{"title":"用宏观结构和粒度分析区分冰川地貌:葡萄牙西北部卡布雷拉山脉","authors":"João Bessa Santos, Madison DeJarlais","doi":"10.1080/02723646.2023.2266199","DOIUrl":null,"url":null,"abstract":"ABSTRACTInformation on the nature of processes occurring in modern glaciers can be obtained through the study of diamictons and landforms that are the product of past glaciations. Macrofabric and grain size analysis of late Quaternary glacial diamictons and moraines present in several valleys of the Serra da Cabreira Mountains in northwest Portugal revealed the presence of two types of diamictons deposited in different stages and were used to re-construct the glacial paleo process history of this mountainous region. Supraglacial melt-out tills and paraglacially reworked tills by debris flows are dominant in this range. Supraglacial melt-out tills, representative of periods of glacial stability followed by recession, present girdle to transitional fabrics and coarser to medium, poorly sorted sediments. Paraglacially reworked tills by debris flows, representative of postglacial mass wasting activity, present girdle fabrics and coarser, poorly sorted sediments. These diamictons and landforms are of particular importance in the reconstruction of the glacial dynamics and history of the Serra da Cabreira Mountains due to a scarcity of chronological data based on absolute dating methods. These Atlantic mountains are also the lowest glaciated range in the Iberian Peninsula, which makes them a compelling area to investigate mountain glacial dynamics in low-elevation Atlantic ranges.KEYWORDS: Glacial geomorphologytill macrofabricgrain sizeSerra da cabreira mountainsNW Portugal AcknowledgmentsWe thank the Department of Geology at San Jose State University and Ryan Portner, Director of the Sedimentology Lab, for supporting the grain size analysis work. We also thank Alberto Gomes, Edgar Figueira, and Jorge Costa from the Department of Geography at the University of Porto, Portugal for fieldwork assistance. A special thank you to Helder Santos for some of the photographic work.Disclosure statementNo potential conflict of interest was reported by the author(s).Data availability statementThe data that support the findings of this study are available from the corresponding author, Joao Santos, upon reasonable request.","PeriodicalId":54618,"journal":{"name":"Physical Geography","volume":"33 1","pages":"0"},"PeriodicalIF":1.1000,"publicationDate":"2023-10-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Distinguishing glacial diamictons and landforms using till macrofabric and grain size analysis: Serra da Cabreira Mountains, NW Portugal\",\"authors\":\"João Bessa Santos, Madison DeJarlais\",\"doi\":\"10.1080/02723646.2023.2266199\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"ABSTRACTInformation on the nature of processes occurring in modern glaciers can be obtained through the study of diamictons and landforms that are the product of past glaciations. Macrofabric and grain size analysis of late Quaternary glacial diamictons and moraines present in several valleys of the Serra da Cabreira Mountains in northwest Portugal revealed the presence of two types of diamictons deposited in different stages and were used to re-construct the glacial paleo process history of this mountainous region. Supraglacial melt-out tills and paraglacially reworked tills by debris flows are dominant in this range. Supraglacial melt-out tills, representative of periods of glacial stability followed by recession, present girdle to transitional fabrics and coarser to medium, poorly sorted sediments. Paraglacially reworked tills by debris flows, representative of postglacial mass wasting activity, present girdle fabrics and coarser, poorly sorted sediments. These diamictons and landforms are of particular importance in the reconstruction of the glacial dynamics and history of the Serra da Cabreira Mountains due to a scarcity of chronological data based on absolute dating methods. These Atlantic mountains are also the lowest glaciated range in the Iberian Peninsula, which makes them a compelling area to investigate mountain glacial dynamics in low-elevation Atlantic ranges.KEYWORDS: Glacial geomorphologytill macrofabricgrain sizeSerra da cabreira mountainsNW Portugal AcknowledgmentsWe thank the Department of Geology at San Jose State University and Ryan Portner, Director of the Sedimentology Lab, for supporting the grain size analysis work. We also thank Alberto Gomes, Edgar Figueira, and Jorge Costa from the Department of Geography at the University of Porto, Portugal for fieldwork assistance. A special thank you to Helder Santos for some of the photographic work.Disclosure statementNo potential conflict of interest was reported by the author(s).Data availability statementThe data that support the findings of this study are available from the corresponding author, Joao Santos, upon reasonable request.\",\"PeriodicalId\":54618,\"journal\":{\"name\":\"Physical Geography\",\"volume\":\"33 1\",\"pages\":\"0\"},\"PeriodicalIF\":1.1000,\"publicationDate\":\"2023-10-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physical Geography\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/02723646.2023.2266199\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical Geography","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/02723646.2023.2266199","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
摘要
【摘要】通过研究过去冰川作用的产物——沉积物和地貌,可以获得关于现代冰川过程性质的信息。通过对葡萄牙西北部Serra da Cabreira山脉多个山谷的晚第四纪冰川碎屑和冰碛的宏观结构和粒度分析,揭示了两种不同时期沉积的碎屑的存在,并用于重建该山区的冰川古过程历史。在这一范围内,冰川上的融化坡道和泥石流的半冰川再造坡道占主导地位。冰川上的融出沉积物,代表了冰川稳定之后的衰退时期,呈现出带状到过渡性织物和较粗到中等、分选差的沉积物。由泥石流改造的准冰川坡地,代表了冰川后的大块消耗活动,呈现出带状结构和较粗、分选差的沉积物。由于缺乏基于绝对测年方法的年代学数据,这些岩块和地貌对重建卡布雷拉山脉的冰川动力学和历史具有特别重要的意义。这些大西洋山脉也是伊比利亚半岛最低的冰川范围,这使得它们成为研究大西洋低海拔山脉冰川动态的一个引人注目的地区。关键词:冰川地貌;宏观结构;粒度;卡布雷拉山;;;;我们还要感谢来自葡萄牙波尔图大学地理系的Alberto Gomes、Edgar Figueira和Jorge Costa提供的实地工作协助。特别感谢Helder Santos的一些摄影作品。披露声明作者未报告潜在的利益冲突。数据可用性声明支持本研究结果的数据可应通讯作者Joao Santos的合理要求获得。
Distinguishing glacial diamictons and landforms using till macrofabric and grain size analysis: Serra da Cabreira Mountains, NW Portugal
ABSTRACTInformation on the nature of processes occurring in modern glaciers can be obtained through the study of diamictons and landforms that are the product of past glaciations. Macrofabric and grain size analysis of late Quaternary glacial diamictons and moraines present in several valleys of the Serra da Cabreira Mountains in northwest Portugal revealed the presence of two types of diamictons deposited in different stages and were used to re-construct the glacial paleo process history of this mountainous region. Supraglacial melt-out tills and paraglacially reworked tills by debris flows are dominant in this range. Supraglacial melt-out tills, representative of periods of glacial stability followed by recession, present girdle to transitional fabrics and coarser to medium, poorly sorted sediments. Paraglacially reworked tills by debris flows, representative of postglacial mass wasting activity, present girdle fabrics and coarser, poorly sorted sediments. These diamictons and landforms are of particular importance in the reconstruction of the glacial dynamics and history of the Serra da Cabreira Mountains due to a scarcity of chronological data based on absolute dating methods. These Atlantic mountains are also the lowest glaciated range in the Iberian Peninsula, which makes them a compelling area to investigate mountain glacial dynamics in low-elevation Atlantic ranges.KEYWORDS: Glacial geomorphologytill macrofabricgrain sizeSerra da cabreira mountainsNW Portugal AcknowledgmentsWe thank the Department of Geology at San Jose State University and Ryan Portner, Director of the Sedimentology Lab, for supporting the grain size analysis work. We also thank Alberto Gomes, Edgar Figueira, and Jorge Costa from the Department of Geography at the University of Porto, Portugal for fieldwork assistance. A special thank you to Helder Santos for some of the photographic work.Disclosure statementNo potential conflict of interest was reported by the author(s).Data availability statementThe data that support the findings of this study are available from the corresponding author, Joao Santos, upon reasonable request.
期刊介绍:
Physical Geography disseminates significant research in the environmental sciences, including research that integrates environmental processes and human activities. It publishes original papers devoted to research in climatology, geomorphology, hydrology, biogeography, soil science, human-environment interactions, and research methods in physical geography, and welcomes original contributions on topics at the intersection of two or more of these categories.