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Synthetic tomography of plume clusters and thermochemical piles

机译:羽簇和热化学桩的合成层析成像

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摘要

Seismic tomography elucidates broad, low shear-wave velocity structures in the lower mantle beneath Africa and the central Pacific with uncertain physical and compositional origins. One hypothesis suggests that these anomalies are caused by relatively hot and intrinsically dense material that has been swept into large thermochemical piles by mantle flow. An alternative hypothesis suggests that they are instead poorly imaged clusters of narrow thermal plumes. Geodynamical calculations predict fundamentally different characters of the temperature fields of plume clusters and thermochemical piles. However the heterogeneous resolution of tomographic models makes direct comparison between geodynamical temperature fields and tomographic shear-wave anomalies tenuous at best. Here, we compute synthetic tomographic images for 3D spherical mantle convection models and evaluate how well thermal plumes and thermochemical piles can be reconciled with actual seismic tomography images. Geodynamical temperature fields are converted to shear-wave velocity using experimental and theoretical mineral physics constraints. The resultant shear-wave velocity fields are subsequently convolved with the resolution operator from seismic model S20RTS to mimic the damping and distortion associated with heterogeneous seismic sampling of the mantle. We demonstrate that plume clusters are tomographically blurred into two broad, antipodal velocity anomalies in agreement with S20RTS and other global seismic models. Large, thermochemical piles are weakly distorted by the tomographic filter. The power spectrum of velocity heterogeneity peaks at spherical harmonic degree 3, unlike the degree-2 maximum in S20RTS, but decays rapidly similar to S20RTS and many other seismic models. Predicted tomography from thermochemical pile and plume cluster models correlate equally well with S20RTS given the uncertainties in the numerical modeling parameters. However, thermochemical piles match tomography better in visual comparison and in the overall character of the harmonic spectrum.
机译:地震层析成像技术阐明了非洲和太平洋中部以下地幔的宽低切变波速度结构,其物理和成分起源均不确定。一种假设表明,这些异常现象是由相对热和本质上密集的物质引起的,该物质已被地幔流扫入大的热化学堆中。另一个假设表明,它们是成像较差的狭窄热羽簇。地球动力学计算预测的是羽状团簇和热化学桩温度场的根本不同特征。但是,层析成像模型的异质分辨率最多可以直接比较地球动力学温度场和层析成像的剪切波异常。在这里,我们为3D球形地幔对流模型计算了层析层析成像图像,并评估了热羽和热化学堆与实际的层析层析成像图像之间的协调程度。利用实验和理论上的矿物物理约束将地球动力学温度场转换为剪切波速度。随后将所得的剪切波速度场与来自地震模型S20RTS的分辨率算符进行卷积,以模拟与地幔非均匀地震采样相关的阻尼和变形。我们证明,与S20RTS和其他全球地震模型相一致,羽状团在层析上被模糊化为两个广泛的对映速度异常。大型X射线断层过滤器会严重扭曲热化学堆。速度异质性的功率谱在球形谐波度3处达到峰值,这与S20RTS中的2度最大值不同,但与S20RTS和许多其他地震模型相似,其衰减迅速。考虑到数值建模参数的不确定性,根据热化学堆和羽状团簇模型预测的层析成像与S20RTS的相关性相同。但是,在视觉比较和谐波频谱的总体特征方面,热化学堆与层析成像的匹配更好。

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