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- W2158762555 abstract "Abstract We studied the variations of the volatile major elements Na and K in Transantarctic Mountain microtektites and Australasian microtektites with distance from the putative source crater location in Indochina. The dataset includes 169 normal-type Australasian microtektites (101 from this study and 68 from the literature) from 24 deep-sea sediment cores up to 8000 km from Indochina, and 54 Transantarctic Mountain microtektites from northern Victoria Land, 11 000 km due southeast of Indochina. Normal-type (MgO 2 = 60–78 wt.%) Transantarctic Mountain microtektites and Australasian microtektites share a common volatilization trend with Na and K contents decreasing with distance from Indochina. The average total alkali (Na 2 O + K 2 O) concentrations at distance ranges of 1000–2000 km, 2000–4000 km, 4000–8000 km and > 8000 km are 4.27 ± 0.67 wt.% ( n = 84), 3.20 ± 1.21 wt.% ( n = 50), 2.10 ± 0.25 wt.% ( n = 35) and 1.25 ± 0.25 wt.% ( n = 54), respectively. The trend highlights a relationship between increasing loss of volatiles in microtektites with longer trajectories and higher temperature-time regimes which should be taken into account in microtektite formation modeling. The trend is consistent with a previous hypothesis that Transantarctic Mountain microtektites belong to the Australasian strewn field and that Indochina is the target region for the parent catastrophic impact." @default.
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- W2158762555 date "2010-04-01" @default.
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- W2158762555 title "A common volatilization trend in Transantarctic Mountain and Australasian microtektites: Implications for their formation model and parent crater location" @default.
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- W2158762555 doi "https://doi.org/10.1016/j.epsl.2010.02.037" @default.
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