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Process / pipelineTime-rock framework

地层对比

地层对比是通过追踪物理或化学信号,在空间上识别等效的岩层或年代地层单位的过程。该方法根植于19世纪对阿尔卑斯冰川序列的研究,并在20世纪由Vail等地理学家将其形式化,他们将全球海平面变化与沉积序列相结合。对比是理解盆地尺度沉积物输运、资源分布和古环境变化的基础。

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Method map

The neighbourhood of related methods — select a node to explore.

来源

  1. Catuneanu, O. (2002). Sequence Stratigraphy of Clastic Systems. Geological Association of Canada. link
  2. Vail, P. R., Mitchum, R. M., & Thompson, S. (1977). Global cycles of relative changes of sea level. American Association of Petroleum Geologists Memoir, 26, 83–97. link
  3. Posamentier, H. W., & Allen, G. P. (2006). Siliciclastic Sequence Stratigraphy: Concepts and Applications. Society for Sedimentary Geology. link

如何引用本页

ScholarGate. (2026, June 3). Stratigraphic Correlation. ScholarGate. https://scholargate.app/zh/geoscience/stratigraphic-correlation

Which method?

Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.

Compare side by side

被引用于

ScholarGateStratigraphic Correlation (Stratigraphic Correlation). 于 2026-06-15 检索自 https://scholargate.app/zh/geoscience/stratigraphic-correlation · 数据集: https://doi.org/10.5281/zenodo.20539026