尼泊尔中部加德满都谷地南部盆地充填沉积物的地层学与沉积环境

M. Paudel, H. Sakai
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引用次数: 5

摘要

为了澄清古加德满都湖形成初期的地层,重建沉积环境,研究了加德满都盆地南部四元线河湖盆填沉积。6个地层单位;在野外观察岩性和沉积分布的基础上,描述了Tarebhir、Lukundol、Itaiti、Kalimati、Sunakothi组和阶地砾石矿床。塔雷希尔组为基底单元,南部为伊塔提组冲积扇覆盖,北部为鲁孔多尔组边缘湖相沉积覆盖。从Jorkhu盆地边缘向北再往北3公里处,Lukundol组被Kalimati组的开阔湖相覆盖。在同一地点,后者被苏纳科提组的河流湖相覆盖。此外,阶地砾石沉积侵蚀覆盖了Sunakothi组。加里玛提组向北增厚,苏纳科提组在盆地中部和南部之间增厚。研究表明,苏纳科提组为河流-湖相(河流-三角洲-浅湖相)成因,从盆地南缘(~1400m)向盆地中部(~1300m)连续延伸。这也表明该地层的沉积物是在湖泊水位上升和下降时沉积的。南缘厚砾石层序代表古加德满都湖形成前(1 Ma以前)的冲积扇,而Sunakothi组上方厚砾石层序代表晚更新世阶地砾石沉积(14C法),沉积于古加德满都湖自南向北萎缩期间和之后。doi: 10.3126/ bg .v11i0.1544尼泊尔加德满都特里布万大学地质系学报,2008年第11卷,第61-70页
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Stratigraphy and depositional environments of basin-fill sediments in southern Kathmandu Valley, Central Nepal
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
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