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Late Quaternary geomorphology, seabed evolution, and terrigenous sediment delivery to the Pandora and Moresby Troughs, Gulf of Papua

机译:晚第四纪地貌,海床演化和陆源沉积物输送到巴布亚湾的潘多拉和莫尔斯比海槽

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摘要

An integrated geology and geophysics investigation has been carried out to study the late Quaternary deepwater depositional system in the Gulf of Papua (NSF-MARGINS focus area) focusing on two contrasting depocentres, Pandora and Moresby troughs. The studies incorporate multi-beam bathymetry, sub-bottom sonar, and core data in order to define and map acoustic and lithofacies; and relate depositional processes, sediment routing, timing and geomorphic products that have developed since Marine Isotope Stage (MIS) 3, ca. 40 cal ka. 3D sea floor visualisation is used to infer sedimentary processes responsible for observed morphology, which are then placed into a chronostratigraphic framework using recently published age models of sediment cores.
机译:已经进行了综合的地质和地球物理学调查,以研究巴布亚湾(NSF-MARGINS重点地区)的第四纪晚期深水沉积系统,重点研究了两个相对的沉积中心潘多拉和莫尔斯比槽。这些研究结合了多波束测深,地下声纳和核心数据,以定义和绘制声波和岩相。以及与自海洋同位素阶段(MIS)3,ca以来形成的沉积过程,沉积物路径,时间和地貌产物有关。 40卡使用3D海床可视化来推断造成观测形态的沉积过程,然后使用最近发布的沉积物年龄模型将其置于年代地层学框架中。

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