Abstract

The paper addresses regularities in the location and conditions of the formation of salt diapirs. Their formation is attributed to a thick salt “cover” characterized by the generation of superhigh pressures owing to phase transformations in closed physicochemical systems. Such transformations are responsible for the flow of salts and their injection along tectonic fractures and faults toward the Earth surface. Similarity of the formation scenario of salt diapirs and mud volcanoes is emphasized. Influence of superhigh pressures on the autonomous orogeny of the sedimentary cover is inferred.

中文翻译：

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沉积岩盆地的热压深度设置及其流体动力学：通讯3.平流层和盐底中的超高压

摘要

该论文探讨了盐底物形成的位置和条件的规律性。它们的形成归因于浓盐“覆盖层”，其特征在于由于封闭的物理化学系统中的相变而产生超高压。这种转变负责盐的流动及其沿构造裂缝和断裂向地球表面的注入。强调了盐底岩和泥火山形成情况的相似性。可以推断出超高压对沉积盖层自主造山作用的影响。