Upper mantle convection driving by density anomaly and a test model
A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model t...
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Published in | Acta seismologica sinica Vol. 18; no. 1; pp. 27 - 33 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Beijing
Springer Nature B.V
2005
School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China |
Subjects | |
Online Access | Get full text |
ISSN | 1674-4519 1000-9116 1867-8777 1993-1344 |
DOI | 10.1007/s11589-005-0003-2 |
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Abstract | A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model takes the density anomalies as the driving force for the mantle convection. We solve the basic equations with different boundary conditions in a domination of wave number by using the FFT arithmetic. In order to test the validity of our theory and method two simple models (higher-lower density body and break off slab) are employed to calculate their flow patters in this paper. Results show that our method can be directly used to investigate the upper mantle convection patterns and its related problems of lithospheric dynamics.[PUBLICATION ABSTRACT] |
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AbstractList | A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model takes the density anomalies as the driving force for the mantle convection. We solve the basic equations with different boundary conditions in a domination of wave number by using the FFT arithmetic. In order to test the validity of our theory and method two simple models (higher-lower density body and break off slab) are employed to calculate their flow patters in this paper. Results show that our method can be directly used to investigate the upper mantle convection patterns and its related problems of lithospheric dynamics. A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model takes the density anomalies as the driving force for the mantle convection. We solve the basic equations with different boundary conditions in a domination of wave number by using the FFT arithmetic. In order to test the validity of our theory and method two simple models (higher-lower density body and break off slab) are employed to calculate their flow patters in this paper. Results show that our method can be directly used to investigate the upper mantle convection patterns and its related problems of lithospheric dynamics.[PUBLICATION ABSTRACT] P315.1; A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model takes the density anomalies as the driving force for the mantle convection. We solve the basic equations with different boundary conditions in a domination of wave number by using the FFT arithmetic. In order to test the validity of our theory and method two simple models (higher-lower density body and break off slab) are employed to calculate their flow patters in this paper. Results show that our method can be directly used to investigate the upper mantle convection patterns and its related problems of lithospheric dynamics. A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. It is assumed that the density anomalies, which are mapped from the seismic tomography data, are responding to the temperature perturbation in the connective system. This model takes the density anomalies as the driving force for the mantle convection. We solve the basic equations with different boundary conditions in a domination of wave number by using the FFT arithmetic. In order to test the validity of our theory and method two simple models (higher-lower density body and break-off slab) are employed to calculate their flow patterns in this paper. Results show that our method can be directly used to investigate the upper mantle convection patterns and its related problems of lithospheric dynamics. |
Author | 傅容珊 王景赟 常筱华 黄建华 戴志阳 查显杰 |
AuthorAffiliation | School of Earth and Space Science University of Science and Technology of China University of Science and Technology of China Hefei 230026 China Hefei 230026 China |
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Cites_doi | 10.1029/GM077p0137 10.1029/RG006i004p00491 10.1016/0012-821X(91)90033-E 10.1016/S0012-821X(00)00081-9 10.1016/S0040-1951(97)00169-8 10.1029/93GL00988 10.1029/GM070p0091 |
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Snippet | A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the density... A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. It is assumed that the density... P315.1; A mathematic-physical convection model in upper mantle is established in this paper. This model is in a three dimensional frame. Assume that the... |
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SubjectTerms | Anomalies Boundary conditions Convection Convection modes Density Driving dynamics Mantle Mathematical models Plate tectonics seismic Seismic engineering Seismic phenomena tomography Upper mantle |
Title | Upper mantle convection driving by density anomaly and a test model |
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