通过1:25 000比例尺的Cogollo组制图,对serrania del perija的地质知识作出贡献,Cogollo组位于塞萨尔贝里尔市东部地区

Milton David Lozada Molina, Frank David Lascarro Navarro, Luisa Fernanda León Díaz, Elías Ernesto Rojas Martínez, Fabio enrique Carrillo Bolaño, Luis Carlos Tapia Tavera, Dino Carmelo Manco Jaraba
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引用次数: 0

摘要

在Becerril市的Cesar省,有大量白垩纪岩石的露头,其石灰质序列属于Lagunitas组和Aguas Blancas组、Cogollo组和La Luna组。本研究展示了贝泽里尔市东部一个25平方公里区域的地图,旨在通过实地工作、地貌单元识别和1:1 . 25 000比例尺的岩石学描述来提供该地区的地质知识。拉古尼塔斯组的特征是一套深灰色块状化石灰岩,其间穿插钙质泥岩和斑岩灰岩。从Aguas Blancas组开始,Animas段被详细识别,由富含有机质的钙质泥岩与黑色泥晶灰岩互层组成,这些灰岩水平分级为具有细粒钙质胶结的砂岩。塔库伊段由钙质粉砂岩、细粒砂岩和碳酸化粘土岩组成。Maracas岩段主要由块状光质石灰岩组成。同样,确定了四种地貌环境:构造、猪背识别单元、同斜脊和山脊;剥蚀,识别单位,如侵蚀陡坡,轻微对折的小山和起伏的溪流;岩溶,以岩溶谷和岩溶坡为单位;和河流,与洪泛平原单位。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Contribución al conocimiento geológico de la Serranía del Perijá mediante cartografía a escala 1:25.000 del Grupo Cogollo, en el sector oriental del municipio de Becerril, Cesar
In the department of Cesar, Municipality of Becerril, there are extensive outcroppings of Cretaceous rocks with calcareous sequences belonging to the Lagunitas and Aguas Blancas Formations, the Cogollo Group, and the La Luna Formation. This study presents the mapping of a 25 km2 are in the eastern sector of the Municipality of Becerril, intended to contribute geological knowledge of this area through field work, identification of geomorphological units and petrographic descriptions at a scale 1:25,000. The Lagunitas Formation is characterized by a succession of dark gray massive fossiliferous limestone intercalated with calcareous mudstone and lumachellic limestone. From the Aguas Blancas Formation, the Animas Member is identified in detail, consisting of calcareous mudstone with abundant organic matter interbedded with black micritic limestones that grades horizontally to sandstones with fine-grained calcareous cement. The Tucuy Member consists of calcareous siltstone, fine-grained sandstone and carbonated claystone. The Maracas Member consists mainly of massive lumachellic limestone. Similarly, four geomorphological environments were identified: structural, identifying units of hog-backs, homoclinal ridges and cuestas; denudation, identifying units such as erosion scarps, lightly bisected hills and undulating interfluves; karstic, with units of karstic valley and karstic slope; and fluvial, with the floodplain unit.
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