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 inActa seismologica sinica Vol. 18; no. 1; pp. 27 - 33
Main Author 傅容珊 王景赟 常筱华 黄建华 戴志阳 查显杰
Format Journal Article
LanguageEnglish
Published Beijing Springer Nature B.V 2005
School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China
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ISSN1674-4519
1000-9116
1867-8777
1993-1344
DOI10.1007/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]
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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FU Rong-shan WANG Jing-yun CHANG Xiao-hua HUANG Jian-hua DAI Zhi-yang ZHA Xian-jie School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China
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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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