This paper gives a brief report on the new occurrence of the Early CambrianQiongzhusi' an Chengjiang fauna in the Haikou area, Kunming and its assemblage feature andthe stratigraphic section of the horizon yielding these fossils. Eight genera and 8 species ofTrilobitoidea are described here, embracing Leanchoilia asiatica Luo et Hu (sp. nov.), Yohoiasinensis Luo et Hu (sp. nov.), Zhongxinia speciosa Luo et Hu (gen. et sp. nov.), Xandarellaspectuculum Hou et al., Dianchia mirabilis Luo et Hu (gen. et sp. nov.), Kuamaia lata Hou,Retifacies longispinus Luo et Hu (sp. nov.) and Sinoburius lunaris Hou et al. 相似文献
Caving-induced fault reactivation and its effects on caving process are widely recognized as serious safety issues in mining and tunnelling industry. In this study, the effects of a variety of factors (i.e. friction coefficient, stick–slip instability, geological structure, pre-mining status, mining and its induced effects) that might exert an influence on fault dynamic behaviour of a 5-seam coal mine are investigated using practical mine-wide finite element numerical models with a normal fault. Based on the research outcomes on R-minimum-based finite element modelling of earthquake dynamics, the node-to-point contact strategy and the nonlinear friction contact law have been used here to simulate and analyse the caving-induced stick–slip frictional instability along the fault and related effects. The simulation results show that: (1) stress distribution before mining is relatively uniform around the fault for a homogenous rock material case, while stress concentration appears around the fault for the model with contrasting rock material properties; (2) the multiple-layered models are in favour of fault reactivation than models with only one material for whole strata; (3) the fault reactivation scale (i.e. dynamic relative motion and fault slip) induced by caving activity is significantly affected by rock mass strength, caving depth and its relative position to the fault. As caving progresses deeper and closer to the fault, the fault reactivation scale increases. Meanwhile, the fault in low strength strata is much more sensitive to fault slip behaviour; (4) seismic source parameters, namely seismic moment and moment magnitude, are adopted to evaluate the magnitude of caving-induced seismicity based on numerical results and fault slip risk and magnitude increase as fault reactivation scale expands; (5) during the caving stage, the failure zone initiates, develops and eventually connects the reactivated fault to the working area, presenting asymmetric failure pattern around the caving zone. The failure zone is obviously larger for the side closer to the fault than the other side due to caving-induced fault reactivation effects. This could help in better understanding fault reactivation and rock failure behaviours towards an optimised design of caving in a faulted region.
