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Stratigraphy and depositional environments of basin-fill sediments in southern Kathmandu Valley, Central Nepal

机译:尼泊尔中部加德满都谷地南部盆地填充沉积物的地层学和沉积环境

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Quatenary fluvio-lacustrine basin-fill sediments in the southern part of the Kathmandu Basin was studied in order to clearify the stratigraphy and reconstruct the sedimentary environment during the initial stage of the Paleo-Kathmandu Lake. Six stratigraphic units; Tarebhir, Lukundol, Itaiti, Kalimati, Sunakothi Formations and Terrace gravel deposits, have been described based on field observation of lithology and sediment distribution. The Tarebhir Formation is the basal unit which is overlained by alluvial fan of the Itaiti Formation in the southern part and by the marginal lacustrine deposit of the Lukundol Formation towards the northern part. Further 3 km toward the north from the basin margin at Jorkhu the the Lukundol Formation is overlain by the open lacustrine facies of the Kalimati Formation. At the same locality the latter is overlain by fluvio-lacustrine facies of the Sunakothi Formation. Moreover, the Terrace gravel deposits erosionally cover the Sunakothi Formation. The Kalimati Formation thickens northward, while the Sunakothi Formation thickens between the central and southern part of the basin. The study shows that the Sunakothi Formation is of fluvio-lacustrine (fluvial, deltaic and shallow lacustrine) origin and extends continuously from the southern margin (~1400m amsl) to the central part (~1300m amsl) of the basin. It also indicates that sediments of this formation were deposited at the time of lake level rise and fall. Thick gravel sequence in the southern margin represents the alluvial fan before the origin (before 1 Ma) of the Paleo-Kathmandu Lake, while thick gravel sequence situated above the Sunakothi Formation is the Terrace gravel deposits of the late Pleistocene age (14C method), deposited during and after the shrinkage of the Paleo-Kathmandu Lake from south to north. ? doi: 10.3126/bdg.v11i0.1544 Bulletin of the Department of Geology, Tribhuvan University, Kathmandu, Nepal, Vol. 11, 2008, pp. 61-70
机译:对加德满都盆地南部的第四纪河流湖盆盆地沉积物进行了研究,以期清除地层并重建古加德满都湖初期的沉积环境。六个地层单位;基于对岩性和沉积物分布的现场观察,已经描述了塔勒布希尔,卢孔多尔,伊塔伊蒂,卡利马蒂,苏纳科西地层和阶地砾石沉积物。 Tarebhir组是基底单元,南部被Itaiti组的冲积扇和北部的Lukundol组的边缘湖相沉积所覆盖。从Jorkhu盆地边缘向北3公里处,Lukundol组被Kalimati组的开放湖相覆盖。在同一地点,后者被Sunakothi组的河流湖相相覆盖。此外,梯田砾石沉积物侵蚀性地覆盖了Sunakothi组。 Kalimati组向北增厚,而Sunakothi组在盆地中部和南部之间增厚。研究表明,Sunakothi组是河流-湖相(河流,三角洲和浅湖相)起源的,并从盆地的南部边缘(〜1400m amsl)连续延伸到盆地的中部(〜1300m amsl)。这也表明这种形成的沉积物是在湖水位上升和下降时沉积的。南缘的厚砾石层序代表古加德满都湖发源之前(1 Ma之前)的冲积扇,而位于Sunakothi组上方的厚​​砾石层序是晚更新世(14C方法)的阶地砾石沉积物,在加德满都湖从南向北收缩期间和之后沉积。 ? doi:10.3126 / bdg.v11i0.1544 Tribhuvan大学地质系公告,尼泊尔加德满都,卷2008年11月,第61-70页

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