现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

禚喜准; 张林炎; 陈骁帅; 闫清涣; 崔建军; 杨雨

doi:10.14027/j.issn.1000-0550.2018.117

ISSN 1000-0550 CN 62-1038/P

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现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

禚喜准, 张林炎, 陈骁帅, 闫清涣, 崔建军, 杨雨

文章导航 > 沉积学报 > 2018 > 36(6): 1119-1130

禚喜准, 张林炎, 陈骁帅, 闫清涣, 崔建军, 杨雨. 现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示[J]. 沉积学报, 2018, 36(6): 1119-1130. doi: 10.14027/j.issn.1000-0550.2018.117

引用本文:

ZHUO XiZhun, ZHANG LinYan, CHEN XiaoShuai, YAN QingHuan, CUI JianJun, YANG Yu. The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake[J]. Acta Sedimentologica Sinica, 2018, 36(6): 1119-1130. doi: 10.14027/j.issn.1000-0550.2018.117

Citation:

ZHUO XiZhun, ZHANG LinYan, CHEN XiaoShuai, YAN QingHuan, CUI JianJun, YANG Yu. The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake[J]. Acta Sedimentologica Sinica, 2018, 36(6): 1119-1130. doi: 10.14027/j.issn.1000-0550.2018.117

引用本文:

Citation:

现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

1.
辽宁工程技术大学地质系, 辽宁阜新 123000;
2.
中国地质科学院地质力学研究所, 北京 100081

基金项目: 国家自然科学基金项目（41402101）；辽宁省教育厅一般项目（14-1167）

详细信息

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者:
张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

中图分类号: P512.2

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文章访问数: 309
HTML全文浏览量: 9
PDF下载量: 541
被引次数: 0

The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

1.
Department of Geology, Liaoning Technical University, Fuxin, Liaoning 123000, China;
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Funds: National Natural Science Foundation of China, No. 41402101; Liaoning Provincial Department of Education General Project, No. 14-1167

摘要

摘要: 盐类析出模拟实验有助于增进对成盐模式的理解，但运用正演模拟进行类比分析的前提是实验模型与盐湖原型的沉积机理具有相似性。基于现代盐湖的野外地质调查，对岩盐析出模型与现代盐湖在沉积物的结构、空间分布以及沉积机理的相似性等方面进行了对比分析。研究表明，深度较小的水槽，以空气-卤水界面析盐和蒸发泵成盐为主；而对于水深和规模较大的现代盐湖来说，上述两种成盐方式主要分布于湖盆边缘的浅水区，水深较大的斜坡带和洼陷带以卤水-湖底沉积物界面析盐为主，反映了水深较浅的水槽无法再现古代盐湖的湖盆底形和沉积物分布特征。现代沉积调查显示，在封闭的内陆盐湖盆地中，岩盐通常形成于湖退期-低位期，其沉积厚度从湖盆边缘向洼陷中心有逐渐增大的趋势，即岩盐的沉积中心和洼陷中心保持一致。岩盐的结构跟沉积环境密切相关，盆缘滨岸带的岩盐多为薄层状与砂岩共存，晶体粒度小；而洼陷带以粗粒结晶的盐岩为主，单层厚度大，常与暗色泥岩互层。岩盐沉积中心和洼陷中心关系的厘定，对于湖盆的古地貌恢复和沉积体的预测，具有重要的理论和现实意义。
- 岩盐 /
- 水槽模拟 /
- 类比分析 /
- 现代沉积 /
- 成盐模式
Abstract: Salt precipitation simulation experiments help enhance our understanding of salt-forming models; however, the premise of using forward modeling is that the experimental model is similar to the sedimentary mechanism of the salt lake prototype. Based on the field geological survey of modern salt lakes, this paper makes an analogy analysis of salt precipitation models and modern salt lakes, in terms of sediment texture, spatial distribution characteristics, and similarity of sedimentation mechanism. The results show that it is mainly the air-brine interface salt and salt formation through evaporation in the smaller depth of the flume; and for the deeper water and large-scale modern salt lake, the two kinds of salt-forming methods are mainly distributed in the shallow waters of the lake basin. The slopes and depressions with larger water depth are mainly brine-lake sediments interfaced with salt precipitation, which reflect the shallow water of the flume cannot reproduce lake basin bottom and sediment distribution characteristics of the ancient salt lake. Modern sediments show that in the closed inland salt lake basin, the rock salt is mainly formed in the lake retreat period-low period, and its depositional thickness gradually increases from the edge of the lake basin to the depression center, i.e. the deposition center of the rock salt and the depression center are consistent. The texture of rock salt is closely related to the sedimentary environment. The rock salt in the edge of the basin mostly coexists with the sandstone, and the grain size is small, while the depression is mainly composed of coarse-grained salt rock, single-layer thickness and is large, often with dark mudstone interbeds. The relationship between the center of the rock salt deposition and the center of the depression is of great theoretical and practical significance for the restoration of paleogeomorphology and sedimentary body of the lake basin.
- rock salt /
- flume simulation experiment /
- analogy analysis /
- modern sedimentation /
- salt-forming model

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[1]	吕奇奇, 王林, 罗顺社, 刘江艳, 闫红果, 孙学虎, 张蕾. 基于单因素水槽模拟实验的湖相细粒浊流沉积动力学机制初探【水槽沉积模拟实验专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.143
[2]	孙浩南, 谈明轩, 姚鹏. 环形水槽物理模拟的沉积学应用进展与发展趋势【水槽沉积模拟实验专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.032
[3]	冯阵东, 李令喜, 吴伟, 王光绪, 王运所, 于静. 河床底部沙火山特征、演化及其研究意义 . 沉积学报, 2022, 40(2): 465-472. doi: 10.14027/j.issn.1000-0550.2021.043
[4]	王菁, 李相博, 刘化清, 张志杰, 完颜容, 王宏波, 黄军平. 陆相盆地滩坝砂体沉积特征及其形成与保存条件——以青海湖现代沉积为例 . 沉积学报, 2019, 37(5): 1016-1030. doi: 10.14027/j.issn.1000-0550.2019.038
[5]	张可, 吴胜和, 冯文杰, 郑定业, 喻宸, 刘照玮. 砂质辫状河心滩坝的发育演化过程探讨——沉积数值模拟与现代沉积分析启示 . 沉积学报, 2018, 36(1): 81-91. doi: 10.3969/j.issn.1000-0550.2018.010
[6]	商晓飞, 郭颖, 侯加根, 段太忠, 赵磊. 湖泊滨岸砂坝内部结构特征剖析及其地质意义——以峡山湖现代砂坝沉积为例 . 沉积学报, 2018, 36(5): 877-889. doi: 10.14027/j.issn.1000-0550.2018.067
[7]	徐中波, 申春生, 陈玉琨, 康凯, 罗宪波, 何新容, 李林, 张博文. 砂质辫状河储层构型表征及其对剩余油的控制——以渤海海域P油田为例 . 沉积学报, 2016, 34(2): 375-385. doi: 10.14027/j.cnki.cjxb.2016.02.016
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[9]	郭岭, 贾超超, 朱毓, 任文波, 段锦川. 现代渭河西安段沉积体沉积相与岩相特征 . 沉积学报, 2015, 33(3): 543-550. doi: 10.14027/j.cnki.cjxb.2015.03.012
[10]	陈仕臻, 林承焰, 任丽华, 刘文婧, 陈和平, 黄文松. 砂质辫状河沉积模式的建立——以委内瑞拉奥里诺科重油带H区块为例 . 沉积学报, 2015, 33(5): 965-971. doi: 10.14027/j.cnki.cjxb.2015.05.012
[11]	王伟锋, 张美. 洪泽凹陷赵集次凹阜宁组四段盐岩深水再沉积成因探讨 . 沉积学报, 2015, 33(2): 242-253. doi: 10.14027/j.cnki.cjxb.2015.02.004
[12]	. 敞流沉积环境中“浅水三角洲前缘砂体体系”研究 . 沉积学报, 2014, 32(2): 260-269.
[13]	于革, 桂峰. 太湖流域营养盐沉积200年的历史模拟研究 . 沉积学报, 2006, (6): 849-856.
[14]	于革桂峰. 太湖流域营养盐沉积200年的历史模拟研究 . 沉积学报, 2006, 24(06): 849-856.
[15]	谢庆宾, 朱筱敏, 管守锐, 王贵文, 刘少宾, 张周良, 陈方鸿, 薛培华, 韩德馨. 中国现代网状河流沉积特征和沉积模式 . 沉积学报, 2003, 21(2): 219-227.
[16]	王平在, 王俊玲. 嫩江现代河流沉积层序及沉积模式 . 沉积学报, 2003, 21(2): 228-233.
[17]	宋春晖, 王新民, 师永民, 晁吉俊, 武安斌. 青海湖现代滨岸沉积微相及其特征 . 沉积学报, 1999, 17(1): 51-57.
[18]	王新民, 宋春晖, 师永民, 晁吉俊, 武安斌. 青海湖现代沉积环境与沉积相特征 . 沉积学报, 1997, 15(S1): 157-162.
[19]	张彭熹. 中国蒸发岩研究中几个值得重视的地质问题的讨论 . 沉积学报, 1992, 10(3): 78-84.
[20]	张吉森, 曾少华, 黄建松, 马振芳, 王泽中. 鄂尔多斯东部地区岩盐的发现、成因及其意义 . 沉积学报, 1991, 9(2): 34-43.

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现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

1. 辽宁工程技术大学地质系, 辽宁阜新 123000;

2. 中国地质科学院地质力学研究所, 北京 100081

基金项目: 国家自然科学基金项目（41402101）；辽宁省教育厅一般项目（14-1167）

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者: 张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

收稿日期: 2017-11-24
修回日期: 2018-01-07
刊出日期: 2018-12-10

中图分类号: P512.2

关键词:

岩盐 /

摘要: 盐类析出模拟实验有助于增进对成盐模式的理解，但运用正演模拟进行类比分析的前提是实验模型与盐湖原型的沉积机理具有相似性。基于现代盐湖的野外地质调查，对岩盐析出模型与现代盐湖在沉积物的结构、空间分布以及沉积机理的相似性等方面进行了对比分析。研究表明，深度较小的水槽，以空气-卤水界面析盐和蒸发泵成盐为主；而对于水深和规模较大的现代盐湖来说，上述两种成盐方式主要分布于湖盆边缘的浅水区，水深较大的斜坡带和洼陷带以卤水-湖底沉积物界面析盐为主，反映了水深较浅的水槽无法再现古代盐湖的湖盆底形和沉积物分布特征。现代沉积调查显示，在封闭的内陆盐湖盆地中，岩盐通常形成于湖退期-低位期，其沉积厚度从湖盆边缘向洼陷中心有逐渐增大的趋势，即岩盐的沉积中心和洼陷中心保持一致。岩盐的结构跟沉积环境密切相关，盆缘滨岸带的岩盐多为薄层状与砂岩共存，晶体粒度小；而洼陷带以粗粒结晶的盐岩为主，单层厚度大，常与暗色泥岩互层。岩盐沉积中心和洼陷中心关系的厘定，对于湖盆的古地貌恢复和沉积体的预测，具有重要的理论和现实意义。

English Abstract

The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

1. Department of Geology, Liaoning Technical University, Fuxin, Liaoning 123000, China;

2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Funds: National Natural Science Foundation of China, No. 41402101; Liaoning Provincial Department of Education General Project, No. 14-1167

Received Date: 2017-11-24
Rev Recd Date: 2018-01-07
Publish Date: 2018-12-10

Keywords:

Abstract: Salt precipitation simulation experiments help enhance our understanding of salt-forming models; however, the premise of using forward modeling is that the experimental model is similar to the sedimentary mechanism of the salt lake prototype. Based on the field geological survey of modern salt lakes, this paper makes an analogy analysis of salt precipitation models and modern salt lakes, in terms of sediment texture, spatial distribution characteristics, and similarity of sedimentation mechanism. The results show that it is mainly the air-brine interface salt and salt formation through evaporation in the smaller depth of the flume; and for the deeper water and large-scale modern salt lake, the two kinds of salt-forming methods are mainly distributed in the shallow waters of the lake basin. The slopes and depressions with larger water depth are mainly brine-lake sediments interfaced with salt precipitation, which reflect the shallow water of the flume cannot reproduce lake basin bottom and sediment distribution characteristics of the ancient salt lake. Modern sediments show that in the closed inland salt lake basin, the rock salt is mainly formed in the lake retreat period-low period, and its depositional thickness gradually increases from the edge of the lake basin to the depression center, i.e. the deposition center of the rock salt and the depression center are consistent. The texture of rock salt is closely related to the sedimentary environment. The rock salt in the edge of the basin mostly coexists with the sandstone, and the grain size is small, while the depression is mainly composed of coarse-grained salt rock, single-layer thickness and is large, often with dark mudstone interbeds. The relationship between the center of the rock salt deposition and the center of the depression is of great theoretical and practical significance for the restoration of paleogeomorphology and sedimentary body of the lake basin.

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现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者:
张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

计量

The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

计量

目录

现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

1. 辽宁工程技术大学地质系, 辽宁阜新 123000;

2. 中国地质科学院地质力学研究所, 北京 100081

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者: 张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

English Abstract

The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

1. Department of Geology, Liaoning Technical University, Fuxin, Liaoning 123000, China;

2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

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现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

作者简介: 禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者: 张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

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The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

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现代盐湖沉积与岩盐析出模拟的相似性及其对成盐模式的启示

doi: 10.14027/j.issn.1000-0550.2018.117

1. 辽宁工程技术大学地质系, 辽宁阜新 123000; 2. 中国地质科学院地质力学研究所, 北京 100081

作者简介: 禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者: 张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

English Abstract

The Similarity of Salt-Forming between Flume Experiment and Modern Salt Lake

1. Department of Geology, Liaoning Technical University, Fuxin, Liaoning 123000, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

通讯作者:
张林炎,男,高级工程师,E-mail:zhanglinyan@126.com

1. 辽宁工程技术大学地质系, 辽宁阜新 123000;

2. 中国地质科学院地质力学研究所, 北京 100081

作者简介:
禚喜准,男,1981年出生,博士,副教授,层序地层学与储层沉积学,E-mail:zhuoxizhun@126.com

1. Department of Geology, Liaoning Technical University, Fuxin, Liaoning 123000, China;

2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China