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and resource distribution in mudrocks
current state-of-play
Each paper deals with a different aspect of the geology and/or the geophysics of the tectonic evolution of the plateau
The recognition of the extreme systems and understanding their controls provide insights that can be used to better model geologic systems
new tectonic models
The Late Eocene Earth-Hothouse, Icehouse, and Impacts 1-1-001-323-4330-323 and resource distribution in mudrocksEditors: Christian Koeberl and Alessandro Montanari Buy the e book (not available in print) The Late Eocene and the Eocene Oligocene (E O) transition mark the most profound oceanographic and climatic changes of the past 50 million years of Earth history, with cooling beginning in the middle Eocene and culminating in the major earliest Oligocene Oi 1 isotopic event. The Late Eocene is characterized by an accelerated global cooling, with a sharp