{"title":"Badania ramanowskie i mikrotermometria inkluzji a możliwości metodyczne i interpretacyjne","authors":"T. Toboła, K. Jarmołowicz-Szulc","doi":"10.7306/2023.21","DOIUrl":null,"url":null,"abstract":"A b s t r a c t. Based on the hitherto existing problems on understanding and interpretation of fluid inclusion microthermometric results and the relatively uncomplicated access to the Raman microspectrometry, both methods have been explained and applied to several samples from the Carpathians and to one sample from a borehole in central Poland (Katarzynin 2). The results of both types of analytical methods are different temperature values of T h – homoge- nization temperature, T e – eutectic temperature, T m – ice melting temperature, and the coalifi- cation of organic matter (MO). They are interpreted together, which gives a wide range of dis-cussion possibilities significant from the geological point of view.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2023-04-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Przeglad Geologiczny","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7306/2023.21","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 0
Abstract
A b s t r a c t. Based on the hitherto existing problems on understanding and interpretation of fluid inclusion microthermometric results and the relatively uncomplicated access to the Raman microspectrometry, both methods have been explained and applied to several samples from the Carpathians and to one sample from a borehole in central Poland (Katarzynin 2). The results of both types of analytical methods are different temperature values of T h – homoge- nization temperature, T e – eutectic temperature, T m – ice melting temperature, and the coalifi- cation of organic matter (MO). They are interpreted together, which gives a wide range of dis-cussion possibilities significant from the geological point of view.
b s t r c t。基于迄今存在的问题对理解和解释的流体包裹体microthermometric结果和相对简单的访问喇曼microspectrometry,解释了这两种方法并应用于几个样本喀尔巴阡山和一个样本在波兰中部钻孔(Katarzynin 2)。这两种分析方法的结果是不同的温度t h - homoge电离作用温度的值,共晶温度、融冰温度和有机质(MO)的煤化作用。它们一起解释,从地质学的角度来看,这提供了广泛的讨论可能性。