颁布单位:[University of Michigan] |
颁布时间:2016 |
实施时间:2016 |
学科分类:[Earth system model simulations show a larger ice-volume response to obliquity than precession, in agreement with ice-volume proxy records, Model results show that removal of regolith from the high-latitudes can explain the change in the ice-volume cycles across the Pleistocene, Earth system model simulations show that the Late Cretaceous cooling was due to a reduction in CO2, not changes in paleogeography, Astronomy, Atmospheric, Oceanic and Space Sciences, Geology and Earth Sciences, Science, Geology]