惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

董桂玉

文章导航 > 沉积学报 > 2007 > 25(3): 343-350

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

引用本文:

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

DONG Guiyu. Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example[J]. Acta Sedimentologica Sinica, 2007, 25(3): 343-350.

Citation:

DONG Guiyu. Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example[J]. Acta Sedimentologica Sinica, 2007, 25(3): 343-350.

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

引用本文:

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

Citation:

惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

董桂玉

成都理工大学沉积地质研究院成都 610059

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董桂玉

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Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

DONG Guiyu

Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059

More Information

Corresponding author: DONG Guiyu

摘要

摘要: 商河地区沙一中广泛发育陆源碎屑与湖相碳酸盐的混合沉积。本文将混积层系、混积岩和呈零星分布的一起定义为广义的混合沉积，并且对于混合沉积来讲，没有一个具体的组分含量标准，只要该沉积物(岩)的确为陆源碎屑与碳酸盐的沉积，而非成岩作用或以后改造的假混合就可认定为混合沉积。研究区内混合沉积特征为陆源碎屑与湖相碳酸盐以较高的频率交互沉积和同一岩层内陆源碎屑组分与碳酸盐组分混合沉积，混合沉积的类型分为三类，即渐变式混合沉积、突变式混合沉积和复合式混合沉积，其中复合式沉积分为复合式沉积Ⅰ和复合式沉积Ⅱ，研究区内复合式沉积Ⅰ发育，复合式沉积Ⅱ不发育。并且本文从研究区混合沉积的区域地质背景、岩石学特征、沉积环境等方面进行了详细分析，建立了混合沉积相模式，进而对混合沉积的控制因素进行了讨论。
- 商河地区 /
- 沙一中 /
- 混合沉积特征 /
- 混合沉积类型 /
- 混合沉积模式
Abstract: Mixed deposits, which is composed of terrigenous fragment and carbonate of lagoonal facies, develops extensively in the middle submember of Member 1 of Shahejie Formation of Shanghe Area. This paper definite mixed deposited which includes Hunji sequence, Hunji rock and some sporadic distribution, and as far as mixed deposits in a broad sense, and there is not a concrete standard range, if only it is for the reason the sediment or sedimentary rock deposits to terrigenous fragment and carbonate not for false mixed to sedimentation or transformation of sedimentation, it can be deeply convinced to be mixed deposits. In the study area, the characteristics of mixed deposits are interbedded strata between terrigenous fragment and carbonate of lagoonal facies in high frequency and mixing deposited between terrigenous fragment constituent and carbonate constituent in one layer. Mixed sedimentary type can be divided into 3 categories, blended mixed deposits, salutatory mixed deposits and complex mixed deposits, and the complex mixed deposits can be divided into complex mixed depositsⅠand complex mixed depositsⅡ.In the study area, complex mixed depositsⅠis developing and complex mixed depositsⅡ is not developing. This paper analyses the mixed deposits of study area carefully, such as geological setting, petrological characteristic and depositional environment, etcl, establishes mixed sedimentaary model and discusses controlling factor of the mixed deposits.
- Shanghe region /
- the middle submember of Member 1 of Shahejie Formation /
- mixed sedimentation characteristics /
- mixed sedimentary type /
- mixed sedimentary model

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[1]	李怡霖, 李飞, 李翔, 王夏, 李杨凡, 王曾俊, 易楚恒, 曾伟, 李雅兰. 寒武系第二统浅水混合沉积发育特征及影响因素——以陕南朱家坝剖面仙女洞组为例 . 沉积学报, 2024, 42(5): 1639-1652. doi: 10.14027/j.issn.1000-0550.2022.116
[2]	刘佳庚, 王艳忠, 操应长, 孙沛沛, 何旭豪, 何瑞武, 郭迎春. 惠民凹陷大芦家地区沙一中亚段沉积特征及储层评价 . 沉积学报, 2023, 41(3): 855-866. doi: 10.14027/j.issn.1000-0550.2021.115
[3]	王昌勇, 刘帅, 李胡蝶, 常玖, 许兴斌, 范亚楠, 旷红伟. 神农架地区中元古界混合沉积特征及其发育模式 . 沉积学报, 2022, 40(6): 1649-1659. doi: 10.14027/j.issn.1000-0550.2021.051
[4]	李泉泉, 鲍志东, 肖毓祥, 陈建阳, 李忠诚, 王振军, 刘敏昭, 李卓伦, 许西挺, 操凡. 混合沉积研究进展与展望 . 沉积学报, 2021, 39(1): 153-167. doi: 10.14027/j.issn.1000-0550.2020.140
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[7]	徐伟, 杜晓峰, 黄晓波, 宋章强, 李正宇. 混合沉积研究进展与关键问题 . 沉积学报, 2019, 37(2): 225-238. doi: 10.14027/j.issn.1000-0550.2018.152
[8]	霍少川, 董桂玉, 王兵杰, 张振国, 刘金华, 刘建宁, 曹玉鹏, 冷春鹏. 金湖凹陷阜宁组二段混合沉积研究 . 沉积学报, 2019, 37(1): 177-188. doi: 10.14027/j.issn.1000-0550.2018.119
[9]	王越. 新疆塔尔朗沟剖面中二叠统扇三角洲混合沉积特征及模式 . 沉积学报, 2019, 37(5): 922-933. doi: 10.14027/j.issn.1000-0550.2018.190
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[16]	江茂生, 沙庆安, 刘敏. 华北地台下中寒武统碳酸盐与陆源碎屑混合沉积──以山东张夏地区为例 . 沉积学报, 1996, 14(S1): 63-74.
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[18]	朱如凯, 孟祥化, 葛铭. 巴彦浩特盆地东缘中奥陶统混合型深水重力流沉积层序及其旋回 . 沉积学报, 1994, 12(2): 77-85.
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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

董桂玉

成都理工大学沉积地质研究院成都 610059

通讯作者: 董桂玉

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-06-10

关键词:

沙一中 /

摘要: 商河地区沙一中广泛发育陆源碎屑与湖相碳酸盐的混合沉积。本文将混积层系、混积岩和呈零星分布的一起定义为广义的混合沉积，并且对于混合沉积来讲，没有一个具体的组分含量标准，只要该沉积物(岩)的确为陆源碎屑与碳酸盐的沉积，而非成岩作用或以后改造的假混合就可认定为混合沉积。研究区内混合沉积特征为陆源碎屑与湖相碳酸盐以较高的频率交互沉积和同一岩层内陆源碎屑组分与碳酸盐组分混合沉积，混合沉积的类型分为三类，即渐变式混合沉积、突变式混合沉积和复合式混合沉积，其中复合式沉积分为复合式沉积Ⅰ和复合式沉积Ⅱ，研究区内复合式沉积Ⅰ发育，复合式沉积Ⅱ不发育。并且本文从研究区混合沉积的区域地质背景、岩石学特征、沉积环境等方面进行了详细分析，建立了混合沉积相模式，进而对混合沉积的控制因素进行了讨论。

English Abstract

Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

DONG Guiyu

Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059

Corresponding author: DONG Guiyu

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2007-06-10

Keywords:

Abstract: Mixed deposits, which is composed of terrigenous fragment and carbonate of lagoonal facies, develops extensively in the middle submember of Member 1 of Shahejie Formation of Shanghe Area. This paper definite mixed deposited which includes Hunji sequence, Hunji rock and some sporadic distribution, and as far as mixed deposits in a broad sense, and there is not a concrete standard range, if only it is for the reason the sediment or sedimentary rock deposits to terrigenous fragment and carbonate not for false mixed to sedimentation or transformation of sedimentation, it can be deeply convinced to be mixed deposits. In the study area, the characteristics of mixed deposits are interbedded strata between terrigenous fragment and carbonate of lagoonal facies in high frequency and mixing deposited between terrigenous fragment constituent and carbonate constituent in one layer. Mixed sedimentary type can be divided into 3 categories, blended mixed deposits, salutatory mixed deposits and complex mixed deposits, and the complex mixed deposits can be divided into complex mixed depositsⅠand complex mixed depositsⅡ.In the study area, complex mixed depositsⅠis developing and complex mixed depositsⅡ is not developing. This paper analyses the mixed deposits of study area carefully, such as geological setting, petrological characteristic and depositional environment, etcl, establishes mixed sedimentaary model and discusses controlling factor of the mixed deposits.

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

引用本文:

董桂玉. 惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例[J]. 沉积学报, 2007, 25(3): 343-350.

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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

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Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

Corresponding author: DONG Guiyu

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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

成都理工大学沉积地质研究院成都 610059

通讯作者: 董桂玉

English Abstract

Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059

Corresponding author: DONG Guiyu

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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

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Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

Corresponding author: DONG Guiyu

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惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例

成都理工大学沉积地质研究院 成都 610059

通讯作者: 董桂玉

English Abstract

Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: taking Shanghe area in Shandong Province for an example

Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059

Corresponding author: DONG Guiyu

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董桂玉

成都理工大学沉积地质研究院成都 610059