利用钻井岩屑进行地层边界的细化和沉积断裂带的识别

A. A. Morova
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引用次数: 0

摘要

通过对巴什基尔时代碳酸盐岩矿床钻探岩屑的研究,表明岩屑的岩性岩相学、物理力学、矿物学和地球化学性质在地层边界打开时发生了变化。盖层学研究证明,岩磁单元通常与地层单元一致,但在某些情况下,通过岩磁节奏分析可以细化地层边界。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
REFINEMENT OF STRATIGRAPHIC BOUNDARIES AND IDENTIFICATION OF ZONES OF BREAKS IN SEDIMENTATION BY WELL DRILLING CUTTINGS
By the example of studying the drilling cuttings from the carbonate deposits of Bashkir age it is shown that lithologic-petrographic, physic-mechanical, mineralogical and geochemical properties of cuttings change at the opening of stratigraphic boundaries. Cappametric research proves that the petromagnetic units, as a rule, coincide with the stratigraphic ones, but in some cases the analysis of the petromagnetic rhythm allows to refine the stratigraphic boundaries.
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