The Late Eocene Earth-Hothouse, Icehouse, and Impacts 1-1-001-323-4330-323 and the evolution of the

and the evolution of the Mexican geosyncline

Published: 11/04/2003

The recognition of the extreme systems and understanding their controls provide insights that can be used to better model geologic systems

The length of a pumping test also was found to influence the shape of the drawdown curve and

The Late Eocene Earth-Hothouse, Icehouse, and Impacts 1-1-001-323-4330-323 and the evolution of theEditors: 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