 张小芹, 陈永慧. 三塘湖盆地芦草沟组细粒岩储集层微观特征[J]. 新疆石油地质, 2023, 44(3): 299-306.
QIN Enpeng, ZHANG Junying, ZHANG Shengbing, LIU Juntian, ZHANG Xiaoqin, CHEN Yonghui. Microscopic Characteristics of Fine-Grained Reservoirs in Lucaogou Formation, Santanghu Basin[J]. Xinjiang Petroleum Geology, 2023, 44(3): 299-306.
图5
三塘湖盆地芦草沟组细粒岩储集层主要储集空间类型 a—构造缝,泥晶白云岩,条34井,3 290.31 m,单偏光;b—层间缝,泥—粉晶含石灰质白云岩,芦1井,3 046.08 m,单偏光;c—树枝状构造缝,泥晶白云岩,马804井,1 881.36 m,单偏光;d—树枝状构造缝,白云质泥岩,马804井,1 909.89 m,单偏光;e—方解石脉溶孔,含凝灰质粉—泥晶白云岩,马804井,1 923.67 m,单偏光;f—方解石脉溶孔、溶蚀缝,泥晶白云岩,马804井,1 918.78 m,单偏光;g—晶间溶孔、构造缝,泥质泥晶石灰质白云岩,芦1井,3 122.60 m,单偏光;h—火山尘溶孔、晶屑溶孔,蚀变火山尘晶屑凝灰岩,条3402H井,3 227.72 m,单偏光;i—脱玻化形成的石英、长石晶间孔,蚀变火山尘晶屑凝灰岩,条3402H井,3 227.72 m,扫描电镜"
图6
三塘湖盆地芦草沟组细粒岩储集层纹层交互特征 a—凝灰质纹层溶孔,蚀变火山尘凝灰岩与凝灰质泥晶白云岩纹层,马804井,1 918.47 m,单偏光;b—凝灰质纹层溶孔,蚀变火山尘凝灰岩与凝灰质泥晶白云岩纹层,马804井,1 918.47 m,正交偏光;c—碳酸盐纹层溶孔,泥晶白云岩中有机质纹层,条3402H井,3 144.03 m,单偏光;d—碳酸盐纹层溶孔,泥晶白云岩中有机质纹层,条3402H井,3 144.03 m,正交偏光;e—泥晶灰岩纹层与硅质纹层,泥晶灰岩,马708H井,2 214.92 m,单偏光;f—泥晶灰岩纹层与硅质纹层,泥晶灰岩,马708H井,2 214.92 m,正交偏光;g—裂缝中见有油质沥青,泥晶白云岩,条34井,3 290.31 m,荧光薄片;h—油质沥青聚集于层间微裂缝中,泥晶白云岩,马804井,1 881.36 m,荧光薄片"
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