乌里扬诺夫斯克-叙兹兰伏尔加河地区古近系砂岩表面显微结构与成因

S. Zorina, K. I. Nikashin, N. Afanasieva, N. Hamada
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引用次数: 0

摘要

通过对乌里扬诺夫斯克-西兹兰伏尔加河地区索斯诺夫卡组古近系砂的标准筛分,分离出石英颗粒,石英颗粒是玻璃制造和建筑的珍贵原料。为了确定砂岩的成因,恢复其形成的相条件,利用光学显微镜和电子显微镜对分离石英颗粒的表面显微结构进行了研究。结果表明,索斯诺夫卡砂碎屑颗粒在水下(海滩)、风成、水下-风成混合(海岸沙丘)、注入和大陆土壤环境下具有多阶段形成的特征。首次描述了深部地层在压力作用下挤压颗粒的微观结构特征和砂层注入机制所固有的微观结构特征。注射剂的诊断复合体包括旋转显微结构、缺口微槽和变形流体包裹体。所列显微结构的相当新颖的外观表明,它们是叠加在海岸-海洋和风成阶段的演化,随后形成了砂侵入体。在索斯诺夫卡砂地质历史的最后阶段,大陆土壤条件形成了颗粒,当二次二氧化硅以球状和簇状的形式粘合石英颗粒时,石英颗粒的表面连接了前几个阶段的特征。在此基础上,提出了综合索斯诺夫卡砂岩重建古环境和形成阶段的各种微结构特征的解释方案。索斯诺夫卡砂岩为砂岩侵入体的发现具有重要的现实意义,为乌里扬诺夫斯克—西兹兰伏尔加河地区古近系索斯诺夫卡组玻璃砂和石英砂的发现和预测提供了新的途径。
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Surface Microtextures of Quartz Grains and Origin of the Paleogene Sands in the Ulyanovsk-Syzran Volga Region
Quartz grains were separated by standard sieving of the Paleogene sands from the Sosnovka Formation of the Ulyanovsk-Syzran Volga region, which are a scarce and valuable raw material for glass making and construction. In order to establish the origin of the sands and restore the facies conditions of their formation, the surface microtextures of the separated quartz grains were examined by optical and electron microscopy. It was shown that the clastic grains of the Sosnovka sands bear the signs of a multi-stage formation process under the conditions of subaquatic (beach zone), eolian, mixed subaquatic-eolian (coastal dunes), injective, and continental pedological settings. For the first time, a complex of microtextures characteristic of the extrusion of grains from deep horizons under pressure and inherent in the injection mechanism of sand formation was described. The diagnostic complex of injectites includes rotational microtextures, notched microtroughs, and deformed fluid inclusions. The rather fresh appearance of the listed microtextures suggests that they were superimposed on the coastal-marine and eolian stages of the evolution with the subsequent formation of sand intrusions. At the final stage of the geological history of the Sosnovka sands, the grains were shaped by the continental pedological conditions, when secondary silica in the form of globules and their clusters cemented the quartz grains, the surface of which concatenated the features of the previous stages. Based on the results of the study, an interpretation scheme summarizing various microtextural features of the reconstructed paleoenvironments and the stages of formation the Sosnovka sands was developed. The finding that the Sosnovka sands are sand intrusions is of great practical importance, as it necessitates new approaches to the discovery and prediction of glass and quartz sand deposits confined to the Paleogene Sosnovka Formation of the Ulyanovsk-Syzran Volga region.
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