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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Pedogenesis of late Quaternary deposits, northern Kyonggi Bay, Korea: Implications for relative sea-level change and regional stratigraphic correlation
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Pedogenesis of late Quaternary deposits, northern Kyonggi Bay, Korea: Implications for relative sea-level change and regional stratigraphic correlation

机译:韩国京畿道北部第四纪晚期沉积物成岩作用:对相对海平面变化和区域地层相关性的影响

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摘要

Late Pleistocene and early Holocene paleosols are described from construction pits and boreholes in the northern Kyonggi Bay, west coast of Korea. Thin-section petrography, chemistry, clay mineralogy and geotechnical properties of the paleosols were examined to infer relative sea-level fluctuations during the late Quaternary. Relict laminae and gradational contacts with underlying tidal rhythmites confirm that the late Pleistocene paleosol is a pedogenically altered tidal deposit. Illuvial clay coatings, rootlets and enrichment of kaolinite and chemically stable oxides indicate that pedogenesis occurred on a well-drained, stable surface during the last glacial period. Redoximorphic features, such as drab-colored root traces and sphaerosiderite, however, suggest that waterlogged conditions developed temporarily due to a rise of the water table at the end of the last glacial period. As sea level rose, an early Holocene paleosol formed in freshwater bog deposits, burying the late Pleistocene paleosol. The early Holocene paleosol has abundant sphaerosiderites and organic material. The presence of weakly developed illuvial clay coatings, oxidized siderites and pellets, however, indicates oxidizing condition associated with water-table fall occurred during the early Holocene. Despite the similarity in the degree of chemical and clay mineralogical weathering, the late Pleistocene paleosol is distinguished from its early Holocene counterpart by thicker and more abundant illuvial clay coatings, more Fe-2(3)O and a greater degree of consolidation. Duration of pedogenesis might be a primary cause for the difference of the pedofeatures with climate playing a secondary role. The widespread presence of similar late Pleistocene paleosols highlights its significance as a key stratigraphic marker for regional correlations along the west coast of Korea. 2005 Elsevier B.V. All rights reserved.
机译:在韩国西海岸的京畿湾北部的建筑坑和钻孔中描述了晚更新世和全新世早期的古土壤。研究了古土壤的薄层岩石学,化学,粘土矿物学和岩土工程特性,以推断第四纪晚期的相对海平面波动。遗留的薄片和与潮汐节律的渐进接触证实了晚更新世的古土壤是由成因改变的潮汐沉积物。潮土粘土涂层,小根以及高岭石和化学稳定氧化物的富集表明,成岩作用发生在最后一个冰川期的排水良好的稳定表面上。但是,氧化还原形态的特征,如淡黄色的根迹和闪粉,表明由于上一个冰川期结束时地下水位的升高,浸水条件暂时发展。随着海平面上升,淡水沼泽沉积物中形成了全新世的古土壤,掩埋了晚更新世的古土壤。早期全新世古土壤含有丰富的方铁矿和有机物。然而,发育较弱的砂土粘土涂层,氧化的菱铁矿和球团的存在表明与全新世早期的地下水位下降有关的氧化条件。尽管化学和粘土矿物风化的程度相似,但更新世晚期古土壤与新世早期古土壤的区别在于较厚的和更丰富的砂土粘土涂层,更多的Fe-2(3)O和更大的固结度。成岩作用的持续时间可能是造成成虫差异的主要原因,而气候起次要作用。类似晚更新世古土壤的广泛存在突出了其作为韩国西海岸区域相关性的关键地层标志的重要性。 2005 Elsevier B.V.保留所有权利。

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