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首页> 外文期刊>Revista Geologica de America Central >Descripci?3n de facies de la formaci?3n suretkaEn los alrededores de Siquirres y su relaci?3n con ambientes de depositaci?3n
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Descripci?3n de facies de la formaci?3n suretkaEn los alrededores de Siquirres y su relaci?3n con ambientes de depositaci?3n

机译:锡基尔周围的苏尔特卡形成相的描述及其与沉积环境的关系

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In this work a description of sedimentary facies identified for the Suretka Formation near the town of Siquirres, Lim?3n, is presented. The description was carried out with the inspections of underground excavations, outcrops in creeks, shafts, and boreholes during the construction stage of the Reventaz?3n Hydroelectric power plant. Three sedimentary facies were identified: conglomerate facies, sandstone lenses with fine to very fine conglomerate and tuff lenses facies. The conglomerate facies is characterized by igneous blocks sumerged in a loam sandy matrix. These facies have metric to decametric bedding with bad gradation. On the other side facies of sandstone lenses and fine conglomerates are described as strata of the centimeter order with presence of both parallel and cross laminations in sandstone lenses and reverse and normal gradations in fine conglomerate lenses. The facies analysis allows the identification of an environment of subareal deposition associated with alluvial fans. For the facies of conglomerates, a proximal alluvial fan environment is established and for the facies of lenses of sandstones and intercalations of fine to very fine conglomerates a environment of medium alluvial fan with meandering sedimentary processes like longitudinal or point bars.
机译:在这项工作中,描述了为Lim?3n的Siquirres镇附近的Suretka组确定的沉积相。该描述是在Reventaz?3n水力发电站施工阶段对地下开挖,小溪露头,竖井和钻孔的检查中进行的。确定了三个沉积相:砾岩相,具有精细至极细砾岩的砂岩晶状体和凝灰岩晶状体。砾岩相的特征是火成岩块聚集在壤质砂质基质中。这些相具有度量等级差的十进制层序。另一方面,砂岩透镜和精细砾岩的相被描述为厘米级的地层,在砂岩透镜中存在平行叠层和交叉分层,在精细砾岩中存在反向和正渐变。相分析允许识别与冲积扇相关的分区下沉积的环境。对于砾岩相,建立了近端冲积扇环境,对于砂岩晶状体和精细至极细砾岩层插相,则建立了中度冲积扇环境,其曲折的沉积过程如纵向或点状条形。

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