{"title":"岩心是由于风化和/或构造作用形成的吗?问题与建议","authors":"C. Twidale, J. R. Vidal Romaní","doi":"10.17979/CADLAXE.2020.42.0.7268","DOIUrl":null,"url":null,"abstract":"Many of the so-called corestones have been developed from rocky blocks that have been apparently affected by subsurface physicochemical weathering that results in lamination, granulation, and eventually a puggy or stiff clay. The truth is that weathering takes advantage of a previous deformation structure and does not create it by weathering.","PeriodicalId":35856,"journal":{"name":"Cadernos do Laboratorio Xeoloxico de Laxe","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2020-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Are corestones due to weathering and/or tectonism? Problems and suggestions\",\"authors\":\"C. Twidale, J. R. Vidal Romaní\",\"doi\":\"10.17979/CADLAXE.2020.42.0.7268\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Many of the so-called corestones have been developed from rocky blocks that have been apparently affected by subsurface physicochemical weathering that results in lamination, granulation, and eventually a puggy or stiff clay. The truth is that weathering takes advantage of a previous deformation structure and does not create it by weathering.\",\"PeriodicalId\":35856,\"journal\":{\"name\":\"Cadernos do Laboratorio Xeoloxico de Laxe\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-12-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Cadernos do Laboratorio Xeoloxico de Laxe\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.17979/CADLAXE.2020.42.0.7268\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Cadernos do Laboratorio Xeoloxico de Laxe","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.17979/CADLAXE.2020.42.0.7268","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
Are corestones due to weathering and/or tectonism? Problems and suggestions
Many of the so-called corestones have been developed from rocky blocks that have been apparently affected by subsurface physicochemical weathering that results in lamination, granulation, and eventually a puggy or stiff clay. The truth is that weathering takes advantage of a previous deformation structure and does not create it by weathering.