Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/7223
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorWu, J-
dc.creatorDeng, K-
dc.creatorChen, YQ-
dc.date.accessioned2015-11-10T08:32:47Z-
dc.date.available2015-11-10T08:32:47Z-
dc.identifier.issn1000-050X-
dc.identifier.urihttp://hdl.handle.net/10397/7223-
dc.language.isozhen_US
dc.publisher武汉大学期刋社en_US
dc.rights© 2003 中国学术期刊电子杂志出版社。本内容的使用仅限于教育、科研之目的。en_US
dc.rights© 2003 China Academic Journal Electronic Publishing House. It is to be used strictly for educational and research use.en_US
dc.subjectDeformation surveyingen_US
dc.subjectNegative dislocationen_US
dc.subjectTectonic movementen_US
dc.subjectGPSen_US
dc.title板块内部层状负位错模型及其反演en_US
dc.typeJournal/Magazine Articleen_US
dc.description.otherinformationAuthor name used in this publication: 伍吉仓en_US
dc.description.otherinformationAuthor name used in this publication: 邓康伟en_US
dc.description.otherinformationAuthor name used in this publication: 陈永奇, CHEN Yongqien_US
dc.description.otherinformationTitle in Traditional Chinese: 板塊內部層狀負位錯模型及其反演en_US
dc.description.otherinformationJournal title in Traditional Chinese: 武漢大學學報 (信息科學版)en_US
dc.identifier.spage671-
dc.identifier.epage674-
dc.identifier.volume28-
dc.identifier.issue6-
dcterms.abstract提出了一种层状负位错模型 ,用于描述下层地壳拖带上层地壳的耦合作用所造成的上伏地壳变形 ,并通过模拟计算 ,给出了这种层状耦合模型的形变场特征 ,以及利用模拟形变数据反演层状负位错模型参数的结果-
dcterms.abstractA horizontal negative dislocation layer is proposed to represent the mechanism of the intraplate crustal deformation. A simulated example is designed to show the crustal deformation pattern of a horizontal negative dislocation layer model and inverse the simulated displacements to determine the model parameters. Because of the heterogeneous geological structures and rock properties of the overlying crust, the coupling between the lower crustal movements and the overlying upper crust is not homogeneous, and the shear deformation zone will occurr along the boundary of the different negative dislocation areas. On the other hand, the observed deformation data such as displacements can be used to determine the layer negative dislocation distributions inversely, so as to divide the monitoring area into different tectonic blocks and to analyze the earthquake risks.-
dcterms.accessRightsopen accessen_US
dcterms.alternativeNegative Dislocation Layer for Intraplate Tectonic Movements and Inversion-
dcterms.bibliographicCitation武汉大学学报. 信息科学版 (Geomatics and information science of Wuhan University), Dec. 2003, v. 28, no. 6, p. 671-674-
dcterms.isPartOf武汉大学学报. 信息科学版 (Geomatics and information science of Wuhan University)-
dcterms.issued2003-
dc.identifier.eissn1671-8860-
dc.identifier.rosgroupidr16960-
dc.description.ros2003-2004 > Academic research: refereed > Publication in refereed journal-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_IR/PIRAen_US
dc.description.pubStatusPublisheden_US
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