synsedimentary faults同沉积断裂
1.The petrological and petrochemical characteristics indicate that the formation of these conglomerates was controlled by synsedimentary faults during the metallogenic e.通过对该类砾岩岩石学和岩石化学研究 ,认为其形成受控于成矿期的同沉积断裂。
3)syn depositional fault zone同沉积断裂带
4)non-syndepositional fault非同沉积断裂
1.This paper discusses the changes in thickness of strata adjacent to faults induced by non-syndepositional faulting according to outcrop-scale structural phenomena,geophysical maps,model experiments and domestic and foreign data.以露头尺度构造现象、物探成果图件、模型模拟实验及国内外有关文献资料为依据,探讨了由非同沉积断裂活动导致的、发生在邻断裂场所的岩层厚度变化的现象及规律。
5)synsedimentary faulting slope break同沉积断裂坡折
1.LST delta distributes below the synsedimentary faulting slope break,while fluvial delta and fan delta mainly develope in HST.沙三段、沙四段层序体系域构成特征属于受同沉积断裂坡折控制的层序,低位体系域主要发育低位三角洲,并分布在同沉积断裂坡折之下;高位体系域主要发育大型河流或扇三角洲沉积体系,并发育四级层序;湖扩展体系域在坡折带之下发育深湖泥岩和油页岩,在坡折之上发育滨浅湖沉积。
6)faulted deposit断裂沉积
延伸阅读
同沉积构造 见构造。
