泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

张廷山

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

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

张廷山

文章导航 > 沉积学报 > 2008 > 26(4): 583-592

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

引用本文:

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

ZHANG Ting-shan. Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province[J]. Acta Sedimentologica Sinica, 2008, 26(4): 583-592.

Citation:

ZHANG Ting-shan. Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province[J]. Acta Sedimentologica Sinica, 2008, 26(4): 583-592.

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

引用本文:

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

Citation:

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

张廷山

西南石油大学资源与环境学院成都 6105002

详细信息

通讯作者:
张廷山

计量

文章访问数: 2577
HTML全文浏览量: 7
PDF下载量: 1248
被引次数: 0

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

ZHANG Ting-shan

Department of Resource and Environment, SW Petroleum University,Chengdu 6105002

More Information

Corresponding author: ZHANG Ting-shan

摘要

摘要: 地质历史中，区域大地构造和区域古地貌单元的不同特征是控制沉积相带展布及发育的主要因素之一。东吴运动形成的泸州古隆起是影响本区沉积相带展布的重要因素。早、中三叠世时，泸州古隆起的高部位向南延伸到太和场以南，宝元以北一带。宝元、龙爪等构造处于泸州古隆起东南部斜坡上，而宝元构造处于古隆起东南部斜坡上部，龙爪构造处于古隆起东南部斜坡中部。此古地貌格局，与区域海平面升降一起，控制了早三叠世沉积相带展布和地层厚度。在古地貌高的隆起区域，由于水体开阔、水动力条件相对较强，沉积了有利于形成储集体的滩相沉积物（生屑滩、砂屑滩、鲕粒滩等）。从泸州古隆起的高部位向古隆起的斜坡区，地层厚度逐渐增大，沉积物向粒度变细、颜色加深的特征相变。
- 泸州古隆起 /
- 沉积环境 /
- 相带展布 /
- 早 /
- 中三叠世 /
- 贵州赤水
Abstract: In the geological history, the distribution and the development of sedimentary facies was controlled by the regional tectonics and the regional relief. The Luzhou Uplift, which under the influence of Dongwu Movement, was one of the important controlling factors for the distribution of the Mesozoic sedimentary environment and the sedimentary facies in the area of southern Sichuan basin. During the Early and the Middle Triassic, the Luzhou Uplift developed and stretched to the south, the regional topography characteristic influenced the local sedimentary environment change and sealevel controlled the sedimentary facies distribution and the thickness of strata. For example, the Baoyuan and the Longzhao are two gasbearing structures, in which the reservoirs distribute in lower Triassic. Both of these two gasbearing structures are located at the south slope of the Luzhou Uplift, but the position of the Baoyua structure is on the upper part of the slope, and the Longzhao structure is on the lower slope. The position of the Baoyuan structure is higher than that of the Longzhao. At the high slope of the Uplift, the open sea environment had the stronger hydroenergy, the different banks such as oncolite and bioclastic could be deposited in this area. This sedimentary environment is better for reservoirs formation. From the higher part to the lower part of the Luzhou Uplift, along with the depth of water inc
- Luzhou Uplift /
- relief /
- sedimentary environment /
- facies distribution /

HTML全文

参考文献(0)

[1]	丁仲昭, 马志鑫, 张启跃, 文芠, 胡世学, 范可静, 蔡金君, 李润根. 云南罗平江边地区中三叠统关岭组二段古环境特征 . 沉积学报, 2021, 39(6): 1406-1424. doi: 10.14027/j.issn.1000-0550.2021.036
[2]	余关美, 时国. 贵阳地区下三叠统安顺组遗迹化石及古环境意义 . 沉积学报, 2016, 34(4): 626-633. doi: 10.14027/j.cnki.cjxb.2016.04.002
[3]	王利波, 李军, 陈正新, 赵京涛, 白凤龙, 胡邦琦, 窦衍光, 翟滨. 晚更新世以来台湾浅滩西部地层结构与古环境演化 . 沉积学报, 2014, 32(6): 1089-1099.
[4]	马志鑫. 四川广元中二叠统栖霞组似球粒灰岩微相特征及沉积学意义 . 沉积学报, 2011, 29(3): 449-457.
[5]	景山. 辽西建昌盆地早白垩世义县组沉积环境分析及盆地演化初探 . 沉积学报, 2009, 27(4): 583-591.
[6]	齐永安. 豫西济源中三叠世油房庄组曲流河岩相类型及沉积相分析 . 沉积学报, 2009, 27(2): 254-264.
[7]	乔占峰. 泸州古隆起地区嘉陵江组层序特征及其对碳酸盐岩储层的控制 . 沉积学报, 2008, 26(1): 92-99.
[8]	罗根明. 西秦岭地区晚二叠世—早三叠世沉积相分析和沉积古环境再造 . 沉积学报, 2007, 25(3): 332-342.
[9]	胡瑛. 黄骅坳陷滩海三马地区烃源岩分子标志物特征及其沉积相指示意义 . 沉积学报, 2006, 24(3): 419-425.
[10]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[11]	谢小平, 王永栋, 沈焕庭. 宁夏中卫晚石炭世沉积相分析与古环境重建 . 沉积学报, 2004, 22(1): 19-28.
[12]	刘志飞, 王成善, 金玮. 可可西里盆地早渐新世雅西措群爬升沙纹层理及其沉积环境意义 . 沉积学报, 2004, 22(4): 560-565.
[13]	赵全民, 杨道庆, 江继刚, 彭江, 徐士忠. 舞阳、襄城凹陷下第三系盐湖相有机地球化学与沉积环境研究 . 沉积学报, 2003, 21(2): 334-339.
[14]	刘志丽, 童金南. 中国南方中三叠世地层及沉积古地理分异 . 沉积学报, 2001, 19(3): 327-332,356.
[15]	江德昕, 杨惠秋. 珠江口盆地早第三纪油源岩形成环境 . 沉积学报, 2000, 18(3): 469-474.
[16]	刘志飞, 王成善. 可可西里盆地早渐新世雅西措群沉积环境分析及古气候意义 . 沉积学报, 2000, 18(3): 355-361.
[17]	岳文浙, 业治铮, 姜月华. 江苏晚白垩世赤山组沉积环境 . 沉积学报, 1997, 15(S1): 1-7.
[18]	刘秉理, 朱忠德, 肖传桃, 胡明毅. 鄂西地区早奥陶世分乡期生物群落演化与沉积环境变迁 . 沉积学报, 1997, 15(4): 97-102.
[19]	舒小辛, 刘志伟, 王慧中, 刘传联, 陈东敬, 洪太原. 东营凹陷第三纪湖相沉积物磁性特征及其与环境变化的关系 . 沉积学报, 1995, 13(S1): 96-101.
[20]	王云飞, 王苏民, 冯敏. 泌阳凹陷下第三系核桃园组湖相隐藻层纹石岩的发现及其环境意义 . 沉积学报, 1990, 8(4): 49-58.

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: 2577
HTML全文浏览量: 7
PDF下载量: 1248
被引次数: 0

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

张廷山

西南石油大学资源与环境学院成都 6105002

通讯作者: 张廷山

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2008-08-10

关键词:

早 /

摘要: 地质历史中，区域大地构造和区域古地貌单元的不同特征是控制沉积相带展布及发育的主要因素之一。东吴运动形成的泸州古隆起是影响本区沉积相带展布的重要因素。早、中三叠世时，泸州古隆起的高部位向南延伸到太和场以南，宝元以北一带。宝元、龙爪等构造处于泸州古隆起东南部斜坡上，而宝元构造处于古隆起东南部斜坡上部，龙爪构造处于古隆起东南部斜坡中部。此古地貌格局，与区域海平面升降一起，控制了早三叠世沉积相带展布和地层厚度。在古地貌高的隆起区域，由于水体开阔、水动力条件相对较强，沉积了有利于形成储集体的滩相沉积物（生屑滩、砂屑滩、鲕粒滩等）。从泸州古隆起的高部位向古隆起的斜坡区，地层厚度逐渐增大，沉积物向粒度变细、颜色加深的特征相变。

English Abstract

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

ZHANG Ting-shan

Department of Resource and Environment, SW Petroleum University,Chengdu 6105002

Corresponding author: ZHANG Ting-shan

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2008-08-10

Keywords:

Abstract: In the geological history, the distribution and the development of sedimentary facies was controlled by the regional tectonics and the regional relief. The Luzhou Uplift, which under the influence of Dongwu Movement, was one of the important controlling factors for the distribution of the Mesozoic sedimentary environment and the sedimentary facies in the area of southern Sichuan basin. During the Early and the Middle Triassic, the Luzhou Uplift developed and stretched to the south, the regional topography characteristic influenced the local sedimentary environment change and sealevel controlled the sedimentary facies distribution and the thickness of strata. For example, the Baoyuan and the Longzhao are two gasbearing structures, in which the reservoirs distribute in lower Triassic. Both of these two gasbearing structures are located at the south slope of the Luzhou Uplift, but the position of the Baoyua structure is on the upper part of the slope, and the Longzhao structure is on the lower slope. The position of the Baoyuan structure is higher than that of the Longzhao. At the high slope of the Uplift, the open sea environment had the stronger hydroenergy, the different banks such as oncolite and bioclastic could be deposited in this area. This sedimentary environment is better for reservoirs formation. From the higher part to the lower part of the Luzhou Uplift, along with the depth of water inc

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

引用本文:

张廷山. 泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J]. 沉积学报, 2008, 26(4): 583-592.

Citation:

全文HTML

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

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

通讯作者:
张廷山

计量

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

Corresponding author: ZHANG Ting-shan

计量

目录

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

西南石油大学资源与环境学院成都 6105002

通讯作者: 张廷山

English Abstract

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

Department of Resource and Environment, SW Petroleum University,Chengdu 6105002

Corresponding author: ZHANG Ting-shan

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

通讯作者: 张廷山

计量

出版历程

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

Corresponding author: ZHANG Ting-shan

计量

出版历程

目录

泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制

西南石油大学资源与环境学院 成都 6105002

通讯作者: 张廷山

English Abstract

Controls of Luzhou Uplift on Sedimentary Environment and Facies  Distribution in Early and Middle Triassic, Chishui, Guizhou Province

Department of Resource and Environment, SW Petroleum University,Chengdu 6105002

Corresponding author: ZHANG Ting-shan

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
张廷山

西南石油大学资源与环境学院成都 6105002