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ObjectiveTo investigate the effect of ultra high pressure water jet on the active components of Rhizoma Gastrodiae.

目的研究超高压水射流处理对天麻有效成分的影响。

Amphibole, an important product during retrogression of UHP eclogite to amphibolite, exhibits few brittle deformation features, and does not show any intragranular microstructures indicative of crystal deformation such as undulose extinction, deformation lamellae, subgrain boundary and bulging.

角闪石是超高压榴辉岩退变质过程的产物,在光学显微镜下没有明显的脆性破裂变形,也不显示任何指示晶体塑性变形的晶粒内部显微构造,例如不均匀消光、变形叶理、亚颗粒边界和凸出褶皱等。

Experimental Study of degreased yellow-fin tuna using UHP.

3超高压脱脂黄鱼加工工艺试验研究。

After analyzing the results, the best processing technique for UHP of degreased yellow-fin tuna is achieved, which is after 30 seconds of the pre-processing, holding it for 15min with the pressure of 350MPa. In this way, the preserving period of the processed degreased yellow-fin tuna is extended to 15 days under normal temperature.

对检测结果进行数学分析后,得到了超高压处理脱脂黄鱼的最优加工工艺,为预处理30s后加压到350MPa保压10min,使加工后的脱脂黄鱼在常温条件下的保质期达到了15天。

After the research it is held that when internal fault takes place in the transmission line where the series compensation device is located, the corresponding protective measures, e.g., the forced triggering the by-pass gap, etc., is the effective approach to avoid the appearance of excessing level of transient recovery voltageand oversize coupling current.

文章结合我国南方电网河池固定串补及平果可控串补工程,对超高压输电线路装设串联电容补偿装置后的系统状况进行了比较深入的研究,指出一些系统问题,如过电压水平升高、潜供电流增大和可能发生的次同步谐振均源于串联电容补偿装置的固有特性,通过研究认为当串补所在输电线路发生内部故障时,采取强制触发旁路间隙等保护措施,是避免出现系统恢复电压水平超标和潜供电流增大等问题的有效途径。

The basin subsided so cosmically that led to deposite the thick mudstone of Quaternary.Although there were two-times hiatuses,the period was short and the reservoir pressure didn't escape.Furthermore,the depth subsided again didn't excess the original depth,which resulted in the formation of overpressured reservoir.

盆地发育中表现出大套的第四系泥岩沉积,虽然区域储层顶部出现过两次沉积间断,但间断时间均较短,未造成油藏泄压,加之再次下沉的深度未超过储层的原沉积深度,最终形成盆地性的超高压油藏。

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 extract was dried under nitrogen stream, redissolved in the mobile phase and defatted with n-hexane saturated by acetonitrile.

利用超高压液相色谱-电喷雾串联四极杆质谱联用技术,建立了一种能在10 min内快速分离和测定牛奶中24种磺胺类药物残留的方法。

The coesite-diamond-bearing eclogite distributed in the northern part of the UHPM belt suffered three stages of metamorphism. The first stage is the Ep amphibolite facies metamorphism, which is represented by the paragenesis of phe+Qtz+Cro/Bar Bar+Ep+Ab occurred as inclusions in Grt and Omp; The second stage is the peak metamorphism of eclogite facies with mineral assembledge of Grt+Omp+Coe±Dia±Ky±Zo±Phe+Rt. The P -T condition is 800±50℃,≥28Kb; The third stage is the amphibolite facies retrograded metamorphism from the peak one, which can be divided intothe early amphibolite facies stage with the mineral assembledge of Amp+ Pl+Di+Qtz±Ep+Ilm/Ttn and the late greenschist facies one with the mineral assembledge of Ep+Chl+Bi+Tr+Ab.

分布于超高压变质带北侧的柯石英榴辉岩经历了3个阶段的变质作用:(1)早期绿帘—角闪岩相阶段,以出现在石榴石和绿辉石中的包体矿物多硅白云母、石英、冰蓝闪石或青铝闪石、钠长石等为代表;(2)峰期柯石英榴辉岩相阶段,其矿物组合为Grt+Omp+Ky+Phe±Zo+Coe±Dia+Rt,其变质温度压力为800±50℃,≥28Kb;(3)退化变质作用阶段,早期为角闪岩相,以Amp+Pl+Di±Ep+Qtz+Tit等退变矿物组合为代表;晚期为绿片岩相,以绿帘石、绿泥石、黑云母、透闪石及钠长石等矿物为代表。

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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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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