马略卡岛洞穴中的岩浆岩(POS):形态学、矿物学和晶体结构分类

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Ana Entrena, Luis F. Auqué, María J. Gimeno, Joan J. Fornós
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引用次数: 0

摘要

洞穴岩浆沉积物(POS)是一种独特的沉淀物,存在于世界上少数沿海洞穴中,如马洛卡岛的洞穴。它们的生长与这些洞穴特有的与海洋相连的咸水湖的水位直接相关,因此,它们可以作为过去海平面的可靠指标。本文介绍的研究对在马略卡岛沿海洞穴中采集的大量 POS 样品进行了特征描述和分类。特征描述不仅包括对 117 个手持样本和 102 个 POS 薄切片的观察,还包括对其矿物学及其在洞穴中位置的研究。这项研究为将所有这些特征系统化奠定了基础,其中一些特征是首次在此报告的 POS 样品。研究结果表明:(1) 大部分 POS 沉淀在钟乳石上;(2) 方解石 POS 的内部和外部纹理呈分支状,最常见的晶体结构是镶嵌方解石;(3) 文石 POS 的外部纹理呈球状,内部纹理呈扇形,主要晶体结构为针状。所有文石樣本均在海平面以上或與現時海平面相同的高度被發現,顯示它們可能是在較暖的氣候下形成。方解石 POS 发现于当前海平面以上和以下的高度,可解释为形成于寒冷多雨时期。本文提出的系统化方法可应用于全球其他 POS 并对其进行检验。此外,将这些结果与对马略卡岛一些洞穴中这些相思岩的降水现状的研究信息相结合,可以深入了解其形成条件,从而扩大这些相思岩作为古环境指标的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Phreatic overgrowths on speleothems (POS) from the Mallorca caves: Morphology, mineralogy, and crystal fabric classification

Phreatic overgrowths on speleothems (POS) from the Mallorca caves: Morphology, mineralogy, and crystal fabric classification

Phreatic overgrowths on speleothems (POS) are unique precipitates that are found in a small number of coastal caves around the world, like those in the Mallorca Island. Their growth is directly related to the water level of the brackish lakes connected to the sea characteristic of these caves and, therefore, they can be very reliable indicators of past sea levels. The study presented here characterizes and classifies an important number of POS samples collected in the coastal caves of Mallorca. The characterization includes not only the observations made on 117 handheld samples and on 102 thin sections from POS, but also the study of their mineralogy and their location in the caves. This study has provided the basis for a systematization of all these characteristics, some of which are reported here for the first time in POS samples. The results indicate that (1) most of the POS precipitate on stalactites, (2) calcite POS show branched internal and external texture and their most common crystal fabric is mosaic calcite and (3) aragonite POS show globular external texture and fan-shaped internal texture, and their principal crystal fabric is needle-like. All the aragonitic samples have been found above or at the same heights as the current sea level, which indicates that they have probably formed during warmer climates. The calcite POS have been found at heights above and below the present sea level and are interpreted as to have formed during cold and rainy periods. The systematization proposed in this paper could be applied and checked in other POS worldwide. Additionally, the combination of these results with the information obtained from studies on the present precipitation of these phreatic speleothems in some Mallorca caves has provided an insight on their formation conditions which will enlarge the utility of these speleothems as palaeoenvironmental indicators.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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