工程基础实验与训练中心课程设计说明书(论文)封面及中、英文摘要范例
南京工程学院
工程基础实验与训练中心
本科课程设计说明书（论文）
题 目：
专 业：
班 级： D机加工051 学 号： 203030807
学生姓名： XXX
指导教师： XXX （职称）
起迄日期： 2009.3.10～2009.6.15
设计地点： 工程中心1号楼
课程设计说明书（论文）中文摘要
I
课程设计说明书（论文）英文摘要
- II -
第二篇：英文摘要格式范例
英文樣張
【英文文體一律使用Times New Roman，摘要頁面為A4一頁，內容包含題目、作者單位及內文一律以字形大小12 書寫；上下邊界2.54cm、左右邊界
3.17cm，無裝訂邊】
Investigation of Strong Aftershock Sequences
Cheng-Horng Lin
Institute of Earth Sciences, Academia Sinica
Abstract
The 1999 Chi-Chi, Taiwan earthquake (Mw=7.6) triggered a huge number of strong aftershocks in the Taiwan area. Those earthquakes provide an ideal opportunity to statistically examine possible mechanisms of both earthquake triggering and fault interaction.
Introduction
The 1999 Chi-Chi, Taiwan earthquake (Mw = 7.6), one of the best instrumentally recorded earthquakes in the world (Teng et al., 2001), has provided another reliable seismic data set with which to examine possible mechanisms of earthquake triggering and fault interaction.
References
Andrew, M.F. and J. Lin, 2001: Delayed triggering of the 1999 Hector Mine earthquake by viscoelastic stress transfer, Nature, 411, 180-183.
Chen, K.C. and J.H. Wang, 1988: A study on two 1986 Hualien, Taiwan earthquakes and their aftershocks, Proc. Geol. Soc. China, 31, 65-72.
Figure 1. Distribution of earthquakes (small dots) after the 1999 Chi-Chi, Taiwan earthquake (a thick circle) and the general geology of the island of Taiwan. Most earthquakes are grouped into two seismic zones (i.e., the Chi-Chi and the Central Range seismic zones) marked by dashed-boxes. The regional seismic network (CWBSN) was marked by triangles.