Syndepositional structural slope-break zone is a basic characteristic of rift-subsidence basin.
发育同沉积构造坡折带是断陷盆地的基本特征。
2
These ore deposits displaying belteddistribution mainly occurred in rift and passive continental margins, related to the syndepositional fractures.
在空间上有成带分布特点，主要分布在裂谷带和被动大陆边缘，与同生断裂密切相关。
3
The structural slope_break zone, resulting in the abrupt change of the depositional slope, is initiated by the long_term activity of syndepositional structure.