POSSIBILITIES OF SEISMIC EXPLORATION IN STUDYING THE FOLDED STRUCTURE OF ANTHRACITES (GORLOVSKY BASIN)

Q4 Earth and Planetary Sciences
B. A. Kanareykin, A. Salnikov, D. P. Napreev, E. Mosyagin, E. Goshko
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引用次数: 0

Abstract

The paper presents the results of experimental and methodological seismic and electrical exploration along the profile crossing the productive formation of coal seams in the Gorlovsky anthracite basin (Doroginskoye deposit, Shadrinsky block). The obtained CDP time cross sections indicate the possibility of displaying some elements of the folded structure of thick anthracite seams in the wave field at depths up to 300-350 m. Seismic tomography with the use of first arrivals of longitudinal waves allows scientists to reconstruct in detail the velocity structure of the near-surface part of the section to depths of 120-150 m and to identify low-velocity local objects corresponding to the upper edges of the thickest coal members in the upper part of Permian deposits.
地震勘探研究无烟煤褶皱构造的可能性(gorlovsky盆地)
本文介绍了Gorlovsky无烟煤盆地(Doroginskoye矿床,Shadrinsky区块)沿剖面穿越煤层生产层的实验和方法地震和电勘探结果。所得的CDP时间剖面表明,在300-350 m深的波场中,可以显示厚无烟煤煤层褶皱结构的一些元素。利用首次到达纵波的地震层析成像使科学家能够详细重建该剖面近地表部分至120-150米深度的速度结构,并识别出与二叠纪矿床上部最厚煤段上边缘相对应的低速局部物体。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geology and Mineral Resources of Siberia
Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
23
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