Özet:

The tunnel, which is a water strontium-borate mineral in the Sarıkaya (Four) borate beds located in the middle of the Eskişehir-Afyon-Kütahya triangle, was found SrB6O10 • 4H2O. Specifically mineralization and formation and distinction from other beds in Turkey in Sarıkaya borat beds, along with the tunelite, are found multiple Na-, Na-Ca-, Ca-, Mg-Ca-, Mg-borat minerals such as ulxite, kurnakovit, kolemanite, inderit, inderborit, meyerhoferite and wanit, primarily boraks. The samples collected from beds were studied using microscopic, chemical and X-ray differentiation methods, and the data obtained in the Cramer and Death Valley regions in California. It was first identified and identified by the tunelite that was compatible with the data. The tunelite, which has a secondary formation in the sarıkaya borat beds, after the beds are covered and buried with young sediments, is made up of high-water primary borats due to increased temperature and pressure, the decrease in the activity of the capilla water, and also the chemical composition in terms of Sr++ is a result of the land enrichment.