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石英颗粒表面结构类型以及它们和形成环境间的对应关系,国外已有初步总结。对石英颗粒表面结构应用于历史环境分析,有着不同的意见。多数研究者认为,对于松散的或未固结的沉积物(主要为第四纪的)中的石英颗粒表面结构,具有显著的环境分析意义,而对于地质年代久远、早已半固结或固结成岩的则看法不一,有的则予以否定。因为,地质年代愈老,成岩作用(包括浅变质作用)影响也就愈大。但也有些情况表明,虽已固结成岩,其物源区的搬运、沉积过程中产生的机械结构,仍然部分或大部分被保存下来,仍可以指示其环境。
Quartz particle surface structure types and their correspondence with the formation of the environment, a preliminary summary of foreign countries. The quartz particle surface structure used in historical environmental analysis, have different opinions. Most researchers believe that the surface texture of quartz grains in loose or unconsolidated sediments (mainly of the Quaternary) has significant environmental significance and is semi-consolidated or consolidated for geological ages The diagenetic view is different, while others are denied. Because, the older the geological age, diagenesis (including shallow metamorphism) the greater the impact. However, there are also some cases in which although the structure of diagenesis has been confirmed, the mechanical structure produced during the handling and deposition of the provenance area is still partially or largely preserved and still indicates its environment.