{"title":"西波美拉尼亚碳岩中分散有机物的岩石学和地球化学初步分析","authors":"G. Nowak, Przemysław Karcz, Barbara Massalska","doi":"10.7306/2023.18","DOIUrl":null,"url":null,"abstract":"Preliminary petrographic and geochemical recognition of organic matter in Carboniferous rocks from Western Pomerania. Prz. Geol., 71: 224–226; doi: 10.7306/2023.18 A b s t r a c t. The paper presents results of organic petrography and Rock-Eval pyrolysis studies of Carboniferous rocks from Western Pomerania (N Poland). Samples for the studies were taken from core of the DŸwirzyno 3 borehole. The thermal maturity level of organic matter is determined by the values of: 1) vitrinite reflectance VR o = 0.82–0.93% and 2) T max = 431–460°C, which indicate oil window maturity. Organic petro- graphy studies have shown a presence of different macerals dispersed in the rocks studied. Vitrinite and inertinite are particles of humic origin, while most liptinite macerals are of aquatic provenance. The Rock-Eval data clearly indicate that the organic matter forms levels made up either of kerogen type III or of kerogen type II.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"1 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2023-05-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Wstępne rozpoznanie petrograficzne i geochemiczne materii organicznej rozproszonej w skałach karbonu Pomorza Zachodniego\",\"authors\":\"G. Nowak, Przemysław Karcz, Barbara Massalska\",\"doi\":\"10.7306/2023.18\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Preliminary petrographic and geochemical recognition of organic matter in Carboniferous rocks from Western Pomerania. Prz. Geol., 71: 224–226; doi: 10.7306/2023.18 A b s t r a c t. The paper presents results of organic petrography and Rock-Eval pyrolysis studies of Carboniferous rocks from Western Pomerania (N Poland). Samples for the studies were taken from core of the DŸwirzyno 3 borehole. The thermal maturity level of organic matter is determined by the values of: 1) vitrinite reflectance VR o = 0.82–0.93% and 2) T max = 431–460°C, which indicate oil window maturity. Organic petro- graphy studies have shown a presence of different macerals dispersed in the rocks studied. Vitrinite and inertinite are particles of humic origin, while most liptinite macerals are of aquatic provenance. The Rock-Eval data clearly indicate that the organic matter forms levels made up either of kerogen type III or of kerogen type II.\",\"PeriodicalId\":35787,\"journal\":{\"name\":\"Przeglad Geologiczny\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-05-31\",\"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/10.7306/2023.18\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Przeglad Geologiczny","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7306/2023.18","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
Wstępne rozpoznanie petrograficzne i geochemiczne materii organicznej rozproszonej w skałach karbonu Pomorza Zachodniego
Preliminary petrographic and geochemical recognition of organic matter in Carboniferous rocks from Western Pomerania. Prz. Geol., 71: 224–226; doi: 10.7306/2023.18 A b s t r a c t. The paper presents results of organic petrography and Rock-Eval pyrolysis studies of Carboniferous rocks from Western Pomerania (N Poland). Samples for the studies were taken from core of the DŸwirzyno 3 borehole. The thermal maturity level of organic matter is determined by the values of: 1) vitrinite reflectance VR o = 0.82–0.93% and 2) T max = 431–460°C, which indicate oil window maturity. Organic petro- graphy studies have shown a presence of different macerals dispersed in the rocks studied. Vitrinite and inertinite are particles of humic origin, while most liptinite macerals are of aquatic provenance. The Rock-Eval data clearly indicate that the organic matter forms levels made up either of kerogen type III or of kerogen type II.