阿尔丹-玛雅油区里芬沉积地震地质与构造特征

I. Gubin, А. E. Kontorovich, S. A. Moiseev
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引用次数: 0

摘要

考虑了Aldan-Maya油区Riphean沉积盖层地质构造的主要特征。利用地震和声波测井资料,研究了Riphean矿床的速度特征。结果表明,主要的声学差异与持续的riphean反射体的形成有关。它们与地层和序列的边界有关。在对9个区域勘探项目地震资料进行综合解释的基础上,绘制了地震地质剖面和构造图,为阿尔丹-玛雅油区境内构造构造分区提供了依据。给出了上卡累利阿-下里芬和上-中里芬两个构造阶段的构造图,指出了它们的根本区别,特别是大的May倾斜隆起只在下里芬的凸起上发育,而在中-上里芬表面不发育。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismogeological and structural characteristic of the Riphean sediments within Aldan-Maya petroleum region
The key features of the geological structure of the Riphean sedimentary cover within the Aldan-Maya petroleum region are considered. Using seismic and acoustic logging data, the velocity characteristics of the Riphean deposits were studied. It was shown that the main acoustic contrasts are associated with the formation of sustained intra-Riphean reflectors. They correlate with the boundaries of formations and series. Based on the results of generalization and interpretation of seismic data on 9 projects of regional prospecting, seismogeological sections and structural maps were constructed, which served as the basis for structural-tectonic zoning of the territory within the Aldan-Maya petroleum region. Tectonic maps are presented for two structural stages - Upper Karelian-Lower Riphean and Upper-Middle Riphean, their fundamental difference is shown, in particular, the large May inclined swell is developed only in the reliefs of the lower Riphean not in the Middle-Upper Riphean surfaces.
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