琼东北八所组ESR年龄及其构造意义
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摘要
八所组是琼东北晚第四纪一个重要地层单位,同时也是河流Ⅱ级阶地(T2)的主要沉积地层,其形成年代对该区域晚第四纪以来的古环境演化及地壳运动的研究有着重要意义。为了限定其形成时代,文章采取ESR的方法,对广泛分布于琼东北珠溪河及古三江河一带的八所组地层进行了系统的测年。结果表明:该套地层形成于晚更新世中晚期(64.36 ka～18.40 ka BP);沉积时代对应末次冰期MIS4～MIS2阶段;河流的下切与T2阶地的形成,一定程度上反映了该时期琼东北海平面的频繁波动及地壳的间歇性抬升;此外,分布于现代海岸风沙强烈作用地带的老红砂与八所组属同期异相的风成堆积,应与八所组地层加以区分。
The Basuo Formation is an important stratigraphic unit in late quaternary and forms the main sedimentary formation of the second-level terrace(T2) in northeastern Hainan Province. Its formation age is of great significance to the study of paleoenvironmental evolution and crustal movement in the study area since late quaternary. In order to precisely define the age of this formation, we conducted a systematic research of the Basuo Formation distributed in Zhuxi River and Gusanjiang River in northeastern Hainan by using the method of Electron Spin Resonance(ESR) and acquired the geochronological data. The results show that the Basuo Formation was formed during 64.36～18.40 ka BP, and the sedimentary age corresponds to the last glacial stage of MIS4～MIS2; The river incision and the formation of T2 terrace, to some extent, reflect the frequent fluctuation of sea level and the intermittent uplift of crust in the northeast of Hainan during this period; moreover, the old red sands in the strong sandstorm action zone of modern coasts is the aeolian accumulation of contemporaneous and heterogeneous with the Baduo formation, which should be distinguished from the Baduo formation.
The Basuo Formation is an important stratigraphic unit in late quaternary and forms the main sedimentary formation of the second-level terrace(T2) in northeastern Hainan Province. Its formation age is of great significance to the study of paleoenvironmental evolution and crustal movement in the study area since late quaternary. In order to precisely define the age of this formation, we conducted a systematic research of the Basuo Formation distributed in Zhuxi River and Gusanjiang River in northeastern Hainan by using the method of Electron Spin Resonance(ESR) and acquired the geochronological data. The results show that the Basuo Formation was formed during 64.36～18.40 ka BP, and the sedimentary age corresponds to the last glacial stage of MIS4～MIS2; The river incision and the formation of T2 terrace, to some extent, reflect the frequent fluctuation of sea level and the intermittent uplift of crust in the northeast of Hainan during this period; moreover, the old red sands in the strong sandstorm action zone of modern coasts is the aeolian accumulation of contemporaneous and heterogeneous with the Baduo formation, which should be distinguished from the Baduo formation.
引文
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