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Abstract

The nature of organic content in Tunisian sedimentary series from Silurian to Oligo- Miocene was extensively studied with a Leitz MPV-SP microscope using both transmitted (T.L), reflected (R.L) and fluorescent (F.L) lights.

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/content/papers/10.3997/2214-4609.201406060
2000-10-01
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406060
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