山西平朔矿区上石炭统太原组11号煤层具有中硫、高灰、较高有机硫的特征,但其中各煤分层的基本性质差异较大,指示其成煤微环境显著变化。地球化学研究表明,Ca/ (Ca +Fe)、Th/U、Al/Ti、V/Zn、δEu、δCe可作为指示11号煤层沉积水介质盐...山西平朔矿区上石炭统太原组11号煤层具有中硫、高灰、较高有机硫的特征,但其中各煤分层的基本性质差异较大,指示其成煤微环境显著变化。地球化学研究表明,Ca/ (Ca +Fe)、Th/U、Al/Ti、V/Zn、δEu、δCe可作为指示11号煤层沉积水介质盐度的标志,St,d、So ,d/Sp,d可分别作为指示水介质氧化还原程度和酸碱度的标志,Ad、V/I、ΣREE可作为指示水介质动力条件的标志。在此基础上,分析了该煤层成煤微环境特征及其演化历程,认为11号煤层形成于波动式海进的半咸水—咸水沉积环境。在此过程中,海水对泥炭沼泽的影响经历了3个发展阶段:第1阶段,泥炭形成于微咸—半咸水条件,水动力条件逐渐增强;第2阶段,泥炭形成于半咸水—咸水条件,水动力条件总体上相对较强,沼泽水体从逐渐加深演化为显著变浅;第3阶段,泥炭形成于半咸水环境,海水影响再次逐渐增强,在泥炭沼泽演化末期水体显著变深,动力条件明显减弱,还原性显著增强。展开更多
In South China four depositional sequences are recognized in the upper part of Upper Devonian and Tournaisian. They are named SQ0 SQ1, SQ2 and SQ3 in ascending order. SQ0 is Strunian (uppermost Devonian), and the othe...In South China four depositional sequences are recognized in the upper part of Upper Devonian and Tournaisian. They are named SQ0 SQ1, SQ2 and SQ3 in ascending order. SQ0 is Strunian (uppermost Devonian), and the other three Tournaisian in age. These four depositional sequences appear to correlate fairly well with the four sequence recognized in Europe, North America and other areas. This may suggest that these sequences are synchronous depos- its resulted from the eustatic changes. The present study on sequence stratigraphy, biostratigraphy and event stratigraphy indicates that in neritic facies areas of South China, the Devonian-Carboniferous boundary, matching the boundary between Siphonodella praesulcata zone and S. sulcata zone in pelagic facies areas, is not only higher than the top of the Cystophrentis zone, but also higher than the top of the Devonian-Carboniferous boundary event bed. In neritic facies areas, the Devonian-Carbonifrerous boundary is marked by the most distinct transgressive surface within the Cystophrentiseudouralina interval zone, i. e. at the base of the TST of the SQ1. This boundary coincides with the top surface of the event bed resulted from the eustatic fall, and approximately corresponds to the basal part of Rseudouralina assemblage zone.展开更多
文摘山西平朔矿区上石炭统太原组11号煤层具有中硫、高灰、较高有机硫的特征,但其中各煤分层的基本性质差异较大,指示其成煤微环境显著变化。地球化学研究表明,Ca/ (Ca +Fe)、Th/U、Al/Ti、V/Zn、δEu、δCe可作为指示11号煤层沉积水介质盐度的标志,St,d、So ,d/Sp,d可分别作为指示水介质氧化还原程度和酸碱度的标志,Ad、V/I、ΣREE可作为指示水介质动力条件的标志。在此基础上,分析了该煤层成煤微环境特征及其演化历程,认为11号煤层形成于波动式海进的半咸水—咸水沉积环境。在此过程中,海水对泥炭沼泽的影响经历了3个发展阶段:第1阶段,泥炭形成于微咸—半咸水条件,水动力条件逐渐增强;第2阶段,泥炭形成于半咸水—咸水条件,水动力条件总体上相对较强,沼泽水体从逐渐加深演化为显著变浅;第3阶段,泥炭形成于半咸水环境,海水影响再次逐渐增强,在泥炭沼泽演化末期水体显著变深,动力条件明显减弱,还原性显著增强。
文摘In South China four depositional sequences are recognized in the upper part of Upper Devonian and Tournaisian. They are named SQ0 SQ1, SQ2 and SQ3 in ascending order. SQ0 is Strunian (uppermost Devonian), and the other three Tournaisian in age. These four depositional sequences appear to correlate fairly well with the four sequence recognized in Europe, North America and other areas. This may suggest that these sequences are synchronous depos- its resulted from the eustatic changes. The present study on sequence stratigraphy, biostratigraphy and event stratigraphy indicates that in neritic facies areas of South China, the Devonian-Carboniferous boundary, matching the boundary between Siphonodella praesulcata zone and S. sulcata zone in pelagic facies areas, is not only higher than the top of the Cystophrentis zone, but also higher than the top of the Devonian-Carboniferous boundary event bed. In neritic facies areas, the Devonian-Carbonifrerous boundary is marked by the most distinct transgressive surface within the Cystophrentiseudouralina interval zone, i. e. at the base of the TST of the SQ1. This boundary coincides with the top surface of the event bed resulted from the eustatic fall, and approximately corresponds to the basal part of Rseudouralina assemblage zone.
