淮南煤田二叠系三、四含煤段古水系特征

彭苏萍; 韩德馨; 张鹏飞; 蓝昌益

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

淮南煤田二叠系三、四含煤段古水系特征

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益

文章导航 > 沉积学报 > 1991 > 9(3): 1-10

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

淮南煤田二叠系三、四含煤段古水系特征

1.
中国矿业大学北京研究生部;
2.
淮南矿业学院

基金项目: 国家青年科学基金

详细信息

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

计量

文章访问数: 530
HTML全文浏览量: 9
PDF下载量: 313
被引次数: 0

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1.
Beijing Graduate School, China University of Mining and Technology;
2.
Huainan Mining Institute

摘要

摘要: 本文通过对淮南煤田二叠系三、四含煤段5千余个钻孔资料的系统分析和煤矿开拓巷道中古流向的实际测量,获得大量有关古水系的第-性资料。研究认为可与现代珠江三角洲上的水系进行类比、进而推断三、四含煤段沉积时的环境为-种由多条陆源河流共同作用形成的复合型三角洲。
- 古水系 /
- 复合型三角洲 /
- 树技状河系 /
- 网状河系
Abstract: The Huainan Coalfield, covering an area of more than 8000 km₂. is concealed by the Quaternary system and the main coal-bearing strata are Permian Members C-D. By the investigation of more than 5000 bores and surveying of undergroud tunnels of the coal mines in the research district, many characteristics of the paleodrainage have been acquired as follows: 1. By undergroud surveying of the main channel sandstones of the members C-D, it is shown that during their deposition the paleocurrent direction is southward. 2.The paleodrainage of the Permian members C-D have two forms, the branched channel system (in member C) and the anastomosing channel system (in member D). The channels composed the drainages are very stable and fail to lateral migration. 3. The results of grainsize analysis and the C-M pattern of the same genetic increment demonstrates that the paleostream flown from north to south, and the south side is more near to the sea. 4. The characteristics of sedimentology and sedimentary geochemistry indicate that the t;ne sediments of member C which deposited in the branched channel system contain much more of the tidal sediments, bur- rows, and Lingula sp. etc. The content of the trace element B. B; Ga and Ca (Fe+Ca) are higher than that of member D To sum up the characteristics discussed above and analyze by means of Walther's Law of correlation of fades. and compare with the drainage on the modern Pearl River, the authers propose that the paleodrainage of the members C-D is more similar to that on the modern Pearl River Delta, that is to say, it can be divided into two parts, the anastomosing fluvial system near the continent and the branched fluvial system close to the sea. It is recognized that the paleodrainage discussed m this paper is different from that on the Mississippi River Delta and’or on the Yangtze River Delta. that could he account for which discussed' in this p:ner is a complex delta formed together by several continental streams, the low-medium thal range and the Coriolis Force exist in the history of the Earth.

HTML全文

参考文献(1)

[1]

1. 黄镇国、李平日等，1982，珠江三角洲形成发育演变，科学普及出版社广州分社.

2. 彭苏萍，1989,科学通报，34卷，17期，1326-1328页.

3. Sorby, H.C., 1859, The Geologist。Vol.2, p.137-147

4. Sorby. H.C., 1879, Quart.J.GeoLSoc., London, Vo1.35, p.56-77.

5. Potter, P. E.&Pettijohn. F. J.，1977. Paleocurrents and basin analysis〔second, corrected and updatededition )，Springer-Verlag.

6. Martin, R., 1966, AAPG Bull., Vo1.50, IVo.10, p.2277-2311.

7. Daniel A.Busch, 1974, Stratigraphic traps m sandstone-exploration techniques, The American Association of Petroleum Geologists Tulsa. Oklahoma. U.S.A

8. Matthews, R.K., 1984, Dynamic Stratigraphy(second edition) DrenOCe-Hall, Inc，Englewood Cliffs. New Jersey，07632.

[1]	张曰静, 修金磊, 谢利华, 石好果, 商丰凯, 张卫平, 冯庚, 关旭同, 冷佳宣, 李严. 准噶尔盆地车排子地区沙一段复合扇三角洲沉积及控制因素 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.132
[2]	陈彬滔, 马轮, 洪亮, 史忠生, 庞文珠, 薛罗, 王磊, 代寒松, 赵艳军. 断陷湖盆陡坡带扇三角洲—滑塌扇复合扇体的沉积演化及油气地质意义 . 沉积学报, 2024, 42(3): 1058-1072. doi: 10.14027/j.issn.1000-0550.2022.087
[3]	马福康, 吴胜和, 陶叶, 陈亚坤, 黎飞凡, 王武荣, 李伟, 徐振华. 季节性湖平面变化下浅水三角洲指状砂坝沉积特征研究 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.091
[4]	周良, 王洋, 杜学斌, 卜建军, 吴俊, 吕万军, 刘秀娟. 珠江三角洲西缘晚第四纪沉积演化和最大海侵古岸线的重建 . 沉积学报, 2022, 40(1): 119-135. doi: 10.14027/j.issn.1000-0550.2020.087
[5]	路晶芳, 刘健, 胡刚, 黄威, 王红, 张道来. 现代黄河三角洲北岸1.9Ma以来孢粉组合及古环境变化 . 沉积学报, 2022, 40(5): 1335-1345. doi: 10.14027/j.issn.1000-0550.2021.030
[6]	袁丙龙, 张辉, 叶青, 张连枝, 陈之贺, 晁彩霞, 董德喜, 郇金来. 基于三角洲复合砂体构型的流动单元划分及剩余油分布模式 . 沉积学报, 2021, 39(5): 1253-1263. doi: 10.14027/j.issn.1000-0550.2020.105
[7]	秦润森, 岳红林, 周凤军, 吴穹螈, 雷源. 河控浅水三角洲前缘席状砂沉积特征及沉积模式探讨——以黄河口凹陷渤中34地区明下段为例 . 沉积学报, 2020, 38(2): 429-439. doi: 10.14027/j.issn.1000-0550.2019.027
[8]	李维, 朱筱敏, 陈刚, 马英俊. 基于等时界面识别的浅水三角洲-河流沉积体系研究——以高邮凹陷黄珏地区古近系垛一段为例 . 沉积学报, 2018, 36(1): 110-119. doi: 10.3969/j.issn.1000-0550.2018.013
[9]	白雪莘, 张卫国, 董艳, 潘大东, 王张华, 孙千里, 陈静, 陈中原, 刘晋嫣. 长江三角洲全新世地层中潮滩沉积磁性特征及其古环境意义 . 沉积学报, 2016, 34(6): 1165-1175. doi: 10.14027/j.cnki.cjxb.2016.06.014
[10]	刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究 . 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010
[11]	. 黄河三角洲ZK1孔晚第四纪以来沉积层序演化及其古环境意义 . 沉积学报, 2013, 31(6): 1050-1058.
[12]	. 基于滨线轨迹的古水深定量计算新方法①——以古近系沙三中段东营三角洲为例 . 沉积学报, 2012, 30(3): 443-450.
[13]	张昌民. 浅水三角洲沉积模式 . 沉积学报, 2010, 28(5): 933-944.
[14]	魏钦廉. 惠州凹陷古近系珠海组海相三角洲高分辨率层序地层学研究 . 沉积学报, 2008, 26(5): 744-752.
[15]	王宇林, 邵显珉, 范国强, 杨福珍, 于常武. 箕状湖盆萎缩阶段两种湖泊三角洲的沉积特征及成因探讨——以平庄、铁法盆地为例 . 沉积学报, 2002, 20(2): 238-242.
[16]	顾家裕, 方辉, 贾进华. 塔里木盆地库车坳陷白垩系辫状三角洲砂体成岩作用和储层特征 . 沉积学报, 2001, 19(4): 517-523.
[17]	钟建华, 马在平. 黄河三角洲变形层理的研究 . 沉积学报, 1998, 16(1): 45-49.
[18]	陈庆强, 李从先. 长江三角洲晚第四纪古土壤与古环境初探 . 沉积学报, 1995, 13(S1): 79-87.
[19]	赖志云, 周维. 舌状三角洲和鸟足状三角洲形成及演变的沉积模拟实验 . 沉积学报, 1994, 12(2): 37-44.
[20]	钱凯, 屈平彦, 宋凯. 古三角洲砂体入湖距离的动力学预测 . 沉积学报, 1984, 2(3): 82-90.

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: 530
HTML全文浏览量: 9
PDF下载量: 313
被引次数: 0

淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

基金项目: 国家青年科学基金

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

收稿日期: 1989-08-10
刊出日期: 1991-09-10

关键词:

古水系 /

复合型三角洲 /

树技状河系 /

网状河系

摘要: 本文通过对淮南煤田二叠系三、四含煤段5千余个钻孔资料的系统分析和煤矿开拓巷道中古流向的实际测量,获得大量有关古水系的第-性资料。研究认为可与现代珠江三角洲上的水系进行类比、进而推断三、四含煤段沉积时的环境为-种由多条陆源河流共同作用形成的复合型三角洲。

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute

Received Date: 1989-08-10
Publish Date: 1991-09-10

Abstract: The Huainan Coalfield, covering an area of more than 8000 km₂. is concealed by the Quaternary system and the main coal-bearing strata are Permian Members C-D. By the investigation of more than 5000 bores and surveying of undergroud tunnels of the coal mines in the research district, many characteristics of the paleodrainage have been acquired as follows: 1. By undergroud surveying of the main channel sandstones of the members C-D, it is shown that during their deposition the paleocurrent direction is southward. 2.The paleodrainage of the Permian members C-D have two forms, the branched channel system (in member C) and the anastomosing channel system (in member D). The channels composed the drainages are very stable and fail to lateral migration. 3. The results of grainsize analysis and the C-M pattern of the same genetic increment demonstrates that the paleostream flown from north to south, and the south side is more near to the sea. 4. The characteristics of sedimentology and sedimentary geochemistry indicate that the t;ne sediments of member C which deposited in the branched channel system contain much more of the tidal sediments, bur- rows, and Lingula sp. etc. The content of the trace element B. B; Ga and Ca (Fe+Ca) are higher than that of member D To sum up the characteristics discussed above and analyze by means of Walther's Law of correlation of fades. and compare with the drainage on the modern Pearl River, the authers propose that the paleodrainage of the members C-D is more similar to that on the modern Pearl River Delta, that is to say, it can be divided into two parts, the anastomosing fluvial system near the continent and the branched fluvial system close to the sea. It is recognized that the paleodrainage discussed m this paper is different from that on the Mississippi River Delta and’or on the Yangtze River Delta. that could he account for which discussed' in this p:ner is a complex delta formed together by several continental streams, the low-medium thal range and the Coriolis Force exist in the history of the Earth.

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

全文HTML

参考文献 (1)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

淮南煤田二叠系三、四含煤段古水系特征

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

计量

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

计量

目录

淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

淮南煤田二叠系三、四含煤段古水系特征

作者简介: 彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

计量

出版历程

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

计量

出版历程

目录

淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部; 2. 淮南矿业学院

作者简介: 彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology; 2. Huainan Mining Institute

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute