| Spatial and temporal variation of gravity field in the capital region |
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| 引用本文： | 华昌才,果勇,刘瑞法,肖钢. Spatial and temporal variation of gravity field in the capital region[J]. 地震学报(英文版), 1995, 8(3): 427-433. DOI: 10.1007/BF02650571 |
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| 作者姓名： | 华昌才 果勇 刘瑞法 肖钢 |
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| 作者单位： | Chang-Cai HUA; Yong GUO;Duan-Fa LIU; Gang XIAO;，J.T.KUO;and Walter BROWN(Institute of Geophysics，State Seismological Bureau，Beijing 100081，China)(Columbia University，U. S. A.) |
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| 摘 要： | Ｓｐａｔｉａｌａｎｄｔｅｍｐｏｒａｌｖａｒｉａｔｉｏｎｏｆ ｇｒａｖｉｔｙ ｆｉｅｌｄｉｎｔｈｅｃａｐｉｔａｌｒｅｇｉｏｎＣｈａｎｇ－ＣａｉＨＵＡ；（华昌才）ＹｏｎｇＧＵＯ；（果勇）Ｄｕａｎ－ＦａＬＩＵ；（刘瑞法）ＧａｎｇＸＩＡＯ；（肖钢），Ｊ．Ｔ．...
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| 收稿时间： | 1994-02-17 |
| 修稿时间： | 1994-09-22 |
Spatial and temporal variation of gravity field in the capital region |
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| Chang-Cai HUA, Yong GUO,Duan-Fa LIU, Gang XIAO,,J.T.KUO,and Walter BROWN. Spatial and temporal variation of gravity field in the capital region[J]. Acta Seismologica Sinica(English Edition), 1995, 8(3): 427-433. DOI: 10.1007/BF02650571 |
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| Authors: | Chang-Cai HUA Yong GUO Duan-Fa LIU Gang XIAO J.T.KUO and Walter BROWN |
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| Affiliation: | (1) Institute of Geophysics, State Seismological Bureau, 100081 Beijing, China;(2) Columbia University, U. S. A. |
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| Abstract: | The high accurate gravity measurement have been carried out many years in the capital region. The main characteristics of the change of gravity field during the latest eight years (1981 - 1988) in the region are presented inthis paper. The more gravitational variation appeared in the southern and south-eastern part, the maximum variation come to 10-6 ms-2. In the northern part, for instance: Chengde City, and Wan-clan County - westTaihang mountain area which are in the westside of the network, were relative stable. The noticeable areas ofgravitational variation were in Tianjin-Baxian-Renqiu which correspon d with the crustal vertical deformation.The main cause of that is related to pump ground water and petroleum. |
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| Keywords: | vertical deformation ground water gravity variation |
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