墨西哥东北部Sabinas盆地Olmos组煤相研究

IF 1.5 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Genaro de la Rosa-Rodríguez , Juan Josué Enciso-Cárdenas , Cristina Fernanda Alves Rodrigues , Manuel João Lemos de Sousa , Luis Fernando Camacho Ortegón , Eduardo González-Partida , Yuriko Yarel Bueno Yamamoto
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引用次数: 0

摘要

这项工作的重点是对来自Sabinas盆地(墨西哥)五个子盆地的Olmos组煤进行有机岩石学研究。主要目的是确定这些矿床的煤相/沉积环境。有机岩相学研究表明,各次盆地的组成各不相同。镜质组含量从Sabinas次盆地的73%到Adjuntas和Las Esperanzas次盆地的89%不等。含砷量从8% (Adjuntas次盆地)到17% (Sabinas次盆地)不等。岩石含量从2% (Adjuntas、Las Esperanzas和San Patricio子盆地)到10% (Sabinas子盆地)不等。镜质组平均随机反射率从0.92% (San Patricio子盆地)到1.38% (Adjuntas子盆地)不等。本研究记录的凝胶化指数值从4.2 (Sabinas子盆地)到10.3 (Adjuntas子盆地)不等,表明泥炭积累过程中湿度相对较高。组织保存指数在0.9 (Saltillito-Lampacitos亚盆地)和2.0 (Adjuntas亚盆地)之间变化,反映了中等至较好保存的植物组织。地下水指数从0.4 (Adjuntas和Las Esperanzas子流域)到1.1 (saltillitto - lampacitos子流域)不等,表明该流域的水文条件介于营养型和流变型之间。植被指数在1.0 (Saltillito-Lampacitos和San Patricio子盆地)和2.1 (Adjuntas子盆地)之间变化,反映有机质以草本植被为主。确定了4个沉积亚环境:(i)沼泽—滨海—滨海条件下的沼泽亚环境(saltillitto - lampacitos子盆地),(ii)滨海条件下的沼泽亚环境(Sabinas和San Patricio子盆地),(iii)沼泽—湿润森林滨海沼泽过渡亚环境(Las Esperanzas子盆地),(iv)湿润森林滨海沼泽亚环境(Adjuntas子盆地)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Coal facies of the Olmos Formation in the Sabinas Basin, Northeastern Mexico

Coal facies of the Olmos Formation in the Sabinas Basin, Northeastern Mexico
This work focuses on an organic petrographic study of the Olmos Formation coal sourced from five sub-basins within the Sabinas Basin (Mexico). The main goal was to determine the coal facies/depositional environment of these deposits. Organic petrographic studies revealed varying compositions across the sub-basins. The vitrinite content ranged from 73 % in the Sabinas Sub-basin to 89 % in the Adjuntas and Las Esperanzas sub-basins. The inertinite content varied from 8 % (Adjuntas Sub-basin) to 17 % (Sabinas Sub-basin). The liptinite content ranged from 2 % (Adjuntas, Las Esperanzas and San Patricio sub-basins) to 10 % (Sabinas Sub-basin). Vitrinite mean random reflectance values ranged from 0.92 % (San Patricio Sub-basin) to 1.38 % (Adjuntas Sub-basin). Gelification Index values recorded in this study varied from 4.2 (Sabinas Sub-basin) to 10.3 (Adjuntas Sub-basin), indicating relatively high wetness conditions during peat accumulation. Tissue Preservation Index values varied between 0.9 (Saltillito-Lampacitos Sub-basin) and 2.0 (Adjuntas Sub-basin), reflecting medium to well-preserved plant tissues. Groundwater Index values ranged from 0.4 (Adjuntas and Las Esperanzas sub-basins) to 1.1 (Saltillito-Lampacitos Sub-basin), suggesting a transition between ombrotrophic and rheotrophic hydrological conditions. The Vegetation Index varied between 1.0 (Saltillito-Lampacitos and San Patricio sub-basins) and 2.1 (Adjuntas Sub-basin), reflecting organic matter dominated by herbaceous vegetation. Four depositional sub-environments were identified: (i) a fen swamp sub-environment under limno-telmatic to telmatic conditions (Saltillito-Lampacitos Sub-basin), (ii) a fen swamp sub-environment under telmatic conditions (Sabinas and San Patricio sub-basins), (iii) a transitional sub-environment between fen and wet forested telmatic swamp (Las Esperanzas Sub-basin), and (iv) a wet forested telmatic swamp sub-environment (Adjuntas Sub-basin).
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来源期刊
Journal of South American Earth Sciences
Journal of South American Earth Sciences 地学-地球科学综合
CiteScore
3.70
自引率
22.20%
发文量
364
审稿时长
6-12 weeks
期刊介绍: Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields: -Economic geology, metallogenesis and hydrocarbon genesis and reservoirs. -Geophysics, geochemistry, volcanology, igneous and metamorphic petrology. -Tectonics, neo- and seismotectonics and geodynamic modeling. -Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research. -Stratigraphy, sedimentology, structure and basin evolution. -Paleontology, paleoecology, paleoclimatology and Quaternary geology. New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.
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