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GUI FENG group mainly is a group of alternate layer that is composed of amaranthine conglomerate, gritstone, and mudstone with fine sand.

圭峰群主要为一套洪——冲积相紫红色砾岩、砂岩、粉砂质泥岩的互层,形成下粗上细的多个沉积旋廻。

Confirmation of high-pressure pelitic rocks in the north. The mineral assemblage of the early stage is gamet-Mg-rich chloritoid +phegite +quartz ±kyanite ±aragonite or gamet+Mg-rich chloritoid+phengite+paragonite+quartz, P-T conditions are 550±30℃ and 1.4~2.0GPa; the mineral assemblage of the late stage is muscovite +chlorite+quartz±albite, which undergone retrograde metamorphism of greenschist facies, P-T conditions are <550℃ and <0.6GPa.

确定北部高压变泥质岩石,早期矿物组合为石榴子石+富镁硬绿泥石+多硅白云母+石英±蓝晶石±文石或石榴子石+富镁硬绿泥石+多硅白云母+钠云母+石英,对应的温压条件为550±30℃和1.4~2.0GPa;晚期矿物组合为白云母+绿泥石+石英±钠长石,经受了绿片岩相的退变质作用,其温度小于550℃,压力低于0.6GPa。

Leopard limestone is composed of dolomitic and marly materials.

组成豹皮灰岩的物质成分有2种,一为白云质成分的豹斑,其余部分为泥灰质。

And the pelite schist is the main rock type, and contains the classic medium pressure metamorphic minerals.

泥质片岩是工作区内分布最多的岩石组合,出现了典型中压类型的标型矿物及矿物组合。

Found in the contact zone of the shale rock, but also common in crystalline schist.

见于接触带的泥质岩石中,也常见于结晶片岩中。

Sanidinite (some have transformed to perthite) and quartz inclusions with radial cracks are often seen in the garnet of eclogite. The geothermal gradient of <10℃/km is recorded in the early stage mineral assemblage of high-pressure metapelitic rocks with relict aragonite. these features imply a possibility that there may be ultra-high-pressure rocks existed in Altun.

根据榴辉岩中石榴石常见透长石和石英包体,并有放射状裂纹的特征,以及高压变泥质岩石早期矿物组合温压条件记录的地温梯度小于10℃/km和残存文石等特征,不排除区内有超高压变质岩石存在的可能性。

Orebodies occur in a fault near the axial region in the southern limb of the Jinjinghe-Hujiamiao inverted secondary anticline in the southern limb of the Hongyansi-Heishan composite syncline. Host rocks are dolomitic rocks in the middle and upper parts of the Devonian Qingshiya Formation. Their spatial distribution is obviously controlled by an interlayer fracture-fissure zone near the axial region in the steeply dipping southern limb of an anticline. Ores are dominantly of nodular and stockwork types and the feature of epigenetic mineralization is very pronounced.

矿体产于红岩寺—黑山复式向斜南翼金井河—胡家沟次级背斜南翼近轴部断裂中,赋矿岩石为泥盆系青石垭组中上部白云质岩,其空间展布明显受背斜陡倾南翼近轴部的层间断裂-裂隙带构造控制,矿石主要有团块状和网脉状,其后生成矿现象非常明显。

The longer treatment time of samples would result in the more reduction of compressive strength and Young's modulus,because the shale or clay in rock sample would get soft by the drilling fluid filling.

岩石矿物中的泥质黏土矿物遇到钻井滤液后产生软化效应,致使岩样呈现:经钻井液处理时间越长,其抗压强度和弹性模量下降越多的趋势。

The paper introduced serious sand production actuality of the quaternary gas reservoir located in Sebei Gas Field,which consists of unconsolidated fine siltstone formations with high content of shale.

介绍了涩北气田第四系高泥质疏松粉细砂岩气藏的出砂现状,通过多年的室内基础理论研究和现场防砂先导性试验成果总结,形成了适合涩北气田的高压一次充填防砂工艺。

The reasons of the silty mudstone disintegration are the expansion of water, the dissolution of cement, the tension stress and the tensile stress caused by dry-wet cycle of the rock.

粉砂质泥岩的崩解是由岩石浸水膨胀、胶结物溶解和干湿循环产生的拉应力与张应力共同引起的。

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