{"title":"意大利南部爱奥尼亚海岸奥特朗托地区第四纪淹没海槽地貌调查","authors":"Nourhan Nour","doi":"10.21608/ejec.2020.96489","DOIUrl":null,"url":null,"abstract":"Submerged notches that indicate negative sea level change evidence during The Quaternary. Through their study, the effects of sea level change and effect of tectonic lifting movements on them during the Quaternary are identified. Submerged notches as negative evidence below MSL are studied in the field work in two areas: The first one is \"San Foca\" area that comprises three parts from north to south:\" Torre di Roca Vecchia bay\" and \"Madonna di Roca Vecchia bay\", the second area is \"Castro\", only \"Porto Castro\" is studied below the current sea level. The studied area located in the Ionian Sea coast, South Italy, its total length is about 53 km. The studied area is the south-east part of the Apulia region (southern Italy), stretching between the Ionian Sea and Adriatic Sea. It is located on the east coast of the Salento peninsula. Its coordinates are 40 ̊ 0 ́ 2.43 ̋ to 40 ̊ 18 ́ 6.85 ̋ N, and 18 ̊ 16 ́ 10.10 ̋ to 18 ̊ 31 ́ 30.99 ̋ E The aims of this paper to define the effects of the Quaternary Sea level change on submerged notches, and study the evolution of coastal karst in current climate conditions. The methodology of this study depended upon extensive field and measurements of submerged notches, an in addition to GPS.","PeriodicalId":211158,"journal":{"name":"The Egyptian Journal of Environmental Change","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2020-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Geomorphic surveying of submerged sea notches in Otranto area during the Quaternary, Ionian Sea coast, South Italy\",\"authors\":\"Nourhan Nour\",\"doi\":\"10.21608/ejec.2020.96489\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Submerged notches that indicate negative sea level change evidence during The Quaternary. Through their study, the effects of sea level change and effect of tectonic lifting movements on them during the Quaternary are identified. Submerged notches as negative evidence below MSL are studied in the field work in two areas: The first one is \\\"San Foca\\\" area that comprises three parts from north to south:\\\" Torre di Roca Vecchia bay\\\" and \\\"Madonna di Roca Vecchia bay\\\", the second area is \\\"Castro\\\", only \\\"Porto Castro\\\" is studied below the current sea level. The studied area located in the Ionian Sea coast, South Italy, its total length is about 53 km. The studied area is the south-east part of the Apulia region (southern Italy), stretching between the Ionian Sea and Adriatic Sea. It is located on the east coast of the Salento peninsula. Its coordinates are 40 ̊ 0 ́ 2.43 ̋ to 40 ̊ 18 ́ 6.85 ̋ N, and 18 ̊ 16 ́ 10.10 ̋ to 18 ̊ 31 ́ 30.99 ̋ E The aims of this paper to define the effects of the Quaternary Sea level change on submerged notches, and study the evolution of coastal karst in current climate conditions. The methodology of this study depended upon extensive field and measurements of submerged notches, an in addition to GPS.\",\"PeriodicalId\":211158,\"journal\":{\"name\":\"The Egyptian Journal of Environmental Change\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-03-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Egyptian Journal of Environmental Change\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.21608/ejec.2020.96489\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Egyptian Journal of Environmental Change","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.21608/ejec.2020.96489","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
表明第四纪期间海平面负变化证据的淹没缺口。通过研究,确定了第四纪海平面变化和构造抬升运动对它们的影响。在两个区域的实地工作中,研究了MSL以下的淹没缺口作为负面证据:第一个区域是“San Foca”区域,由北向南三部分组成:“Torre di Roca Vecchia bay”和“Madonna di Roca Vecchia bay”,第二个区域是“Castro”,仅研究了当前海平面以下的“Porto Castro”。研究区位于意大利南部爱奥尼亚海沿岸,全长约53公里。研究区域是阿普利亚地区(意大利南部)的东南部,延伸到爱奥尼亚海和亚得里亚海之间。它位于萨伦托半岛的东海岸。坐标为40°0°2.43°~ 40°18°6.85°N, 18°16°10.10°~ 18°31°30.99°E。本文旨在明确第四纪海平面变化对淹没槽的影响,研究当前气候条件下海岸岩溶的演化。本研究的方法依赖于广泛的野外和水下凹痕的测量,以及GPS。
Geomorphic surveying of submerged sea notches in Otranto area during the Quaternary, Ionian Sea coast, South Italy
Submerged notches that indicate negative sea level change evidence during The Quaternary. Through their study, the effects of sea level change and effect of tectonic lifting movements on them during the Quaternary are identified. Submerged notches as negative evidence below MSL are studied in the field work in two areas: The first one is "San Foca" area that comprises three parts from north to south:" Torre di Roca Vecchia bay" and "Madonna di Roca Vecchia bay", the second area is "Castro", only "Porto Castro" is studied below the current sea level. The studied area located in the Ionian Sea coast, South Italy, its total length is about 53 km. The studied area is the south-east part of the Apulia region (southern Italy), stretching between the Ionian Sea and Adriatic Sea. It is located on the east coast of the Salento peninsula. Its coordinates are 40 ̊ 0 ́ 2.43 ̋ to 40 ̊ 18 ́ 6.85 ̋ N, and 18 ̊ 16 ́ 10.10 ̋ to 18 ̊ 31 ́ 30.99 ̋ E The aims of this paper to define the effects of the Quaternary Sea level change on submerged notches, and study the evolution of coastal karst in current climate conditions. The methodology of this study depended upon extensive field and measurements of submerged notches, an in addition to GPS.