砂岩中碱性溶蚀研究进展

田建锋; 喻建; 张志国

doi:10.19509/j.cnki.dzkq.2022.0195

砂岩中碱性溶蚀研究进展

doi: 10.19509/j.cnki.dzkq.2022.0195

田建锋^{1a, 1b,},
喻建²,
张志国³

1a.
西安石油大学地球科学与工程学院，西安 710065
1b.
西安石油大学陕西省油气成藏地质学重点实验室，西安 710065
2.
中国石油长庆油田分公司，西安 710018
3.
中国石油长庆油田分公司第三采油厂，银川 750006

基金项目:

国家自然科学基金项目 41202105

国家自然科学基金项目 41772140

详细信息

作者简介:
田建锋(1980—), 男, 副教授, 主要从事储层地质学方面的教学和科研工作。E-mail: tjf21991@xsyu.edu.cn

中图分类号: P618.1
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- 文章访问数: 699
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- 被引次数: 0
出版历程
- 收稿日期: 2022-03-08
- 网络出版日期: 2022-11-10

Advance in alkaline dissolution of sandstone

1a.
School of Earth Sciences and Engineering, Xi′an Shiyou University, Xi′an 710065, China
1b.
Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi′an Shiyou University, Xi′an 710065, China
2.
PetroChina Changqing Oilfield Company, Xi′an 710018, China
3.
No.3 Oil Producing Plant, PetroChina Changqing Oilfield Company, Yinchuan 750006, China

摘要

摘要:
火山物质和长石碱性溶蚀形成的绿泥石、浊沸石、钠长石、伊利石等碱性自生矿物，是砂岩储层研究的重点，而碱性溶蚀本身却常被忽略。通过对碱性溶蚀机理、控制因素及成岩特征的分析，发现砂岩中发育石英颗粒碱性溶蚀、火山物质水解溶蚀、蒙脱石伊利石化导致的钾长石溶蚀、高岭石伊利石化导致的钾长石溶蚀和斜长石钠长石化5种碱性溶蚀作用，它们常与酸性溶蚀先后叠加发生，不易直接确定碱性溶蚀的类型和规模，常被忽略或误判为酸性溶蚀。依据碱性溶蚀与其伴生胶结物的成因关系，分析了部分含油气储层的碱性溶蚀类型及溶蚀规模，我国含油气盆地碱性溶蚀十分普遍，前4种碱性溶蚀形成的次生孔隙分别可达2%~7%, 5%~10%, 1.32%, 1.63%。
- 碱性溶蚀 /
- 成岩作用 /
- 次生孔隙 /
- 火山物质水解 /
- 蒙脱石伊利石化
Abstract:
Alkaline authigenic minerals such as chlorite, laumontite, albite, and illite formed by alkaline dissolution of volcanic materials and feldspar are the focus of sandstone reservoir research, but alkaline dissolution itself is often ignored. Through analysis of the alkaline dissolution mechanism, controlling factors and diagenetic characteristics, it is found that alkaline dissolution includes five types: alkaline dissolution of quartz grains, hydrolysis and dissolution of volcanic materials, K-feldspar dissolution caused by illitization of montmorillonite, K-feldspar dissolution caused by illitization of kaolinite, and albitization of plagioclase. As alkaline dissolution is often superimposed with acid dissolution, it is difficult to directly determine the type and scale of alkaline dissolution and is often ignored or misjudged as acid dissolution. Based on the genetic relationship between alkaline dissolution and its associated cements, the type and scale of alkaline dissolution of some sandstone reservoirs are analyzed. Alkaline dissolution is very common in the petroliferous basin of China, and the secondary pores formed by the first four kinds of alkaline dissolution can reach 2%-7%, 5%-10%, 1.32% and 1.63%, respectively.
- alkaline dissolution /
- diagenesis /
- secondary porosity /
- hydrolysis of volcanic materials /
- illitization of montmorillonite

HTML全文

图 1 砂岩碱性溶蚀微观特征

A.石英颗粒表面溶蚀呈雨滴状^[33]；B.石英加大受绿泥石包膜影响呈不规则状，鄂尔多斯盆地陕北地区塞261井长6；C.火山物质溶蚀呈球状、港湾状，鄂尔多斯盆地姬塬地区盐130井长9；D.钾长石溶蚀呈铸模孔，鄂尔多斯盆地合水地区庄185井长7；E.钾长石溶蚀和不规则片状I-S混层，鄂尔多斯盆地合水地区里180井长7；F.高岭石伊利石化形成的纤维状伊利石^[38]；G.斜长石溶蚀孔内充填自生钠长石，鄂尔多斯盆地镇北地区镇492-45井长8；H.斜长石钠长石化和浊沸石胶结，鄂尔多斯盆地陕北地区王516井长9

Figure 1. Microscopic characteristics of alkaline dissolution in sandstone

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表 1 砂岩中碱性溶蚀与有机酸侵入酸性溶蚀特征对比

Table 1. Correlation of characteristics of alkaline dissolution and organic acid dissolution in sandstone

类型	火山物质水解	斜长石钠长石化	蒙脱石伊利石化	高岭石伊利石化	石英颗粒碱性溶蚀	有机酸
代表岩性	富火山碎屑砂岩	长石砂岩	泥质砂岩、泥岩所夹砂岩	前期酸性溶蚀发育砂岩	盐碱湖沉积砂岩	煤系地层中的长石砂岩、岩屑砂岩
pH值	升高	升高	升高	不变	降低	升高
主要温度区间	>40℃	70~110℃	60~100℃	120~140℃	65~85℃	80~120℃
被溶蚀物	火山物质	斜长石	钾长石(蒙脱石)	高岭石、钾长石	石英	岩屑、长石、沸石、碳酸盐
伴生胶结	绿泥石、浊沸石、石英	浊沸石、钠长石、方解石	伊利石、石英、钠长石、方解石		—	高岭石、石英
典型代表区	鄂尔多斯盆地延长组、准噶尔盆地二叠系	鄂尔多斯盆地陕北长6	鄂尔多斯盆地合水长7	北海和挪威大陆架侏罗系	泌阳凹陷核桃园组	鄂尔多斯盆地延安组
溶蚀规模	5%~10%	?	1.32%	1.63%	2%~7%	1%~6%

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