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Beijing China
Common-midpoint spatial autocorrelation analysis of seismic ambient noise obtained from a spatially unaliased sensor distribution
Correction of P / S Amplitude Ratios for Low‐Magnitude Seismic Events Based on Bayesian Kriging Method
The positioning of buried pipelines from magnetic data
The application of ambient noise and reflection seismic exploration in an urban active fault survey
Fault Attitude of the North Section of Huangzhuang-Gaoliying Fault at Beijing, China and its Effects on the Ground Rupture
Identification of interstratified mica and pyrophyllite monolayers within chlorite using advanced scanning/transmission electron microscopy
Comparison Between Different Apparent Resistivity Definitions of Csamt
Improving the Accuracy of near Real-Time Seismic Loss Estimation using Post-Earthquake Remote Sensing Images
Chemical lattice expansion of natural zircon during the magmatic-hydrothermal evolution of A-type granite
V S 30 Empirical Prediction Relationships Based on a New Soil‐Profile Database for the Beijing Plain Area, China
Tangent Line/Second-Order Bounded Mean Oscillation Waveform Analysis for Short TDR Probe
A transformation in the tectonic regime affected the continental crust of eastern China during the Middle–Late Jurassic period by changing tectonic trends from E-W to NE and then NNE. The Mesozoic Yanshan tectonic belt in northern China has a distinctive three-segment geometry. This includes a segment south and west of Beijing with a NE trend, a central E-W segment near and east of Beijing, and a NNE-trending segment farther to the east. Field investigations of Mesozoic thrust faults and folds, granitic intrusions and dikes, combined with zircon sensitive high-resolution ion microprobe (SHRIMP) and laser-ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) dating, constrain the age of the NE-SW–trending tectonic belts that occurred during ca. 170–150 Ma. Melting of the lower crust and crust-mantle interaction resulted in volcanic eruptions and granitic intrusions (ca. 165–155 Ma), and widespread NW-SE to NNW-SSE shortening and transpression in the Yanshan tectonic belt were associated with the movement of the upper part of intracontinental crust (ca. 170–150 Ma) upon a basal decollement located between crystalline basement and overlying rocks (layered crustal rotation). After this transformation, deformation, basin sedimentation, and magmatism occurred in NNE-trending tectonic belts that paralleled the eastern Asian continental margin. This tectonic transformation was temporally and spatially linked to the rapid formation of the Pacific plate at 180–160 Ma.