杨玉春, 李清林, 栗文山. 西藏高原地区重力测量与研究[J]. 华北地震科学, 1991, 9(4): 1-11.
引用本文: 杨玉春, 李清林, 栗文山. 西藏高原地区重力测量与研究[J]. 华北地震科学, 1991, 9(4): 1-11.
Yang Yuchun, Li Qinglin, Li Wenshan. GRAVITY SURVEY AND STUDIES IN XIZANG PLATEAU REGION[J]. North China Earthquake Sciences, 1991, 9(4): 1-11.
Citation: Yang Yuchun, Li Qinglin, Li Wenshan. GRAVITY SURVEY AND STUDIES IN XIZANG PLATEAU REGION[J]. North China Earthquake Sciences, 1991, 9(4): 1-11.

西藏高原地区重力测量与研究

GRAVITY SURVEY AND STUDIES IN XIZANG PLATEAU REGION

  • 摘要: 对实测的西藏高原布格重力异常和自由空间异常的分析发现,青藏高原四周为重力异常梯级带、地壳厚度陡变带和一系列深大断裂带,从而推断青藏高原可能为一断块高原;现代欧亚板块和印度板块碰撞挤压带不是雅鲁藏布江断裂带,而是在喜马拉雅山和雅鲁藏布江的中间地带。对重力复测资料分析的结果表明,西藏地区重力场变化之敏感点在雅鲁藏布江与其稍偏南一带以及该区北东向的深大断裂带上。西藏地区的地壳运动尤其是新生代以来的地壳活动也集中表现在深大断裂带及其附近。

     

    Abstract: An analysis of observed data of Bouguer gravity anomaly and free-air anomaly shows that there are anomalous gravity gradient zone, steeply varing zone of crustal thickness and a series of deep great fracture zones around Qinghai-Xizang plateau.Thus Qinghai-Xizang plateau can be deduced as a fault-block plateau.The recent collision-compressive zone of Eurasian plate with Indian plate is on the intermediate zone between the Himalayas and the Yarlung Zangbo river rather than the Yarlung Zangbo river fracture zone.The analytic results of repeated measuring data of gravity show that sensitive points of giavity field variation in Xizang region are on the Yarlung Zangbo river and its south, as well as on the deep-great fracture zone with north east strike in this region.The crustal movements, specially crustal activities since Cenozoic Era, in Xizang have been embodied mainly in the deep great fracture zone and its vicinity.

     

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