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

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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

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通讯作者:
张廷山

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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 /

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[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
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[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.
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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.

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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

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

Corresponding author: ZHANG Ting-shan

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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

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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

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

Corresponding author: ZHANG Ting-shan

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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

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目录

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期刊在线

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通讯作者:
张廷山

西南石油大学资源与环境学院成都 6105002