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Method for identifying event layer in sediment core of rock

机译:岩石沉积物中识别事件层的方法

摘要

PROBLEM TO BE SOLVED: To obtain a method for identifying an event layer in a rock core of a sediment. The present invention discloses a method for identifying an event layer in a rock core of a sediment. It includes: (1) The rock core of the sediment is divided, and the elements of the rock core of the sediment are scanned by X-ray to obtain the intensity data of the elements contained in the rock core of the sediment. (2) Based on the obtained element intensity data, the analysis index of the sedimentary layer is determined according to the endowment characteristics of the element in the sedimentary layer. (3) Obtain a change curve for each depth based on the analysis index, analyze the intensity data of the elements using a statistical analysis method, and determine the magnitude of the threshold value. A straight line parallel to the depth is created in the analysis index curve by the threshold value, and the straight line intersects with the change curve of the analysis index after normalization. Furthermore, accurate identification of the event layer is realized according to the identification criteria of the event layer. This proposal not only can identify minute event layers in rock cores, but also has high identification efficiency and accuracy, provides powerful technical support for the development of paleoclimate and paleoenvironmental research in the ocean, and has high practical value. There is.
机译:要解决的问题:获得用于在沉积物的岩石核心中识别事件层的方法。本发明公开了一种用于在沉积物的岩心识别事件层的方法。它包括:(1)沉积物的岩心被分割,且沉积物的岩心的元件用X射线扫描,以获得包含在所述沉积物的岩心的元件的强度数据。 (2)基于所获得的元件的强度数据,所述沉积层的分析指数是根据在沉积层中的元件的禀赋特性确定。 (3)获得针对基于分析索引的每个深度的变化曲线,分析使用统计分析的方法的元件的强度数据,并且确定所述阈值的幅度。在分析索引曲线上通过阈值创建平行于深度的直线,并且直线与归一化后分析指数的变化曲线相交。此外,事件层的准确识别根据所述事件层的识别标准来实现。这个建议不仅能够识别微小的事件层的岩石核心,而且具有很高的识别效率和准确性,为古气候古环境和研究在海洋中发展强有力的技术支持,并具有很高的实用价值。有。

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