Reconstruction of the Paleoenvironment of the Lignite Deposit at Pontokomi (Sector 6), Ptolemaida Basin, Greece, Based on Its Maceral Composition

P. Antoniadis, S. M. Abatzi, E. Mavridou, T. Gentzis
{"title":"Reconstruction of the Paleoenvironment of the Lignite Deposit at Pontokomi (Sector 6), Ptolemaida Basin, Greece, Based on Its Maceral Composition","authors":"P. Antoniadis, S. M. Abatzi, E. Mavridou, T. Gentzis","doi":"10.1080/009083190518998","DOIUrl":null,"url":null,"abstract":"The lignite deposit at Pontokomi (Sector 6) in the Ptolemaida Basin of Greece was studied petrographically so that the conditions that prevailed in the paleo-environment could be analyzed. The above deposit is situated in the northwestern part of the broader basin of Ptolemaida in Macedonia, Greece. It consists of alternating beds of lignite and interbedded strata. The interburden is made of clay marls, occasionally enriched in sand. Thirty-seven samples of lignite were taken for analysis from two representative coreholes (Δ3 and Δ5) located in the central part of the lignite deposit. The study showed that macerals of the huminite group were dominant, followed by inertinite macerals. Liptinites made up a small percentage of the total population. Densinite, attrinite, eu-ulminite, corpohuminite and detrogelinite were the most abundant huminite group macerals, respectively. Inertodetrinite and fusinite were the dominant inertinite macerals, while sporinite and resinite were the predominant litpinite macerals. Mineral matter consisted mainly of clays, carbonates and pyrite. Detailed maceral analysis allowed us to obtain indices related to the wetness in the peat swamp (GI), degree of vegetation growth (VI), level of water table (GWI), and preservation of plant tissues (TPI). By comparing ratios of these indices and correlating them to ternary diagrams developed by different authors, we were able to obtain valuable information as to the conditions that dominated in the original peat swamp. The ratio of VI/GWI provided data on the hydrology and nutrient supply in the peat-forming environment, whereas the ratio of TPI/GI was used to interpret the paleo-environment in relation to the water table. Evaluation of the data showed that the environment that hosted the parent flora was limnic (open water) dominated by grasses and sedges under rheotrophic to mesotrophic nutrient supply conditions.","PeriodicalId":11841,"journal":{"name":"Energy Sources","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2005-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Energy Sources","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/009083190518998","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

The lignite deposit at Pontokomi (Sector 6) in the Ptolemaida Basin of Greece was studied petrographically so that the conditions that prevailed in the paleo-environment could be analyzed. The above deposit is situated in the northwestern part of the broader basin of Ptolemaida in Macedonia, Greece. It consists of alternating beds of lignite and interbedded strata. The interburden is made of clay marls, occasionally enriched in sand. Thirty-seven samples of lignite were taken for analysis from two representative coreholes (Δ3 and Δ5) located in the central part of the lignite deposit. The study showed that macerals of the huminite group were dominant, followed by inertinite macerals. Liptinites made up a small percentage of the total population. Densinite, attrinite, eu-ulminite, corpohuminite and detrogelinite were the most abundant huminite group macerals, respectively. Inertodetrinite and fusinite were the dominant inertinite macerals, while sporinite and resinite were the predominant litpinite macerals. Mineral matter consisted mainly of clays, carbonates and pyrite. Detailed maceral analysis allowed us to obtain indices related to the wetness in the peat swamp (GI), degree of vegetation growth (VI), level of water table (GWI), and preservation of plant tissues (TPI). By comparing ratios of these indices and correlating them to ternary diagrams developed by different authors, we were able to obtain valuable information as to the conditions that dominated in the original peat swamp. The ratio of VI/GWI provided data on the hydrology and nutrient supply in the peat-forming environment, whereas the ratio of TPI/GI was used to interpret the paleo-environment in relation to the water table. Evaluation of the data showed that the environment that hosted the parent flora was limnic (open water) dominated by grasses and sedges under rheotrophic to mesotrophic nutrient supply conditions.
希腊Ptolemaida盆地Pontokomi(6段)褐煤矿床的矿物组成及其古环境重建
对希腊托勒梅达盆地Pontokomi(6区)褐煤矿床进行了岩石学研究,分析了其在古环境中占优势的条件。上述矿床位于希腊马其顿广阔的托勒梅达盆地的西北部。它由褐煤层和互层地层交替组成。夹层由粘土泥灰岩构成,偶尔富含沙子。从位于褐煤矿床中部的两个具有代表性的岩心孔(Δ3和Δ5)中采集了37个褐煤样品进行分析。研究表明,腐殖岩类矿物占主导地位,惰质矿物次之。利普顿人只占总人口的一小部分。辉石、亚克力石、欧铝石、硅铝石和硅铝石分别是最丰富的腐殖石组矿物。惰泥质和丝质是主要的惰泥质矿物,孢子质和树脂质是主要的岩质矿物。矿物主要由粘土、碳酸盐和黄铁矿组成。详细的显微分析使我们能够获得与泥炭沼泽的湿度(GI)、植被生长程度(VI)、地下水位(GWI)和植物组织保存(TPI)相关的指标。通过比较这些指数的比率,并将它们与不同作者开发的三元图相关联,我们能够获得有关原始泥炭沼泽占主导地位的条件的宝贵信息。VI/GWI比值提供了泥炭形成环境的水文和养分供应数据,而TPI/GI比值用于解释古环境与地下水位的关系。结果表明,在流变-中营养化条件下,原生植物区系为以禾草和莎草为主的沼泽(开阔水域)环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信