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由地面、卫星重力资料研究岩石层密度
引用本文:张赤军,操华胜,罗少聪. 由地面、卫星重力资料研究岩石层密度[J]. 地球物理学报, 1988, 31(6): 664-671
作者姓名:张赤军  操华胜  罗少聪
作者单位:中国科学院测量与地球物理研究所 武汉
摘    要:地球内部物质密度的分布决定了地球表面及外空的重力场,不过在特定的条件下,也可以根据地面或外空的重力场推求地球内部异常密度的分布。本文在单层位理论的基础上,利用上述资料确定了我国大陆下面地球深部的异常密度,试用分离重力场长、短波长的方法,求出了地球外层-岩石层内异常密度的侧向分布,对此,还初步作了地球物理的解释,其结果与地震测深的较为一致。

关 键 词:重力异常  大地水准面  岩石层  异常密度  
收稿时间:1986-11-18

INVESTIGATION OF ANOMALY DENSITY IN LITHO-SPHERE BY USING THE GROUND GRAVITY DATA AND SATELLITE OBSERVATIONS
ZHANG CHI-JUN CAO HUA-SHENG LUO SHAO-CONG. INVESTIGATION OF ANOMALY DENSITY IN LITHO-SPHERE BY USING THE GROUND GRAVITY DATA AND SATELLITE OBSERVATIONS[J]. Chinese Journal of Geophysics, 1988, 31(6): 664-671
Authors:ZHANG CHI-JUN CAO HUA-SHENG LUO SHAO-CONG
Affiliation:Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan
Abstract:The gravity field of the earth's surface and outer space depends on the interior mass density distribution of the earth. But under specified conditions the interior anomaly density distribution of the earth can also be derived according to the ground and outer space gravity field. In this paper, on the basis of the single layer potential theory the earth's depth anomaly density under continent in China is determined by utilizing the above mentioned data, mainly, the lateral distribution of anomaly density within the earth outer layer--lithosphere, is calculatedusing the method of long and short wave-lengths. In addition, the preliminary geophysical interpretation for this problle mis made. Its results are the same as seismological depth-measurement.
Keywords:Gravity anomaly   Geoid   Lithosphere   Anomaly density.
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