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作 者:方中华[1,3] 李攀峰 杨源[1,3] 杨慧良 陆凯[1,3] 杨佳佳 单瑞 Fang Zhonghua;Li Panfeng;Yang Yuan;Yang Huiliang;Lu Kai;Yang Jiajia;Shan Rui(Qingdao Institute of Marine Geology,China Geological Survey,Qingdao 266071,China;Yantai Center of Coastal Zone Geological Survey,China Geological Survey,Yantai 264003,China;Laboratory for Marine Mineral Resources,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266237,China)
机构地区:[1]中国地质调查局青岛海洋地质研究所,山东青岛266071 [2]中国地质调查局烟台海岸带地质调查中心,山东烟台264003 [3]青岛海洋科学与技术试点国家实验室海洋矿产资源评价与探测技术功能实验室,山东青岛266237
出 处:《海洋学报》2022年第3期53-60,共8页
基 金:中国地质调查局项目(DD20191003)。
摘 要:本文依托菲律宾海浅地层剖面资料,结合前人已发表的该区域样品资料和钻孔资料,对九州-帕劳海脊以及与海脊相邻的西菲律宾海盆和帕里西维拉海盆浅层沉积物特征进行了初步研究。研究认为海底以下浅层沉积物一般存在3个波阻抗界面,根据其反射特征划分为4个基本类型,并对剖面特征的成因进行了初步探讨,认为在沉积物的沉积过程中,沉积物供给、构造活动、地形以及水动力条件等都对深水沉积起到了重要的作用。本文通过对菲律宾海浅地层沉积特征和控制因素的分析,可为进一步开展菲律宾海深水浅层沉积物研究提供参考。Based on the data of Philippine shallow strata profile, combined with the sample data and borehole data in this area, this paper has a preliminary understanding of the shallow sediment characteristics of Kyushu-Palau Ridge and the West Philippine Basin and Parisi Vera Basin adjacent to the ridge. There are generally three wave impedance interfaces below the seabed, and the reflection characteristics of the shallow stratum profile are divided into four basic types. The causes of the profile characteristics are preliminarily discussed. It is believed that the sediment supply, tectonic activities, topography and hydrodynamic conditions play an important role in the deep-water sedimentation during the sedimentation process. Besides being influenced by the main control factors, most of them are also superimposed with the transformation effects of various factors in the later period. In this paper, the sedimentary characteristics and controlling factors of shallow strata in Philippine Sea are analyzed, which can provide useful reference for further study of deep shallow sediments in Philippine Sea.
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