塔中地区晚奥陶世碳酸盐台缘与台内沉积差异&mdash;&mdash;定性和定量的碳酸盐岩微相综合分析

付坤荣; 黄理力; 祝怡; 冯翔艺蓝; 章巧; 关小丽; 高达

doi:10.3969/j.issn.1000-0550.2018.012

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塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

付坤荣, 黄理力, 祝怡, 冯翔艺蓝, 章巧, 关小丽, 高达

文章导航 > 沉积学报 > 2018 > 36(1): 101-109

付坤荣, 黄理力, 祝怡, 冯翔艺蓝, 章巧, 关小丽, 高达. 塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析[J]. 沉积学报, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012

引用本文:

FU KunRong, HUANG LiLi, ZHU Yi, FENG XiangYiLan, ZHANG Qiao, GUAN XiaoLi, GAO Da. The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012

Citation:

FU KunRong, HUANG LiLi, ZHU Yi, FENG XiangYiLan, ZHANG Qiao, GUAN XiaoLi, GAO Da. The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012

引用本文:

Citation:

FU KunRong, HUANG LiLi, ZHU Yi, FENG XiangYiLan, ZHANG Qiao, GUAN XiaoLi, GAO Da. The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012

塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

1.
长江大学地球科学学院, 武汉 430100;
2.
中国地质大学(北京)地球科学与资源学院, 北京 100083;
3.
中国石油杭州地质研究院, 杭州 310023;
4.
中国地质大学(北京)能源学院, 北京 100083;
5.
长江大学沉积盆地研究中心, 武汉 430100

基金项目: 国家自然科学基金项目（41502104，41130422）；长江大学大学生创新创业计划项目（2015013）；长江大学长江青年基金项目（2015cqn30）

详细信息

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者:
高达,男,副教授,E-mail:gaoda18@gmail.com

中图分类号: P588.24⁺5

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文章访问数: 738
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The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

1.
School of Geosciences, Yangtze University, Wuhan 430100, China;
2.
School of Earth Science and Resources, China University of Geosciences(Beijing), Beijing 100083, China;
3.
PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;
4.
School of Energy Resources, China University of Geosciences(Beijing), Beijing 100083, China;
5.
Basin Analysis Center, Yangtze University, Wuhan 430100, China

Funds: National Natural Science Foundation of China, No. 41502104, 41130422;Program of Innovation and Entrepreneurship for Undergraduates, No. 2015013;the Yangtze Youth Fund, No.2015cqn30

摘要

摘要: 为揭示塔中地区东部的晚奥陶世镶边型碳酸盐台地边缘与台地内部的沉积差异，利用钻井岩芯及薄片资料，对良里塔格组开展了定性的和定量的碳酸盐岩微相分析研究。研究表明，台缘-台内沉积区发育9种微相类型（MF1~MF9），不同颗粒岩类微相所代表的几种颗粒滩具有典型差别的粒度累积频率曲线样式。台地边缘主要发育各种高能颗粒滩的微相组合（MF1~MF4），与台缘生物礁构成礁滩复合体；台地内部主要发育代表中-低能的潮坪-潟湖沉积的微相组合（MF5~MF9）。结合定量的粒度分析分析认为生屑砂屑颗粒灰岩微相（MF1）、生屑砾屑灰岩微相（MF2）和鲕粒颗粒灰岩微相（MF3）是冲流带（前滨）环境的产物，分别代表着台地边缘生屑滩、鲕粒滩和礁前砾屑滩沉积；球粒颗粒灰岩微相（MF5）为位于受障壁的台地内部、中等能量波浪控制的球粒滩；棘屑泥粒灰岩-漂浮岩微相（MF4）发育于台缘礁后的中-高能生屑滩。
- 碳酸盐岩微相 /
- 粒度分析 /
- 台地边缘 /
- 台地内部 /
- 颗粒滩 /
- 良里塔格组
Abstract: In order to reveal the deposition diversity between platform margin and platform interior on the Late Ordovician carbonate rimmed platform of Tazhong area, we made an integrated microfacies analysis from both qualitative and quantitative aspects by using core and thin section data of the Lianglitage Formation. The result show that nine types of microfacies (MF1~MF9) can be recognized, and each type of the grainstones which represents different type of carbonate sand shoals has distinct shape of grain-size accumulation curves. The platform margin is composed of several types of microfacies (MF1~MF4) indicating high-energy sand shoals that form reef-shoal complex together with platform margin reefs. The platform interior is composed of these types of microfacies (MF5~MF9) that representing medium-to low-energy lagoon and tidal flat deposits. Combining with the quantitative grain-size analysis results, these microfacies including bioclast intraclast grainstone (MF1), bioclast rudstone (MF2) and ooid grainstone (MF3) were deposited in foreshore environment, respectively indicating platform margin bioclast sand shoals, ooid sand shoals, and reef-front gravel shoals. The peloid grainstone (MF5) was deposited in the barrier platform interior that was dominated by moderate wave energy. The enchinoid packstone and floatstone (MF4) was deposited just at the back of platform reef forming bioclast sand shoal.
- carbonate microfacies analysis /
- grain-size analysis /
- platform margin /
- platform interior /
- carbonate sand shoal /
- Lianglitage Formation

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[1]	翁晓爱, 姜守一, 韩中, 胡修棉, 晏雄. 藏南Kioto碳酸盐台地对早侏罗世普林斯巴晚期碳循环扰动的沉积和生物响应 . 沉积学报, 2024, 42(2): 415-433. doi: 10.14027/j.issn.1000-0550.2023.078
[2]	芦飞凡, 谭秀成, 王利超, 唐青松, 肖笛, 董少峰, 苏成鹏, 潘政屹. 川中地区中二叠统栖霞组滩控岩溶型白云岩储层特征及主控因素 . 沉积学报, 2021, 39(2): 456-469. doi: 10.14027/j.issn.1000-0550.2020.020
[3]	马腾, 谭秀成, 李凌, 曾伟, 金民东, 罗冰, 洪海涛, 胡平. 四川盆地早寒武世龙王庙期沉积特征与古地理 . 沉积学报, 2016, 34(1): 33-48. doi: 10.14027/j.cnki.cjxb.2016.01.003
[4]	高达, 林畅松, 胡明毅, 黄理力. 利用自然伽马能谱测井识别碳酸盐岩高频层序——以塔里木盆地塔中地区T1井良里塔格组为例 . 沉积学报, 2016, 34(4): 707-715. doi: 10.14027/j.cnki.cjxb.2016.04.011
[5]	肖笛, 谭秀成, 山述娇, 彭浩, 陈虹宇, 万伟超, 熊鹰, 李顺. 四川盆地南部中二叠统茅口组二段沉积微相研究 . 沉积学报, 2015, 33(6): 1182-1191. doi: 10.14027/j.cnki.cjxb.2015.06.011
[6]	杨雪飞, 王兴志, 唐浩, 姜楠, 杨跃明, 谢继荣, 罗文军. 四川盆地中部磨溪地区龙王庙组沉积微相研究 . 沉积学报, 2015, 33(5): 972-982. doi: 10.14027/j.cnki.cjxb.2015.05.013
[7]	. 塔里木盆地奥陶系碳酸盐岩颗粒滩沉积组合及展布特征 . 沉积学报, 2014, 32(3): 418-428.
[8]	屈海洲, 王振宇, 张正红, 张云峰, 于红枫, 郑剑. 塔中地区晚奥陶世镶边台地沉积演化 . 沉积学报, 2014, 32(5): 823-831.
[9]	. 塔中地区良里塔格组台缘颗粒滩沉积特征及分布规律 . 沉积学报, 2014, 32(2): 354-364.
[10]	谭秀成. 陆表海碳酸盐岩台地沉积期微地貌恢复方法研究——以四川盆地磨溪气田嘉二2亚段A层为例 . 沉积学报, 2011, 29(3): 486-494.

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塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

1. 长江大学地球科学学院, 武汉 430100;

2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;

3. 中国石油杭州地质研究院, 杭州 310023;

4. 中国地质大学(北京)能源学院, 北京 100083;

5. 长江大学沉积盆地研究中心, 武汉 430100

基金项目: 国家自然科学基金项目（41502104，41130422）；长江大学大学生创新创业计划项目（2015013）；长江大学长江青年基金项目（2015cqn30）

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者: 高达,男,副教授,E-mail:gaoda18@gmail.com

收稿日期: 2016-11-10
修回日期: 2017-01-04
刊出日期: 2018-02-10

中图分类号: P588.24⁺5

关键词:

颗粒滩 /

摘要: 为揭示塔中地区东部的晚奥陶世镶边型碳酸盐台地边缘与台地内部的沉积差异，利用钻井岩芯及薄片资料，对良里塔格组开展了定性的和定量的碳酸盐岩微相分析研究。研究表明，台缘-台内沉积区发育9种微相类型（MF1~MF9），不同颗粒岩类微相所代表的几种颗粒滩具有典型差别的粒度累积频率曲线样式。台地边缘主要发育各种高能颗粒滩的微相组合（MF1~MF4），与台缘生物礁构成礁滩复合体；台地内部主要发育代表中-低能的潮坪-潟湖沉积的微相组合（MF5~MF9）。结合定量的粒度分析分析认为生屑砂屑颗粒灰岩微相（MF1）、生屑砾屑灰岩微相（MF2）和鲕粒颗粒灰岩微相（MF3）是冲流带（前滨）环境的产物，分别代表着台地边缘生屑滩、鲕粒滩和礁前砾屑滩沉积；球粒颗粒灰岩微相（MF5）为位于受障壁的台地内部、中等能量波浪控制的球粒滩；棘屑泥粒灰岩-漂浮岩微相（MF4）发育于台缘礁后的中-高能生屑滩。

English Abstract

The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

1. School of Geosciences, Yangtze University, Wuhan 430100, China;

2. School of Earth Science and Resources, China University of Geosciences(Beijing), Beijing 100083, China;

3. PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China;

4. School of Energy Resources, China University of Geosciences(Beijing), Beijing 100083, China;

5. Basin Analysis Center, Yangtze University, Wuhan 430100, China

Funds: National Natural Science Foundation of China, No. 41502104, 41130422;Program of Innovation and Entrepreneurship for Undergraduates, No. 2015013;the Yangtze Youth Fund, No.2015cqn30

Received Date: 2016-11-10
Rev Recd Date: 2017-01-04
Publish Date: 2018-02-10

Keywords:

Abstract: In order to reveal the deposition diversity between platform margin and platform interior on the Late Ordovician carbonate rimmed platform of Tazhong area, we made an integrated microfacies analysis from both qualitative and quantitative aspects by using core and thin section data of the Lianglitage Formation. The result show that nine types of microfacies (MF1~MF9) can be recognized, and each type of the grainstones which represents different type of carbonate sand shoals has distinct shape of grain-size accumulation curves. The platform margin is composed of several types of microfacies (MF1~MF4) indicating high-energy sand shoals that form reef-shoal complex together with platform margin reefs. The platform interior is composed of these types of microfacies (MF5~MF9) that representing medium-to low-energy lagoon and tidal flat deposits. Combining with the quantitative grain-size analysis results, these microfacies including bioclast intraclast grainstone (MF1), bioclast rudstone (MF2) and ooid grainstone (MF3) were deposited in foreshore environment, respectively indicating platform margin bioclast sand shoals, ooid sand shoals, and reef-front gravel shoals. The peloid grainstone (MF5) was deposited in the barrier platform interior that was dominated by moderate wave energy. The enchinoid packstone and floatstone (MF4) was deposited just at the back of platform reef forming bioclast sand shoal.

引用本文:

Citation:

FU KunRong, HUANG LiLi, ZHU Yi, FENG XiangYiLan, ZHANG Qiao, GUAN XiaoLi, GAO Da. The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis[J]. Acta Sedimentologica Sinica, 2018, 36(1): 101-109. doi: 10.3969/j.issn.1000-0550.2018.012

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塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者:
高达,男,副教授,E-mail:gaoda18@gmail.com

计量

The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

计量

目录

塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

1. 长江大学地球科学学院, 武汉 430100;

2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;

3. 中国石油杭州地质研究院, 杭州 310023;

4. 中国地质大学(北京)能源学院, 北京 100083;

5. 长江大学沉积盆地研究中心, 武汉 430100

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者: 高达,男,副教授,E-mail:gaoda18@gmail.com

English Abstract

The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

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塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

作者简介: 付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者: 高达,男,副教授,E-mail:gaoda18@gmail.com

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The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

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出版历程

目录

塔中地区晚奥陶世碳酸盐台缘与台内沉积差异——定性和定量的碳酸盐岩微相综合分析

doi: 10.3969/j.issn.1000-0550.2018.012

1. 长江大学地球科学学院, 武汉 430100; 2. 中国地质大学(北京)地球科学与资源学院, 北京 100083; 3. 中国石油杭州地质研究院, 杭州 310023; 4. 中国地质大学(北京)能源学院, 北京 100083; 5. 长江大学沉积盆地研究中心, 武汉 430100

作者简介: 付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者: 高达,男,副教授,E-mail:gaoda18@gmail.com

English Abstract

The Depositional Diversity between Platform Margin and Platform Interior on the Late Ordovician Carbonate Rimmed-platform of Tazhong Area: A case study of qualitative and quantitative integrated microfacies analysis

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com

通讯作者:
高达,男,副教授,E-mail:gaoda18@gmail.com

1. 长江大学地球科学学院, 武汉 430100;

2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;

3. 中国石油杭州地质研究院, 杭州 310023;

4. 中国地质大学(北京)能源学院, 北京 100083;

5. 长江大学沉积盆地研究中心, 武汉 430100

作者简介:
付坤荣,男,1995年出生,硕士研究生,构造地质学,E-mail:1024359968@qq.com