Sea-floor spreading, carbonate dissolution level, and the nature of horizon a |
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Authors: | Gartner S |
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Abstract: | Evidence from leg 2 of the Deep Sea Drilling Project suggests a constant spreading rate for the floor of the North Atlantic over the past 80 million years; a major lowering of the carbonate dissolution level during the early Pliocene; and an early to middle Eocene age for horizon A. |
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