障壁岛&mdash;潟湖沉积特征及模式:以美国普拉姆岛上更新统&mdash;全新统为例<sup>*</sup>

doi:10.7605/gdlxb.2022.06.077

古地理学报 ›› 2022, Vol. 24 ›› Issue (6): 1073-1083. doi: 10.7605/gdlxb.2022.06.077

• 岩相古地理学及沉积学 • 上一篇下一篇

障壁岛—潟湖沉积特征及模式:以美国普拉姆岛上更新统—全新统为例^*

李伟茹¹, 李志华², 李胜利³, 李顺利³, 邵家澍⁴

1 廊坊师范学院电子信息工程学院,河北廊坊 065000;
2 廊坊师范学院教育学院,河北廊坊 065000;
3 中国地质大学(北京)能源学院,北京 100083;
4 华北科技学院矿山安全学院,河北廊坊 065201

收稿日期:2022-05-09 修回日期:2022-08-15 出版日期:2022-12-01 发布日期:2022-12-05
通讯作者: 李志华,男,1986年生,博士,助理研究员,主要从事沉积学与地层学方面的研究工作。E-mail: abclizhi@126.com。
作者简介:李伟茹,女,1986年生,硕士,讲师,主要从事碎屑岩沉积学与构造地质方面的研究工作。E-mail: grace_9133@126.com。
基金资助:
*国家自然科学基金项目(编号: 42172112)和廊坊师范学院博士(后)科研启动项目(编号: XBQ202050)资助

Sedimentary characteristics and model of barrier island-lagoon: an example from the Upper Pleistocene-Holocene in Plum island,USA

LI Weiru¹, LI Zhihua², LI Shengli³, LI Shunli³, SHAO Jiashu⁴

1 School of Electronic Information Engineering,Langfang Normal University,Hebei Langfang 065000,China;
2 School of Education,Langfang Normal University,Hebei Langfang 065000,China;
3 School of Energy Resources,China University of Geosciences(Bejing),Beijing 100083,China;
4 School of Mine Safety, North China Institute of Science and Technology, Hebei Langfang 065201, China

Received:2022-05-09 Revised:2022-08-15 Online:2022-12-01 Published:2022-12-05
Contact: LI Zhihua,born in 1986,Ph.D.,assistant research fellow,is mainly engaged in research on sedimentology and stratigraphy. E-mail: abclizhi@126.com.
About author:LI Weiru,born in 1986,is a lecturer,mainly engaged in research on sedimentology and geology of clastic rocks. E-mail: grace_9133@126.com.
Supported by:
Co-funded by the National Natural Science Foundation of China(No.42172112),and PhD Project of Langfang Normal University(No. XBQ202050)

摘要/Abstract

摘要：

普拉姆岛(Plum island)是美国东北部缅因湾最大的障壁海岸,岛内向陆一侧为新英格兰地区最大潟湖和沼泽区,它们是晚第四纪末次冰期冰川作用和冰后期海岸作用的沉积响应。通过普拉姆岛研究区上更新统—全新统160个钻孔描述,识别出8种沉积物: 泥炭、冰川黏土、黏土、粉砂、细砂、中粗砂、砾、坠石。根据沉积物类型及其组合特征,结合沉积环境,共划分出8种沉积微相: 障壁沙丘、滨岸沙、水下临滨沙、河道、潮汐水道、潟湖、潮坪、沼泽。研究区在晚第四纪末次冰盛期(MIS2)被劳伦斯蒂德冰盖(Laurentide Ice Sheet)覆盖,发育冰川地貌,冰川泥覆盖在基岩之上,形成底层沉积; 冰后期(MIS1),冰盖消融,海平面发生变化,在冰川地貌鼓丘附近形成沙坝,最终沉积演化为障壁岛—潟湖环境,潟湖通过潮汐水道与广海相连通。

关键词: 普拉姆岛, 上更新统—全新统, 障壁岛—潟湖, 冰川沉积, 沉积微相, 沉积模式

Abstract:

Plum island is the largest barrier island in the Gulf of Maine in the northeastern United States. On the continental side of Plum island are the largest lagoon and salt marsh in New England,which are the sedimentary responses to the late Quaternary glacial and coastal processes. Through the description of 160 boreholes in the Upper Pleistocence-Holocene the Plum island study area,eight types of sediments were identified: peat,glacial clay,clay,silt,fine sand,medium-coarse sand,gravel and dropstone. According to the characteristics of sediments and deposition phenomena,the sedimentary microfacies of Plum island can be divided into eight types: barrier dune,beachface deposits,offshore sand sheet deposits,salt marsh,fluvial channel,tidal inlet channel,lagoon and tidal flat. During the Last Glacial Maximum(MIS2),the study area was covered by the Laurentide Ice Sheet and glacial landform developed. Glacial clay accumulated above the bedrock and formed the basal deposits. During the Post-Glacial period(MIS1),the ice sheet melted and the sea level changed in New England,forming sand bars near the drumlins of the glacier landform,and finally evolving into a barrier island-lagoon environment. The lagoon was connected with the open sea through tidal inlet channels.

Key words: Plum island, Upper Pleistocene-Holocene, barrier island-lagoon, glacial deposit, sedimentary microfacies, sedimentary model

中图分类号:

P512.32

李伟茹, 李志华, 李胜利, 李顺利, 邵家澍. 障壁岛—潟湖沉积特征及模式:以美国普拉姆岛上更新统—全新统为例^*[J]. 古地理学报, 2022, 24(6): 1073-1083.

LI Weiru, LI Zhihua, LI Shengli, LI Shunli, SHAO Jiashu. Sedimentary characteristics and model of barrier island-lagoon: an example from the Upper Pleistocene-Holocene in Plum island,USA[J]. JOPC, 2022, 24(6): 1073-1083.

http://www.gdlxb.cn/CN/Y2022/V24/I6/1073

参考文献

[1] 程林,田海兰,刘西汉,王艳霞. 2020. 近44年来滦河口障壁岛演变过程及其影响因素研究: 以唐山市龙岛为例. 海洋科学, 44(6): 22-30.
[Cheng L,Tian H L,Liu X H,Wang Y X. 2020. Variations and influencing factors of the barrier islands near the Luan River estuary in the past 44 years: a case study of the Loong island in Tangshan. Marine Sciences, 44(6): 22-30]
[2] 纪占胜,姚建新,武桂春,蒋忠惕,傅渊慧. 2005. 拉萨北部旁多群坠石沉积的发现及其意义. 地质通报, 24(6): 542-548.
[Ji Z S,Yao J X,Wu G C,Jiang Z T,Fu Y H. 2005. Discovery of dropstones in the Poindo group,northern LhaSa,Tibet,China,and its significance. Geological Bulletin of China, 24(6): 542-548]
[3] 李从先,陈刚,高曼娜,庄振业. 1982. 砂坝—潟湖体系的沉积和发育. 海洋地质研究, 2(1): 49-58.
[Li C X,Chen G,Gao M N,Zhuang Z Y. 1982. Sedimentation and development of the barrier-lagoon systems along the coastal zone of east China. Marine Geological Research, 2(1): 49-58]
[4] 李从先,庄振业. 1983. 关于砂坝—潟湖体系的几个问题. 海洋科学,7(4): 56-59.
[Li C X,Zhuang Z Y. 1983. Some questions on barrier-lagoon systems. Marine Science,7(4): 56-59]
[5] 李从先,陈刚,王平. 1991. 我国沿岸晚第四纪砂坝—潟湖体系的沉积模式. 沉积学报, 9(4): 12-18.
[Li C X,Chen G,Wang P. 1991. The stratigraphic model of the late-Quaternary barrier-lagoon depositional systems along the coast of China. Acta Sedimentologica Sinica, 9(4): 12-18]
[6] 李胜利,于兴河,张志杰,朱庆荣,王庆如,梁卫,周锦. 2004. 珠江口盆地西江30-2油田新近系中新统沉积微相及层序地层分析. 古地理学报, 6(1): 30-40.
[Li S L,Yu X H,Zhang Z J,Zhu Q R,Wang Q R,Liang W,Zhou J. 2004. Sedimentary microfacies and sequence stratigraphy of the Miocene of Neogene in Xijiang 30-2 oil field,Pearl river mouth basin. Journal of Palaeogeography(Chinese Edition), 6(1): 30-40]
[7] 秦松,孙传敏,杨继友,张伟,尼玛次仁. 2015. 冈底斯东段色日绒地区冈瓦纳相冰海杂砾岩特征及其意义. 地球科学进展, 30(11): 1239-1249.
[Qin S,Sun C M,Yang J Y,Zhang W,Nima Ciren. 2015. Characteristics and its significance of glacial-marine diamictite of Gondwana facies in the Serirong area,Eastern Gangdese Belt. Advances in Earth Science, 30(11): 1239-1249]
[8] 沙雪梅,梁苏娟. 2021. 陆源障壁岛砂坝有效储层综合预测技术与应用: 以韦德迈阿盆地 B 区块泥盆系为例. 天然气地球科学, 32(3): 447-456.
[Sha X M,Liang S J. 2021. Comprehensive reservoir prediction of terrigenous barrier bar and its application: case study of Devonian in block B,Oued Mya Basin,Algeria. Natural Gas Geoscience, 32(3): 447-456]
[9] 王德英,刘立,王东坡. 1996. 沉积地层中坠石的成因及其研究意义. 世界地质, 15(4): 21-25.
[Wang D Y,Liu L,Wang D P. 1996. The origin and studying significance of dropstone in stratigraphy. World Geology, 15(4): 21-25]
[10] 严隽猷. 1985. 障壁岛体系. 海洋地质动态,1(10): 4-5.
[Yan J Y. 1985. The barrier-lagoon systems. Marine Geology Letters,1(10): 4-5]
[11] 于兴河. 2008. 碎屑岩系油气储层沉积学(第二版). 北京: 石油工业出版社,438-439.
[Yu X H. 2008. Sedimentology of Oil and Gas Reservoirs in Clastic Rocks(2nd Edition). Beijing: Petroleum Industry Press,438-439]
[12] 朱筱敏,王贵文,谢庆宾. 1997. 塔里木盆地东河塘石炭系障壁岛后冲溢扇研究. 沉积学报, 15(1): 43-47.
[Zhu X M,Wang G W,Xie Q B. 1997. Study on the carboniferous washover fan behind barrier island in Donghetang of Tarim basin. Acta Sedimentologica Sinica, 15(1): 43-47]
[13] Andrews J T,Dyke A S. 2013. Late Quaternary glaciation in North America. In: Elias S A,Mock C J(eds). Encyclopedia of Quaternary Science(2nd Edition). Amsterdam: Elesvier Press,245-249.
[14] Farron S J,Hughes Z J,Fitzgerald D M. 2020. Assessing the response of the Great Marsh to sea-level rise: migration,submersion or survival. Marine Geology, 425: 1-13.
[15] Hartwell A D. 1970. Hydrography and Holocene sedimentation of the Merrimack River Estuary,Massachusetts. In: Hayes M O(ed). Coastal Environments of Northeastern Massachusetts and New Hampshire(Field Trip Guidebook). Amherst: University of Massachusetts Press,428-440.
[16] Hein C J,FitzGerald D M,Carruthers E A,Stone B D,Barnhardt W A,Gontz A M. 2012. Refining the model of barrier island formation along a paraglacial coast in the Gulf of Maine. Marine Geology,307-310(5): 40-57.
[17] Hein C J,Fitzsimons G G,FitzGerald D M,Fallon A R. 2016. Records of migration and ebb-delta breaching at historic and ancient tidal inlets along a river-fed paraglacial barrier island. Journal of Coastal Research,Special Issue, 75: 228-232.
[18] Jones J R,Cameron B. 1987. Surface distribution of foraminifera in a New England salt marsh: Plum island,Massachusetts. Maritime Sediments and Atlantic Geology, 23(3): 131-140.
[19] Langston A K,Vinent O D,Herbert E R,Kirwan M L. 2020. Modeling long term salt marsh response to sea level rise in the sediment deficient Plum island estuary,MA. Limnology and Oceanography, 65(9): 2142-2157.
[20] McCormick C L. 1969. Holocene stratigraphy of the marshes at Plum island,Massachusetts. In: Hayes M O(ed). Coastal Environments of Northeastern Massachusetts and New Hampshire(Field Trip Guidebook). Amherst: University of Massachusetts Press,368-390.
[21] McIntire W G,Morgan J P. 1962. Recent geomorphic history of Plum island,Massachusetts and adjacent coasts. In: Louisiana State University(ed). Atlantic Coastal Studies. Technical Report No.19,1-44.
[22] McIntire W G,Morgan J P. 1964. Recent geomorphic history of Plum Island,Massachusetts,and adjacent coasts. Baton Rouge: Louisiana State University Press,1-44.
[23] Oldale R N,Colman S M,Jones G A. 1993. Radiocarbon ages from two submerged strandline features in the western Gulf of Maine and a sealevel curve for the northeastern Massachusetts coastal region. Quaternary Research, 40(1): 38-45.
[24] Pico T,Creveling J R,Mitrovica J X. 2017. Sea-level records from the U.S. mid-Atlantic constrain Laurentide Ice Sheet extent during Marine Isotope Stage 3. Nature Communications, 8: 1-6.
[25] Rhodes E G. 1973. Pleistocene-Holocene sediments interpreted by seismic refraction and wash-bore sampling,Plum Island-Castle Neck,Massachusetts. U.S. Army Corps of Engineers Technical Publication 40,63-75.
[26] Stutz M L,Pilkey O H. 2001. A review of global barrier island distribution. Journal of Coastal Research,Special Issue, 34: 15-22.

选择文件类型/文献管理软件名称

选择包含的内容

障壁岛—潟湖沉积特征及模式:以美国普拉姆岛上更新统—全新统为例^*

Sedimentary characteristics and model of barrier island-lagoon: an example from the Upper Pleistocene-Holocene in Plum island,USA

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	祁柯宁, 旷红伟, 柳永清, 彭楠, 王玉冲, 陈骁帅. 扬子西南缘滇中成冰系南沱组沉积特征及其上红层归属讨论^*[J]. 古地理学报, 2024, 26(6): 1305-1324.
[2]	陈宏逵, 朱筱敏, 肖坤叶, 杜业波, 袁志云, 张新顺, 王晓雪. 乍得Doseo盆地东部坳陷下白垩统Kedeni组层序地层格架与沉积体系分布^*[J]. 古地理学报, 2024, 26(4): 796-815.
[3]	文祖超, 沈玉林, 李壮福, 敬宇鸿, 党志英, 祝玉琳, 孟艳, 李林超. 混合沉积特征精细刻画: 以江苏徐州寒武系馒头组为例^*[J]. 古地理学报, 2024, 26(4): 846-862.
[4]	黄有根, 许杰, 郑小鹏, 刘燕, 钟寿康, 李琳, 张道锋, 谭秀成. 鄂尔多斯盆地中东部下二叠统太原组灰岩沉积特征与沉积模式^*[J]. 古地理学报, 2024, 26(4): 911-925.
[5]	郭文建, 郭瑞婧, 唐勇, 纪友亮, 马铮涛, 刘笑语, 梁涛, 马玉龙. 准噶尔盆地二叠系上乌尔禾组退覆式扇(辫状河)三角洲前缘-滩坝复合砂砾岩沉积特征及控制因素^*[J]. 古地理学报, 2024, 26(3): 584-599.
[6]	刘国庆, 苏中堂, 郝志磊, 魏柳斌, 任军锋, 廖慧鸿, 吴浩文. 鄂尔多斯盆地马家沟组碳酸盐岩-膏盐岩共生体系沉积微相与沉积模式^*[J]. 古地理学报, 2024, 26(2): 279-295.
[7]	李发有, 班舒悦, 王光付, 孙建芳, 丁峰, 孙钰, 王腾宇, 徐海, 陈诗望, 夏昌盛, 郑乃熙, 鲍志东. 南美奥连特盆地白垩系Napo组Main-M1亚段沉积体系重建及油气勘探意义^*[J]. 古地理学报, 2024, 26(1): 17-27.
[8]	张忠民, 李依霖, 郑乃熙, 曹喆, 吕雪雁, 李宗峰, 孙润明, 夏昌盛, 李磊, 牛博, 宿宇驰, 张浩飞, 冯志强, 季汉成, 鲍志东. 北非地区Ghadames盆地早古生代岩相古地理演化特征^*[J]. 古地理学报, 2024, 26(1): 45-57.
[9]	朱筱敏, 叶蕾, 谢爽慧, 杨棵, 秦祎. 低可容空间陆相湖盆富砂浅水三角洲沉积模式及实例分析^*[J]. 古地理学报, 2023, 25(5): 959-975.
[10]	季汉成, 陈亮, 孙予舒, 史燕青, 向鹏飞, 杨志波. 冀中坳陷杨税务地区奥陶系岩相古地理特征及其对潜山内幕储集层的控制作用^*[J]. 古地理学报, 2023, 25(5): 976-991.
[11]	张自力, 李琦, 朱筱敏, 谈明轩, 张锐锋, 曹兰柱, 李凤勋, 单帅强. 陆相断陷湖盆重力流湖底扇沉积与地震响应特征分析: 以渤海湾盆地霸县凹陷古近系沙河街组为例^*[J]. 古地理学报, 2023, 25(5): 1049-1068.
[12]	吕奇奇, 辛红刚, 王林, 罗顺社, 淡卫东, 冯胜斌. 鄂尔多斯盆地宁县地区三叠系延长组7段湖盆细粒重力流沉积类型、特征及模式^*[J]. 古地理学报, 2023, 25(4): 823-840.
[13]	刘圣乾, 何幼斌, 姜在兴, 罗进雄, 朱雪清, 朱青, 唐卫. 湖相碳酸盐岩礁滩体系沉积特征、主控因素及成因模式: 以东营凹陷西部沙四上亚段为例^*[J]. 古地理学报, 2023, 25(4): 872-888.
[14]	王集, 王峰, 赵伟波, 虎建玲, 吴静仪, 肖云宵, 陈洪德, 刘磊, 王志伟, 朱淑玥. 鄂尔多斯盆地西缘上石炭统羊虎沟组岩相类型及沉积模式^*[J]. 古地理学报, 2023, 25(3): 573-597.
[15]	罗垚, 谭秀成, 赵东方, 罗文军, 刘耘, 肖笛, 乔占峰, 曾伟. 埃迪卡拉系微生物碳酸盐岩沉积特征及其地质意义:以川中磨溪8井区灯影组四段为例^*[J]. 古地理学报, 2022, 24(2): 278-291.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

障壁岛—潟湖沉积特征及模式:以美国普拉姆岛上更新统—全新统为例*

Sedimentary characteristics and model of barrier island-lagoon: an example from the Upper Pleistocene-Holocene in Plum island,USA

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

障壁岛—潟湖沉积特征及模式:以美国普拉姆岛上更新统—全新统为例^*