首页> 外文期刊>Journal of the Brazilian Chemical Society >Method development for 234U and 230Th determination and application to fossil deep-water coral and authigenic carbonate dating from the Campos Basin - Brazil
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Method development for 234U and 230Th determination and application to fossil deep-water coral and authigenic carbonate dating from the Campos Basin - Brazil

机译:234U和230Th的测定方法开发并将其应用到坎波斯盆地的化石深水珊瑚和自生碳酸盐中-巴西

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A 234U and 230Th determination method based on an extraction chromatographic separation followed by ICP-MS with quadrupole (ICP-QMS) was developed. For authigenic carbonates, a second separation step with ion exchange chromatography in a HNO3 solution was added. These methods were applied to seven fossil deep-water coral and two authigenic carbonate samples from the continental slope of the Campos Basin - Brazil. The ages determined for the fossil corals samples from the same sediment core ranged from 9 to 202 ky with a 1% uncertainty, consistent with the values determined by 14C dating and with those determined by 230Th/234U using flow injection coupled to an ICP-QMS. One of the authigenic carbonates analyzed presented an age of approximately 80 ky. The other sample exhibited a 230Th/234U activity ratio close to equilibrium and out of the application range of the method.
机译:提出了一种基于萃取色谱分离,然后采用四极杆ICP-MS(ICP-QMS)的234U和230Th测定方法。对于自生碳酸盐,添加了在HNO3溶液中进行离子交换色谱分离的第二步。这些方法应用于来自巴西坎波斯盆地大陆坡的七个化石深水珊瑚和两个自生碳酸盐样品。对于相同沉积物岩心的化石珊瑚样品,确定的年龄范围为9至202 ky,不确定度为1%,与14C测年和230Th / 234U(采用流动注射和ICP-QMS测得)确定的值一致。分析的一种自生碳酸盐的年龄约为80 ky。另一个样品的230Th / 234U活性比接近平衡,超出了该方法的应用范围。

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