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Post-rift sequence architecture and stratigraphy in the Oligo-Miocene Sardinia Rift (Western Mediterranean Sea)
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文摘
The tectonic vs climatic control in Miocene Sardinia Rift basin evolution is studied. Sequence stratigraphic and depositional models of the Porto Torres Basin are revised. The climatic control is increasing at the transition from the syn-to postrift stage. Rhodalgal slope progradation in Sardinia at the onset of the postrift stage.

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