背景噪声面波与布格重力异常联合反演:山西断陷带三维地壳结构

讨论了利用面波与布格重力异常联合反演三维地壳速度结构的新方法,并利用该方法联合反演获得山西断陷带地壳S波速度结构.通过建立速度与密度之间的经验关系,利用非线性迭代反演方法获得最终速度模型.结果显示,联合反演获得的速度模型可以同时提高对面波及重力数据的观测拟合程度,而面波单独反演得到的速度模型则无法很好的拟合重力观测数据.相比较,联合反演速度模型中的大同火山区中下地壳的低速异常幅值小于面波单独反演模型中低速异常体的幅值.联合反演速度模型结果揭示,吕梁山地区在中下地壳存在低速异常,并且和北部的大同火山区低速异常相连接,说明可能导致新生代以来大同火山区岩浆活动的上地幔构造活动(上地幔局部上涌,地幔柱)可能对山西断陷带的形成和构造活动起到了一定的控制作用,并且导致了吕梁山地区中下地壳的低速异常.

Three-dimensional crustal model of Shanxi graben from 3D joint inversion of ambient noise surface wave and Bouguer gravity anomalies

The main objective of this study is to obtain a model that can explain the surface wave data and Bouguer gravity anomaly simultaneously and also to alleviate the non-uniqueness of surface wave inversion. We applied a novel non-linear joint inversion technique using both surface wave and gravity anomalies to obtain high resolution 3D shear-wave velocity crustal model of Central North China Craton including Shanxi graben. The crustal model helps us to understand the crust and mantle dynamics and the evolution history of the Shanxi rift.#br#We bandpass filtered WGM2012 global Bouguer gravity anomaly data to remove the data with wavelength less than 50 km and greater than 200 km. We then projected the gravity data and surface wave data from ambient noise tomography to a Cartesian coordinate system with grid spacing 50 km×50 km. The joint inversion was performed in this coordinate system. The inversion volume is much larger than the target region. This parameterization strategy was chosen to minimize the likelihood edge effects from gravity modelling. We used Crust 2.0 global model as our initial model in the inversion. An approximate non-linear P velocity and density relationship is derived from combing Birch's law and Nafe-Drake's curve. For each iteration of inversion, the sensitivity kernel of surface wave and gravity data were recalculated and updated until the inversion converged. We did several experiments to obtain an optimized weighting parameter to balance the influences of both datasets. A surface-wave-only inversion was also performed to compare the results of joint inversion.#br#Both shear wave velocity models from joint inversion and surface-wave-only inversion can fit surface wave data well though only the joint inversion provides an acceptable fit to the gravity data. Gravity misfits decrease from >30 mGal to ~3.4 mGal after joint inversion. The velocity anomalies from both inversions all show a remarkable correlation with surface geology and upper crustal structures beneath Shanxi rift. The Lüliang mountain region and Datong volcanic region all show relatively high shear wave velocity in the upper crust. Meanwhile, the basins in the southern rift show slow velocities. The southern part of the Shanxi rift is slower than the northern part in the upper crust. The Cenozoic extension started from the northern rift and then passed on to the southern rift. However, in the mid-and-lower crust beneath the Datong volcanic region, the surface-wave-only inversion resolves much slower shear wave velocity compared to the joint inversion model. The most pronounced difference occurs in the mid-and-lower crust beneath the Lüliang mountain region. The joint inversion reveals a slow velocity anomaly with amplitude about 2%, while the surface-wave-only inversion model shows a fast velocity.#br#The Datong volcanic region, north part of the Shanxi rift, might have experienced mantle upwelling since the Cenozoic time. The hot and buoyant mantle heated the upper most mantle and the crust, which caused the large-scale mid and lower crust slow velocity and negative gravity anomaly in the Datong volcanic region. The slow velocity anomaly beneath the Lüliang mountain region is also related to the mantle upwelling beneath the Datong volcanic region. The Cenozoic mantle upwelling might control the formation and evolution of the Shanxi rift.