7 Result(s)
within
Chapter
**ao-Liang **e
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Chapter and Conference Paper
Visual-Based Anomaly Detection for BGP Origin AS Change (OASC) Events
To complement machine intelligence in anomaly event analysis and correlation, in this paper, we investigate the possibility of a human-interactive visual-based anomaly detection system for faults and security ...
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Chapter and Conference Paper
A Delay Sensitive Feedback Control Data Aggregation Approach in Wireless Sensor Network
In wireless sensor networks (WSN) real-time data delivery is a challenging issue, especially when bursty events happen and many emergent packets appear. The cluster-based data aggregation has emerged as a basi...
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Chapter and Conference Paper
Max-Margin Dictionary Learning for Multiclass Image Categorization
Visual dictionary learning and base (binary) classifier training are two basic problems for the recently most popular image categorization framework, which is based on the bag-of-visual-terms (BOV) models and ...
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Chapter and Conference Paper
Selecting Optimal Orientations of Gabor Wavelet Filters for Facial Image Analysis
Gabor wavelet-based methods have been widely used to extract representative features for face analysis. However, the existing methods usually suffer from high computational complexity of Gabor wavelet transfor...
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Chapter and Conference Paper
Blind Image Deblurring with Modified Richardson-Lucy Deconvolution for Ringing Artifact Suppression
In this paper, we develop a unified image deblurring framework that consists of both blur kernel estimation and non-blind image deconvolution. For blind kernel estimation, we propose a patch selection procedur...
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Chapter
Examples—Taking the Ordovician Wufeng Formation-Silurian Longmaxi Formation in Southern Sichuan and Its Periphery as an Example
Taking the Ordovician Wufeng Formation-Silurian Longmaxi Formation as an example of shale gas development in the Southern Sichuan Basin and its periphery. According to the guiding of “Lithofacies paleogeograph...
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Chapter
Hirnantian Glaciation
The major ice caps in the late Ordovician lay between the base of the N. extraordinarius biozone and lower part of the N. persculptus biozone, consistent with the low values of CIA, CIW and PIA for the Huadi No. ...
