地球科学进展 ›› 2017, Vol. 32 ›› Issue (1): 75 -82. doi: 10.11867/j.issn.1001-8166.2017.01.0075

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最新全球重力数据库V23中陆域重力资料质量评估
张春灌 1( ), 袁炳强 1, 张国利 2   
  1. 1.西安石油大学 地球科学与工程学院, 陕西 西安 710065
    2.中国地质调查局 天津地质调查中心, 天津 300170
  • 收稿日期:2016-10-27 修回日期:2016-12-20 出版日期:2017-01-20
  • 基金资助:
    *中国地质调查局项目“新疆东部地质—地球物理资料综合研究”(编号:121201011000150012-01);西安石油大学项目“新疆东北部盆地基底构造属性及盆山构造关系研究”(编号:2016BS10)资助.

Quality Evaluation of Land Gravity Data in the Latest Global Gravity Database V23

Chunguan Zhang 1( ), Bingqiang Yuan 1, Guoli Zhang 2   

  1. 1.School of Earth Science and Engineering, Xi’an Shiyou University, Xi’an 710065, China;
    2.Tianjin Geological Survey Center, China Geological Survey, Tianjin 300170, China
  • Received:2016-10-27 Revised:2016-12-20 Online:2017-01-20 Published:2017-01-10
  • About author:

    First author:Zhang Chunguan (1981-), male, Yudu County, Jiangxi Province, Associate professor. Research areas include integrated geophysical exploration and tectonophysics. E-mail: chunguan-zhang@163.com

  • Supported by:
    Project supported by the China Geological Survey Project “Integrated study of the geological data and geophysical data in Eastern Xinjiang” (No. 121201011000150012-01);Xi’an Shiyou University Project “Tectonic attribute of basin basement and basin-mountain tectonic relation of the Northeastern Xinjiang” (No. 2016BS10).

为了评估最新全球重力数据库V23中陆域重力资料的质量问题,选择了美国、秘鲁、爱尔兰、南非、肯尼亚、澳大利亚、中国等7个国家的8个区块约133万km2的重力数据进行对比分析。基于V23中自由空间重力异常数据,利用纯球坐标系内重力校正方法获得了这些区块的计算布格重力异常。利用相关分析的方法对这些区块的实测布格重力异常和计算布格重力异常进行相关分析,得到了相应的相关系数。通过对实测布格重力异常和计算布格重力异常之间相关系数及差值特征的综合分析,评估了全球重力数据库V23中选取的8个区块重力数据的质量。研究结果表明,斯克里普斯海洋研究所发布的最新全球重力数据库V23中陆域重力资料融合了大量测量年代较早的地面重力数据或者航空重力数据,而近十几年新完成的地面重力资料或者航空重力资料可能未融合进该数据库。具有大量年代较早的地面或者航空重力测量资料的区域,该数据库中陆域重力资料的质量较高,而重力工作程度较低的区域,其资料的质量则较低。

In order to evaluate the quality of the land gravity data in the latest global gravity database V23, the authors chose the gravity data of eight blocks with a total area of 1 330 000 km2 to compare and analyze, and these blocks involved seven countries, including the United States, Peru, Ireland, South Africa, Kenya, Australia, and China. Based on the free-air gravity anomaly data of the latest global gravity database V23, the authors obtained the calculated Bouguer gravity anomaly using the gravity correction methods within the pure spherical coordinate system in these eight blocks. Then, the correlation coefficients between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly were calculated by the correlation analysis method in these eight blocks. Finally, through comprehensive analysis of the features of these correlation coefficients and differences between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly in these eight blocks, the quality of the gravity data of these eight blocks was evaluated in the latest global gravity database V23. The results showed that the latest global gravity database V23, released by Scripps Institution of Oceanography, integrated a large number of the ground or airborne gravity data measuring in an earlier era, and the newly surveyed ground or airborne gravity data may not be integrated into the database. The quality of land gravity data is relatively high in the areas with a large number of older ground or airborne gravity data, otherwise it is low in the zones with a lower gravity working degrees.

中图分类号: 

图1 数据对比区块分布图
Fig.1 The block distribution map for data comparison
图2 南半球区块数据对比图
(a)澳大利亚区块;(b)南非区块;(c)秘鲁区块;(d)肯尼亚区块;1.实测布格重力异常;2.计算布格重力异常;3.实测布格重力异常与计算布格重力异常的差值;4.实测布格重力异常与计算布格重力异常的相关系数;c4中黑色十字点为重力路线测点;d4中黑色十字点为2008年重力测点、红色圆点为早期重力路线测点
Fig.2 The data comparison map in the Southern Hemisphere
(a)Australia block;(b)South Africa block;(c)Peru block;(d)Kenya block; 1.Measured Bouguer gravity anomaly; 2.Calculated Bouguer gravity anomaly; 3.The difference between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly; 4.The correlation coefficient between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly; The black cross points are the points of gravity lines in c4; The black cross points are the gravity points in 2008 and the red dots are the points of early gravity lines in d4
图3 北半球区块数据对比图
(a)爱尔兰区块;(b)美国区块;(c)渭河区块;(d)青藏区块;1.实测布格重力异常;2.计算布格重力异常;3.实测布格重力异常与计算布格重力异常的差值;4.实测布格重力异常与计算布格重力异常的相关系数
Fig.3 The data comparison map in the Northern Hemisphere
(a)Ireland block;(b)America block;(c)Weihe block;(d)Qinghai Tibet block; 1.Measured Bouguer gravity anomaly; 2.Calculated Bouguer gravity anomaly; 3.The difference between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly; 4.The correlation coefficient between the measured Bouguer gravity anomaly and the calculated Bouguer gravity anomaly
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