Well-preserved garnet growth zoning in granulite from the Dabie Mountains, central China

Ultra-high pressure eclogites and granulites both occur in the Dabie Mountains, central China. A garnet porphyroblast from felsic granulite in the Dabie Mountains has been analysed for compositional zoning by electron microprobe. Two segments of the porphyroblast have opposite compositional variations. Segment I (from centre outward 9  mm to analytical point 18) has decreasing X_Sps and increasing X_Pyr, while Segment II (from analytical point 18, 1  mm outward to the rim) has increasing X_Sps and X_Alm and decreasing X_Pyr and X_Grs. The compositional zoning in segment I is considered as growth zoning and that in Segment II as diffusive retrograde zoning. Garnet growth zoning records a P–T  path prior to the peak granulite metamorphism. The minimum P – T  conditions are estimated to be 1.35  GPa and 850  °C for peak metamorphism, based on the highest Mg/(Fe+Mg) composition in the garnet (analytical point 18) and matrix hypersthene, biotite and plagioclase. A symplectitic corona surrounds the porphyroblast and appears to have formed at 0.6  GPa and 700  °C. The well-preserved growth zoning in garnet suggests a short residence time for the granulite at peak metamorphism and thus rapid tectonic uplift history. The P–T  path is consistent with that of ultra-high-pressure eclogite in the area. Tectonic movements during a collisional event could have brought both the granulite and the eclogite to their present positions.     

滨海城市环境工程地质问题发育特点分析

本文分析了我国滨海城市环境工程地质问题的主要类型,研究了环境工程地质问题的发育特点。     

优化偏最小二乘光度法同时测定铑铱钯的研究

采用局部加权、随机矩阵法等步骤,使建立的校准模型能充分反映未知样品的数字结构特征,达到优化的目的,从而改善偏最小二乘法在处理实际未知样品数据时的解析能力,以提高计算结果的精度。用该优化偏最小二乘法对模拟地质样品中痕量贵金属Ｒｈ、Ｉｒ、Ｐｄ进行多组分光度测定,其分析结果的相对误差均小于１０％;分别测定９．５μｇ／Ｌ、３５．０μｇ／Ｌ、６６．０μｇ／Ｌ含量的Ｒｈ、Ｉｒ和Ｐｄ７次,其标准偏差Ｒｈ为０．２;Ｉｒ为１．１;Ｐｄ为２．０。     

等离子体发射光谱法测定重晶石中钡铁和硅

重晶石经Ｎａ２ＣＯ３熔融,水浸取,过滤。沉淀经ＨＣｌ溶解后,用电感耦合等离子体发射光谱法同时测定主成分ＢａＳＯ４和次量成分Ｆｅ２Ｏ３以及滤液中的ＳｉＯ２,结果与部颁标准方法符合。方法精密度好,主量组分ＢａＳＯ４测定的ＲＳＤ（ｎ＝６）为０．２４％,次量组分Ｆｅ２Ｏ３和ＳｉＯ２的ＲＳＤ（ｎ＝６）分别是３．６９％和１．４５％。     

新疆北部后碰撞幔源岩浆活动与陆壳纵向生长

新疆北部后碰撞幔源岩浆活动强烈。Nd、Sr和Pb同位素资料表明,在330～250Ma的后碰撞期间,有大量的幔源花岗岩类和少量的镁铁—超镁铁杂岩在上地壳侵位。与加里东、海西和喜马拉雅等造山带起源于再循环陆壳的花岗岩类不同,新疆北部后碰撞岩浆岩一般表现出ε_(Nd)(t)值高、(~(87)Sr/~(86)Sr)值相对较低、Nd和Pb模式年龄年轻等特点。阿尔泰山和天山的一些后碰撞花岗岩类可能具有陆壳源区的特点或表现出地壳物质对幔源岩浆及其分异产物有不同程度的混染,东、西准噶尔花岗岩类很少甚至没有受到陆壳物质混染。新疆北部后碰撞花岗岩类和镁铁—超镁铁杂岩主要是幔源岩浆及其分异产物在上地壳侵位的结果。这些幔源花岗岩类代表了新生的初始地壳,其时代可代表地壳形成时代。在后碰撞阶段,新疆北部的陆壳以纵向生长为特征。     

玻镁安山岩中辉石枝晶的形貌与晶体生长方式

川西乡城地区的玻镁安山岩基质中辉石微晶具有奇特的枝晶形貌。通过高倍率光学显微镜和扫描电镜观察,较详细地分析了辉石枝晶的形貌细节。辉石枝晶一般发育三级分枝,各分枝间以近于90°和110°交角沿单斜辉石结晶学主轴方位优先生长,各级分校具有整体一致的光学性质,如同单个晶体。玻镁安山岩浆流动性大,呈薄层状。快速冷凝作用和强的结晶能力是辉石枝晶发育的前提条件。初步探讨了在远离平衡态结晶时,辉石枝晶生长方式和界面稳定性对晶体形貌的控制作用。     

菊花石生长几何模型

通过与ＤＬＡ模型类比,建立起一个菊花石生长几何模型,分析了菊花石生长过程中的“间距分叉”现象及花瓣间距Ｈ的演变规律及速率,并对比分析了菊花石实际形貌与生长模型形态的异同和原因。     

CHARGING OF DUST GRAINS IN COMETARY PLASMA ENVIRONMENTS

The equilibrium potential of fluffy dust grains in plasma environments is modeled numerically for comet P/Halley. It is found that the dust grain acquires its largest negative potential and probability of disruption at about 50, 000km from the comet where the mass spectrum measured by the spacecraft took a great change.     

区域经济研究的几个理论问题

研究区域经济,首先要明确区域经济赖以存在的逻辑基础,好资源的稀缺性、人类经济活动的音空有限性和生产要素在空间上的非安全充分流动性。从这一逻辑推演,区域经济学是一门学多学科交叉的边缘学科。它所研究的主要内容是探索区域经济增长的一般规律并制定协同区域经济增长差异的政策。     

On the agricultural growth and structural changes in Suzhou Wuxi Changzhou region

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