希腊中希腊海槽煤矿床的综合研究

N. Koukouzas, P. Krassakis, P. Koutsovitis, C. Karkalis
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引用次数: 6

摘要

在希腊的中希腊海槽内蕴藏着相当数量的煤矿。它被认为是Hellenides最后造山阶段最大和最重要的盆地,被解释为晚渐新世至中新世期间形成的弧后盆地。本文以中希腊海槽成煤产状为重点,建立了简化地质图。这项工作是通过地理信息系统(GIS)完成的,并通过地理数据库组织为GIS数据文件(特征类)。在绘制地质图的过程中,对不同的地质图、原始源图和传统图进行了适当的均质化和离散化表示。下一步是使用多边形方法与相应的表格信息进行地质统计分析。根据地层年龄和与产煤地理分布相关的岩石学资料,将其划分为渐新统、中中新统和中新统上三大类煤,表现出不同的物理化学和拓扑特征。上中新世煤的面积和周长值最大,中中新世煤的周长值最小。坡向(角向)和山阴(阴起伏)等地形模型既反映了研究区煤体赋存与形态构造的空间关系,又反映了研究区的几何特征。煤主要属腐殖岩,其中以腐殖岩群矿物为主(90%)。它们的S含量可能来自母本植物或母本植物与海水硫酸盐的结合。水分含量与能源生产中煤炭使用的可持续性密切相关,而它们的碳化等级与它们的年龄密切相关,并由它们的反射率值表示。所有这些数据都已插入一个综合数据库,可用于采矿前或采矿后的活动(例如规划、分析、管理、恢复)。本研究的结果可用于有效评估现有的煤炭资源,可与可再生能源结合使用,提供可持续的解决方案,并结合即将推出的创新CCS和CCU技术。结果还表明,中第三纪海槽煤具有优良的品质特征。然而,由于缺乏经济可采储量,它们作为可燃煤的价值非常低。过去已开采出最大的煤透镜体,其余的矿点不超过几千吨。根据现有文献和地理空间估算,中希腊海槽盆地的煤炭储量不能被认为具有经济开采价值。
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An integrated approach to the coal deposits in the Mesohellenic Trough, Greece
A considerable amount of coal deposits occur within the Mesohellenic Trough in Greece. It is considered as the largest and most important basin of the last orogenic stage of the Hellenides, which is interpreted as a back-arc basin that evolved during the period of Late Oligocene to Miocene. In this study, a simplified geological map has been constructed emphasizing on the coal formation occurrences of the Mesohellenic Trough. This work has been accomplished, through Geographic Information Systems (GIS) and has been organized via geodatabase as GIS data files (feature classes). For the creation of the geological map suitable homogenization and discrete representation has been implemented different geological sheets, original source and traditional maps. Next step was the geostatistical analysis using polygonal methods linked to the corresponding tabular information. Regarding the stratigraphical age, and petrographic data related to geographic distribution of the coal occurrences, these are divided into three categories: Oligocene, Middle Miocene and Upper Miocene coals, exhibiting various physicochemical and topological properties. Upper Miocene coal exhibits the greatest area and perimeter values, while the lowest values correspond to those of the Middle Miocene. Terrain models such as aspect (angle-direction) and hillshade (shaded relief) showed the spatial relation between coal occurrences and morphotectonic as long as geometrical characteristics of the study area. Coals are mainly classified as huminites including mainly huminite group minerals (90%). Their S contents can probably derive from parent plant material or a combination of parent plant material with seawater sulfates. Moisture contents are strongly connected with the sustainability of the coal use in the energy production, while their carbonation grade is strongly associated with their age and expressed by their reflectivity values. All these data have been inserted in an integrated database and can be useful for pre-mining or post mining activities (e.g. planning, analysis, management, restoration). Results of this study are available for the effective evaluation of the existing coal occurrences, which can be used with renewable energy sources providing sustainable solutions, in combination with the upcoming innovative CCS and CCU technologies. Results also showed that coals from the Mesohellenic Trough present excellent quality traits. However, their value as combustible coal is very low due to the absence of economically recoverable reserves. The largest coal lenticular bodies have been extracted in the past and the remaining occurrences do not exceed several thousand tones. Based upon existing literature and from geospatial estimations, coal deposits in the Mesohellenic Trough Basin cannot be considered as economically valuable for exploitation.
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