2篇
您的检索式：作者名="ChenWenbin"
|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | High—Speed Clock Tree Simulation with Fast Wavelet Collocation Method显示文摘In this paper, we propose a fast wavelet collocation algorithm for high-speed clock tree simulation.Taking advantage of the specific structure of clock trees and the superior computational property of wavelets, the proposed algorithm presents the following merits: (1) It can perform both transient simulation and steady-state analysis with arbitrary input; (2) It employs nonlinear buffer model and nonuniform interconnect wire model; (3)It has a low computational complexity O(N) and can deal with considerably large circuits; (4) The Fast Wavelet Col-location Method works in time domain so that the simula-tion error in time domain can be well-controlled. Numer-ical experimental results demonstrate the promising fea-tures of the proposed algorithm in high-speed clock tree simulations. | LIXin ZENGXuan SHIJianlei CHENWenbin ZHOUDian LINGXieting | 2003 | Chinese Journal of Electronics2003，12，2： | 0 |
| 2 | Slip Rate on the Altyn Tagh Fault on the West of the Cherchen River (Between 85°~ 85°45′E) Since Late Quaternary显示文摘Because of the significance to the formation and evolution of the Tibetan plateau, the displacement and slip rate of the Altyn Tagh fault have been topics full of disputation. Scientists who hold different opinions on the evolution of Tibet insist on different slip rates and displacements of the fault zone. In the article, study is focused on the late Quaternary slip rate of the Altyn Tagh fault west of the Cherchen River (between 85°E and 85°45’E). On the basis of high resolution SPOT images of the region, three sites, namely Koramlik, Aqqan pasture and Dalakuansay, were chosen for field investigation. To calculate the slip rate of the fault, displacement of terraces was measured on SPOT satellite images or in situ during fieldwork and thermo-luminescence (TL) dating method was used. To get the ages of terraces, samples of sand were collected from the uppermost sand beds that lie just under loess. The method for calculating slip rate of fault is to divide the displacement of terrace risers by the age of its neighboring lower terrace. The displacement of rivers is not considered in this article because of its uncertainties. At Koramlik, the slip rate of the Altyn Tagh fault is 11.6±2.6mm/a since 6.02±0.47ka B.P and 9.6±2.6mm/a since 15.76±1.19ka B.P. At Aqqan pasture, about 30km west of Koramlik, the slip rate is 12.1±1.9mm/a since 2.06±0.16 ka B.P. At Dalakuansayi, the slip rate of the fault is 12.2±3.0mm/a since 4.91±0.39ka B.P. Hence, we get the average slip rate of 11.4±2.5mm/a for the western part of the Altyn Tagh Fault since Holocene. This result is close to the latest results from GPS research. | WangFeng LiMing XuXiwei ZhengRongzhang ChenWenbin | 2004 | Earthquake Research in China2004，18，4： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员