{"title":"对马德拉岛以北150英里处海底山的地球物理调查","authors":"A.S. Laughton, M.N. Hill , T.D. Allan","doi":"10.1016/0146-6313(60)90016-2","DOIUrl":null,"url":null,"abstract":"<div><p>An elongated seamount rising to 678 fathoms was surveyed by echo-sounding, dredging, photography, magnetic and seismic methods, the results of which are described. The feature appears to be the result of volcanic extrusion along a fault running obliquely across a broad rise.</p></div>","PeriodicalId":100361,"journal":{"name":"Deep Sea Research (1953)","volume":"7 2","pages":"Pages 117-122, IN6-IN7, 123-128, IN8-IN15, 129-132, IN16-IN17, 133-141"},"PeriodicalIF":0.0000,"publicationDate":"1960-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0146-6313(60)90016-2","citationCount":"24","resultStr":"{\"title\":\"Geophysical investigations of a seamount 150 miles north of Madeira\",\"authors\":\"A.S. Laughton, M.N. Hill , T.D. Allan\",\"doi\":\"10.1016/0146-6313(60)90016-2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>An elongated seamount rising to 678 fathoms was surveyed by echo-sounding, dredging, photography, magnetic and seismic methods, the results of which are described. The feature appears to be the result of volcanic extrusion along a fault running obliquely across a broad rise.</p></div>\",\"PeriodicalId\":100361,\"journal\":{\"name\":\"Deep Sea Research (1953)\",\"volume\":\"7 2\",\"pages\":\"Pages 117-122, IN6-IN7, 123-128, IN8-IN15, 129-132, IN16-IN17, 133-141\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1960-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0146-6313(60)90016-2\",\"citationCount\":\"24\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep Sea Research (1953)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0146631360900162\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep Sea Research (1953)","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0146631360900162","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Geophysical investigations of a seamount 150 miles north of Madeira
An elongated seamount rising to 678 fathoms was surveyed by echo-sounding, dredging, photography, magnetic and seismic methods, the results of which are described. The feature appears to be the result of volcanic extrusion along a fault running obliquely across a broad rise.
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