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The way in which irradiated food spoils is likely to be different from the way fresh food spoils because the populations of micro -organisms are modified by irradiation.

辐照食物变质的方式,很可能与新鲜食物变质的方式不同,这是因为辐照减少了食品中微生物的种类及数量。

The way in which irradiated food spoil s is likely to be different from the way fresh food spoil s because the populations of micro-organisms are modified by irradiation.

辐照食物变质的方式,很可能与新鲜食物变质的方式不同,这是因为辐照减少了食品中微生物的种类及数量。

Most of amphiboles are retrograde phase in the eclogite,with barroisite,magnesiocatophorite and so on.

榴辉岩峰期变质的矿物组合为石榴子石+绿辉石+多硅白云母+金红石,变质温度在500℃左右,压力在2.3Gpa左右。

Mafic granulite and gabbro xenoliths are also found in the same kimberlitic pipes from the Eastern-North China platform, and suggest that multi-accretion events took place. The gabbro was formed lighly earlier with the host kimberlite. The underplating of the mafic magmas was related to the continental orogeny in the late middle-Ordovician Period.

金伯利岩中强烈变质的基性麻粒岩以及变质不彻底的粗粒辉长岩在同一岩管中共存,表明华北古老岩石圈地幔所发生的多次增生作用事件,特别是后者的变质不彻底变质作用暗示其形成时代与金伯利岩相近,这种基性岩浆的底侵作用与华北地台中奥陶世晚期的造陆抬升有关。

Changed in structure or composition as a result of metamorphism.

变质的因变质作用而导致的结构变化或成分变化。

Using KI index method can distinguish the extremely lowly metamorphose rock from non-metamorphose rock,and can disti...

使用伊利石结晶度指数法可以将极低级变质与未变质的岩石类型区分开,也可以将极低级变质与浅变质的岩石类型区分开,从而解决了沉积岩与浅变质岩之间过渡岩石类型划分的难题。

For giving an explaintion of strong transmogrification but feebleness metamorphism of and their corresponding relation of the Triassic stratum in Songpan-Ganzi area and opening out the temperature and stress condition, this paper summarized study production of predecessors, and put forward 5 conclusions about Songpan-Ganzi area Triassic main lithology(slate, sandrock,and blastopsammitic) through field geological investigation , actual measurement section plane study and combining indoor slice identification , electron probing and fluid enclosure testing analysis:1.Field outcrop strongly transmogrification, and often developed same cleavages(S1) erection or approximately erection 'B'fold and symmetry similituded fold. 2.The metamorphosed mineral combination is simple, and the typical metamorphosed mineral combination is Al+Chl+Ser+Cc+Q, etc. The metamorphosed mineral develops mainly along the cleavages of the territorial cleavages faces(S1), bearing territorial dynamic metamorphism character and belonging to the lawsonite-albite-chlorite face of slightly metamorphism. 3.Territorial metamorphism P-T change focus on T:180~200oC, P:1~2kbar

为了对松潘-甘孜地区三叠系强变形浅变质的特征及变质与变形的对应关系作出解释,揭示变质与变形的温-压条件,本论文总结前人研究成果,通过野外地质调查和实测剖面研究,结合室内薄片鉴定、电子探针和流体包裹体测试分析,对松潘-甘孜地区三叠系主体岩性(板岩、砂板岩、变质砂岩及千枚岩)的变质作用得出5 个认识结论:1、整个松潘-甘孜地区经受了自北向南的强大挤压;2、变质矿物组合简单,除雏晶黑云母外,典型的变质矿物组合为Al+Chl+Ser+Cc+Q等,变质矿物主要沿区域性劈理面(S1)的劈理域发育,具有区域动力变质作用特征,属于低级变质作用中的硬柱石-钠长石-绿泥石相;3、区域变质作用P-T 变化集中在T:180~200oC,P:1~2kbar

The metamorphic rocks of the area consist of granulite, plagioclase-gneis, biotite leptite and various kinds of schists of granulite to amphibolite facies By reconstruction, this metamorphic series is composed of three original formations which inciude five originai rock types: intermediate-acid volcanics formation at the bottom basic-felsic bimodae volcanits formation in the middle and basic-andesitic-felsic volcanics formation at the top...

区内太古代变质岩系广泛发育,其下部为深变质的麻粒岩相地层,上部为中深变质的角闪岩相地层,后者产出红透山式铜锌矿床多处,以及张胡子沟铜矿床和大荒沟硫铁矿床等一系列块状硫化物矿床(图1)。矿石中铅同位素年令为25~26亿年,在形成时代上可以和鞍本地区鞍山群对比。

The microstructural nomograph of these Al-Si alloys is constructed to provide for the selection of optimum addition of Sr or Sb in production practice Experimental results indicate a threshold of Sr content in Al-Si alloy modification, over it, the structure of Al-Si alloy may be completely modified even at quite slow cooling rate down to 4.5℃/min.

实验结果表明,Al-Si合金加Sr后变质存在一个变质阈值,超过这个阈值时,即便在投缓慢的冷速(4.5℃/min)下,仍能获得完全变质的组织。这个变质阈值随着冷速的减慢而增大。

Therefore,the northern Sulu UHPM zone can be divided into four petrological tectonic units from southeast to northwest:Haiyangsuo metamorphic complex (eclogitized crystalline basement of the Yangtze craton),Rongcheng UHPM complex,Weihai metamorphic complex (granulites retrograded from UHPM eclogites) and Kunyushan boundary metamorphic magmatic complex.

由此笔者将苏鲁变质带北部由南向北划分为海阳所变质地块(榴辉岩化扬子陆块基底变质单元)、荣成变质地块、威海变质地块(麻粒岩相叠加变质的超高压构造岩片)、昆嵛山边界杂岩带。

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