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

计量

文章访问数: 648
HTML全文浏览量: 8
PDF下载量: 558
被引次数: 0

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

HTML全文

参考文献(33)

[1]	[
[2]	张锦泉,叶红专.论碳酸盐与陆源碎屑的混合沉积.成都地质学院学报,1989,16(2):87～92[Zhang Jinquan and Ye Hongzhuan. Study on carbonate and siliciclastic mixed sediments. Journal college of Chengdu of Geology,1989,16(2): 87～92]
[3]	杨朝青,沙庆安.云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积.沉积学报,1990,8(2):59～66[Yang Chaoqing and Sha Qingan. Sedimentary environment of the middle Devonian Qujiang formation, a kind of mixing sedimentation of terrigenous clastics and carbonate.Acta Sedimentologica Sinica,1990,8(2):59～66]
[4]	张雄华. 混积岩的分类和成因.地质科技情报,2000,19(4):31～34[Zhang Xonghua. Classification and origin of mixosedimentite. Ge0logical Science and Technology Ingormation,2000,19(4):31～34]
[5]	沙庆安. 混合沉积和混积岩的讨论.古地理学报,2001,3(3):63～66[Sha Qingan. Discussion on mixing deposit and Hunji rock. Journal of Palaeogeography,2001,3(3):63～66]
[6]	王国忠. 南海北部大陆架现代礁源碳酸盐与陆源碎屑的混合沉积作用.古地理学报,2001,3(2):47～54[Wang Guozhong. Mixed sedimentation of recent reefoid carbonates and terrigenous clastics in the North continental shelf of the South China sea. Journal of Palaeogeography,2001,3(2):47～54]
[7]	Zuff G G. Hybrid arenites: Their composition and classification. Journal of Sedimentary Petrology, 1980,50(1):21～29
[8]	关士聪,演怀玉,丘东洲,等.中国晚元古代至三叠纪海域沉积环境模式探讨.石油与天然气地质,1980,1(1):2～17[Guan Shicong,Yan Huaiyu and Qiu Dongzhou. Investigations on the marine sedimentary environmental model of China in late Proterozoic to Triassic periods. Oil & Gas Geology,1980,1(1):2～17]
[9]	刘宝珺,余光明,王成善,等.珠穆朗玛峰地区侏罗纪沉积环境.沉积学报,1983,1(2):1～16[Liu Baojun,Yu Guangming, Wang Chengshan, et al. Jurassic sedimentary environment in the Qomolangma region. Acta Sedimetologica Sinica,1983,1(2):1～16]
[10]	Mount J F. Mixing of siliciclastics and carbonate sediments in shallow shelf environments. Geology,1984,12:432～435
[11]	Mount J F. Mixed siliclastic and carbonate sediments: A proposed first-order textural and compositional classification. Sedimentology, 1985,32:435～442
[12]	王国忠,吕炳全,全松青.现代碳酸盐岩与陆源碎屑的混合沉积作用-涠洲岛珊瑚岸礁实例.石油与天然气地质,1987,8(1):15～25[Wang Guozhong,Lu Bingquan and Quan Songqing. Mixed sedimentation of recent carbonates and terrigenous clastics. Oil & Gas Geology,1987,8(1):15～25]
[13]	郭福生.江山石炭纪和二叠纪沉积相.华东地质学院学报,1990,13(4):57～65[Guo Fusheng. Sedimentary facies of the Carboniferous and Permian in Jiangshan. Journal of East China College of Geology,1990,13(4):57～65]
[14]	郭福生.浙江江山晚古生代岩相古地理及其构造控制.岩相古地理,1993,13(6):44～52[Guo Fusheng. Late Palaeozoic sedimentary facies and Palaeogeography and their tectonic controls in Jiangshan, Zhejiang. Sedimentary Facies and Palaeogeography, 1993,13(6):44～52]
[15]	张锦泉,陈洪德,叶红专.碳酸盐与陆源碎屑的混合沉积.见:冯增昭,王英华,刘焕杰.中国沉积学.北京:石油工业出版社,1994. 623～631[Zhang Jinquan,Chen Hongde and Ye Hongzhuan. Mixing depositional of carbonate and terrigenous clastics.In: Feng Zengzhao,Wang Yinghua and Liu Huajie. Sedimentary Petrology of China. Beijing: Petroleum Industry Publishing House,1994. 623～631]
[16]	江茂生,沙庆安,刘敏.华北下中寒武统碳酸盐与陆源碎屑混合沉积--以山东张夏地区为例.沉积学报,1996,14(增刊):63～74[Jiang Maosheng,Sha Qingan and Liu Min. Mixed siliciclastic-carbonate sediment during the lower-middle Cambrian in the North China Platform. Acta Sedimentologica Sinica,1996,14(Suppl.):63～74]
[17]	殷勇,董玉珊,高长林,等. 中天山马鞍桥石炭纪沉积特征及构造意义.沉积学报,2000,18(1):100～106[Yin Yong,Dong Yushan,Gao Changlin,et al. Depositional characteristics of Carboniferous and its tectonic significance in Maanqiao area, middle Tianshan. Acta Sedimentologica Sinica,2000,18(1):100～106]
[18]	王冠民. 西藏措勤盆地下白垩统多巴组沉积环境分析.沉积学报,2000,18(3):349～354[Wang Guanmin. Sedimentary environment of the lower Cretaceous Duoba Formation of the Cuoqin Foreland basin in Tibet. Acta Sedimentologica Sinica,2000,18(3):349～354]
[19]	沙庆安. 混积岩一例--滇东震旦系陡山沱组砂质砂屑白云岩的成因.古地理学报,2001,3(4):56～60[Sha Qingan. An example of Hunji rock-origin of sandy doloarenite of the Sinian Doushantuo Formation in Eastern Yunnan province. Journal of Palaeogeography,2001,3(4):56～60]
[20]	蒋凌志,顾家裕. 塔里木盆地麦盖提斜坡石炭系碳酸盐岩和碎屑岩交替沉积的沉积环境分析.石油实验地质,2002,24(1):41～47[Jiang Lingzhi and Gu Jiayu. Application of depositional base-level concept in sequence stratigraphic division,correlation and litho-stratigraphic traps prediction. Petroleum Geology & Experiment,2000,24(1):41～47]
[21]	徐德斌,白志达,王敦则,等.河北省兴隆地区大红峪组沉积古环境研究.地层学杂志,2002,26(1):73～79[Xu Debin,Bai Zhida,Wang Dunze,Mei Minxiang and Li Zhizhong. On sedimentary environment of the Dahongyu Formation in Xinglong region, Hebei. Journal of Stratigraphy,2002,26(1):73～79]
[22]	刘宝珺,王剑,谢渊,等. 当代沉积学研究的新进展与发展趋势--来自第三十一届国际地质大会的信息.沉积与特提斯地质,2002,22(1):1～6[Liu Baojin,Wang Jian,Xie Yuan,Xu Qiang,Mu Chuanlong,Zhu Tongxing,Luo Jianning,Tan Fuwen and Li Zhixong. The development and trend in the research of modern sedimentology- from the 31st International Geology Convention. Sedimentary Geology and Tethyan Geology,2002,22(1):1～6]
[23]	全国地层委员会.全国地层会议学术报告汇编(浙西地层现场会议).北京:科学出版社,1963[Stratum Committee of China. Reports Compilation of China Stratum Convention (Western Zhejiang Province Stratum Convention). Beijing: Science Press,1963]
[24]	韩乃仁.浙江江山古生代地层研究述评.桂林工学院学报,1996,16(3):203～216 [Han Nairen. Comment on the research on palaeontology and strata from Jiangshan, Zhejiang. Journal of Gulin Institute of Technology,1996,16(3):203～216]
[25]	卢衍豪,穆恩之.浙西古生代地层新见.地质知识,1955,(2):1～6[Lu Yanhao and Mu Enzhi. Re-cognition of Paleozoic strata of Western Zhejiang. Geological Knowledge,1955,(2):1～6 ]
[26]	浙江省区域地层表编写组.华东地区区域地层表(浙江省分册).北京:地质出版社,1979.93～106[Compilation Group of Region Stratigraphical Table of Zhejiang Province. Regional Stratigraphical Table of East China Area (Fascicule of Zhejiang Province). Beijing: Geological Publishing House,1979. 93～106]
[27]	陈联儿.江山的石炭系和二叠系.华东地质学院学报,1990,13(4): 35～48 [Chen Lianer. The Carboniferous and Perian of Jiangshan. Journal of East China College of Geology, 1990, 13 (4): 35～48]
[28]	郭福生.浙江江山岩石地层单位的厘定及应用研究.华东地质学院学报,1994,17(3):254～263 [Guo Fusheng. On collating and applying of the lithostratigraphic units in Jiangshan area, Zhejiang. Journal of East China College of Geology,1994,17(3):254～263]
[29]	浙江省地质矿产局.浙江省区域地质志.北京:地质出版社,1989. 96～98,102～104 [Bureau of Geology and Mineral Resources of Zhejiang Province. Regional Geology of Zhejiang Province. Beijing: Geological Publishing House,1989. 96～104]
[30]	江西省地质矿产厅.江西省岩石地层.武汉:中国地质大学出版社,1997. 189～192 [Department of Geology and Mineral Resources of Jiangxi Province. Stratigraphy (Lithostratic) of Jiangxi Province. Wuhan: China University of Geosciences Press,1997. 189～192]
[31]	安徽省区域地层表编写组.华东地区区域地层表(安徽省分册).地质出版社,1978. 216～249 [Compilation Group of Region Stratigraphical Table of Anhui Province. Region Stratigraphical Table of East China Area (Fascicule of Anhui Province). Geological Publishing House, 1978.216～249]
[32]	田京辉,倪培,范建国. 永平铜矿成矿流体特征研究.地质找矿论丛,2001,16(1)24～27[Tian Jinghui,Ni Pei and Fan Jianguo. Ore-forming fluid characteristics research of Yongping copper deposit. Contributions to Geology and Mineral Resources Research,2001,16(1):24～27]
[33]	汪华敏.中国南方中晚石炭世沉积相及沉积模式.沉积学报,1986,4(3):57～65[Wang Huamin. Middle-late Carboniferous sedimentary facies and model in the South China. Acta Sedimentologica Sinica,1986,4(3): 57～65]

[1]	查显锋, 李平, 高晓峰, 计文化, 茹乾, 王志华. 北天山构造带晚侏罗世构造隆升与沉积学响应 . 沉积学报, 2022, 40(5): 1250-1264. doi: 10.14027/j.issn.1000-0550.2021.040
[2]	卢树藩, 陈祎, 罗香建, 何犇, 符宏斌. 贵州石炭系黑色页岩层系沉积特征及分布规律研究 . 沉积学报, 2021, 39(3): 672-685. doi: 10.14027/j.issn.1000-0550.2020.114
[3]	李泉泉, 鲍志东, 肖毓祥, 陈建阳, 李忠诚, 王振军, 刘敏昭, 李卓伦, 许西挺, 操凡. 混合沉积研究进展与展望 . 沉积学报, 2021, 39(1): 153-167. doi: 10.14027/j.issn.1000-0550.2020.140
[4]	曾楷, 李飞, 龚峤林, 唐浩, 苏成鹏, 车正强, 邓嘉婷, 胡广, 李凌, 曾伟, 谭秀成. 寒武系第二统仙女洞组混合沉积特征及古环境意义——以川北旺苍唐家河剖面为例 . 沉积学报, 2020, 38(1): 166-181. doi: 10.14027/j.issn.1000-0550.2019.015
[5]	霍少川, 董桂玉, 王兵杰, 张振国, 刘金华, 刘建宁, 曹玉鹏, 冷春鹏. 金湖凹陷阜宁组二段混合沉积研究 . 沉积学报, 2019, 37(1): 177-188. doi: 10.14027/j.issn.1000-0550.2018.119
[6]	伏美燕, 李娜, 黄茜, 刘磊. 滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例 . 沉积学报, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003
[7]	伊硕, 黄文辉, 金振奎, 高白水. 滨里海盆地东缘石炭系KT-II层碳酸盐岩微相特征与沉积环境研究——以扎纳若尔地区为例 . 沉积学报, 2017, 35(1): 139-150. doi: 10.14027/j.cnki.cjxb.2017.01.014
[8]	谭梦琪, 刘自亮, 沈芳, 谢润成, 刘成川, 邓昆, 徐浩. 四川盆地回龙地区下侏罗统自流井组大安寨段混积岩特征及模式 . 沉积学报, 2016, 34(3): 571-581. doi: 10.14027/j.cnki.cjxb.2016.03.015
[9]	李婷婷, 朱如凯, 白斌, 王崇孝, 李铁峰. 混积岩储层特征——以酒泉盆地青西凹陷下白垩统混积岩为例 . 沉积学报, 2015, 33(2): 376-384. doi: 10.14027/j.cnki.cjxb.2015.02.017
[10]	. 云南会泽石炭系摆佐组白云岩地球化学特征及其成因分析 . 沉积学报, 2014, 32(1): 118-125.
[11]	. 柴达木盆地北缘下干柴沟组下段湖相混合沉积发育特征及其对储层的影响 . 沉积学报, 2013, 31(04): 724-729.
[12]	. 青藏高原北部新生代构造演化在柴达木盆地中的沉积记录 . 沉积学报, 2013, 31(05): 824-833.
[13]	曹桐生. 内蒙古阿尔山地区下寒武统苏中组混合沉积特征及形成环境研究 . 沉积学报, 2011, 29(1): 55-63.
[14]	卫平生, 李天顺, 李安春, 王建功. 巴彦浩特盆地石炭系沉积相及沉积演化 . 沉积学报, 2005, 23(2): 240-247.
[15]	宋春晖, 孙淑荣, 方小敏, 孙东. 酒西盆地晚新生代沉积物重矿物分析与高原北部隆升 . 沉积学报, 2002, 20(4): 552-559.
[16]	宋春晖, 方小敏, 高军平, 孙东, 范马洁. 青藏高原东北部贵德盆地新生代沉积演化与构造隆升 . 沉积学报, 2001, 19(4): 493-500.
[17]	殷勇, 董玉珊, 高长林, 江建春, 范小林. 中天山马鞍桥石炭纪沉积特征及构造意义 . 沉积学报, 2000, 18(1): 100-106.
[18]	蔡进功, 李从先. 内蒙古西南部石炭系砂坝─泻湖沉积体系的比较沉积学分析 . 沉积学报, 1994, 12(2): 45-53.
[19]	徐兴, 张广忠, 韩作振, 张维胜. 鲁西石炭纪煤系中的火山事件沉积 . 沉积学报, 1993, 11(3): 93-104.
[20]	杨朝青, 沙庆安. 云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积 . 沉积学报, 1990, 8(2): 59-66.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 648
HTML全文浏览量: 8
PDF下载量: 558
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

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

计量

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

计量

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

计量

出版历程

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

计量

出版历程

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

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