邓文彬,苏丹竞,高宇潇,许闯

• 1:新疆大学建筑工程学院测绘工程系
• 2:广东工业大学土木与交通工程学院测绘工程系
• 3:中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室
• 4:武汉大学测绘遥感信息工程国家重点实验室

摘要(Abstract)：

针对当前少有学者研究不同重力场模型对莫霍面地形反演的影响,该文利用Parker-Olderburg方法深入讨论纯GRACE重力场模型、纯GOCE重力场模型以及GRACE和GOCE混合重力场模型对青藏高原地区莫霍面反演的影响。实验结果表明,不同重力场模型所反演的莫霍面地形整体空间分布上比较一致,但也存在10 m量级的细微差异;该地区莫霍面地形分布呈顺时针旋转模式,可以较好反映主要构造结构的特点;最深的莫霍面约为70 km,远超过了其他地区正常地壳的厚度。

关键词(KeyWords)： 莫霍面;重力场;青藏高原;反演;地形

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(51868074,51368056,41974014);; 2016自治区高校科研计划项目(XJEDU2016I015);; 2016新疆大学博士科学基金项目(BS160250);; 大地测量与地球动力学国家重点实验室开发基金项目(SKLGED2018-1-3-E);; 武汉大学测绘遥感信息工程国家重点实验室开放基金资助项目(19P01)

作者(Author): 邓文彬,苏丹竞,高宇潇,许闯

DOI: 10.16251/j.cnki.1009-2307.2020.04.001

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