首页> 中文期刊>极地研究 >普里兹湾陆架表层沉积物粒度特征及其环境指示意义

普里兹湾陆架表层沉积物粒度特征及其环境指示意义

     

摘要

Grain size characteristics of surface sediments on the Prydz Bay shelf , East Antarctica , together with dynamic environment , were analyzed to illustrate sediment types , compositions and relevant glaciomarine sedimentation .The surface sediments were classified into nine types:gravel, muddy sandy gravel, gravelly mud, gravelly muddy sand, slightly gravelly mud , slightly gravelly muddy sand , sand , sandy silt , and silt .The study area could be divided in-to two sections based on sediment grain size and topography , a gravelly mud section in the east of the bay and a gravelly sand section in the west .In the eastern gravelly mud section , including Four Ladies Bank , the Svenner Channel , the Prydz Channel and the Amery Basin , sedimentation is mainly controlled by marine circulation with lit-tle contribution from iceberg , and then sediments are relatively fine and contain a large amount of clay and fine silt . In contrast , the coarse-grained sediments in the western gravelly sand section , including the Fram Bank and the Amery Ice Shelf front , are products of iceberg , current and Amery ice shelf with an exception of fine-grain sediment occurring in the polynya .%基于对普里兹湾陆架表层沉积物粒度分析,结合海区动力环境特点,初步探讨了考察区类型、组成及冰海沉积作用特点。研究区表层沉积物大体可分为:砾( G)、泥质砂质砾( msG)、砾质泥( gM)、砾质泥质砂( gmS)、含砾泥((g)M)、含砾泥质砂((g)mS)、砂(S)、砂质粉砂(sZ)和粉砂(Z)九种类型。依据沉积物粒度特征与地形变化,可将研究区划分为东部含砾泥质区和西部含砾砂质区。在东部含砾泥质区,包括四夫人浅滩、Svenner水道区、普里兹水道区和埃默里海盆区,沉积作用主要受海流影响,冰筏碎屑的影响有限,沉积物总体较细,粘土和细粉砂含量较高,粗粉砂和砂含量较低。在西部含砾砂质区,包括弗拉姆浅滩和埃默里冰架前缘,沉积作用受冰山、埃默里冰架和海流的共同影响,沉积物中粘土含量较低,砂和砾石含量较高,但也有个别站位可能受冰间湖的影响,沉积物粒度偏细。

著录项

相似文献

  • 中文文献
  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号