Determining the grainsize of sediment with increasing depth in core GC11, located in the Capricorn Channel
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资源简介:
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size fractions to determine the % of each grainsize at each sample depth. Although not overly accurate, the information is correlated with analyses of other parameters to impart clues to the environmental changes within the core. The smallest size fraction (
重力岩心(gravity core)GC11采自大堡礁(Great Barrier Reef,GBR)南部的摩羯海峡(Capricorn Channel)海域,采样位置水深为海底以下502米(meters below sea level,mbsl)。研究人员将样品划分为不同粒度组分,以测定每个样品深度处各粒度组分的百分比占比。尽管该分析方法的精度并非极高,但通过将此类数据与其他参数的分析结果进行关联,可为该岩心所记录的环境变化提供相关线索。其中最小的粒度组分(
提供机构:
Australian Ocean Data Network



