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]	施辉, 王波, 胡俊杰, 吴志雄, 马立成. 柴北缘西段早石炭世构造—沉积格局——来自下石炭统怀头他拉组稀土元素的证据 . 沉积学报, 2025, 43(2): 408-422. doi: 10.14027/j.issn.1000-0550.2023.040
[2]	陈臻, 王丽娟, 李娟, 何佳伟, 杨用彪, 邓涛, 关俊朋, 龚海艇, 胡修棉. 下扬子早古生代碳酸盐岩微相与沉积环境演化 . 沉积学报, 2024, 42(6): 2191-2203. doi: 10.14027/j.issn.1000-0550.2023.026
[3]	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
[4]	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
[5]	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.
[6]	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.
[7]	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.
[8]	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.
[9]	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.
[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.

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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

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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

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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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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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