首页 | 本学科首页   官方微博 | 高级检索  
     检索      

基于重力大数据的中国大陆区域地质构造解析
引用本文:葛,粲李修钰李晓晖李加好,李永东袁,峰.基于重力大数据的中国大陆区域地质构造解析[J].地质科学,2017,0(3):714-726.
作者姓名:  粲李修钰李晓晖李加好  李永东袁  
作者单位:合肥工业大学资源与环境工程学院 合肥 230009;; 合肥工业大学矿集区立体探测实验室 合肥 230009;; 合肥工业大学安徽省矿产资源与矿山环境工程技术研究中心 合肥 230009;; 安徽省地质调查院 合肥 230001;; 中国地质大学地球物理与空间信息学院 武汉 430074
摘    要:本文从重力异常角度对中国大陆区域地质构造的深部结构进行了研究。基于卫星重力大数据,利用改进后的位场分离方法获取了从地表到上地幔顶部不同深度的重力异常场。分析了各个碰撞-俯冲带、造山带及盆地等地区上地幔顶部(参考深度约为72~76 km)和中地壳(参考深度约为12~16 km)深度的异常特征。结合地质构造、地球化学和地球物理学证据,重点讨论了重力异常产生的原因及其与中国大陆主要构造之间的关系,获得了中国大陆在环太平洋动力学体系和特提斯动力学体系这两大动力作用下不同地区差异性的壳幔响应。

关 键 词:插值切割法  中国大陆  重力异常  区域地质构造分析  大数据处理
收稿时间:2017-03-27
修稿时间:2017-03-27;

Analysis of regional geological structure in China basedon gravity big data
Ge CanLi Xiuyu Li XiaohuiLi JiahaoLi YongdongYuan Feng.Analysis of regional geological structure in China basedon gravity big data[J].Chinese Journal of Geology,2017,0(3):714-726.
Authors:Ge CanLi Xiuyu Li XiaohuiLi JiahaoLi YongdongYuan Feng
Institution:School of Resource and Environmental Engineer, Hefei University of Technology, Hefei  230009;Laboratory of Three-Dimension Exploration for Mineral District, Hefei University of Technology, Hefei  230009;Anhui Province Engineering Research Center for Mineral Resources and Mine Environments, Hefei University of Technology, Hefei  230009;Geological Survey of Anhui Province, Hefei  230001;Institute of Geophysics and Geomatics, China University of Geoscience, Wuhan  430074
Abstract:This paper studies the regional geological deep structure of mainland China from the perspective of gravity anomaly. Based on the satellite gravity big data, the improved field separation method is utilized to obtain the anomalous field of different depths from the surface to the top of the upper mantle. Anomaly features of the middle crustal depths(reference depth about 12~16 km)and the upper mantle(reference depth about 72~76 km)are discussed in each collision-subduction zones, orogenic belts and basins. Combined with geological structure,geochemistry and geophysical evidences, the causes of gravity anomalies and its relationship with the main geological structure of mainland China have been analyzed and discussed.Diverse crust-mantle responses in different regions of the Chinese mainland, under the two major driving forces of the central Pacific dynamic system and the Tethys dynamical system,were obtained.
Keywords:Interpolation-cut method  Mainland China  Gravity anomaly  Analysis of regional geological structure  Big data processing
点击此处可从《地质科学》浏览原始摘要信息
点击此处可从《地质科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号