%0 Journal Article
%T Geophysical characteristics of Daxinganling gravitational gradient zone in the East China and its geodynamic mechanism<br>中国东部大兴安岭重力梯级带域地球物理场特征及其成因
%A YANG Bao-Jun
%A LIU Wan-Song
%A WANG Xi-Chen
%A LI Qin-Xue WANG Jian-Min
%A ZHAO Xue-Ping
%A LI Rui-Lei
%A <br>杨宝俊
%A 刘万崧
%A 王喜臣
%A 李勤学
%A 王建民
%A 赵雪平
%A 李瑞磊
%J 地球物理学报
%D 2005
%I 
%X Integrating geophysical data 7 Geoscience transects (GGT), we make the study on the geophysical characteristics model of crust and mantle along the Daxinganling gravitational gradient belt. We analyses 3 kinds of factors to generate the above-mentioned geophysical characteristics, such as the mantle current movement, the mantle thermal plume and the three plates movement surrounding around the continental margin. The forward and fitting results of gravity anomaly along Daxinganling gravitational gradient belt demonstrate the combination of the Earth material density variation in the crust and upper mantle and the Moho interface fluctuation leading to the gravity anomaly of the belt. The stress fields crossed at the continental margin in the East Asia and formed a series along the geophysical characteristics of the gravitational gradient zone. At last, we study the origin of the gravitational gradient zone along Daxinganling Mountain-Taihang Mountain-Wuling Mountain, and present the triple-junction model with dynamic force of compression stress and the upwelling action.
%K Daxinganling Mountain-Taihang Mountain-Wuling Mountain
%K Gravitational gradient zone
%K Continental margin zone in the East Asia
%K Plate motion
%K Triple-junction model<br>大兴安岭—太行山—武陵山
%K 重力梯级带
%K 东亚大陆边缘地带
%K 板块运动
%K 三结点模型
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=1E44AE713D8A6DE0&jid=14DC41C59CBF6770055A7D610D53AE46&aid=8DD5D6621CD7EB40&yid=2DD7160C83D0ACED&vid=B6DA1AC076E37400&iid=CA4FD0336C81A37A&sid=7AA74D31F1FF2DCE&eid=C3BF5C58156BEDF0&journal_id=0001-5733&journal_name=地球物理学报&referenced_num=13&reference_num=71