Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography
Current chemostratigraphical studies of the Jurassic System primarily involve the use of one sedimentary component (marine organic carbon), one divalent transition metal substituted in carbonate (manganese), and two isotopic tracers: strontium-isotope ratios (87Sr/86Sr) and carbon-isotope ratios (13...
| Format: | Journal article |
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| Izdano: |
Geological Society Publishing House
2002
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