资料报告:IODP 354考察队U1450和U1451站点孟加拉扇沉积物粒度分析

S. K. Adhikari, T. Sakai, Kohki Yoshida
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引用次数: 4

摘要

用激光衍射法测定了国际海洋发现计划(IODP) 354远征队U1450和U1451地点311份沉积物样品的粒度分布。大多数样品来自浊积岩,但也检查了一些半深海床。平均粒度值表明粉砂颗粒是主要的结构类别,而粒度值范围从粘土到粗粒砂。平均粒度值总体上呈上升趋势,显示出轻微的粗化趋势。然而,其他参数如标准差、偏度和峰度与孔深没有系统的关系。分析的样品涵盖了从近代到中新世早期的年龄范围。Shepard结构分类图显示沉积物主要为砂质粉砂、粉质砂和粘质粉砂,少量粉砂和砂也存在。单个浊积层样品的频率曲线图显示,U1450站点浊积层以反级积层最为常见,而U1451站点浊积层以较厚的块状层为主。
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Data report: grain size analysis of Bengal Fan sediments at Sites U1450 and U1451, IODP Expedition 354
Grain size distributions of 311 sediment samples from Sites U1450 and U1451 of International Ocean Discovery Program (IODP) Expedition 354 were determined using laser diffraction. Most of the samples were from turbidites, but some hemipelagic beds were also examined. The mean grain size values show that siltsized particles are the dominant textural class, whereas the grain size values range from clay to coarse-grained sand. An overall upward change in mean grain size value reveals a slight coarseningupward trend. However, other parameters such as standard deviation, skewness, and kurtosis show no systematic relationship with depth in the holes. The analyzed samples cover the age range from recent to early Miocene. Shepard textural classification plots show the sediments are mostly sandy silts, silty sands, and clayey silts with a few silts and sands also present. Frequency curve plots of samples from individual turbidite beds show inversely graded beds are most common at Site U1450, whereas thicker massive beds are dominant at Site U1451.
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