Page 275 - Physical Principles of Sedimentary Basin Analysis
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7.16 Stretching and thinning of the sediments     257

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                depth [km]  75          700   900       800          (a) t=310Ma
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                                                                         Sediments1R
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                depth [km]  75      700 800           900            (c) t=160Ma  Mantle
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                depth [km]  75                    1000  900 700  800  (d) t=140Ma  Crust
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                depth [km]  75         1000         700 800   900    (f) t=56Ma
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            Figure 7.36. The lithosphere at the beginning and end of the three last rift phases.
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