鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

张天付

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鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

张天付

文章导航 > 沉积学报 > 2009 > 27(6): 1033-1042

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

引用本文:

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

Citation:

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

引用本文:

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

Citation:

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

张天付

中国石油杭州地质研究院杭州310023

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通讯作者:
张天付

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Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

ZHANG Tianfu

Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou310023

More Information

Corresponding author: ZHANG Tianfu

摘要

摘要: 鲕粒灰岩是重要的碳酸盐岩油气储层。通过常温常压下，北京西山鲕粒灰岩的溶解动力学实验发现，鲕粒灰岩的溶解主要受岩石和矿物的结构和化学成分控制。结构上表现为构造裂缝、鲕粒结合纹、颗粒晶体结合带等结构薄弱带优先发生溶蚀。成分上表现为白云岩化组分不仅自身较易溶蚀，而且能促进鲕粒灰岩的整体溶解；粘土矿物、石英等杂质组分常与鲕粒和白云岩化颗粒伴生，其对两者的阻溶效应更大。溶解过程中，鲕粒灰岩的构造裂隙、鲕粒放射结合纹和同心圈层等首先发生溶蚀，产生溶隙、粒内溶孔和粒间溶孔；其次为白云质组分以及白云质组分与方解石结合处而产生晶间溶孔、粒内溶孔；随着溶蚀强度的加强，围绕鲕粒形成环状溶蚀沟，在鲕粒溶蚀脱落后而形成鲕模孔。
- 鲕粒灰岩储层溶解动力学形貌演化
Abstract: Oolitic limestone is an crucial oil reservoir. Through dissolution kinetics experiment under normal temperature and pressure, this paper discussed dissolution kinetics characteristics and morphology evolution of oolitic limestone. The result indicates that oolitic limestone dissolution is main controlled by petrotextural features and chemical composition. Petrotextural feature control is characterized by selective dissolving textural weakness, such as tectonic microfracture, crack in ooid especially oolitic radiate crack, binding domain between grains and crystals and so on. Chemical composition control is characterized by prior dissolution of dolomitized particles and inhabitations of clay mineral and quartz. To dolomitized particles, they not only dissolve easer itself, but also could accelerate rock dissolution. However, to clay mineral and quartz, their inhabitations are more harmful to ooids and dolomitized particles' dissolution than to substrate. During oolitic limestone dissolution, firstly, it brought dissolved crack, intergranular pore, intercrystalliine pore after tectonic microfracture and crack in ooid. Secondly, it led to interpartide pore and intercrystalliine pore with dolomitized particles and calcite around them dissolved. Then, along with further dissolution, annular channel could be formed around ooids. Finally, it would form oolitic moldic pore in surface after ooids fell off substrate.
- oolitic limestone

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[1]	李忠. 沉积盆地深层—超深层成岩动力学：若干研究进展与专属问题 . 沉积学报, 2023, 41(6): 1768-1780. doi: 10.14027/j.issn.1000-0550.2023.089
[2]	黄军平, 杨田, 张艳, 李相博, 董岐石, 杨占龙, 郑泽宇. 湖相细粒沉积岩沉积动力学机制与沉积模式 . 沉积学报, 2023, 41(4): 1227-1239. doi: 10.14027/j.issn.1000-0550.2022.041
[3]	吕大炜, 初航, 任建国. 沉积学和盆地动力学现状及发展动态简析 . 沉积学报, 2022, 40(2): 281-291. doi: 10.14027/j.issn.1000-0550.2021.155
[4]	伍坤宇, 熊鹰, 谭秀成, 刘向君, 张云峰, 陈晓冬, 李亚锋, 郭荣涛, 曹喆, 王鹏. 储层孔隙系统“水—岩”反应结晶动力学研究进展 . 沉积学报, 2022, 40(4): 996-1009. doi: 10.14027/j.issn.1000-0550.2021.029
[5]	古强, 邢凤存, 钱红杉, 孙汉骁. 川东北飞仙关组鲕粒特征与水动力相关性研究 . 沉积学报, 2021, 39(6): 1371-1386. doi: 10.14027/j.issn.1000-0550.2021.059
[6]	蒋裕强, 何沅翰, 邢凤存, 谷一凡, 蒋婵. 下三叠统鲕粒灰岩中微生物矿化组构特征及意义——以川东北地区飞仙关组为例 . 沉积学报, 2019, 37(2): 268-277. doi: 10.14027/j.issn.1000-0550.2018.132
[7]	. 煤岩、泥岩密闭体系下热解产物特征及动力学分析 . 沉积学报, 2011, 29(6): 1190-1198.
[8]	王恕一. 川东北普光气田鲕粒白云岩储层粒内溶孔的成因 . 沉积学报, 2010, 28(1): 10-16.
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鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

张天付

中国石油杭州地质研究院杭州310023

通讯作者: 张天付

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2009-12-10

关键词:

鲕粒灰岩储层溶解动力学形貌演化

摘要: 鲕粒灰岩是重要的碳酸盐岩油气储层。通过常温常压下，北京西山鲕粒灰岩的溶解动力学实验发现，鲕粒灰岩的溶解主要受岩石和矿物的结构和化学成分控制。结构上表现为构造裂缝、鲕粒结合纹、颗粒晶体结合带等结构薄弱带优先发生溶蚀。成分上表现为白云岩化组分不仅自身较易溶蚀，而且能促进鲕粒灰岩的整体溶解；粘土矿物、石英等杂质组分常与鲕粒和白云岩化颗粒伴生，其对两者的阻溶效应更大。溶解过程中，鲕粒灰岩的构造裂隙、鲕粒放射结合纹和同心圈层等首先发生溶蚀，产生溶隙、粒内溶孔和粒间溶孔；其次为白云质组分以及白云质组分与方解石结合处而产生晶间溶孔、粒内溶孔；随着溶蚀强度的加强，围绕鲕粒形成环状溶蚀沟，在鲕粒溶蚀脱落后而形成鲕模孔。

English Abstract

Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

ZHANG Tianfu

Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou310023

Corresponding author: ZHANG Tianfu

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2009-12-10

Keywords:

oolitic limestone

Abstract: Oolitic limestone is an crucial oil reservoir. Through dissolution kinetics experiment under normal temperature and pressure, this paper discussed dissolution kinetics characteristics and morphology evolution of oolitic limestone. The result indicates that oolitic limestone dissolution is main controlled by petrotextural features and chemical composition. Petrotextural feature control is characterized by selective dissolving textural weakness, such as tectonic microfracture, crack in ooid especially oolitic radiate crack, binding domain between grains and crystals and so on. Chemical composition control is characterized by prior dissolution of dolomitized particles and inhabitations of clay mineral and quartz. To dolomitized particles, they not only dissolve easer itself, but also could accelerate rock dissolution. However, to clay mineral and quartz, their inhabitations are more harmful to ooids and dolomitized particles' dissolution than to substrate. During oolitic limestone dissolution, firstly, it brought dissolved crack, intergranular pore, intercrystalliine pore after tectonic microfracture and crack in ooid. Secondly, it led to interpartide pore and intercrystalliine pore with dolomitized particles and calcite around them dissolved. Then, along with further dissolution, annular channel could be formed around ooids. Finally, it would form oolitic moldic pore in surface after ooids fell off substrate.

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

引用本文:

张天付. 鲕粒灰岩的溶解动力学特征和微观形貌的发育演化[J]. 沉积学报, 2009, 27(6): 1033-1042.

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

Citation:

ZHANG Tianfu. Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1033-1042.

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鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

通讯作者:
张天付

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Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

Corresponding author: ZHANG Tianfu

计量

目录

鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

中国石油杭州地质研究院杭州310023

通讯作者: 张天付

English Abstract

Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou310023

Corresponding author: ZHANG Tianfu

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鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

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Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

Corresponding author: ZHANG Tianfu

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出版历程

目录

鲕粒灰岩的溶解动力学特征和微观形貌的发育演化

中国石油杭州地质研究院杭州310023

通讯作者: 张天付

English Abstract

Dissolution Kinetic Characteristics and Morphology Evolution of Oolitic Limestone

Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou310023

Corresponding author: ZHANG Tianfu

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