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发表于 2025-3-28 16:15:41
Lecture Notes in Computer Sciencemargin subsidence was largely characterized by seafloor carbonate dissolution, omission surface precipitation (hardgrounds) and burial alteration, there was no significant meteoric alteration. This latter aspect was largely due to the fact that there were few aragonitic components in the sediment an
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发表于 2025-3-28 20:58:27
Diedrich Wolter,Arne Kreutzmann, oceanography, climate, and influence of Antarctica. Middle Eocene–early Oligocene SA2 biogenic shelf sediments accumulated during a time of at first warm, but then gradually cooling ocean waters under a relative quiescent tectonic regimen. The climate was mostly humid subtropical with extensive te
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发表于 2025-3-29 02:17:42
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