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青海地区现今垂直形变场概貌及与构造运动和强震活动性的关系

THE OUTLINE OF RECENT VERTICAL DEFORMATION FIELD AND THE RELATIONSHIP BETWEEN VERTICAL DEFORMATION AND RECENT TECTONIC MOTION AND STRONG EARTHQUAKES ACTIVITY IN QINGHAI AREA
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摘要 本文利用青海地区近几十年的大地测量资料,探讨了该区现今地壳垂直形变与现代构造运动及强震活动之间的关系,认为青藏高原北部目前仍处于强烈的构造运动活跃期,判定了两处有可能是未来发生强震的场所,并对青藏高原北部强震成因提出了作者的看法。 Based on date of geodetic survey of recent decades in Qinghai area, the relationship between vertical deformation snd recent tectonic motion and strong earthquake activity is discussed in this paper. It is said that north Qinghai-Tibet Plateau is in strong tectonic motion activity period and two areas have been judged as potential source region of strong earthquake in future. The idea of genetic factor of strong earthquakes in the north Qinghai-Tibet Pleateau has been subjected also.
作者 邹文卫
出处 《高原地震》 1994年第2期24-29,共6页 Plateau Earthquake Research
关键词 地壳形变 垂直形变图 现代地壳运动 青藏高原 Crustal deformation Vertical deformation map Recent crushal movement Qinghai-Tibet Plateau
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