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首页> 外文期刊>Russian journal of Pacific geology >Space Geodesy in Geodynamic Studies:Recent Movements in the Zeya—Bureya Basin
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Space Geodesy in Geodynamic Studies:Recent Movements in the Zeya—Bureya Basin

机译:地球动力学研究中的空间大地测量学:Zeya-Bureya盆地的近期运动

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摘要

The Amur–Zeya geodynamic test ground was set up in 2000 to study recent intracontinental crustaldeformations. The velocity field calculations for the period of 2000 to 2003 describe three movements scales.The general level is characterized by the vectors of IGS sites in the eastern part of Asia, the BLAG (Blagovesh-chensk) site included. The southeast movement of the IRKT (Irkutsk) site of the stable Siberian Platform isindicative of deformations in the northeastern part of the Amur Plate. Measurement data on the regional near-latitudinal profile Blagoveshchensk–Sutara, which crosses the Nizhnyaya Zeya Basin, demonstrate a south-westward displacement of the Badzhal–Bureya–Lesser Khingan block relative to the North China block. Thedynamic effect of the convergent boundary between the Amur and Okhotsk Sea plates is assumed to extendinland also involving the Zeya–Bureya Basin area. The measurements on the local geodynamic test site relatethe deformations of buildings and constructions in the Settlement of Konstantinovka to the mobility of base-ment faults in the southern part of the Nizhnyaya Zeya Basin. Aseismic. deformations are determined by slowhorizontal tectonic movements in the junction zone of NNE-trending structures of the latter basin and near-lat-itudinal faults of the Khailar–Xunhei Belt.
机译:阿穆尔-泽亚(Amur-Zeya)地球动力学试验场建立于2000年,用于研究最近的洲内地壳形变。 2000年至2003年期间的速度场计算描述了三个运动尺度。总体水平以亚洲东部IGS站点的矢量为特征,其中包括BLAG(Blagovesh-chensk)站点。稳定的西伯利亚平台IRKT(伊尔库茨克)站点的东南运动表明阿穆尔板块东北部的变形。跨下Nizhnyaya Zeya盆地的区域近纬剖面Blagoveshchensk–Sutara的测量数据表明,Badzhal–Bureya–Lesser Khingan区块相对于华北区块向西南位移。假定阿穆尔河与鄂霍次克海板块之间会聚边界的动力效应向内陆扩展,也涉及Zeya-Bureya盆地地区。局部地球动力学试验场的测量结果表明,Konstantinovka聚落中建筑物的变形与Nizhnyaya Zeya盆地南部基底断裂的活动性有关。抗震变形是由后盆地NNE趋势构造的交汇区的慢水平构造运动和Khailar–Xunhei带的近纬断层决定的。

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