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首页> 外文期刊>Geodinamica Acta >Actualistic approaches to the systematics and facies relations of clastic karst deposits
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Actualistic approaches to the systematics and facies relations of clastic karst deposits

机译：碎屑岩溶矿床系统和岩相关系的实在方法

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Clastic karst deposits occur at different positions within karst areas, whereas surface karst deposits, sediments of the crack filling facies, the cave entrance facies and the inner cave facies have to be distinguished. The karstification itself is of minor importance for the formation of clastic deposits. Except for incasional debris and impure limestones or marls the contribution of carbonate rocks to clastic karst deposits is low. The majority of clastic material is allogenic and siliciclastic. Regarding the depositional processes cave sediments can be divided into fluvial cave deposits, gravitative or percolative deposits, decomposition deposits and rock breakdown. An actualistic approach could be a useful tool for the identification of fluvial cave deposits. By means of the depositional features of recent cave sediments and classical sedimentological features cave deposits of unknown origin can be classified.
机译：碎屑岩溶沉积物发生在岩溶区域内的不同位置，而表层岩溶沉积物，裂缝填充相的沉积物，洞穴入口相和内部洞穴相必须加以区分。岩溶作用本身对碎屑沉积物的形成次要作用很小。除了偶然的碎片和不纯的石灰石或泥灰岩外，碳酸盐岩对碎屑岩溶岩沉积的贡献很低。大部分碎屑物质是同种和硅碎屑。关于沉积过程，洞穴沉积物可分为河床沉积物，重力或渗滤沉积物，分解沉积物和岩石分解。现实主义方法可能是识别河床沉积物的有用工具。借助于最近的洞穴沉积物的沉积特征和经典的沉积学特征，可以对未知来源的洞穴沉积物进行分类。

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