Late Mesozoic Paleotectonic Stress Fields Inferred from Fault-slip Data in Central and Western Yanshan Orogenic Belt: Implications for Destructive Geodynamics of North China Craton

doi:10.19657/j.geoscience.1000-8527.2019.05.01

Abstract

Abstract:

A dataset of 2,321 fault-slip data were collected from 116 sites in Late Mesozoic plutons in the central and western Yanshan orogenic belt. Paleostress field inversion was carried out via Tensor from these data. A five-generation sequence of paleostress fields has been established from the inversion results combined with regional tectonic deformation analysis. We found that: (1) Latest Jurassic-Earliest Cretaceous (148-127 Ma) compression with N-S-trending maximum principle stress (σ₁) (D₁); (2) Early Cretaceous (143-127 Ma) compression with NW-trending σ₁ (D₂); (3) Multidirectional extension with a nearly vertical σ₁ (D₃, ~120-110 Ma); (4) Compression with NE-trending σ₁ (D₄), and (5) Compression with E-trending σ₁ (D₅). D₁ and D₂ are interpreted as the far-field effects correlated with the closing of Mongol-Okhotsk Ocean and west-dipping subduction of paleo-Pacific plate, respectively. These two tectonic systems have major impact on the deformation of the Yanshan orogenic belt. D₃ may have reflected the vertical compression derived from deep mantle activity. Tectonic events unambiguously related to D₄ and D₅ have not been reported so far, which implies relatively weak paleostress field, and their geodynamic setting remains unclear. We suggest that a model of multidirectional extension induced from vertical compression may be applicable to the peak destruction of the North China Craton, instead of a passive rifting model dominated by subduction roll-back of the paleo-Pacific plate as previously proposed.

Key words: fault-slip datum, paleostress field, Late Mesozoic, destruction of North China Craton, Yanshan orogenic belt

CLC Number:

P548
P55

GAO Jianweng, LIN Yi, ZHANG Changhou, DING Zhaoyue, HOU Liyu, HUANG Yingzhu. Late Mesozoic Paleotectonic Stress Fields Inferred from Fault-slip Data in Central and Western Yanshan Orogenic Belt: Implications for Destructive Geodynamics of North China Craton[J]. Geoscience, 2019, 33(05): 919-936.

Figures/Tables 13

Fig.1 Geologic map of Changping-Huairou-Miyun area, north of Beijing and western Luanping, Hebei Province (modified from Ref.[47])

Fig.2 Stratigraphic and structural framework of the study area xν σ 2 2 .中元古代新地斜长岩; lξ o 2 2 .中元古代兰营石英正长岩;xν4.晚古生代下窝铺变质辉长岩; gγ δ 5 2 .官山花岗闪长岩; ch δ 5 2 .长园闪长岩; shγ δ 5 2 .水峪花岗岩; xγ δ 5 3 .西后峪花岗岩; y γ 5 3 .蒙山花岗岩; hη γ 5 3 .黄花甸子二长花岗岩; f γ 5 3 .冯家峪—西白莲峪花岗闪长质复式岩体; xη ν 5 3 .薛家石梁二长辉长岩; h η 5 3 .黑山寨二长岩; h ξ 5 3 .湖门正长岩; h γ 5 3 .黑山陀花岗岩

Fig.3 Photos of striations and kinematic markers

Fig.4 Fisher distribution of maximum (σ1) and minimum (σ3) principal stress

Fig.5 Chronological matrix analysis of paleostress fields

Fig.6 Distributions of N-S compressional stress tensors

Fig.7 Distributions of NW-SE compressional stress tensors

Fig.8 Distributions of NW-SE extensional stress tensors

Fig.9 Distributions of NE-SW extensional stress tensors

Fig.10 Distributions of N-S extensional stress tensors

Fig.11 Distributions of E-W extensional stress tensors

Fig.12 Distributions of NE-SW compressional stress tensors

Fig.13 Distributions of E-W compressional stress tensors

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