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应用X射线荧光录井岩石元素光谱分析技术对TK1247井岩石样品进行分析,岩石中的XRF元素呈现出明显的旋回变化特征,而其中元素的分配及比值的变化和组合特征都在一定程度上指示着古沉积环境的演化和沉积相的不同。通过该井岩石元素变化趋势可以看出,该分析手段是判断沉积环境的一个有效方法,提出了塔河油田艾丁区块XRF元素变化规律的地质意义。同时,也指出了今后XRF元素分析的研究趋势。
The rock samples from TK1247 were analyzed by X-ray fluorescence spectroscopy. The XRF elements in the rocks show obvious gyration characteristics, and the distribution of elements, the change of ratio and the combination characteristics are all indicated to a certain extent The evolution of the sedimentary environment and sedimentary facies different. It can be seen from the variation trend of rock elements in the well that the analysis method is an effective method to judge the depositional environment and put forward the geological significance of the XRF variation in the Aiding block of the Tahe oilfield. At the same time, it also points out the trend of XRF elemental analysis in the future.