• “潜伏”脉金矿限于武系以硅质为顶板的碳明显成矿前产生的韧性剪切带控制。

    Gold mineralization of the zone is confined only to the Cambrian carbonaceous shale overlain by siliceous rocks, and apparently controlled by a premineral tough shear zone.

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  • 质岩中硅同位素显示热水成因之特点

    The Silicon and Oxygen isotopes also demonstrate the characteristics of hydrothermal origin.

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  • 研究多孔硅质矿粉掺入普通酸盐水泥水泥性能影响

    The effect of porous silicon rock powder mixing with ordinary Portland cement on properties of cement is studied.

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  • 油浸显微镜下鉴定干酪组成多为有机碎片微粒体,并显示微弱各向异性

    Microscopic studies of the kerogen from the chert samples show that the main components of the kerogen are organic fragments and microsome with weak anisotropy.

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  • 太原燧石结核或条带作用阶段硅质交代成因

    In limestone of Taiyuan Group, Origin of nodular chert and banded chert is that they had been replaced in diagenesis phase.

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  • 本文对深海硅质界线地层牙形石动物群特征进行了简要描述

    We also concisely described the characteristics of the conodont fauna through the boundary strata.

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  • 通过拉尔玛金矿热水成因硅质岩分子古生物学的研究,指出硅质岩关系密切的生物母源为海生低等生物。

    Molecular paleontology in thermal chert in Laerma gold deposit shows that the organic precursors intimately associated with gold are marine bacteria and algae.

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  • 研究结果表明矿化煤层互层热水沉积成因,矿化煤层主要来自形成硅质岩的热水溶液,这种热水溶液锗则主要由盆地基底的锗花岗所提供。

    The results show that the siliceous rocks intercalated with the coal seams were deposited from a hydrothermal medium through which germanium was enriched in the coal beds. The primary source...

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  • 研究结果表明矿化煤层互层热水沉积成因,矿化煤层主要来自形成硅质岩的热水溶液,这种热水溶液锗则主要由盆地基底的锗花岗所提供。

    The results show that the siliceous rocks intercalated with the coal seams were deposited from a hydrothermal medium through which germanium was enriched in the coal beds. The primary source...

    youdao

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