浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

郭福生

浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

郭福生^1,2

1.
东华理工学院地球科学系江西抚州 344000;
2.
中国地质大学北京 100083

基金项目: 江西省重点学科“地质工程”基金资助项目;国防科工委重点专业“资源勘查工程”建设基金资助项目

详细信息

作者简介:
郭福生,男,1962年出生,教授,沉积学与区域地质

中图分类号: P588.2

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Characteristics and Tectonic Significance of Mixing Sediments of Siliciclastics and Carbonate of Outangdi Formation in Jiangshan, Zhejiang Province

GUO Fu sheng^1,2

1.
East China Instituteof Technology,Fuzhou, Jiangxi 344000;
2.
China University of Geosciences, Beijing 100083

摘要

摘要: 浙江江山藕塘底组是晚石炭世威宁期陆源碎屑与碳酸盐的混合沉积,包括两种组分在同一岩层内相互混杂形成混积岩和陆源碎屑岩与碳酸盐岩互层形成混积层系。藕塘底组是海陆交互环境的沉积产物,剖面结构具有下细上粗的岸进序列。混积岩形成于滨岸浅滩环境,由沿岸流和回流将河口或滨岸海滩的石英砂带到滨岸浅滩和潮坪相碳酸盐沉积区混杂而成。具两种混积层系类型,即浅海滨岸环境中砂岩与碳酸盐岩互层、河流相碎屑岩与海相碳酸盐岩互层。研究表明,混合沉积成因属“相混合”,主要受区域构造隆升、全球海平面上升和盆地水介质条件特性控制。区域海平面周期性变化和岸进序列可能是华夏古陆强烈隆起的结果。作者还讨论了混合沉积的分类和命名,将陆源碎屑与碳酸盐层相互交替构成的互层和夹层组合称为“混积层系”,并建议将“混积岩”一词用来表征两种组分相互混杂这种特殊沉积事件,而不用作具体岩石名称.
- 藕塘底组 /
- 混合沉积 /
- 混积岩 /
- 混积层系 /
- 石炭系 /
- 沉积环境 /
- 构造隆升
Abstract: Outangdi Formation in Jiangshan, Zhejiang is the mixing deposits of terrigenous clastics and carbonatein Weiningian of late 2 Carboniferous. The mixing deposits include the interbedding which constitutes a series of in 2terbedded clastic beds and carbonate beds and the mixing within in the same bed which forms the ” Hunji rock ”.Outangdi Formation has the features of intercalated marine and terrestrial deposits with the progradational se 2quences with lower fine and upper coarse of sedimentary granularity in the section. Hunji rock isformed in seashoreenvironment, mixed carbonate sediment in beach or tideland facies with quartz sand taken from bayou or beach bycoastwise flow and circumfluence. There are two kinds of Hunji sequences: interbeds of sandstone and carbonaterock in seashore environment, interbeds of clastics in river facies and carbonate rock in ocean facies. It is indicatedthat mixing deposition belong to ” facies mixing ”, affected mainly by regional toctonic uplift, rise of global sea leveland dynamics of water medium in the basin. Regional sea level periodic change and progradational sequences wereprobably due to intense uplift of the oldland called Cathaysia. The classification and name of mixed sediments arealso discussed in this paper. Interbeds and alternated beds of clastic and carbonate beds are named as ” hunji se 2quence ”, a new genetic term. It is suggested that Hunji rock means a special sedimentary event of mixing of ter 2rigenous clastics and carbonate instead of a term of specific rock.
- Outangdi Formation /
- mixing deposits /
- Hunji rock /
- Hunji sequence /
- carboniferous /
- sedimentary en-vironment /
- tectonic uplift

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参考文献(33)

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浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

作者简介:
郭福生,男,1962年出生,教授,沉积学与区域地质

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Characteristics and Tectonic Significance of Mixing Sediments of Siliciclastics and Carbonate of Outangdi Formation in Jiangshan, Zhejiang Province

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浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

1. 东华理工学院地球科学系江西抚州 344000;

2. 中国地质大学北京 100083

作者简介:
郭福生,男,1962年出生,教授,沉积学与区域地质

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Characteristics and Tectonic Significance of Mixing Sediments of Siliciclastics and Carbonate of Outangdi Formation in Jiangshan, Zhejiang Province

1. East China Instituteof Technology,Fuzhou, Jiangxi 344000;

2. China University of Geosciences, Beijing 100083

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浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

作者简介: 郭福生,男,1962年出生,教授,沉积学与区域地质

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Characteristics and Tectonic Significance of Mixing Sediments of Siliciclastics and Carbonate of Outangdi Formation in Jiangshan, Zhejiang Province

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浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义

1. 东华理工学院地球科学系 江西抚州 344000; 2. 中国地质大学 北京 100083

作者简介: 郭福生,男,1962年出生,教授,沉积学与区域地质

English Abstract

Characteristics and Tectonic Significance of Mixing Sediments of Siliciclastics and Carbonate of Outangdi Formation in Jiangshan, Zhejiang Province

1. East China Instituteof Technology,Fuzhou, Jiangxi 344000; 2. China University of Geosciences, Beijing 100083

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作者简介:
郭福生,男,1962年出生,教授,沉积学与区域地质

1. 东华理工学院地球科学系江西抚州 344000;

2. 中国地质大学北京 100083

作者简介:
郭福生,男,1962年出生,教授,沉积学与区域地质

1. East China Instituteof Technology,Fuzhou, Jiangxi 344000;

2. China University of Geosciences, Beijing 100083