Luis Alvaro Botero-Gómez, Pablo Osorio, Hugo Murcia, C. Borrero, Jeny Alejandra Grajales
{"title":"哥伦比亚安第斯山脉中央科迪勒拉山脉villamaria - termales单生火山田(第一部分):形态特征和时间关系","authors":"Luis Alvaro Botero-Gómez, Pablo Osorio, Hugo Murcia, C. Borrero, Jeny Alejandra Grajales","doi":"10.18273/REVBOL.V40N3-2018005","DOIUrl":null,"url":null,"abstract":"The Villamaría-Termales Monogenetic Volcanic Field (VTMVF) is located in the middle of the Central Cordillera of Colombia. It is part of the San Diego Cerro Machín Volcano Tectonic Province (SCVTP), and is related to the Nevado del Ruiz Volcanic Complex (NRVC). The VTMVF is composed of at least 14 monogenetic volcanoes; 12 of them are conical and subconical (domes), one is massif (dome), and one is irregular (lava flow). Based on the morphometric and geomorphological analysis reported in this study, we define the VTMVF as a volcanic field affected by a variety of geomorphological and glacial processes. This field occupies an area of 114.5 km2, where the Villamaría-Termales fault system controlled the volcanic dispersion. These volcanic centers have an age range between 1.8 Ma and <38,000 years (Calabrian-Late Pleistocene). The morphometric analysis as volume and separation and grouping indexes allowed us to define the spatial relationship (i.e. distance between the volcanoes and their geoforms) between the volcanic centers that make up the VTMVF.","PeriodicalId":44188,"journal":{"name":"Boletin de Geologia","volume":" ","pages":""},"PeriodicalIF":0.5000,"publicationDate":"2018-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"9","resultStr":"{\"title\":\"Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte I): Características morfológicas y relaciones temporales\",\"authors\":\"Luis Alvaro Botero-Gómez, Pablo Osorio, Hugo Murcia, C. Borrero, Jeny Alejandra Grajales\",\"doi\":\"10.18273/REVBOL.V40N3-2018005\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Villamaría-Termales Monogenetic Volcanic Field (VTMVF) is located in the middle of the Central Cordillera of Colombia. It is part of the San Diego Cerro Machín Volcano Tectonic Province (SCVTP), and is related to the Nevado del Ruiz Volcanic Complex (NRVC). The VTMVF is composed of at least 14 monogenetic volcanoes; 12 of them are conical and subconical (domes), one is massif (dome), and one is irregular (lava flow). Based on the morphometric and geomorphological analysis reported in this study, we define the VTMVF as a volcanic field affected by a variety of geomorphological and glacial processes. This field occupies an area of 114.5 km2, where the Villamaría-Termales fault system controlled the volcanic dispersion. These volcanic centers have an age range between 1.8 Ma and <38,000 years (Calabrian-Late Pleistocene). The morphometric analysis as volume and separation and grouping indexes allowed us to define the spatial relationship (i.e. distance between the volcanoes and their geoforms) between the volcanic centers that make up the VTMVF.\",\"PeriodicalId\":44188,\"journal\":{\"name\":\"Boletin de Geologia\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":0.5000,\"publicationDate\":\"2018-09-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"9\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Boletin de Geologia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18273/REVBOL.V40N3-2018005\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Boletin de Geologia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18273/REVBOL.V40N3-2018005","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
Campo Volcánico Monogenético Villamaría-Termales, Cordillera Central, Andes colombianos (Parte I): Características morfológicas y relaciones temporales
The Villamaría-Termales Monogenetic Volcanic Field (VTMVF) is located in the middle of the Central Cordillera of Colombia. It is part of the San Diego Cerro Machín Volcano Tectonic Province (SCVTP), and is related to the Nevado del Ruiz Volcanic Complex (NRVC). The VTMVF is composed of at least 14 monogenetic volcanoes; 12 of them are conical and subconical (domes), one is massif (dome), and one is irregular (lava flow). Based on the morphometric and geomorphological analysis reported in this study, we define the VTMVF as a volcanic field affected by a variety of geomorphological and glacial processes. This field occupies an area of 114.5 km2, where the Villamaría-Termales fault system controlled the volcanic dispersion. These volcanic centers have an age range between 1.8 Ma and <38,000 years (Calabrian-Late Pleistocene). The morphometric analysis as volume and separation and grouping indexes allowed us to define the spatial relationship (i.e. distance between the volcanoes and their geoforms) between the volcanic centers that make up the VTMVF.