Titlebook: Natural Language Processing and Chinese Computing; 7th CCF Internationa Min Zhang,Vincent Ng,Hongying Zan Conference proceedings 2018 Sprin

Hallucination

書目名稱Natural Language Processing and Chinese Computing影響因子(影響力)




書目名稱Natural Language Processing and Chinese Computing影響因子(影響力)學(xué)科排名




書目名稱Natural Language Processing and Chinese Computing網(wǎng)絡(luò)公開度




書目名稱Natural Language Processing and Chinese Computing網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Natural Language Processing and Chinese Computing被引頻次




書目名稱Natural Language Processing and Chinese Computing被引頻次學(xué)科排名




書目名稱Natural Language Processing and Chinese Computing年度引用




書目名稱Natural Language Processing and Chinese Computing年度引用學(xué)科排名




書目名稱Natural Language Processing and Chinese Computing讀者反饋




書目名稱Natural Language Processing and Chinese Computing讀者反饋學(xué)科排名

MEET

homeostasis

Chuanqi Tan,Furu Wei,Qingyu Zhou,Nan Yang,Weifeng Lv,Ming Zhou

otic-capsule

Visual-Acuity

Fan Yang,Jianhu Zhang,Gongshen Liu,Jie Zhou,Cheng Zhou,Huanrong Sun

ANTIC

al weakness to another. This minimizes the energy needed for break-up of the continents. Harmonization of local variations of spreading ridge orientation with the overall regional extension thus determines the original rift geometry. Such a control of old continental lineaments over the segmentation

Cloudburst

象形文字

Yang Li,Qingliang Miao,Ji Geng,Christoph Alt,Robert Schwarzenberg,Leonhard Hennig,Changjian Hu,Feiyusolidation of thick slurries involves the presence of forces not taken into account by the kinematical model. Careful observations of batch settling of flocculated suspensions have shown that two distinguishable zones appear in the settling column separated by a discontinuity. The upper zone, lastin

BOON

Hao Wang,Xiaodong Zhang,Houfeng Wangsediments are negatively skewed and finer sediments are positively skewed. In monsoon,?>60% of the sediments is platykurtic or leptokurtic in nature which indicates the high energy environment in this season. Proportion of sand, silt and clay in sediments ranges between 38–91%, 4–61% and 1–41% respe

鍵琴

rs 1973 and 2016. . and . of sedimentation in the lower reach are explained and understood with the detailed study of channel forms and patterns, stream hydraulics, tidal character, sediment load, sediment grain size and related critical and available shear stress and identification of the environme