摘要
分布在华南沿海各种第四纪碳酸盐岩与海岸带的海陆变迁,新构造运动有明显的相关关系。研究表明,华南全新世以来海陆变动受新构造运动制约而不同于华北,华中地区,其各岸段之间的变化也有先后之分。应当从地貌学、岩石学、沉积学等多学科综合地研究第四纪碳酸盐岩的成岩机制,以便取得比较客观的科学解释。
Distribution of various Quaternary carbonates in the coast
area of South China has close relations with coasline shift and neotectonic movement.The study indicates that the change between the sea and the land since Holocene in coast area of South China differ with that in North China and Center China due to the effects of neotectonic movement and there are some differences in different coastline.Besides, we should syntheticaly study the formational mechanism at the angle of geomorphology, sedimentography, petrology etc, in this way, objective scientific interpets will be gained.
出处
《华南地震》
1990年第3期25-33,共9页
South China Journal of Seismology
关键词
第四纪
碳酸盐岩
成岩机制
Coast area in South China, Quaternary carbonates, Mechanism of forming rock, Significance of Neotectonics
