Depositional environments and sequence stratigraphy of paralic glacial, paraglacial and postglacial Upper Ordovician siliciclastic deposits in the Murzuq Basin, SW Libya

Earth and Planetary Sciences

• Depositional Sequence 100%
• Sequence Boundary 60%
• Continental Shelf 60%
• Sea Level Rise 60%
• Deep Water 60%
• Famine 40%
• Glacier Advance 40%
• Ice-Rafted Debris 20%
• Fluvial Deposit 20%
• Glacier Retreat 20%
• Incised Valley 20%
• Transgression 20%
• Estuarine Sediment 20%
• Temporal Distribution 20%
• Hydrocarbon Exploration 20%
• Siliciclastic Deposit 20%
• Shallow Water 20%
• Mudstone 20%
• Glacier 20%
• Deltaic Deposit 20%