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-  2017 

时变重力测量确定青藏高原地壳隆升与增厚速率
Determination of Crust Uplifting and Thickening of Qinghai-Tibetan Plateau from Time-Variable Gravity Measurements

DOI: 10.13203/j.whugis20140898

Keywords: 绝对重力,卫星重力,重力测量,重力变化,隆升,增厚,
absolute gravity
,satellite gravity,gravity measurements,gravity change,uplift,thickening

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Abstract:

联合绝对重力和重力反演与气候实验卫星(gravity recovery and climate experiment, GRACE)重力多年观测数据,获得了青藏高原多个基准站区域的地壳垂直形变速率。研究结果表明,绝对重力呈明显的负变化,绝对重力和卫星重力的时变系统差也呈较一致的负值,鼎新(DXIN)、德令哈(DLHA)、西宁(XNIN)、拉萨(LHAS)和仲巴(XZZB)5个基准站的区域地壳垂直形变呈明显的隆升状态,即拉萨块体、祁连块体和阿拉善块体处于地壳隆升状态,隆升速率分别约为2.01±0.15 mm/a、1.88±0.19mm/a、1.91±0.10 mm/a。在印度板块和欧亚板块的双向挤压下,青藏高原的地壳在不断的隆升与增厚,平均隆升速率约为1.94±0.17 mm/a,平均增厚速率约为2.35±3.30 mm/a

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