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花岗岩化

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Ore mineralization and alteration are mainly distributed in external contact zone of Yanshanian moyite and marble of Jining rock group, outcrop of three strip ore bodies, a lenticular, vein, cystic and so, for direct prospecting signs of iron and manganese cap.

矿体及矿化蚀变带主要分布在燕山期钾长花岗岩与集宁岩群大理岩的外接触带上,地表出露三条带状矿体,呈透镜状、脉状、囊状等,直接找矿标志为铁锰帽。

Low-T tectonites also include several mylonitized porphyritic monzogranite intrusions in the lower plate.

低温构造岩也包括发育于下盘的几个糜棱岩化似斑状二长花岗岩侵入体。

This class of deposits is characterized by the abundance of iron oxide in the ores and the associated intensive regional sodic alteration. They may occur in Proterozoic intracraton or Phanerozoic continental margin volcanic arcs with nearby intrusive complex or evaporite. The spatially and temporally associated intrusive rocks are magnetite-series granitoids. Mineralization mainly occurs in second order echelon structures near the main regional structure.

该类矿床以矿石中含有大量的铁氧化物且伴有很强的区域性钠质蚀变为特征,可以产于元古代克拉通内或新生代大陆边缘岛弧环境,其周围具火成岩或含蒸发盐层,时空上与之有关的侵入岩为磁铁矿系列花岗岩,矿化主要产于近区域主断裂的羽状次级断裂中。

The profile is classified into 6 grades I-VI as residual soil, completely weathered, stronly weathered, moderately weathered, slightly weathered and unweathered rocks.

花岗岩风化壳剖面适用六分法(残积土层、全风化带、强风化带、中等风化带、微风化带和未风化带)。

During the early stage of Yanshan Movement in the Mesozoic Era, when the North China Plate had completed joining the Yangtze Plate to become a new united Craton massif, the tectonic movement turned to intracontinental orogenic stage, resulting in widespread magmatic activity and migmatization so that Tianzhu granitic batholith intruded the area on a large scale to form an embryo of the granite peak forest in the Tianzhu mountain area and ultrahigh pressure metamorphic zone further retraced its way, and consequently outcropped on the crust surface.

中生代燕山早期,华北、扬子板块已完成对接拼合,形成了新的统一的克拉通地块,构造运动已转入陆内造山阶段,引起广泛的岩浆作用和混合岩化作用,天柱山花岗质岩基大规模侵入,形成了区内天柱山花岗岩峰林胚胎,并导致超高压变质带进一步折返,并最终出露地表。

The vitrified soil, as hard as granite, can be used for landfill.

玻璃化的土壤类似坚硬的花岗岩,可以用于填埋。

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