摘要
对取自南黄海西部陆架区的SYS-0803孔上部的岩心样品进行了粒度分析,分离出了对沉积环境变化较敏感的粒度组分,并将粒度参数的垂向分布序列与浅地层剖面反射特征进行了对比研究。结果表明,岩心样品的粒度变化特征较好地指示了该区域古环境的演化过程,自下而上依次经历了滨浅海沉积—河流沉积—河口湾沉积—滨浅海沉积—陆架沉积等环境。
Grain-size analysis was carried out for the sediments taken from the upper part of the Core SYS- 0803 drilled in the western South Yellow Sea. The components sensitive to depositional environment are carefully studied. The vertical variation in sediment grain size, in combination with the reflection charac- teristic of seismic profiles, suggests that the sediment grain size parameters may effectively indicate the pa- leo-environment evolution. The study area has passed through a sequence of environmental changes from coastal-shallow water to fluvial deposition, to estuary deposition and to coastal - shallow water, and en- ded in an environment of continental shelf in an ascending order.
出处
《海洋地质与第四纪地质》
CAS
CSCD
北大核心
2014年第5期13-24,共12页
Marine Geology & Quaternary Geology
基金
国土资源部海洋油气资源和环境地质重点实验室开放基金(MRE201321)
国家自然科学基金(41376079)
国土资源部地质调查项目(1212010611401)
1:25万青岛幅海洋区域地质调查(试点)(GZH200900501)
关键词
粒度组分
环境演化
南黄海
sediment components
environment evolution
South Yellow Sea