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Applying stand-off LIBS to paleoclimatic research: A case study on geochemical content of carbonate rocks

机译:偏距LIBS在古气候研究中的应用:以碳酸盐岩地球化学含量为例

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摘要

Carbonate rocks, mainly limestone and dolostone, have made up 10% to 15% of sedimentary rocks in the Earth. Geochemical contents of carbonate rocks could reflect a series of key geological information of ancient environment, such as temperature, precipitation, salinity and geologic event. Stand-off LIBS provides an approach to rapidly, accurately and nondestructively determine the elemental concentrations in difficult carbonate rock samples, such as cliff rocks, small reefs and karst caves. In this study, we have determined Mg/Ca ratio and Sr/Ca ratio in either limestones from Xinjiang, Guangdong, Hunan or dolostones from Yunnan at a distance of 15 meters. 2D Mapping data of Mg/Ca and Sr/Ca ratios of rocks from Yunnan clearly exhibit spatial variation of geochemical contents. These variations are correlated to the temperature changes along the geologic times, which has been proved to influence the Magnesium incorporation of rocks.
机译:碳酸盐岩,主要是石灰岩和白云岩,占地球沉积岩的10%至15%。碳酸盐岩的地球化学含量可以反映出一系列古代环境的关键地质信息,如温度,降水,盐分和地质事件。固定式LIBS提供了一种方法,可以快速,准确且无损地确定困难的碳酸盐岩石样品中的元素浓度,例如悬崖岩石,小礁石和喀斯特洞穴。在这项研究中,我们确定了新疆,广东,湖南的石灰岩或云南的白云岩在15米处的Mg / Ca比值和Sr / Ca比值。云南岩石Mg / Ca和Sr / Ca比值的二维制图数据清楚地表明了地球化学含量的空间变化。这些变化与沿地质时期的温度变化有关,事实证明这会影响岩石中镁的掺入。

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