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| 断层模型在火山区形变和重力反演中的应用 | |
| 引用本文： | 施行觉,胡亚轩,毛竹,赵慈平,施发奇,邵德晟.断层模型在火山区形变和重力反演中的应用[J].大地测量与地球动力学,2004,24(3):24-28. |
| 作者姓名： | 施行觉 胡亚轩 毛竹 赵慈平 施发奇 邵德晟 |
| 作者单位： | 1. 中国科学技术大学地球和空间学院,合肥,200026 2. 中国科学技术大学地球和空间学院,合肥,200026中;国地震局第二监测中心,西安,710054 3. 云南省地震局,昆明,650041 |
| 基金项目： | 国家自然科学基金 (4 0 2 740 5 7)，地震科学联合基金(10 2 0 99) |
| 摘 要： | 利用腾冲火山区1998～2002年的垂直形变和重力测量资料，应用多元Mogi模型对测区的等效岩浆房位置及大小进行了反演计算，得出了最佳拟合值。但当对形变和重力资料联合分析时却发现：实测重力数据比用球形Mogi模型计算所得的值要大得多。为了对此进行合理的解释，提出了断层模型。当岩浆沿断层上升时，充填了断层中原先存在的大量空隙．因而可以只对重力产生影响．而不对形变产生影响。为此沿断层积分得出上升岩浆所产生的重力异常，其结果与实测重力资料拟合得较好。同时断层模型也对负的岩浆源(即岩浆的流失)作出了较为合理的解释。 |
| 关 键 词： | 断层模型 火山区 重力反演 重力测量 地表重力变化 |
| 文章编号： | 1671-5942(2004)03-0024-05 |
| 修稿时间： | 2004年4月4日 |
APPLICATION OF FAULT MODEL IN VERTICAL DEFORMATION AND GRAVITY ANALYSES IN TENGCHONG VOLCANIC AREA |
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| Shi Xingjue,Hu Yaxuan,Mao Zhu,Zhao Ciping,Shi Faqi and Shao Desheng College of Earth and Space,University of Science and Technology of China,Hefei\ Second Monitoring and Application Center,CEA,Xi'an\ Earthquake Administration of Yunnan Province,Kunming\.APPLICATION OF FAULT MODEL IN VERTICAL DEFORMATION AND GRAVITY ANALYSES IN TENGCHONG VOLCANIC AREA[J].Journal of Geodesy and Geodynamics,2004,24(3):24-28. | |
| Authors: | Shi Xingjue Hu Yaxuan Mao Zhu Zhao Ciping Shi Faqi and Shao Desheng College of Earth and Space University of Science and Technology of China Hefei\ Second Monitoring and Application Center CEA Xi'an\ Earthquake Administration of Yunnan Province Kunming\ |
| Institution: | Shi Xingjue1),Hu Yaxuan1,2Mao Zhu1),Zhao Ciping3),Shi Faqi3) and Shao Desheng3) 1) College of Earth and Space,University of Science and Technology of China,Hefei\ 200026 2) Second Monitoring and Application Center,CEA,Xi'an\ 710054 3) Earthquake Administration of Yunnan Province,Kunming\ 650041 |
| Abstract: | Based on four years(1998-2002) vertical deformation and gravity data,we inversed the equivalent magma's position and size with the Mogi model and got best result.However,when analyzing the measured deformation and gravity together,we found a much greater value measured gravity than that calculated by the Mogi model.In order to explain the reasons,we brought forward the fault model.If the magma ascends along the fault,it will fill the plenty of space in the fault and has only influence on the gravity but not on the deformation.The gravity abnormity calculated by the integration along the fault matches very well with the measured one.On the other hand,it explained more reasonable to the negative magma which flows out. |
| Keywords: | fault model Mogi model vertical deformation gravity variation volcanic area |
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