{"title":"哥伦比亚洛斯科科斯火山链(CVLC)相关结构的形态测定","authors":"Wveimar Samacá, John J. Sánchez","doi":"10.18273/REVBOL.V40N3-2018001","DOIUrl":null,"url":null,"abstract":"The Coconucos Volcanic Chain (CVLC-from its acronym in Spanish) is made up by 14 volcanic centers (nine composite volcanoes and five monogenetic volcanoes) oriented along the Coconucos Lineament. Two more centers, maar-type volcanoes, are also located to the SW, in the vicinity of the CVLC. To study the development of these volcanic centers, the ellipticity ( e i ) and irregularity ( i i ) morphometric parameters as well as the base-to-height H/W B for composite volcanoes and the height-of-cone to width-of-cone H co /W co ratios for monogenetic centers, were evaluated. The values for morphometric parameters and dimensional ratios vary as follows: 1.27< e i <3.24; 1.12< i i <1.53; 0.04< H/W B <0.24 and 0.02< H co /W co <0.34. Graphs of morphometric parameters ordered according to the spatial position of the volcanic centers allowed identification of partial tendencies in the evolution of composite volcanoes and patterns in the state of preservation for monogenetic centers: e i increases to the SE; i i decreases to the SE; H/W B increases to the SE and H co /W co increases to the NE. Together, these values and patterns suggest not only variability of endogenous and exogenous processes that affect the shapes of volcanoes, but also possible cycles of constructive activity and affectation of morphology and morphometry of the volcanic structures.","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":"0","resultStr":"{\"title\":\"Morfometría de las estructuras asociadas a la Cadena Volcánica de Los Coconucos (CVLC), Colombia\",\"authors\":\"Wveimar Samacá, John J. Sánchez\",\"doi\":\"10.18273/REVBOL.V40N3-2018001\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Coconucos Volcanic Chain (CVLC-from its acronym in Spanish) is made up by 14 volcanic centers (nine composite volcanoes and five monogenetic volcanoes) oriented along the Coconucos Lineament. Two more centers, maar-type volcanoes, are also located to the SW, in the vicinity of the CVLC. To study the development of these volcanic centers, the ellipticity ( e i ) and irregularity ( i i ) morphometric parameters as well as the base-to-height H/W B for composite volcanoes and the height-of-cone to width-of-cone H co /W co ratios for monogenetic centers, were evaluated. The values for morphometric parameters and dimensional ratios vary as follows: 1.27< e i <3.24; 1.12< i i <1.53; 0.04< H/W B <0.24 and 0.02< H co /W co <0.34. Graphs of morphometric parameters ordered according to the spatial position of the volcanic centers allowed identification of partial tendencies in the evolution of composite volcanoes and patterns in the state of preservation for monogenetic centers: e i increases to the SE; i i decreases to the SE; H/W B increases to the SE and H co /W co increases to the NE. Together, these values and patterns suggest not only variability of endogenous and exogenous processes that affect the shapes of volcanoes, but also possible cycles of constructive activity and affectation of morphology and morphometry of the volcanic structures.\",\"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\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Boletin de Geologia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18273/REVBOL.V40N3-2018001\",\"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.V40N3-2018001","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOLOGY","Score":null,"Total":0}
Morfometría de las estructuras asociadas a la Cadena Volcánica de Los Coconucos (CVLC), Colombia
The Coconucos Volcanic Chain (CVLC-from its acronym in Spanish) is made up by 14 volcanic centers (nine composite volcanoes and five monogenetic volcanoes) oriented along the Coconucos Lineament. Two more centers, maar-type volcanoes, are also located to the SW, in the vicinity of the CVLC. To study the development of these volcanic centers, the ellipticity ( e i ) and irregularity ( i i ) morphometric parameters as well as the base-to-height H/W B for composite volcanoes and the height-of-cone to width-of-cone H co /W co ratios for monogenetic centers, were evaluated. The values for morphometric parameters and dimensional ratios vary as follows: 1.27< e i <3.24; 1.12< i i <1.53; 0.04< H/W B <0.24 and 0.02< H co /W co <0.34. Graphs of morphometric parameters ordered according to the spatial position of the volcanic centers allowed identification of partial tendencies in the evolution of composite volcanoes and patterns in the state of preservation for monogenetic centers: e i increases to the SE; i i decreases to the SE; H/W B increases to the SE and H co /W co increases to the NE. Together, these values and patterns suggest not only variability of endogenous and exogenous processes that affect the shapes of volcanoes, but also possible cycles of constructive activity and affectation of morphology and morphometry of the volcanic structures.