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基于实验分析的乳房状石钟乳成因机理初步研究——以湖北阳新地心大峡谷洞穴沉积形态为例
引用本文:段武辉,周现金,潘洋,徐柯健,郭申祥,谭明. 基于实验分析的乳房状石钟乳成因机理初步研究——以湖北阳新地心大峡谷洞穴沉积形态为例[J]. 中国岩溶, 2021, 40(6): 907-913. DOI: 10.11932/karst20210601
作者姓名:段武辉  周现金  潘洋  徐柯健  郭申祥  谭明
作者单位:1.中国科学院地质与地球物理研究所北京100029
摘    要:目前,关于乳房状石钟乳成因的研究仍然停留在"科学猜想"阶段.通过对湖北阳新"地心大峡谷"洞穴内采集的一对孪生乳房状石钟乳样品进行矿物构成、晶体形态以及年代学分析,获得如下新认识:①乳房状石钟乳由致密—疏松互层递序生长的方解石构成.②致密层方解石呈菱面体晶型,无色透明,垂直向下生长,没有横向扩张;疏松层方解石呈细小颗粒状...

关 键 词:乳状石钟乳石  形成机理  实验分析  阳新地心大峡谷洞穴
收稿时间:2021-04-30

Forming mechanism of breast-like stalactites based on the experimental analysis of cave deposition from Dixin canyon,Yangxin, Hubei
Abstract:The current study on the forming mechanism of breast-like stalactites is still at the stage of "scientific conjecture". In this study,samples of a pair of twin breast-like stalactites were collected in a cave of Dixin canyon at Yangxin county, Hubei Province. We carried out the mineral composition, crystal morphology and geochronology studies on the samples, and obtained new understanding. The breast-like stalactite is composed of calcite that formed the compact/porous inter-layers. The calcite of compact layer is rhombohedral,colorless and transparent,growing vertically downwards without lateral expansion. The calcite of porous layer is in the form of fine particles,milky white and opaque,and aggregates in a "coating" structure, with a certain degree of lateral expansion, which accounts for the expansion of the base and trunk of the breast-like stalactite. The dating results suggest that the compact and porous layers do not grow continuously, but existing significant hiatus. The 232Th content of the porous layer is generally one to two orders of magnitude higher than that of the compact layer,indicating that the content of water-insoluble impurities in the porous layer is significantly higher than that of the compact layer. Based on the experimental results and the observations that the "coating" depositions are also on the walls and roofs of the cave,we speculate that the solution recharging "coating" depositions seeps from surrounding rocks or solid sediments (stalactites). The porous structure of "coating" deposition may be due to the diversion of underground river, the deterioration of the cave sealing, the decrease of CO2 concentration in the cave, and resultant acceleration of calcite crystallization rate. These factors make calcite crystal more defects and messy accumulation. 
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