The aim of this paper is to produce a detailed geologic record of late Cenozoic glacial and non-glacial sedimentation and paleoclimate change. The Quatermain Mountains are ideal for recording ice-sheet fluctuations and paleoclimate change because
Antarctique ; Calotte glaciaire ; Changement global ; Glaciaire ; Niveau marin ; Tectonique ; Variation climatique ; Volcanisme
Antarctica ; Climatic variation ; Glacial features ; Global change ; Ice sheet ; Sea level ; Tectonics ; Volcanism
There are two primary views concerning the stability of the East Antarctic Ice Sheet. After summarising the status of the two hypotheses, the AA. explain the rationale for this volume. Building on the Vega Symposium of April 1993, it presents