The Oligo–Miocene closure of the Tethys Ocean and evolution of the proto-Mediterranean Sea

Keyphrases

• Late Miocene 100%
• Tethys Evolution 100%
• Proto-Mediterranean Sea 100%
• Mass Accumulation Rate 100%
• Tethys Ocean 100%
• Eastern Mediterranean 50%
• Carbonate 50%
• Crash 50%
• Levantine Basin 50%
• Mid-Miocene 50%
• Chronos 50%
• Seaway 50%
• Deep Sea 50%
• Miocene Climate Optimum 50%
• Climate Patterns 50%
• Indian Ocean 50%
• Exact Timing 50%
• Ocean Climate 50%
• Tortonian 50%
• Arabian Plate 50%
• Circulation Patterns 50%
• Cenozoic 50%
• Primary Productivity 50%
• Eurasian Plate 50%
• Miocene Carbonates 50%
• Oligocene-Miocene 50%
• Carbonate Crash 50%
• Early Onset 50%
• Red Sea Rifting 50%
• Biostratigraphy 50%
• Serravallian 50%
• Deep Borehole 50%
• Oceanic Circulation 50%

Earth and Planetary Sciences

• Miocene 100%
• Mediterranean Sea 100%
• Tethys 100%
• Accumulation Rate 66%
• Red Sea 33%
• Levant 33%
• Deep Sea 33%
• Oligocene 33%
• Rifting 33%
• Tortonian 33%
• Eurasian Plate 33%
• Indian Ocean 33%
• Hiatus 33%
• Oceanic Circulation 33%
• Stratigraphy 33%
• Arabian Plate 33%
• Oceanic Climate 33%
• Borehole 33%
• Serravallian 33%