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 >Ar-40/Ar-39 dating links Albuquerque Volcanoes to the Pringle Falls excursion and the Geomagnetic Instability Time Scale
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Ar-40/Ar-39 dating links Albuquerque Volcanoes to the Pringle Falls excursion and the Geomagnetic Instability Time Scale

机译:Ar-40 / Ar-39约会将阿尔伯克基火山与普林格尔瀑布游览和地磁不稳定时标联系起来

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摘要

Incremental heating of basaltic lava groundmass from the Albuquerque Volcanoes, New Mexico, and plagioclase from Ash D at Pringle Falls, Oregon, yield Ar-40/Ar-39 isochron ages of 218 +/- 14 and 211 +/- 13 ka, respectively. Sediments in which Ash D was deposited and the eight lava flows of the Albuquerque Volcanoes display excursional paleomagnetic data with virtual geomagnetic poles (VGPs) in the southern hemisphere and together with the statistically indistinguishable Ar-40/Ar-39 dates, establish that both sites record the Pringle Falls excursion. This excursion is also recorded by the 227 +/- 8 ka Mamaku Ignimbrite, New Zealand, and by high deposition rate sediments at ODP site 919 in the North Atlantic Ocean that are dated astrochronologically at 209-207 ka. We propose that the names "Albuquerque" and "Jamaica" excursion be abandoned and that a radioisotopic age of 211 +/- 13 ka be adopted for the Pringle Falls excursion, which is one of five globally expressed, well-documented excursions in marine sediment cores or dated by Ar-40/Ar-39 methods that took place from 220 to 30 ka. Together with at least five other well-dated excursions between 730 and 520 ka, some ten excursions define the Geomagnetic Instability Time Scale (GITS) for the Bruhnes Chron. Eight of these excursions have been dated using Ar-40/Ar-39 methods. If the temporal clustering of excursions in the GITS is not a sampling artefact, this suggests that the geodynamo is not intrinsically unstable, but rather that instability in the flow pattern of the outer core fluid flow causes the main dipole field to be considerably weakened such that it becomes unstable with a 200 to 300 ka recurrence interval. Excursions are an important part of dynamo behavior over geologic time scales that, in addition to reversals of the main dipole field, need to be fully considered when assessing whether theoretical and numerical simulations of the dynamo produce earth-like results.
机译:逐步加热来自新墨西哥州阿尔伯克基火山的玄武岩熔岩地层和来自俄勒冈州普林格尔瀑布的灰烬D的斜长石,分别产生218 +/- 14和211 +/- 13 ka的Ar-40 / Ar-39等时年龄。沉积灰分D的沉积物和阿尔伯克基火山的八次熔岩流显示了具有南半球虚拟地磁极(VGP)的偏移古地磁数据,以及统计上难以区分的Ar-40 / Ar-39日期,从而确定了这两个地点记录普林格尔瀑布游览。新西兰227 +/- 8 ka Mamaku Ignimbrite以及北大西洋ODP 919站的高沉积速率沉积物也记录了这一偏移,该沉积物在时间上按时间顺序记为209-207 ka。我们建议放弃名称“ Albuquerque”和“ Jamaica”的游览,并建议将Pringle Falls游览的放射性同位素年龄定为211 +/- 13 ka,这是五个全球表达的,有据可查的海洋沉积物游览之一核或用Ar-40 / Ar-39方法测定的日期为220至30 ka。再加上至少730到520 ka之间的至少五个其他日期合适的偏移,大约十个偏移定义了Bruhnes Chron的地磁不稳定时间标度(GITS)。这些游览中有八次使用Ar-40 / Ar-39方法确定日期。如果GITS中的时间偏移不是暂时性的,则表明地球动力学并不是本质上不稳定的,而是外芯流体流动模式的不稳定性导致主偶极子场大大减弱,从而间隔200至300 ka时,它变得不稳定。在地质时间尺度上,漂移是发电机行为的重要组成部分,除了主偶极子场的反转外,在评估发电机的理论和数值模拟是否产生类似地球的结果时,还需要充分考虑。

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