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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Magnetite (U-Th)/He dating and its application to the geochronology of intermediate to mafic volcanic rocks
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Magnetite (U-Th)/He dating and its application to the geochronology of intermediate to mafic volcanic rocks

机译:磁铁矿(U-Th)/ He定年及其在中,镁铁质火山岩年代学中的应用

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摘要

We present a new approach to dating intermediate to mafic volcanic rocks using magnetite (U-Th)/He geochronology. Magnetite is common in volcanic rocks that typically do not contain easily datable minerals such as sanidine or zircon. Analytical procedures for producing magnetite (U-Th)/He ages have been developed, including mineral separation, sample air-abrasion to correct for a-ejection effects, He extraction/measurement, sample dissolution, and anion-exchange column chemistry procedures. Dated magnetite crystals were non-skeletal, euhedral to subhedral, and 100-300 mu m in size. To test the reliability of this new geochronometer, four basaltic to andesitic samples lacking sanidine or zircon were dated by both magnetite (U-Th)/He and whole-rock Ar-40/(39) Ar methods. For two samples, the ages from the different geochronometers are in excellent agreement (< 1 %). A third sample with a poorly behaved Ar-40/Ar-39 age spectrum affected by Ar-39 recoil yielded a well-defined magnetite (U-Th)/He age that is consistent with Ar-40/(39) Ar age data from similar nearby volcanic rocks. The final sample, however, exhibited a near 40% discrepancy between the two methods, despite yielding reproducible magnetite (U-Th)/He ages. In all cases, the multi-aliquot magnetite (U-Th)/He ages (n > 7) exhibit 3-11% (2 sigma) variation about the mean age, indicating that reproducibility for magnetite (U-Th)/He ages is comparable to that of apatite and zircon (U-Th)/He analyses. In order to assess the He retentivity, we conducted a single magnetite helium diffusion experiment, yielding a well-behaved Arrhenius relationship and a closure temperature of similar to 250 degrees C (dT/dt= 10 degrees C/myr). Magnetite's high He retentivity coupled with (U-Th)/He age reproducibility demonstrates good potential for magnetite (U-Th)/He dating as an alternative volcanic geochronometer, particularly in cases where samples yield inconclusive or uninterpretable Ar-40/Ar-39 ages. (c) 2007 Elsevier B.V.. All rights reserved.
机译:我们提出了一种利用磁铁矿(U-Th)/ He年代学对中性镁铁质火山岩进行测年的新方法。磁铁矿在火山岩中很常见,这些火山岩通常不包含易脱硫的矿物,如山梨或锆石。已经开发出用于生成磁铁矿(U-Th)/ He年龄的分析程序,包括矿物分离,校正a喷射效应的样品空气磨损,He提取/测量,样品溶解和阴离子交换柱化学程序。过时的磁铁矿晶体是非骨架的,从正反面到正反面,尺寸为100-300微米。为了测试这种新型天文钟的可靠性,采用磁铁矿(U-Th)/ He和全岩石Ar-40 /(39)Ar方法对4种缺少山定或锆石的玄武岩样品至安山药样品进行了测年。对于两个样本,不同天文钟的年龄非常吻合(<1%)。受Ar-39反冲影响的Ar-40 / Ar-39年龄谱表现不佳的第三份样品产生了明确的磁铁矿(U-Th)/ He年龄,与Ar-40 /(39)Ar年龄数据一致来自附近类似的火山岩。然而,尽管产生了可重复的磁铁矿(U-Th)/ He时效,但最终样品在两种方法之间显示出近40%的差异。在所有情况下,多等分磁铁矿(U-Th)/ He年龄(n> 7)在平均年龄上均表现出3-11%(2 sigma)的变化,表明磁铁矿(U-Th)/ He的再现性与磷灰石和锆石(U-Th)/ He分析相当。为了评估He的保持力,我们进行了一次磁铁矿氦气扩散实验,得出了行为正常的Arrhenius关系和接近250摄氏度的封闭温度(dT / dt = 10摄氏度/米尔)。磁铁矿的高He保持力与(U-Th)/ He年龄可再现性相结合,显示出磁铁矿(U-Th)/ He约会作为火山地球测年仪的潜力,特别是在样品产生不确定或无法解释的Ar-40 / Ar-39的情况下年龄。 (c)2007 Elsevier B.V.。保留所有权利。

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