Geochemical controls on the elemental composition of siderite: Implications for palaeo-environmental reconstructions
The elemental composition of siderite (FeCO3) has been widely used as a palaeo-environmental proxy, and commonly utilised in the diagnosis of marine influences on Phanerozoic coastal wetland sediments. That siderite might reflect marine or freshwater sources is based on the premise that a marine ori...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Elsevier
2019
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