High-pressure eclogites in northern Jiangsu – southern Shandong province, eastern China

Abstract Eclogites are distributed for more than 500 km along a major tectonic boundary between the Sino-Korean and Yangtze cratons in central and eastern China. These eclogites usually have high-P assemblages including omphacite + kyanite and/or coesite (or its pseudomorph), and form a high-P eclogite terrane. They occur as isolated lenses or blocks 10 cm to 300 m long in gneisses (Type I), serpentinized garnet peridotites (Type II) and marbles (Type III). Type I eclogites were formed by prograde metamorphism, and their primary metamorphic mineral assemblage consists mainly of garnet [pyrope (Prp) = 15–40 mol%], omphacite [jadeite (Jd) = 34–64 mol%], pargasitic amphibole, kyanite, phengitic muscovite, zoisite, an SiO₂ phase, apatite, rutile and zircon. Type II eclogites characteristically contain no SiO₂ phase, and are divided into prograde eclogites and mantle-derived eclogites. The prograde eclogites of Type II are petrographically similar to Type I eclogites. The mantle-derived eclogites have high MgO/(FeO + Fe₂O₃) and Cr₂O₃ compositions in bulk rock and minerals, and consist mainly of pyrope-rich garnet (Prp = 48–60 mol%), sodic augite (Jd = 10–27 mol%) and rutile. Type III eclogites have an unusual mineral assemblage of grossular-rich (Grs = 57 mol%) garnet + omphacite (Jd = 30–34 mol%) + pargasite + rutile. Pargasitic and taramitic amphiboles, calcic plagioclase (An₆₈), epidote, zoisite, K-feldspar and paragonite occur as inclusions in garnet and omphacite in the prograde eclogites. This suggests that the prograde eclogites were formed by recrystallization of epidote amphibolite and/or amphibolite facies rocks with near-isothermal compression reflecting crustal thickening during continent–continent collision of late Proterozoic age. Equilibrium conditions of the prograde eclogites range from P > 26 kbar and T= 500–750°C in the western part to P > 28 kbar and T= 810–880°C in the eastern part of the high-P eclogite terrane. The prograde eclogites in the eastern part are considered to have been derived from a deeper position than those in the western part. Subsequent reactions, manifested by (1) narrow rims of sodic plagioclase or paragonite on kyanite and (2) symplectites between omphacite and quartz are interpreted as an effect of near-isothermal decompression during the retrograde stage. The conditions at which symplectites re-equilibrated tend to increase from west (P < 10 kbar and T < 580°C) to east (P > 9 kbar and T > 680°C). Equilibrium temperatures of Type II mantle-derived eclogites and Type III eclogite are 730–750°C and 680°C, respectively.     

济南岩溶地下水化学成分的形成

本文研究济南岩溶排泄区地下水化学成分的形成。先用Cl-和NO3-浓度作为示踪剂分析补给区的大气降水输入,鉴别出西郊和平安店排泄区地下水没有被明显污染,市区和东郊排泄区地下水受到明显污染,污染主要来自当地浅层地下水或近地面土层。之后,利用西郊排泄区的测试数据进行了横向径流带的水-岩作用定量分析,与示踪剂研究结果一致,市区和东郊排泄区地下水被明显污染,同时提出地下水在径流过程中发生脱白云石化过程的趋势线。     

嵩县螃蟹沟隐爆角砾岩体与钼金矿化成因探讨

螃蟹沟隐爆角砾岩体是河南省嵩县西北部众多含钼、金角砾岩体之一,这些角砾岩体具有成群、成带分布的特点.螃蟹沟角砾岩体的定位与分布受北西向背形、北西向和北东向断裂构造的复合控制,由燕山期钙碱性岩体与岩脉的侵入,以及随后发生的隐蔽爆发-坍塌作用而生成了角砾岩体.其中包括了震碎角砾岩、隐爆角砾岩、侵入角砾岩及坍塌角砾岩.岩体被后期断裂构造作用所复合叠加,致使钼、金富集成矿,形成"多型一体"的钼金矿床.     

A Numerical Study on the Structure and Dynamics of Turbulence in Oscillatory Bottom Layer Flow over A Flat or Rippled Bed

1 .IntroductionUnder the influence of surface waves ,sandripples often appear on beaches . Whenthe amplitudeof water oscillationis sufficientlylarge ,vortices are formed onthe lee of every sand ripple crest . A-mongthese vortices ,the most important are t…     

健康型牛蛙饲料养殖牛蛙的试验

本研究采用5种中草药添加剂配方的膨化饲料进行了为期36d的牛蛙养殖对比试验.结果表明，饲料中添加有中草药制剂的日摄食量明显大于对照组，日增重显著比对照组的高.而且大大加快了生长速度，缩短养殖周期，同时减少了染病机率，牛蛙体色鲜艳、光泽度极佳.     

全液压多功能登船梯介绍

舟山群岛岙山五万吨级油码头使用的全液压登船梯，具有提升、变幅、回转和调位四大功能，文章还对液压系统，电器系统的特点作了介绍。     

化学物质对硬壳蛤幼虫变态的诱导

用KCl、肾上腺素（EPI）、去甲肾上腺素（NE）、L—DOPA和GABA（γ-氨基丁酸）进行了不同浓度不同处理时间对硬壳蛤（Mercenaria mercenaria L ）幼虫变态诱导实验。结果表明，KCl、肾上腺素、去甲肾上腺素和DDOPA对硬壳蛤幼虫的变态均有诱导作用，而GABA的诱导作用不显著。KCl的最佳诱导浓度随处理时间不同而有所不同。处理时间为1～24，48，72h时KCl的最佳诱导浓度分别为33．56，20．13～26．85，13．42mmol／L。肾上腺素和去甲肾上腺素的诱导作用与浓度和处理时间均有关。肾上腺素的最佳处理浓度为100μmol／L，最佳处理时间均为8h，此时幼虫变态率提高最大，为36．97个百分点。当去甲肾上腺素的诱导浓度为100μmol／L，处理时间为8～16h时，幼虫变态率提高也较大，均大于18个百分点，死亡率增加，但均低于30个百分点，当去甲肾上腺素诱导浓度为500μmol／L时，虽然在8～16h的处理时间范围内，幼虫变态提高率也较大，均大于18个百分点，但当处理时间超过8h，在16～48h范围内，幼虫死亡率提高明显增大，均大于50个百分点。L-DOPA的适宜诱导浓度为10～50μmol／L，适宜处理时间为8～24h，此时幼虫变态率均提高30个百分点以上，最高可提高79．43个百分点。GABA的诱导作用较弱，最佳诱导浓度随处理时间的不同而有所不同，处理时间为24h和48h时，最佳诱导浓度为0．1μmol／L；处理时间为0．5～16h时，最佳诱导浓度为100μmol／L。     

现代黄河三角洲粉土触变性研究及其应用

通过对现代黄河三角洲砂质粉土和粉质粘土触变性的对比试验研究，阐述了黄河口粉土的触变性。试验结果对解释粉土的失稳机制、解决工程地基的稳定性和防止地质灾害等具有重要的现实意义。     

酶解鲐鱼蛋白制备低分子肽制品

介绍了以鲐鱼为原料 ,采用双酶水解技术 ,制备高质量的低分子肽粉末制品的最佳工艺。对鲐鱼水解液 4种脱苦脱腥的方法进行了比较 ,认为活性碳脱除法既可脱腥 ,又可脱苦、脱色 ,是鲐鱼水解液脱苦脱腥较好的方法。经正交试验得其最佳组合 :每升水解液中活性碳的用量为 1 0 g;时间为 40 min;温度为 40℃。制品为一种淡黄色粉末 ,含有较多的二肽、三肽等低分子肽 ,氨基酸种类齐全 ,富含人体所需矿物质元素的高质量的食品原料。     

最小弧菌热不稳定型溶血素基因克隆与序列分析

根据已发表的最小弧菌热不稳定型溶血素（heat-labile hemolysin）基因核苷酸序列，设计和合成一对特异性引物，以最小弧菌96-6-3的基因组DNA为模板，PCR扩增得到热不稳定型溶血素基因片段，克隆到质粒载体pMD-18T中进行测序和分析．其结果表明扩增的热不稳定型溶血素基因片段与已发表的最小弧菌热不稳定型溶血素的同源性高达98％，扩增片段编码由446个氨基酸组成的多肽，推测分子量为50200．软件分析表明编码的氨基酸有较高的抗原性，可作为基因工程疫苗的候选基因片段．