基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

赖海成; 李志忠; 靳建辉; 邓涛; 姜锋; 于晓莉; 苑秀全; 申健玲; 龚松柏

doi:10.14027/j.cnki.cjxb.2016.04.004

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

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

赖海成, 李志忠, 靳建辉, 邓涛, 姜锋, 于晓莉, 苑秀全, 申健玲, 龚松柏

文章导航 > 沉积学报 > 2016 > 34(4): 645-652

赖海成, 李志忠, 靳建辉, 邓涛, 姜锋, 于晓莉, 苑秀全, 申健玲, 龚松柏. 基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究[J]. 沉积学报, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004

引用本文:

LAI HaiCheng, LI ZhiZhong, JIN JianHui, DENG Tao, JIANG Feng, YU XiaoLi, YUAN XiuQuan, SHEN JianLing, GONG SongBai. Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar[J]. Acta Sedimentologica Sinica, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004

Citation:

LAI HaiCheng, LI ZhiZhong, JIN JianHui, DENG Tao, JIANG Feng, YU XiaoLi, YUAN XiuQuan, SHEN JianLing, GONG SongBai. Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar[J]. Acta Sedimentologica Sinica, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004

引用本文:

Citation:

LAI HaiCheng, LI ZhiZhong, JIN JianHui, DENG Tao, JIANG Feng, YU XiaoLi, YUAN XiuQuan, SHEN JianLing, GONG SongBai. Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar[J]. Acta Sedimentologica Sinica, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

赖海成^1,2,
李志忠^1,2,3,,
靳建辉^1,2,3,
邓涛^1,2,
姜锋^1,2,
于晓莉^1,2,
苑秀全^1,2,
申健玲^1,2,
龚松柏^1,2

1.
福建师范大学地理科学学院福州 350007;
2.
湿润亚热带生态地理过程省部共建教育部重点实验室福州 350007;
3.
福建师范大学地理研究所福州 350007

基金项目: 国家自然科学基金项目（41271031,41301012）；国家自然科学基金委员会—福建省人民政府促进海峡两岸科技合作联合基金（U1405231）

详细信息

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者:
李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

中图分类号: P512.2

计量

文章访问数: 543
HTML全文浏览量: 0
PDF下载量: 900
被引次数: 0

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

LAI HaiCheng^1,2,
LI ZhiZhong^{1,2,3
,},
JIN JianHui^1,2,3,
DENG Tao^1,2,
JIANG Feng^1,2,
YU XiaoLi^1,2,
YUAN XiuQuan^1,2,
SHEN JianLing^1,2,
GONG SongBai^1,2

1.
College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China;
2.
Key Laboratory of Humid Subtropical Eco-geographical Process (Fujian Normal University), Ministry of Education, Fuzhou 350007, China;
3.
Institute of Geography, Fujian Normal University, Fuzhou 350007, China

Funds: National Natural Science Foundation of China, No. 41271031, 41301012; National Natural Science Foundation of China-Joint Foundation for Promoting Scientific and Technological Cooperation between two sides of the Straits of Fujian Gov. CN, No. U1405231

摘要

摘要: 福建海坛岛北部海岸发育一座覆盖淡灰黄色风成砂层、相对高度达30 m的大沙山，外貌很像风成大沙丘，但同时又具有冲积扇形态。其成因和沉积环境有待考证，而探明大沙山内部沉积构造是判别其成因的主要途径之一。在野外考察的基础上，运用探地雷达（GPR）对大沙山内部沉积构造进行探测，获得约20 m深度范围内的沉积构造图像数据。结果表明：大沙山中上部发育由棱角状砾石或粗砂细砂组成的沉积旋回和沟槽沉积构造，显示出冲积扇上部的沉积构造组合特点；中下部层面中交替呈现弧形沉积构造，大沙山南侧发育有向南倾斜28°～30°的前积层理。结合大沙山西侧冲沟剖面沉积构造、大沙山表面的棱角状砾石特征以及现代风沙地貌分布规律，初步认为大沙山是山前多期沟谷洪流携带的碎屑物沉积形成的冲积扇残余堆积体，沉积间隙受海岸带风沙活动影响。
- 探地雷达 /
- 冲积扇 /
- 沉积构造 /
- 海岸带 /
- 福建海坛岛
Abstract: Alluvial fan could provide valuable information in recording local climate change, reflecting neotectonic movement and rebuilding paleogeographic environment. Compared with inland areas, coastal zone as the interface of three layers of atmosphere, ocean and land has distinct differences in depositional environment, resulting in unique material sources and dynamic condition. Thus, alluvial fan in coastal zone may have special geological landscape process and sedimentary structure characteristics. There is a great sandy hill which covered by grayish yellow eolian sand layer in the northern Junshan along the coast of Haitan island, Fujian Province. It seems to be a big aeolian dunes, but in fact alluvial fan shape. In this paper, we used the ground penetrating radar (GPR) to detect the internal sedimentary structure of the great sandy hill, and tried to find out its origin. Detection results show that in the middle-upper part of the great sandy hill, there developed sedimentary cycle composed of angular gravel or coarse to fine sand and groove depositional structure, which presents the depositional characteristics of traditional alluvial fan; in the middle-lower part of the great sandy hill, there developed curved depositional structure presented alternately in the layer. Based on the results, we also found that detecting depth of the alluvial fan record the wide range of three to five times of piedmont ancient flood sedimentary history. Combining the geological investigation in the great sandy hill, we assumed that the great sandy hill is the remnant of alluvial fan, which contains the characteristics of aeolian sediments along the coastal zone. The research is benefit for further understanding of the evolution of paleogeographic environment in the coastal zone of South China, and enriching the research of dynamic geomorphological processes on coastal zone and the sedimental structures of alluvial fan.
- ground penetrating radar (GPR) /
- alluvial fan /
- sedimentary structures /
- coastal zone /
- Haitan Island of Fujian

HTML全文

参考文献(0)

[1]	时志强, 彭深远, 王美玲, 乔丹. 假泥裂：上扬子地区下三叠统飞仙关组灰岩薄层中的网纹沉积构造 . 沉积学报, 2024, 42(4): 1200-1211. doi: 10.14027/j.issn.1000-0550.2023.032
[2]	高志勇, 冯佳睿, 石雨昕, 罗忠, 张宇航. 干旱气候下冲积扇—冲积平原曲流河沉积演化过程与展布 . 沉积学报, 2023, 41(6): 1954-1970. doi: 10.14027/j.issn.1000-0550.2022.122
[3]	郭芪恒, 史书婷, 金振奎, 李阳, 王金艺, 任奕霖, 王凌. 河口湾潮坪潮汐水道发育特征及地质意义 ——以钱塘江为例 . 沉积学报, 2022, 40(1): 182-191. doi: 10.14027/j.issn.1000-0550.2020.071
[4]	陈留勤, 李鹏程, 郭福生, 刘鑫, 李馨敏. 粤北丹霞盆地晚白垩世丹霞组沉积相及古气候意义 . 沉积学报, 2019, 37(1): 17-29. doi: 10.14027/j.issn.1000-0550.2018.118
[5]	徐希旺, 陈世悦, 王越, 张关龙, 鄢继华, 汪誉新, 李佳, 邓远. 吐哈盆地大河沿地区塔尔朗组细粒沉积岩特征 . 沉积学报, 2017, 35(4): 705-713. doi: 10.14027/j.cnki.cjxb.2017.04.005
[6]	白毛伟, 谢小平, 陈芝聪, 叶卉, 徐文阳, 江若辰, 李冰, 李佳丽. 龙门山北东段山前涪江第四纪冲洪积扇地貌演化及其构造响应 . 沉积学报, 2017, 35(1): 85-92. doi: 10.14027/j.cnki.cjxb.2017.01.009
[7]	孟祥超, 蒋庆平, 李亚哲, 孔垂显, 吴爱成, 王力宝, 贾俊飞, 肖芳伟, 刘午牛. 同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例 . 沉积学报, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014
[8]	印森林, 刘忠保, 陈燕辉, 吴小军. 冲积扇研究现状及沉积模拟实验——以碎屑流和辫状河共同控制的冲积扇为例 . 沉积学报, 2017, 35(1): 10-23. doi: 10.14027/j.cnki.cjxb.2017.01.002
[9]	. 广西海岸带近百年来人类活动影响下环境演变的沉积记录 . 沉积学报, 2012, 30(2): 325-332.
[10]	刘疆. 广西横县六景古近纪冲积物特征 . 沉积学报, 2009, 27(1): 87-93.
[11]	罗平, 张兴阳, 顾家裕, 汪圣国, 林鹏. 塔里木盆地奥陶系生物礁露头的地球物理特征 . 沉积学报, 2003, 21(3): 423-427.
[12]	郭建华, 朱美衡, 杨申谷, 刘辰生. 辽河盆地曙一区馆陶组湿地冲积扇沉积 . 沉积学报, 2003, 21(3): 367-372.
[13]	孙景耀, 陈辉军, 朱明春. 黄河济南以下河段某些异常地质作用及几种典型沉积构造研究 . 沉积学报, 2001, 19(1): 79-84.
[14]	沈浩杰. 东海大陆架南缘海域地层声学剖面及地质解释 . 沉积学报, 1999, 17(1): 78-83.
[15]	吴智勇, 郭建华, 吴东胜, 何宏. 东濮断陷湖盆下第三系沙二段的冲积扇沉积 . 沉积学报, 1999, 17(3): 449-453.
[16]	董冬. 断陷湖盆陡坡带碎屑流沉积单元的沉积序列和储集特征——以东营凹陷永安地区为例 . 沉积学报, 1999, 17(4): 566-571.
[17]	章泽军. 长——平陆相红色盆地北东段量化沉积学特征及其演化 . 沉积学报, 1998, 16(4): 55-61.
[18]	梁百和, 朱素琳. 湘西吉首地区寒武系碳酸盐岩沉积环境的初步探讨 . 沉积学报, 1992, 10(2): 39-44.
[19]	柯保嘉, 陈昌明, 陈志明, 汪寿松, 姜好仁, 惠斌耀. 鄂尔多斯盆地西缘砾质冲积扇沉积学特征 . 沉积学报, 1991, 9(3): 11-21.
[20]	李凡. 白沙口海岸带沉积物的床面形态及层理构造 . 沉积学报, 1983, 1(3): 98-108.

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: 543
HTML全文浏览量: 0
PDF下载量: 900
被引次数: 0

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

1. 福建师范大学地理科学学院福州 350007;

2. 湿润亚热带生态地理过程省部共建教育部重点实验室福州 350007;

3. 福建师范大学地理研究所福州 350007

基金项目: 国家自然科学基金项目（41271031,41301012）；国家自然科学基金委员会—福建省人民政府促进海峡两岸科技合作联合基金（U1405231）

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者: 李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

收稿日期: 2015-06-29
修回日期: 2015-12-02
刊出日期: 2016-08-10

中图分类号: P512.2

关键词:

探地雷达 /

冲积扇 /

沉积构造 /

海岸带 /

福建海坛岛

摘要: 福建海坛岛北部海岸发育一座覆盖淡灰黄色风成砂层、相对高度达30 m的大沙山，外貌很像风成大沙丘，但同时又具有冲积扇形态。其成因和沉积环境有待考证，而探明大沙山内部沉积构造是判别其成因的主要途径之一。在野外考察的基础上，运用探地雷达（GPR）对大沙山内部沉积构造进行探测，获得约20 m深度范围内的沉积构造图像数据。结果表明：大沙山中上部发育由棱角状砾石或粗砂细砂组成的沉积旋回和沟槽沉积构造，显示出冲积扇上部的沉积构造组合特点；中下部层面中交替呈现弧形沉积构造，大沙山南侧发育有向南倾斜28°～30°的前积层理。结合大沙山西侧冲沟剖面沉积构造、大沙山表面的棱角状砾石特征以及现代风沙地貌分布规律，初步认为大沙山是山前多期沟谷洪流携带的碎屑物沉积形成的冲积扇残余堆积体，沉积间隙受海岸带风沙活动影响。

English Abstract

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

1. College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China;

2. Key Laboratory of Humid Subtropical Eco-geographical Process (Fujian Normal University), Ministry of Education, Fuzhou 350007, China;

3. Institute of Geography, Fujian Normal University, Fuzhou 350007, China

Received Date: 2015-06-29
Rev Recd Date: 2015-12-02
Publish Date: 2016-08-10

Keywords:

Abstract: Alluvial fan could provide valuable information in recording local climate change, reflecting neotectonic movement and rebuilding paleogeographic environment. Compared with inland areas, coastal zone as the interface of three layers of atmosphere, ocean and land has distinct differences in depositional environment, resulting in unique material sources and dynamic condition. Thus, alluvial fan in coastal zone may have special geological landscape process and sedimentary structure characteristics. There is a great sandy hill which covered by grayish yellow eolian sand layer in the northern Junshan along the coast of Haitan island, Fujian Province. It seems to be a big aeolian dunes, but in fact alluvial fan shape. In this paper, we used the ground penetrating radar (GPR) to detect the internal sedimentary structure of the great sandy hill, and tried to find out its origin. Detection results show that in the middle-upper part of the great sandy hill, there developed sedimentary cycle composed of angular gravel or coarse to fine sand and groove depositional structure, which presents the depositional characteristics of traditional alluvial fan; in the middle-lower part of the great sandy hill, there developed curved depositional structure presented alternately in the layer. Based on the results, we also found that detecting depth of the alluvial fan record the wide range of three to five times of piedmont ancient flood sedimentary history. Combining the geological investigation in the great sandy hill, we assumed that the great sandy hill is the remnant of alluvial fan, which contains the characteristics of aeolian sediments along the coastal zone. The research is benefit for further understanding of the evolution of paleogeographic environment in the coastal zone of South China, and enriching the research of dynamic geomorphological processes on coastal zone and the sedimental structures of alluvial fan.

引用本文:

Citation:

LAI HaiCheng, LI ZhiZhong, JIN JianHui, DENG Tao, JIANG Feng, YU XiaoLi, YUAN XiuQuan, SHEN JianLing, GONG SongBai. Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar[J]. Acta Sedimentologica Sinica, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004

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

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者:
李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

计量

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

计量

目录

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

1. 福建师范大学地理科学学院福州 350007;

2. 湿润亚热带生态地理过程省部共建教育部重点实验室福州 350007;

3. 福建师范大学地理研究所福州 350007

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者: 李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

English Abstract

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

1. College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China;

2. Key Laboratory of Humid Subtropical Eco-geographical Process (Fujian Normal University), Ministry of Education, Fuzhou 350007, China;

3. Institute of Geography, Fujian Normal University, Fuzhou 350007, China

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

作者简介: 赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者: 李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

计量

出版历程

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

计量

出版历程

目录

基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究

doi: 10.14027/j.cnki.cjxb.2016.04.004

1. 福建师范大学地理科学学院 福州 350007; 2. 湿润亚热带生态地理过程省部共建教育部重点实验室 福州 350007; 3. 福建师范大学地理研究所 福州 350007

作者简介: 赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者: 李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

English Abstract

Unravelling the Sedimentary Structure of Coastal Alluvial Fan and its Origin in the Northern Haitan Island, Fujian, Using Ground Penetrating Radar

1. College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; 2. Key Laboratory of Humid Subtropical Eco-geographical Process (Fujian Normal University), Ministry of Education, Fuzhou 350007, China; 3. Institute of Geography, Fujian Normal University, Fuzhou 350007, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

通讯作者:
李志忠,男,教授,E-mail:lizz@fjnu.edu.cn

1. 福建师范大学地理科学学院福州 350007;

2. 湿润亚热带生态地理过程省部共建教育部重点实验室福州 350007;

3. 福建师范大学地理研究所福州 350007

作者简介:
赖海成,男,1992年出生,硕士研究生,地貌过程与环境演变,E-mail:laihaicheng2015@163.com

1. College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China;

2. Key Laboratory of Humid Subtropical Eco-geographical Process (Fujian Normal University), Ministry of Education, Fuzhou 350007, China;

3. Institute of Geography, Fujian Normal University, Fuzhou 350007, China