Authigenic or detrital origin of pyrrhotite in sediments?: Resolving a paleomagnetic conundrum
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Horng, Chorng-Shern; Roberts, Andrew
Description
Monoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagenesis in anoxic sedimentary environments. In contrast, geochemical literature indicates that pyrrhotite formation is extremely slow below 180 °C, which mak
Collections | ANU Research Publications |
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Date published: | 2006 |
Type: | Journal article |
URI: | http://hdl.handle.net/1885/22568 |
Source: | Earth and Planetary Science Letters |
DOI: | 10.1016/j.epsl.2005.11.008 |
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01_Horng_Authigenic_or_detrital_origin_2006.pdf | 775.69 kB | Adobe PDF |
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