碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律&mdash;&mdash;以豫西奥陶系马家沟组三段为例

胡亚洲; 牛永斌; 崔胜利; 董小波

doi:10.14027/j.issn.1000-0550.2018.172

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碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

胡亚洲, 牛永斌, 崔胜利, 董小波

文章导航 > 沉积学报 > 2019 > 37(4): 690-701

胡亚洲, 牛永斌, 崔胜利, 董小波. 碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例[J]. 沉积学报, 2019, 37(4): 690-701. doi: 10.14027/j.issn.1000-0550.2018.172

引用本文:

HU YaZhou, NIU YongBin, CUI ShengLi, DONG XiaoBo. Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province[J]. Acta Sedimentologica Sinica, 2019, 37(4): 690-701. doi: 10.14027/j.issn.1000-0550.2018.172

Citation:

HU YaZhou, NIU YongBin, CUI ShengLi, DONG XiaoBo. Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province[J]. Acta Sedimentologica Sinica, 2019, 37(4): 690-701. doi: 10.14027/j.issn.1000-0550.2018.172

引用本文:

Citation:

HU YaZhou, NIU YongBin, CUI ShengLi, DONG XiaoBo. Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province[J]. Acta Sedimentologica Sinica, 2019, 37(4): 690-701. doi: 10.14027/j.issn.1000-0550.2018.172

碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

1.
河南理工大学资源环境学院, 河南焦作 454003;
2.
西北大学地质学系, 西安 710069;
3.
河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003

基金项目: 国家自然科学基金项目（41102076，41472104）；河南理工大学创新科研团队项目（17IRTSTHN025）

详细信息

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者:
牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

中图分类号: Q913;P618.13

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文章访问数: 545
HTML全文浏览量: 21
PDF下载量: 158
被引次数: 0

Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

1.
Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China;
2.
Department of Geology, Northwest University, Xi'an 710069, China;
3.
Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China

Funds: National Natural Sci-ence Foundation of China, No.41102076, 41472104; The Program for Innovative Research Team (in Science and Technology) in University of Henan Province, No. 17IRTSTHN025

摘要

摘要: 豫西奥陶系马家沟组三段碳酸盐岩中生物潜穴十分发育。在野外露头实地观测的基础上，利用偏光显微镜、阴极发光显微镜及扫描电镜对研究区碳酸盐岩中生物潜穴的充填特征及其诱导孔隙演化规律进行了研究。结果表明：1）研究区奥陶系碳酸盐岩中生物潜穴多呈全充填和半充填，潜穴充填物主要以白云石和方解石为主，局部生物潜穴呈现未充填状态；2）生物潜穴诱导发育的孔隙，主要有溶蚀孔隙、微裂隙两种类型，在生物潜穴与围岩两者的交界处尤为发育；3）生物潜穴孔隙的发育主要受埋藏白云化作用与海西早期和印支期以来的表生溶蚀作用的影响，浅埋藏白云化作用对晶间孔隙起到促进作用，海西早期的表生溶蚀形成了潜穴中大部分的溶蚀孔隙；4）生物潜穴的选择性溶蚀主要受潜穴中白云石充填物结晶程度的影响，宏观上的选择性溶蚀可划分为四个阶段，微观上的选择性溶蚀主要是粒间孔在流体的作用下逐渐扩大所形成。
- 生物潜穴 /
- 孔隙演化 /
- 碳酸盐岩 /
- 马家沟组 /
- 奥陶系
Abstract: Numerous burrows occur in the third member of the Ordovician Majiagou Formation in western Henan Province. A study of the filling characteristics of burrows and the evolution of burrow-mediated pores was conducted on burrow-fills in the research area,based on the observation of outcrops together with polarizing optical microscope, cathodoluminescence microscope and scanning electron microscope. The results showed that macro-scale selective dissolution occurred in four stages. (1) Burrows are almost all either fully filled or semi-filled,mostly with calcite or dolomite;occasional burrows are unfilled. (2) Burrow-mediated pores occur commonly,consisting of dissolution pores and micro-cracks,mainly around the burrow boundary. (3) Burrow-mediated pores were controlled by burial dolomitization and dissolution in the early Hercynian cycle and Indo-Chinese epoch. Most of the dissolution pores were formed in the Hercynian period. (4) Burrow-mediated selective dissolution depends on the degree of crystalliza-tion of the dolomite in the burrow-fills. Micro-dissolution pore formation is influenced by the presence of fluids.
- burrows /
- pore evolution /
- carbonate rocks /
- Majiagou Formation /
- Ordovician

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[1]	张显坤, 何幼斌, 李华, 何一鸣, 姜纯伟, 吴吉泽, 姚凤南. 深水斜坡背景下的重力流水道-朵叶体系沉积特征及演化——以内蒙古乌海市奥陶系拉什仲组三段露头为例 . 沉积学报, 2025, (): -. doi: 10.14027/j.issn.1000-0550.2025.009
[2]	王炳森. 川中蓬莱地区震旦系灯影组四段储层成岩作用、孔隙演化及油气充注 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.012
[3]	党文龙, 高岗, 刘建平, 刚文哲, 王成云, 杨尚儒, 雷宇, 张莉莉, 段延娟. 鄂尔多斯盆地马家沟组烃源岩受石炭系充填影响的研究 . 沉积学报, 2023, 41(3): 879-889. doi: 10.14027/j.issn.1000-0550.2021.133
[4]	赵佳如, 牛永斌, 王敏, 徐资璐, 崔胜利, 王培俊. 塔河油田奥陶系生物扰动型碳酸盐岩储集层特征及其孔隙度计算样本检验模型 . 沉积学报, 2021, 39(2): 482-492. doi: 10.14027/j.issn.1000-0550.2020.023
[5]	谭飞, 张云峰, 王振宇, 董兆雄, 黄正良, 王前平, 高君微. 鄂尔多斯盆地奥陶系不同组构碳酸盐岩埋藏溶蚀实验 . 沉积学报, 2017, 35(2): 413-424. doi: 10.14027/j.cnki.cjxb.2017.02.018
[6]	牛永斌, 单婷婷, 董小波, 周硕, 高文秀. 豫西北奥陶系马家沟组遗迹化石及其沉积环境 . 沉积学报, 2015, 33(2): 211-225. doi: 10.14027/j.cnki.cjxb.2015.02.001
[7]	姚泾利. 鄂尔多斯盆地下奥陶统马家沟组马五段白云岩的地球化学特征 . 沉积学报, 2009, 27(3): 381-389.
[8]	陈景山. 塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布 . 沉积学报, 2007, 25(6): 858-868.
[9]	朱创业. 陕甘宁盆地下奥陶统马家沟组层序沉积有机相特征及其烃源岩分布 . 沉积学报, 2000, 18(1): 57-62.
[10]	高永丰, 魏瑞华. 吕梁－陕北地区马家沟组中小层序特征及其成因 . 沉积学报, 1995, 13(3): 32-38.

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碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

1. 河南理工大学资源环境学院, 河南焦作 454003;

2. 西北大学地质学系, 西安 710069;

3. 河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003

基金项目: 国家自然科学基金项目（41102076，41472104）；河南理工大学创新科研团队项目（17IRTSTHN025）

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者: 牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

收稿日期: 2018-07-26
修回日期: 2018-09-25
刊出日期: 2019-08-10

中图分类号: Q913;P618.13

关键词:

摘要: 豫西奥陶系马家沟组三段碳酸盐岩中生物潜穴十分发育。在野外露头实地观测的基础上，利用偏光显微镜、阴极发光显微镜及扫描电镜对研究区碳酸盐岩中生物潜穴的充填特征及其诱导孔隙演化规律进行了研究。结果表明：1）研究区奥陶系碳酸盐岩中生物潜穴多呈全充填和半充填，潜穴充填物主要以白云石和方解石为主，局部生物潜穴呈现未充填状态；2）生物潜穴诱导发育的孔隙，主要有溶蚀孔隙、微裂隙两种类型，在生物潜穴与围岩两者的交界处尤为发育；3）生物潜穴孔隙的发育主要受埋藏白云化作用与海西早期和印支期以来的表生溶蚀作用的影响，浅埋藏白云化作用对晶间孔隙起到促进作用，海西早期的表生溶蚀形成了潜穴中大部分的溶蚀孔隙；4）生物潜穴的选择性溶蚀主要受潜穴中白云石充填物结晶程度的影响，宏观上的选择性溶蚀可划分为四个阶段，微观上的选择性溶蚀主要是粒间孔在流体的作用下逐渐扩大所形成。

English Abstract

Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China;

2. Department of Geology, Northwest University, Xi'an 710069, China;

3. Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China

Funds: National Natural Sci-ence Foundation of China, No.41102076, 41472104; The Program for Innovative Research Team (in Science and Technology) in University of Henan Province, No. 17IRTSTHN025

Received Date: 2018-07-26
Rev Recd Date: 2018-09-25
Publish Date: 2019-08-10

Keywords:

Abstract: Numerous burrows occur in the third member of the Ordovician Majiagou Formation in western Henan Province. A study of the filling characteristics of burrows and the evolution of burrow-mediated pores was conducted on burrow-fills in the research area,based on the observation of outcrops together with polarizing optical microscope, cathodoluminescence microscope and scanning electron microscope. The results showed that macro-scale selective dissolution occurred in four stages. (1) Burrows are almost all either fully filled or semi-filled,mostly with calcite or dolomite;occasional burrows are unfilled. (2) Burrow-mediated pores occur commonly,consisting of dissolution pores and micro-cracks,mainly around the burrow boundary. (3) Burrow-mediated pores were controlled by burial dolomitization and dissolution in the early Hercynian cycle and Indo-Chinese epoch. Most of the dissolution pores were formed in the Hercynian period. (4) Burrow-mediated selective dissolution depends on the degree of crystalliza-tion of the dolomite in the burrow-fills. Micro-dissolution pore formation is influenced by the presence of fluids.

引用本文:

Citation:

HU YaZhou, NIU YongBin, CUI ShengLi, DONG XiaoBo. Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province[J]. Acta Sedimentologica Sinica, 2019, 37(4): 690-701. doi: 10.14027/j.issn.1000-0550.2018.172

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碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者:
牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

计量

Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

计量

目录

碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

1. 河南理工大学资源环境学院, 河南焦作 454003;

2. 西北大学地质学系, 西安 710069;

3. 河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者: 牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

English Abstract

Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China;

2. Department of Geology, Northwest University, Xi'an 710069, China;

3. Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China

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碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

作者简介: 胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者: 牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

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Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

计量

出版历程

目录

碳酸盐岩中生物潜穴充填特征及其诱导孔隙演化规律——以豫西奥陶系马家沟组三段为例

doi: 10.14027/j.issn.1000-0550.2018.172

1. 河南理工大学资源环境学院, 河南焦作 454003; 2. 西北大学地质学系, 西安 710069; 3. 河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003

作者简介: 胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者: 牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

English Abstract

Characteristics of Filled Burrows in Carbonates and the Evolution of Burrow-mediated Pores: A case study from the third member of the Ordovician Majiagou Formation, western Henan province

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China; 2. Department of Geology, Northwest University, Xi'an 710069, China; 3. Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China

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期刊在线

联系我们

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

通讯作者:
牛永斌,男,副教授,E-mail:niuyongbin@hpu.edu.cn

1. 河南理工大学资源环境学院, 河南焦作 454003;

2. 西北大学地质学系, 西安 710069;

3. 河南省生物遗迹与成矿过程重点实验室, 河南焦作 454003

作者简介:
胡亚洲,男,1992年生,博士研究生,沉积学和遗迹学,E-mail:15538903514@163.com

1. Institute of Resources and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China;

2. Department of Geology, Northwest University, Xi'an 710069, China;

3. Key Laboratory of Biogenic Traces and Sedimentary Minerals of Henan Province, Jiaozuo, Henan 454003, China