摘要
作为古潮汐研究窗口的现代潮汐沉积体系,其研究的不断深入为古地层序列中潮汐沉积环境的重建提供了重要的理论基础与识别依据。潮汐体系的不同分类与潮坪环境的异样分带,为多样的潮汐信号提供了独特的沉积环境;现代潮汐体系中的微生物研究不断扩展生物成因古潮汐信号的涵盖范畴,物理成因潮汐信号的丰硕成果为古沉积环境重建奠定了坚实基础。结合潮汐沉积体系中古潮汐信号的新进展,分析了豫西元古界鲁山剖面的沉积特征,旨为区域古环境重建提供借鉴意义。
Recent researches unveil that the modern tidal depositional system, tidal deposits, has provided a theoretical foundation and a recognition basis f tidal depositional environment. The different tidal classification and tidal fl as a window of ancient or the reconstruction of at zoning systems were made upon the response of sedimentary environment to various tidal signatures. The research of mi- crobiological deposits in the modern tidal system suggests that the biogenic tidal signal should be a- dopted to the study of ancient tidal deposits. The fruitful achievements of physical palaeotidal signa- ture may provide a solid foundation for paleoenvironmental reconstruction. Based on the new progress in palaeotidal signatures, this paper takes the sedimentary sequence of the Lushan section in the Yuxi district as an example to provide a reference for regional paleoenvironmental reconstruction.
出处
《海洋地质前沿》
2014年第1期1-11,共11页
Marine Geology Frontiers
基金
国家自然科学基金(40472065)
关键词
潮汐沉积体系
古潮汐信号
豫西
元古界
tidal sedimentary system
palaeotidal signature
Yuxi
Proterozoic
