1887

Abstract

Complex construction achimov sandy layers AchBS11 is shown on example clinoform deposits cyclite BS11 in Surgut structured-facial zone of Western Siberia, the sequence of their accumulation and condition of the formation. The sandy layers were formed consecutively one for others, changing form and area of the spreading depending on directions and intensities of the undertows, brought sedimentary material

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/content/papers/10.3997/2214-4609.20143160
2012-09-10
2021-10-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20143160
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