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

Q4 Earth and Planetary Sciences
G. Nowak, Przemysław Karcz, Barbara Massalska
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引用次数: 0

摘要

西波美拉尼亚石炭系岩石有机质的岩石学和地球化学初步识别。Prz。青烟。中华医学杂志,71:224-226;本文介绍了波兰西部波美拉尼亚石炭系岩石的有机岩石学和岩石热解研究结果。研究样本取自DŸwirzyno 3钻孔的岩心。有机质热成熟度由镜质体反射率VR = 0.82 ~ 0.93%和tmax = 431 ~ 460℃确定,反映油窗成熟度。有机岩石学研究表明,所研究的岩石中分散着不同的矿物。镜质组和惰质组为腐殖质颗粒,而大多数脂质组的物源为水生。Rock-Eval数据明确表明有机质形成水平由干酪根III型和干酪根II型组成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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.
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来源期刊
Przeglad Geologiczny
Przeglad Geologiczny Earth and Planetary Sciences-Geology
CiteScore
0.70
自引率
0.00%
发文量
24
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