摘要
<正>1. Introduction One of the major challenges in Geoscience is to understand how the formation and evolution of the Earth System are governed by timescales e that is, how the various geological processes that continue to contribute to its present-day structure and composition operated in the deep past. The traditional view of such processes refers to events that occur at immense spatial scales and over hundreds of millions of years, constrained in most cases by the ages of rocks determined using isotopic dating methods or the fossil record. However, the modern view of geological processes has increasingly acknowledged that their durations can be significantly shorter than previously thought possible, or indeed detectable
引文
Barnes, S.J., Robertson, J.C., 2019. Time scales and length scales in magma flow pathways and the origin of magmatic Ni-Cu-PGE ore deposits. Geoscience Frontiers 10(1), 77-87.
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Trepmann, C.A., Seybold, L., 2019. Deformation at low and high stress-loading rates.Geoscience Frontiers 10(1), 43-54.
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