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

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

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

详细信息

通讯作者:
董桂玉

计量

文章访问数: 1979
HTML全文浏览量: 19
PDF下载量: 721
被引次数: 0

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

HTML全文

参考文献(0)

[1]	朱柏宇, 印森林, 郭海平, 唐攀, 赵俊威, 陈旭, 雷章树. 陆相混合细粒岩沉积微相及其对甜点的控制作用 . 沉积学报, 2024, 42(3): 839-856. doi: 10.14027/j.issn.1000-0550.2023.051
[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
[5]	曾楷, 李飞, 龚峤林, 唐浩, 苏成鹏, 车正强, 邓嘉婷, 胡广, 李凌, 曾伟, 谭秀成. 寒武系第二统仙女洞组混合沉积特征及古环境意义——以川北旺苍唐家河剖面为例 . 沉积学报, 2020, 38(1): 166-181. doi: 10.14027/j.issn.1000-0550.2019.015
[6]	邓双林, 宋金民, 刘树根, 罗平, 李智武, 杨迪, 孙玮, 李金玺, 余晶洁, 李立基. 四川盆地灯影组三段混积特征及其地质意义 . 沉积学报, 2020, 38(3): 598-609. doi: 10.14027/j.issn.1000-0550.2019.109
[7]	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
[8]	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
[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
[10]	伏美燕, 李娜, 黄茜, 刘磊. 滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例 . 沉积学报, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003
[11]	谈明轩, 朱筱敏, 耿名扬, 刘常妮. 沉积物重力流流体转化沉积-混合事件层 . 沉积学报, 2016, 34(6): 1108-1119. doi: 10.14027/j.cnki.cjxb.2016.06.009
[12]	. 柴达木盆地北缘下干柴沟组下段湖相混合沉积发育特征及其对储层的影响 . 沉积学报, 2013, 31(04): 724-729.
[13]	. 辽河西部凹陷雷家地区古近系沙四段混合沉积特征研究 . 沉积学报, 2012, 30(2): 283-290.
[14]	曹桐生. 内蒙古阿尔山地区下寒武统苏中组混合沉积特征及形成环境研究 . 沉积学报, 2011, 29(1): 55-63.
[15]	郭福生. 浙江江山藕塘底组陆源碎屑与碳酸盐混合沉积特征及其构造意义 . 沉积学报, 2004, 22(1): 136-141.
[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.
[17]	汪云亮, 刘峰, 杨世发, 孙书勤. 沉积岩系互稀释混合元素丰度关系 . 沉积学报, 1995, 13(3): 137-146.
[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.
[19]	刘文汇, 徐永昌. 天然气的混合类型及其判识 . 沉积学报, 1993, 11(3): 44-51.
[20]	杨朝青, 沙庆安. 云南曲靖中泥盆统曲靖组的沉积环境:一种陆源碎屑与海相碳酸盐的混合沉积 . 沉积学报, 1990, 8(2): 59-66.

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: 1979
HTML全文浏览量: 19
PDF下载量: 721
被引次数: 0

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.

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

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

通讯作者:
董桂玉

计量

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

计量

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

通讯作者: 董桂玉

计量

出版历程

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

计量

出版历程

目录

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

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
董桂玉

成都理工大学沉积地质研究院成都 610059