Archaean asteroid impacts, banded iron formations and MIF-S anomalies: A discussion
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Description
The origin of mass-independent fractionation (MIF-S) of sulphur isotopes (δ33S) recorded in sediments older than 2.45 Ga is widely interpreted in terms of UV-triggered reactions under oxygen-poor ozone-depleted atmosphere conditions (Farquhar, J., Bao, H
| Collections | ANU Research Publications |
|---|---|
| Date published: | 2010 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/31528 |
| Source: | Icarus |
| DOI: | 10.1016/j.icarus.2009.11.024 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Glikson_Archaean_asteroid_impacts,_2010.pdf | 795.73 kB | Adobe PDF | Request a copy | |
| 02_Glikson_Archaean_asteroid_impacts,_2010.pdf | 609.13 kB | Adobe PDF | Request a copy |
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