Seven students of Jian'an (建安七子), additionally translated because the "seven philosophers of Jian'an", or the "seven masters of Jian'an", consists of 7 chinese language intellectuals of the japanese Han interval. The identify used to be coined by means of Cao Pi. "Jian'an" refers back to the 196—220 interval through the rulership of the Emperor Xian of Han. often called the time of unrest previous the 3 Kingdoms period, the interval won reputation within the East Asian culture.
The seven students are Wang Can, Chen Lin, Ruan Yu (阮瑀), Liu Zhen (劉楨), Xu Gan, Ying Chang (應瑒), and Kong Rong.
Ruan Yu was once the daddy of Ruan Ji, one of many Seven Sages of the Bamboo Grove.
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Additional resources for Collection of Seven Scholars of Jian'an (Chinese classical literature series) (中国古典文学基本丛书:建安七子集)
B) More detailed maps of the Red River fault and its relation to the rock units of the northeastern part of the Lanping-Simao unit in the Ailao Shan (lower left) and faults of the southeastern part of the Red River fault and adjacent Cenozoic rocks. Inset map in upper right shows location to regional structures (XX = Xianshuihe fault; RR = Red River fault) . Xianshuihe-Xiaojiang, Red River, and Dali fault systems, China west– to north-trending axes and cut by thrust faults with similar trend. The active Chenghai fault forms the northwestern boundary of the Chuxiong basin (Fig.
L993, l995), but the mylonitic rocks in the Xuelong Shan have not been dated. The Mesozoic rocks of the LanpingSimao belt narrow and pinch out northward against Triassic volcanic rocks along the Tongdian fault. Mesozoic rocks of the Lanping-Simao belt were folded in Eocene, Oligocene, and postOligocene time. Folds trend north to northwest and form arcuate patterns, whereas the belt of metamorphic rocks in the Ailao Shan, Diancang Shan, and Xuelong Shan form a linear belt. Folds of the Lanping-Siamo fold belt generally strike obliquely, with a more northerly strike, into the metamorphic rocks.
At the map scale, the right-slip Qujiang and Jian- shui faults appear to be left-laterally bent, but whether that shear is being taken up on numerous small faults with small displacements or low slip rate is unknown. There are discrete faults that we have not included in the specific faults discussed as part of the Xianshuihe-Xiaojiang system because their displacement is small. For example, a fault with small, but measurable, displacement lying west of the Songming basin forms a boundary of the north-trending Heilongtan basin filled with Quaternary sediments (Fig.