THEORETICAL ANALYSIS OF FOLD DEFORMATION

作     者：余祖成 YU ZUCHENG (Institute of Geology, Academia Sinica, Beijing)

作者机构：Institute of Geology Academia Sinica Beijinginear folds in strata are usually considered as the compressional structures because they result from the action of horizontal-compression tectonic stress in the crust. Since the mathematical-mechanical model of simply-supported beam compressed longitudinally has been introduced to the traditional geology the structural line is then considered to be coincident 

出 版 物：《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期：1987年第32卷第11期

页      面：754-760页

学科分类：0709[理学-地质学] 081803[工学-地质工程] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

主　　题：strata tectonic geology folds stratum crust compressed simply directional sedimentary 

摘      要：Linear folds in strata are usually considered as the compressional structures, because they result from the action of horizontal-compression tectonic stress in the crust. Since the mathematical-mechanical model of simply-supported beam compressed longitudinally has been introduced to the traditional geology, the structural line is then considered to be