川滇黔桂地区泥盆系层序地层分析

覃建雄; 陈洪德; 田景春; 彭军; 侯中健; 寿建峰; 杨晓宁; 沈安江; 陈子炓

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

川滇黔桂地区泥盆系层序地层分析

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓

文章导航 > 沉积学报 > 2000 > 18(2): 172-179

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

引用本文:

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

QIN Jian xiong, CHEN Hong de, TIAN Jing chun, PENG Jun, HOU Zhong jian, SHOU Jian feng, YANG Xiao ning, SHENG An jiang, CHEN Zhi liao. Sequence Stratigraphy of Devonian in the Youjiang Basin[J]. Acta Sedimentologica Sinica, 2000, 18(2): 172-179.

Citation:

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

引用本文:

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

Citation:

川滇黔桂地区泥盆系层序地层分析

1 成都理工学院沉积地质研究所成都 610059;
2 杭州石油地质研究所杭州 310023

详细信息

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

中图分类号: P539.2

计量

文章访问数: 511
HTML全文浏览量: 1
PDF下载量: 543
被引次数: 0

Sequence Stratigraphy of Devonian in the Youjiang Basin

1 Institute of Sedimentary Geology, Chengdu University of Technol ogy, Chengdu 610059;
2 Hangzhou Institute of Petroleum Geology, Hangzhou 310023

摘要

摘要: 根据层序关键界面、体系域叠置关系及内部构型特征,结合生物地层资料,右江盆地泥盆系可划分为17个三级层序,其中下统 7个、中统 5个、上统 5个,包括 9个Ⅰ型层序、8个Ⅱ型层序,代表17次三级相对海平面变化产物。在此基础上,对不同沉积背景的层序进行了对比,建立了相应的层序格架模型。结果表明,不同沉积相带的层序内部构型和成因格架存在一定的差异,但由于海平面变化这一共同因素的影响,它们仍可进行对比和追踪。
- 层序地层 /
- 泥盆纪 /
- 右江盆地
Abstract: Based on key sequence boundary, sedimentary system tracts, in conjunc tion with bio-stratigraphy, sequence stratigraphy during the Devonian in the Yo ujiang Basin has been studied in detail. 17 3rd-order sequences have been recog nized for the first time, 7 sequences in the Lower, 5 sequences in the Middle an d 5 sequences in the Upper Devonian, including 10 Ⅰ-type sequences and 7 Ⅱ-t ype sequences, representing 17 3rd-order relative sea level changes. Moreover, sequences in different sedimentary backgruonds have been correlated and then cor responding seqence stratigaphic framework has also been established. This paper demonstrated that sequence internal architecture and genetic framework within va rious sedimentary facies zones are obviously different, but they can be correlat ed and traced because of the same control factor-relative sea level changes. The Devonian transgression in this area extended from south to north overlappe d in the formation of the transgression-type sequences. These sequences were co ntrolled by sea-level change and tectonic activities. At least three 2nd-order rising sea level stages have been distinguished. During the basin evolution, the late stage of Early and Middle Devonian and the early of Late Devonian correspo nd to the eustatic change of sea level. During these periods the tectonic, volca nism and sedimentary differentiation might be very strong. Devonian basin can be subdivided into stability and riftplatform. the former distributes in Lochkovian, Pragian, Eifelian, Frasnian and Famenian, and the latter in Emrian and Givetian. In the stability age, sequences can be correlated one by one. But in tectonic area period, sequences are clearly different. The r esult of research shows that Devonian sequence of stabilized platform area is ma inly controlled by sea ieel change and tectonic movement of the globe or the r egion, and the sequence of the rift trough in the platform is controlled by the basement tectonics of the basin and the episodic subsidence.
- sequence stratigraphy /
- Devonian /
- Youjiang Basin

HTML全文

参考文献(7)

[1]	陈代钊，陈其英.华南泥盆系沉积演化及海水进退规程[J] .地质科学，1994，2 9(3)：246～255
[2]	陈洪德，曾允孚.右江盆地的性质及演化讨论[J] .岩相古地理，1990，24(1) ：28～37
[3]	曾允孚，刘文均.华南右江盆地沉积构造演化[M] .北京：地质出版社，1993
[4]	吴诒，龚一鸣等.华南泥盆纪层序地层及海平面变化[M] .武汉：中国地质大学出版社，1997.15～24
[5]	陈代钊等.泥盆纪海相碳酸盐岩碳同位素组成及演化[J] .岩相古地理，1995，1 5(5)：22～28
[6]	陈景石.古海洋同位素演化[J] .地球科学，1995，30(4)：338～347
[7]	陈代钊，陈英其.华南泥盆纪的沉积盆地特征、沉积作用和成矿作用[J] .地质学报，1994.24(3)：12～23

[1]	惠潇, 侯云超, 陈修, 龙盛芳, 喻建, 赵俊峰, 刘永涛. 鄂尔多斯盆地陇东地区延长组层序地层再认识及地质意义 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.064
[2]	. 准噶尔盆地南缘中下侏罗统含煤层系层序地层及聚煤控制因素 . 沉积学报, 2014, 32(1): 61-67.
[3]	. 鄂尔多斯盆地奥陶系层序地层格架 . 沉积学报, 2014, 32(1): 44-60.
[4]	杨明慧. 鄂尔多斯盆地东北缘晚古生代陆表海含煤岩系层序地层研究 . 沉积学报, 2008, 26(6): 1005-1013.
[5]	唐洪三. 合肥盆地白垩纪层序地层格架、沉积体系配置及演化 . 沉积学报, 2008, 26(6): 982-993.
[6]	. 鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析 . 沉积学报, 2006, 24(4): 549-554.
[7]	杨玉峰, 王占国, 张维琴. 松辽盆地湖相泥岩地层有机碳分布特征及层序分析 . 沉积学报, 2003, 21(2): 340-344.
[8]	刘洛夫, 康永尚, 齐雪峰, 唐勇, 熊正祥. 准噶尔盆地侏罗系层序地层格架中的烃源岩评价 . 沉积学报, 2002, 20(4): 687-694.
[9]	沈守文, 彭大钧, 颜其彬, 黄先律, 李志军. 吐哈盆地侏罗系层序地层学研究 . 沉积学报, 2001, 19(2): 263-270.
[10]	田景春, 陈洪德, 彭军, 覃建雄, 侯中健. 右江盆地深水沉积层序地层学研究 . 沉积学报, 2000, 18(2): 210-214.
[11]	陈洪德, 覃建雄, 田景春, 彭军, 侯中健. 右江盆地层序充填动力学初探 . 沉积学报, 2000, 18(2): 165-171.
[12]	陈洪德, 覃建雄, 田景春, 彭军, 侯中健. 右江盆地层序格架中的生储盖组合特征及勘探意义 . 沉积学报, 2000, 18(2): 215-220.
[13]	侯中健, 陈洪德, 田景春, 覃建雄, 彭军. 右江盆地海相泥盆系-中三叠统层序界面成因类型与盆地演化 . 沉积学报, 2000, 18(2): 205-209.
[14]	陈洪德, 王成善, 刘文均, 覃建雄. 华南二叠纪层序地层与盆地演化 . 沉积学报, 1999, 17(4): 528-535.
[15]	李祥辉, 曾允孚. 扬子西缘泥盆纪碳酸盐与陆源碎屑的混积层序和层序混积模式 . 沉积学报, 1999, 17(3): 339-344.
[16]	杜远生, 龚一鸣, 吴诒, 冯庆来, 刘本培. 黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化 . 沉积学报, 1997, 15(4): 11-17.
[17]	杜小弟, 王璞君, 匡立春, 王东坡. 塔里木盆地震旦—泥盆纪古海平面变化再造及形成机理分析 . 沉积学报, 1997, 15(3): 14-17.
[18]	孟庆任, 梅志超, 于在平, 张国伟. 南秦岭北缘镇安盆地晚泥盆世浊积岩系及盆地发展 . 沉积学报, 1996, 14(S1): 25-32.
[19]	许效松, 牟传龙, 林明. 中国南方泥盆纪板内盆地层序地层与控矿 . 沉积学报, 1994, 12(1): 1-7.
[20]	辛建荣. 广西南丹泥盆纪缺氧盆地沉积模式及其演化 . 沉积学报, 1991, 9(3): 90-97.

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: 511
HTML全文浏览量: 1
PDF下载量: 543
被引次数: 0

川滇黔桂地区泥盆系层序地层分析

1 成都理工学院沉积地质研究所成都 610059;

2 杭州石油地质研究所杭州 310023

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

收稿日期: 1999-06-30
刊出日期: 2000-06-10

中图分类号: P539.2

关键词:

层序地层 /

泥盆纪 /

右江盆地

摘要: 根据层序关键界面、体系域叠置关系及内部构型特征,结合生物地层资料,右江盆地泥盆系可划分为17个三级层序,其中下统 7个、中统 5个、上统 5个,包括 9个Ⅰ型层序、8个Ⅱ型层序,代表17次三级相对海平面变化产物。在此基础上,对不同沉积背景的层序进行了对比,建立了相应的层序格架模型。结果表明,不同沉积相带的层序内部构型和成因格架存在一定的差异,但由于海平面变化这一共同因素的影响,它们仍可进行对比和追踪。

English Abstract

Sequence Stratigraphy of Devonian in the Youjiang Basin

1 Institute of Sedimentary Geology, Chengdu University of Technol ogy, Chengdu 610059;

2 Hangzhou Institute of Petroleum Geology, Hangzhou 310023

Received Date: 1999-06-30
Publish Date: 2000-06-10

Keywords:

Abstract: Based on key sequence boundary, sedimentary system tracts, in conjunc tion with bio-stratigraphy, sequence stratigraphy during the Devonian in the Yo ujiang Basin has been studied in detail. 17 3rd-order sequences have been recog nized for the first time, 7 sequences in the Lower, 5 sequences in the Middle an d 5 sequences in the Upper Devonian, including 10 Ⅰ-type sequences and 7 Ⅱ-t ype sequences, representing 17 3rd-order relative sea level changes. Moreover, sequences in different sedimentary backgruonds have been correlated and then cor responding seqence stratigaphic framework has also been established. This paper demonstrated that sequence internal architecture and genetic framework within va rious sedimentary facies zones are obviously different, but they can be correlat ed and traced because of the same control factor-relative sea level changes. The Devonian transgression in this area extended from south to north overlappe d in the formation of the transgression-type sequences. These sequences were co ntrolled by sea-level change and tectonic activities. At least three 2nd-order rising sea level stages have been distinguished. During the basin evolution, the late stage of Early and Middle Devonian and the early of Late Devonian correspo nd to the eustatic change of sea level. During these periods the tectonic, volca nism and sedimentary differentiation might be very strong. Devonian basin can be subdivided into stability and riftplatform. the former distributes in Lochkovian, Pragian, Eifelian, Frasnian and Famenian, and the latter in Emrian and Givetian. In the stability age, sequences can be correlated one by one. But in tectonic area period, sequences are clearly different. The r esult of research shows that Devonian sequence of stabilized platform area is ma inly controlled by sea ieel change and tectonic movement of the globe or the r egion, and the sequence of the rift trough in the platform is controlled by the basement tectonics of the basin and the episodic subsidence.

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

引用本文:

覃建雄, 陈洪德, 田景春, 彭军, 侯中健, 寿建峰, 杨晓宁, 沈安江, 陈子炓. 川滇黔桂地区泥盆系层序地层分析[J]. 沉积学报, 2000, 18(2): 172-179.

Citation:

全文HTML

参考文献 (7)

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

川滇黔桂地区泥盆系层序地层分析

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

计量

Sequence Stratigraphy of Devonian in the Youjiang Basin

计量

目录

川滇黔桂地区泥盆系层序地层分析

1 成都理工学院沉积地质研究所成都 610059;

2 杭州石油地质研究所杭州 310023

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

English Abstract

Sequence Stratigraphy of Devonian in the Youjiang Basin

1 Institute of Sedimentary Geology, Chengdu University of Technol ogy, Chengdu 610059;

2 Hangzhou Institute of Petroleum Geology, Hangzhou 310023

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

川滇黔桂地区泥盆系层序地层分析

作者简介: 覃建雄,男,1967年出生,副教授(博士),沉积学

计量

出版历程

Sequence Stratigraphy of Devonian in the Youjiang Basin

计量

出版历程

目录

川滇黔桂地区泥盆系层序地层分析

1 成都理工学院沉积地质研究所 成都 610059; 2 杭州石油地质研究所 杭州 310023

作者简介: 覃建雄,男,1967年出生,副教授(博士),沉积学

English Abstract

Sequence Stratigraphy of Devonian in the Youjiang Basin

1 Institute of Sedimentary Geology, Chengdu University of Technol ogy, Chengdu 610059; 2 Hangzhou Institute of Petroleum Geology, Hangzhou 310023

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

1 成都理工学院沉积地质研究所成都 610059;

2 杭州石油地质研究所杭州 310023

作者简介:
覃建雄,男,1967年出生,副教授(博士),沉积学

1 Institute of Sedimentary Geology, Chengdu University of Technol ogy, Chengdu 610059;

2 Hangzhou Institute of Petroleum Geology, Hangzhou 310023