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南北构造带中段的壳幔结构与岩石圈动力学特征
引用本文:刘晓华.南北构造带中段的壳幔结构与岩石圈动力学特征[J].大地测量与地球动力学,1993(3).
作者姓名:刘晓华
作者单位:中国地质大学 武汉
摘    要:本文利用WDM—89地球重力模型(完整到180阶)的位系数计算了南北构造带中段的30—50阶、50—100阶、100—150阶、150—180阶及2—180阶卫星重力异常,并探讨了该区的壳幔结构。结果表明,该区上地幔存在一个规模较大的低密度区。若尔盖和雅江一带有两个底部相连的高密度地幔块体。该区壳幔结构不但横向很不均匀,而且纵向也极为复杂。据此对区域岩石圈动力学特征进行了讨论。

关 键 词:南北构造带  卫星重力异常  壳幔结构  岩石圈动力学特征

STRUCTURE OF THE CRUST AND UPPER MANTLE AND FEATURE OF LITHOSPHERIC GEODYNAMICS IN THE N--S TECTONIC BELT (MIDDEL PART)
Liu Xiaohua.STRUCTURE OF THE CRUST AND UPPER MANTLE AND FEATURE OF LITHOSPHERIC GEODYNAMICS IN THE N--S TECTONIC BELT (MIDDEL PART)[J].Journal of Geodesy and Geodynamics,1993(3).
Authors:Liu Xiaohua
Abstract:In this paper, the satellite gravity anomalies of 30--50,50--100,100--150,150--180 and 2--180 degrees are computed in the N-S tectonic belt (middle part) by use of the coefficients of WDM--89 earth gravity model (to 180 degrees). The structure in the crust and upper mantle is also analysed. The results show that there exists a large zone of low density in the upper mantle. In Ruoergaiand Yajiang there are two high-denstiy mantle blocks whose bottoms connect. The structure in the crust and upper mantle is not only inhomogeneous laterally, but complicated vertically. Moreover,the Lithospheric geodynamics in the zone is discussed.
Keywords:the N-S tectonic belt  satellite gravity anomaly  the structure of crust and upper mantie  the feature of lithospheric geodynamics
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