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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Ar-40-Ar-39 step heating ages of North American tektites and of impact melt rock samples from the Chesapeake Bay impact structure
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Ar-40-Ar-39 step heating ages of North American tektites and of impact melt rock samples from the Chesapeake Bay impact structure

机译:AR-40-AR-39北美Tektites的加热年龄和Chesapeake湾冲击结构的影响熔体岩石样品

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摘要

This study presents Ar-40-Ar-39 step heating ages of four North American tektites (three bediasites and one georgiaite) and of two groundmass samples extracted at different depths from clast-rich impact melt rocks (CB-W61 and CB-W84) recovered by the USGS-ICDP Eyreville B drill-core about 9 km from the centre of the Chesapeake Bay impact structure. Radiometric age determination on both North American tektites and impact melt rocks from within Chesapeake Bay crater offers the first possibility to confirm the origin of these tektites. For this aim, argon isotopic data from 13 samples/aliquots of tektite rims, cores and bulk, and 4 samples/aliquots from two impact melt rocks were obtained over 15 to 26 step heating extractions. Age spectra of all tektite samples show plateaux comprising 62-98% of the Ar-39 release over consecutive intermediate and high temperature heating steps. Few low temperature extractions indicate excess Ar-40. Inverse isochron Ar-40/Ar-36 intercepts of tektite samples are indistinguishable from air (295.5). However, impact melt rock spectra presented complex Ar-release affecting primarily the low temperature heating-steps. Inverse isochrones indicate excess argon from which the Ar-40/Ar-36 intercept was used to correct the age calculation. CB-W61 and CB-W61-2 Ar-40/Ar-36 intercepts are 354.5 +/- 2.5 and 327.2 +/- 6.3, respectively, and those for CB-W84 and CB-W84-2 are 332.0 +/- 7.3 and 329.6 +/- 5.6, respectively. The inverse isochron weighted mean age (according to currently suggested K-decay constants revisions by Schwarz et al. (2011) and Renne et al. (2011)) for all four tektites is 34.86 +/- 0.25 Ma (MSWD = 0.96, P = 0.41; n = 4) and for the two impact melt rocks is 37.16 +/- 3.65 Ma (MSWD = 0.83, P = 0.36). The combined tektite and impact melt rocks isochron mean age of 34.86 +/- 0.23 (0.32) Ma (MSWD = 0.87, P = 0.43) is slightly - though not significantly - higher than the plateau mean age of 34.55 +/- 0.27 (0.36) Ma (MSWD = 0.66, P = 0.6
机译:本研究介绍了四个北美Tektites(三种床头酸盐和一个Georgiaite)的AR-40-AR-39步骤加热衰退,并在不同深度从富含碎屑的冲击熔体岩石(CB-W61和CB-W84)提取的两种仿生样品USGS-ICDP Eyreville B钻机恢复了大约9公里的Chesapeake湾冲击结构。北美Tektites和Chesapeake Bay Crater内的北美Tektites和冲击熔体岩石的辐射尺度确定提供了确认这些tektites的起源的可能性。为此目的,从15至26步加热萃取过程中获得来自13个样品/排水的Tektite轮辋,核和体积的等份/等分试样的氩同位素数据,以及来自两个冲击熔体岩体的4个样品/等分试样。所有Tektite样品的年龄光谱显示出包含62-98%的Ar-39在连续的中间体和高温加热步骤中释放的平亮度。很少有低温萃取表示过量的Ar-40。逆等色素AR-40 / AR-36 Tektite样品的截距可与空气无法区分(295.5)。然而,撞击熔体岩体呈现复杂的Ar释放,主要是低温加热步骤。逆等色调表明过量氩气从中使用AR-40 / AR-36截距来校正年龄计算。 CB-W61和CB-W61-2AR-40 / AR-36截距分别为354.5 +/- 2.5和327.2 +/- 6.3,CB-W84和CB-W84-2的截止值分别为332.0 +/- 7.3和329.6 +/- 5.6分别。逆等待加权平均年龄(根据目前建议的K-Decay常量由Schwarz等人修改。(2011)和Renne等人。 = 0.41; n = 4),对于两个冲击熔体岩石为37.16 +/- 3.65 mA(Mswd = 0.83,p = 0.36)。泰克和撞击熔体岩体同胞均为34.86 +/- 0.23(0.32)mA(mswd = 0.87,p = 0.43)略微显着 - 高于高原平均年龄为34.55 +/- 0.27(0.36 )MA(MSWD = 0.66,P = 0.6

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