Contributions to sequence stratigraphy from analogue and numerical experiments
Contributions to sequence stratigraphy from analogue and numerical experiments
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DOI：
10.1144/jgs2015-127
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发表时间：
2016-06
影响因子：
2.7
通讯作者：
T. Muto;R. Steel;P. Burgess
中科院分区：
文献类型：
--
作者：
T. Muto;R. Steel;P. Burgess
层序地层学模型虽然不再侧重于海平面升降和可容纳空间，但直到最近仍主要基于对露头和地下数据的观察和解释。如果当前的模型对观察到的内容和如何解释观察结果施加了限制，这种方法可能会受到限制。为了在理解地层方面取得进展，层序地层学模型和方法应该对照并充分结合理论和实验结果，这些结果提供了关于(1)自生作用、(2)固有地层响应、(3)冲积等级和(4)适合于随着相对海平面变化而演变的单一沉积体系的尺度的新知识。更广泛地纳入模拟和数值实验结果可能会导致对现有层序地层模型的重大修改和改进。
The sequence stratigraphic model, although no longer focused on eustasy and accommodation, has been until recently based largely on observation and interpretation of outcrop and subsurface data. This approach may be restrictive if the current model places limits on what is observed and how observations are interpreted. To make progress in our understanding of strata, the sequence stratigraphic model and method should be tested against and fully incorporate theoretical and experimental results that provide new knowledge of (1) autogenesis, (2) intrinsic stratigraphic responses, (3) alluvial grade, and (4) scales appropriate to single depositional systems evolving with relative sea-level changes. More extensive inclusion of analogue and numerical experimental results could lead to significant modification and refinement of existing sequence stratigraphic models.