湘西黔东下、中寒武统沉积环境

梁仁枝; 李汉瑜; 刘宝珺; 许效松

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

湘西黔东下、中寒武统沉积环境

梁仁枝, 李汉瑜, 刘宝珺, 许效松

文章导航 > 沉积学报 > 1991 > 9(2): 16-24

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

引用本文:

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

Citation:

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

引用本文:

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

Citation:

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

湘西黔东下、中寒武统沉积环境

1.
淮南矿业学院;
2.
成都地质学院;
3.
地矿部成都地质矿产研究

详细信息

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

计量

文章访问数: 653
HTML全文浏览量: 24
PDF下载量: 412
被引次数: 0

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

1.
Huainan Mining College;
2.
Chengdu College of Geology;
3.
heligcu of Geology and Resources

摘要

摘要: 本文论述了对湘西黔东地区早、中寒武世的碳酸盐岩和陆源碎屑沉积的分析研究结果,着重探讨了控制该区陆表海沉积层序的各种动力因素。在研究区内,4种垂向层序均具有向上变浅的旋回性。早寒武世晚期的藻丘缓斜坡与中寒武世的鲕粒陡斜坡上的沉积动力学特征为:滨岸正常波浪潮汐流,滨岸及内陆棚的风暴营力,垂直于古岸线的大规模地滑和重力流,沿古岸线及斜坡的等深流。沉积小旋回的成因系构造断块的脉动,而盆地边缘的海退序列则由板块相对扩张、海平面变动及碳酸盐岩自身成长所控制。
- 下 /
- 中寒武统 /
- 盆地分析 /
- 重力流 /
- 等深流 /
- 藻丘 /
- 鲕滩
Abstract: By using graphic analysis to study carbonate and terrigenous clastic sediments of the western Hunan and eastern Guizhou provinces, the different dynamic factors uneiital carbonate sequences in this area are studied especially. With the analysis, the ooidalpisolitic grainstone, oncolitic packstone and intraclastic gram and tidal dominated environments are discussed.Furthermore, the characten and gravity flow sediments are analyzed, and the sedimentary mechanics of st is idscussed. Particularly, the authors studied the hummocky cross-stratifie in tempestite sequence. Which was to be the product of unidirectional back-flow of gradient current- formed by storm interpays with storm wave action, this bed-form is a transitional type betwwen syn ripples with straight crest and the upper flat bed- form of gradient currents.Pale rent sis of Cambrian contour currents in studied area indicates the paleocurrent flown from NE to S and along the edge of the basin. Four ki difterent veruend es are recognized, which includes the shallowing-upward cycles, and minor" transgoressive regressive pulses. Lateral distribution of facies may indicates paleogeograp ter diferent periods: a gentle slope consists of algal mound during the early Cambrian and a steep slope consists of ooidal shoal in the middle Cambrian.The sedimentary dynamics of the mentioned slope is suggested: (1) wavy and tidal action that affected the shore belt; (2) storm events that influenced the shore and shelf environments; ( 3) sliding and gravity flow that developed across to the shoreline; (4) contour current that flowed along the slope and parallelled to the shoreline. Comparision of minor cycles suggests that the dynamic factors controlling these cycles may be derived from the block faulting. The regressive sequence of basinal edge was controlled by the.interaction of plate spreading, sealevel changing and the developing of carbonate itself.

HTML全文

参考文献(1)

[1]

1. 刘宝珺、余光明、效伯龙，1983.沉积学报，1卷，2期，1-13页。

2. 高振中、段太忠，1985，沉积字报，3卷，3期，7-22页。

3. Dott, R.H.Jr., and Bourgeois. J.1982, GSA BuILV.93, p.663-680.

4. Dott.R.H.Jr.. 1983; :982, J.Sediment petrol, V.53, p.5-23

5. Enos 0.1983, AAPG 11em.Vol.33. p.267-295.

6. Loreau J. P. at;d Purser. B. H.，1973, the persian Gulf. Holocene Carbonate Sedimentation in a Shallow epiconlinental Sea: Nco-York-Heidelberg-Berlin. Springer-Verlag.p.279-328.

7. Waiken R. G 1979 Modcl Geoscl Canada, Reprint Ser. led. Kitchener Ontarto Ainsworthprss.

8. Wilson I.L.. 1975. Carbonate facres in geologic history, Springer-Verlag, Berlin, p.471.

[1]	杨仁超, 李作福, 张学才, 慈兴华, 方旭庆, 李传华, 刘海宁. 异重流沉积研究进展与展望 . 沉积学报, 2023, 41(6): 1917-1933. doi: 10.14027/j.issn.1000-0550.2023.008
[2]	彭雲, 于谦, 万洁颖, 杜智运, 王黎, 王韫玮, 高抒. 江苏海岸中部近岸沉积物重力流输运过程 . 沉积学报, 2023, 41(6): 1755-1767. doi: 10.14027/j.issn.1000-0550.2023.091
[3]	李华, 何明薇, 邱春光, 王英民, 何幼斌, 徐艳霞, 何瑞武. 深水等深流与重力流交互作用沉积（2000—2022年）研究进展 . 沉积学报, 2023, 41(1): 18-36. doi: 10.14027/j.issn.1000-0550.2022.027
[4]	郭恒玮, 伏美燕, 宋荣彩, 刘文, 赵亮, 沈秋媛. 川中高石梯地区灯四段藻丘类型与沉积模式 . 沉积学报, 2022, 40(1): 217-228. doi: 10.14027/j.issn.1000-0550.2020.065
[5]	侯云超, 樊太亮, 李一凡, 蔡文杰, 王宏语, 刘隆隆, 尹思琪, 李冬. 盐构造与深水重力流的相互作用及响应 . 沉积学报, 2022, 40(1): 22-33. doi: 10.14027/j.issn.1000-0550.2020.123
[6]	刘艺萌, 张藜, 黄晓波, 郑敬贵, 徐伟. 辽中凹陷北洼古近系东二下亚段湖底扇沉积类型及时空演化机理分析 . 沉积学报, 2019, 37(6): 1280-1295. doi: 10.14027/j.issn.1000-0550.2019.007
[7]	李华, 何幼斌, 黄伟, 刘朱睿鸷, 张锦. 鄂尔多斯盆地南缘奥陶系平凉组深水沉积特征及其与古环境关系——以陕西富平赵老峪地区为例 . 沉积学报, 2018, 36(3): 483-499. doi: 10.14027/j.issn.1000-0550.2018.031
[8]	江宁, 何敏, 刘军, 庞雄, 张向涛, 薛怀艳. 东沙隆起南缘第四系等深流沉积特征及成因机制 . 沉积学报, 2018, 36(1): 120-131. doi: 10.3969/j.issn.1000-0550.2018.014
[9]	徐伟, 李正宇, 刘艺萌, 刘军钊, 王启明. 渤中25-1油田沙三段重力流沉积模式及油气地质意义 . 沉积学报, 2018, 36(3): 557-569. doi: 10.14027/j.issn.1000-0550.2018.075
[10]	张景军, 李凯强, 王群会, 王志坤, 韩江波. 渤海湾盆地南堡凹陷古近系重力流沉积特征及模式 . 沉积学报, 2017, 35(6): 1241-1253. doi: 10.14027/j.cnki.cjxb.2017.06.015
[11]	李华, 何幼斌. 等深流沉积研究进展 . 沉积学报, 2017, 35(2): 228-240. doi: 10.14027/j.cnki.cjxb.2017.02.003
[12]	孙福宁, 杨仁超, 李冬月. 异重流沉积研究进展 . 沉积学报, 2016, 34(3): 452-462. doi: 10.14027/j.cnki.cjxb.2016.03.003
[13]	杜锦霞. 松辽盆地北部青山口组重力流特征研究及其地质意义 . 沉积学报, 2015, 33(2): 385-393. doi: 10.14027/j.cnki.cjxb.2015.02.018
[14]	杨家静, 王一刚, 王兰生, 文应初, 刘划一, 周国源. 四川盆地东部长兴组——飞仙关组气藏地球化学特征及气源探讨 . 沉积学报, 2002, 20(2): 349-353.
[15]	刘善印, 钟大赉, 吴根耀. 滇西南景谷—镇沅地区第三纪重力流沉积及其地质意义 . 沉积学报, 1998, 16(2): 50-54.
[16]	沙庆安, 江茂生. 粒滩相与藻坪相沉积——鲁西地区中寒武统张夏组剖析 . 沉积学报, 1998, 16(4): 62-70.
[17]	郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用 . 沉积学报, 1994, 12(4): 77-86.
[18]	杨瑞东. 黔中、黔南下、中三叠统沉积相和层序地层 . 沉积学报, 1993, 11(4): 24-29.
[19]	李思田. 论沉积盆地分析领域的追踪与创新 . 沉积学报, 1992, 10(3): 10-15.
[20]	端木合顺, 朱莲芳. 酒西盆地下白垩统下沟组重力流水下扇沉积 . 沉积学报, 1990, 8(2): 75-86.

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: 653
HTML全文浏览量: 24
PDF下载量: 412
被引次数: 0

湘西黔东下、中寒武统沉积环境

1. 淮南矿业学院;

2. 成都地质学院;

3. 地矿部成都地质矿产研究

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

收稿日期: 1989-01-25
刊出日期: 1991-06-10

关键词:

下 /

中寒武统 /

盆地分析 /

重力流 /

等深流 /

藻丘 /

鲕滩

摘要: 本文论述了对湘西黔东地区早、中寒武世的碳酸盐岩和陆源碎屑沉积的分析研究结果,着重探讨了控制该区陆表海沉积层序的各种动力因素。在研究区内,4种垂向层序均具有向上变浅的旋回性。早寒武世晚期的藻丘缓斜坡与中寒武世的鲕粒陡斜坡上的沉积动力学特征为:滨岸正常波浪潮汐流,滨岸及内陆棚的风暴营力,垂直于古岸线的大规模地滑和重力流,沿古岸线及斜坡的等深流。沉积小旋回的成因系构造断块的脉动,而盆地边缘的海退序列则由板块相对扩张、海平面变动及碳酸盐岩自身成长所控制。

English Abstract

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

1. Huainan Mining College;

2. Chengdu College of Geology;

3. heligcu of Geology and Resources

Received Date: 1989-01-25
Publish Date: 1991-06-10

Abstract: By using graphic analysis to study carbonate and terrigenous clastic sediments of the western Hunan and eastern Guizhou provinces, the different dynamic factors uneiital carbonate sequences in this area are studied especially. With the analysis, the ooidalpisolitic grainstone, oncolitic packstone and intraclastic gram and tidal dominated environments are discussed.Furthermore, the characten and gravity flow sediments are analyzed, and the sedimentary mechanics of st is idscussed. Particularly, the authors studied the hummocky cross-stratifie in tempestite sequence. Which was to be the product of unidirectional back-flow of gradient current- formed by storm interpays with storm wave action, this bed-form is a transitional type betwwen syn ripples with straight crest and the upper flat bed- form of gradient currents.Pale rent sis of Cambrian contour currents in studied area indicates the paleocurrent flown from NE to S and along the edge of the basin. Four ki difterent veruend es are recognized, which includes the shallowing-upward cycles, and minor" transgoressive regressive pulses. Lateral distribution of facies may indicates paleogeograp ter diferent periods: a gentle slope consists of algal mound during the early Cambrian and a steep slope consists of ooidal shoal in the middle Cambrian.The sedimentary dynamics of the mentioned slope is suggested: (1) wavy and tidal action that affected the shore belt; (2) storm events that influenced the shore and shelf environments; ( 3) sliding and gravity flow that developed across to the shoreline; (4) contour current that flowed along the slope and parallelled to the shoreline. Comparision of minor cycles suggests that the dynamic factors controlling these cycles may be derived from the block faulting. The regressive sequence of basinal edge was controlled by the.interaction of plate spreading, sealevel changing and the developing of carbonate itself.

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

引用本文:

梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境[J]. 沉积学报, 1991, 9(2): 16-24.

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

Citation:

Liang Renzhi, Li Hanyu, Lui Baojun, Xu Xiaosong. Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou[J]. Acta Sedimentologica Sinica, 1991, 9(2): 16-24.

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

湘西黔东下、中寒武统沉积环境

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

计量

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

计量

目录

湘西黔东下、中寒武统沉积环境

1. 淮南矿业学院;

2. 成都地质学院;

3. 地矿部成都地质矿产研究

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

English Abstract

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

1. Huainan Mining College;

2. Chengdu College of Geology;

3. heligcu of Geology and Resources

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

湘西黔东下、中寒武统沉积环境

作者简介: 梁仁枝,男,26岁,硕士,沉积学.

计量

出版历程

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

计量

出版历程

目录

湘西黔东下、中寒武统沉积环境

1. 淮南矿业学院; 2. 成都地质学院; 3. 地矿部成都地质矿产研究

作者简介: 梁仁枝,男,26岁,硕士,沉积学.

English Abstract

Dynamic Stratigraphy of Lower and Middle Collbrian in Western Hunan and Eastern Guizhou

1. Huainan Mining College; 2. Chengdu College of Geology; 3. heligcu of Geology and Resources

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

1. 淮南矿业学院;

2. 成都地质学院;

3. 地矿部成都地质矿产研究

作者简介:
梁仁枝,男,26岁,硕士,沉积学.

1. Huainan Mining College;

2. Chengdu College of Geology;

3. heligcu of Geology and Resources