| Polar research | |
| Eruption age of the Sverrefjellet volcano, Spitsbergen Island, Norway | |
| Allan H. Treiman1  | |
| [1] Lunar and Planetary Institute 3600 Bay Area BoulevardHouston TX 77058, USA Correspondence | |
| 关键词: Svalbard; Spitsbergen; basalt; Knipovich Ridge; Ar–Ar; | |
| DOI : 10.3402/polar.v31i0.17320 | |
| 学科分类:自然科学(综合) | |
| 来源: Co-Action Publishing | |
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【 摘 要 】
Sverrefjellet is a Pleistocene-age basaltic volcanic construct on north-western Spitsbergen Island (Svalbard Archipelago, Norway). Published ages for the Sverrefjellet eruption range between 6000 years and ca. 1 million years before present. The age of eruption is dated here as 1.05±0.07 (1σ) My, consistent with Ar–Ar isochron and plateau ages of several analysed samples. Radiogenic Ar represents a small proportion of the released Ar, <15% in nearly all samples. Non-radiogenic Ar components include air, excess 40Ar (seen as inverse isochron intercept values >40Ar/36Ar = 295.5), low-temperature alterations (Ar release at low temperature, with high Cl/K), carbonates and zeolites (Ar release at intermediate temperature) and xenolithic material (Ar release at high temperature, high Ca/K). The effects of the largely non-radiogenic argon sources are also seen in the total-gas Ar–Ar “ages”, which range from 1.3 to 10.3 My, significantly larger than the inferred eruption age. It is likely that total-gas Ar–Ar “ag...
【 授权许可】
CC BY-NC
【 预 览 】
| Files | Size | Format | View |
|---|---|---|---|
| RO201902017723067ZK.pdf | 1292KB |
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