Magmatism and deformation times of the Xidatan rock series,East Kunlun Mountains

The Xidatan rock series consist of mylonite, gneiss and granite. The U-Pb age shows that the granite was formed at 206 Ma, and the⁴⁰Ar/³⁹Ar ages of the biotite display that the mylonite was formed at 145 Ma when the Xidatan ductile shearzone occurred. At about 110—100 Ma, the Xidatan Fault reactivated again. As a result, the biotite and muscovite of Xidatan rock series opened their argon isotope system.     

Magmatism and deformation times of the Xidatan rock series,East Kunlun Mountains

The Xidatan rock series consist of mylonite, gneiss and granite. The U-Pb age shows that the granite was formed at 206 Ma, and the⁴⁰Ar/³⁹Ar ages of the biotite display that the mylonite was formed at 145 Ma when the Xidatan ductile shearzone occurred. At about 110—100 Ma, the Xidatan Fault reactivated again. As a result, the biotite and muscovite of Xidatan rock series opened their argon isotope system.

     

Tectonic setting discrimination and ~(40)Ar/~(39)Ar isotope geochronology of the Miba granite

The Miba granite is located in the juncture of Kang County in eastern Gansu Provinceand Lueyang County in Shanxi Province. It is considered to be the post-orogenic granite(POG-type) by major element discrimination method of Maniar. ~40Ar/~39Ar dating indicates that itsemplacement time is about 240-230 Ma and it is the result of the Indo-Sinian magmatism. In theearly Yanshan period (about 193.8 Ma), a thermal event resulted in the partial opening of the ar-gon isotope system of the biotite.     

Unroofing around Qaidam Basin of northern Tibet at 30 Ma: constraints from ~(40)Ar/~(39)Ar and FT thermochronology on granitoids

An ~(40)Ar/~(39)Ar and fission track thermochronological study has been carried out on threesuites of granitoids collected along the northern and southern edges of the Qaidam Basin to betterconstrain the mechanisms accommodating the India-Asia collision around the Qaidam Basin(northern Tibet), in order to understand the evolution of the entire deformation area. Mica andK-feldspar have been analyzed and the cooling histories of the latter have been modeled. Thecooling histories based upon K-feldspar modeling and fission track ages show that samples simul-taneously recorded an important cooling event (7.5-10.7℃/Ma) around 30 Ma, which is thoughtto reflect an increase of denudation rate related to the tectonic activity in this area associated withuplift suggesting significant crustal thickening starting around 30 Ma in this area. The estimatedsedimentation rate in the Qaidam Basin, the propagation rate along the Altyn Tagh fault and fieldobservations support this deduction.     

Tectonic setting discrimination and<Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar isotope geochronology of the Miba granite

The Miba granite is located in the juncture of Kang County in eastern Gansu Province and Lueyang County in Shanxi Province. It is considered to be the post-orogenic granite (POG-type) by major element discrimination method of Maniar.⁴⁰Ar/³⁹Ar dating indicates that its emplacement time is about 240—230 Ma and it is the result of the Indo-Sinian magmatism. In the early Yanshan period (about 193.8 Ma), a thermal event resulted in the partial opening of the argon isotope system of the biotite.     

Tectonic setting discrimination and40Ar/39Ar isotope geochronology of the Miba granite

The Miba granite is located in the juncture of Kang County in eastern Gansu Province and Lueyang County in Shanxi Province. It is considered to be the post-orogenic granite (POG-type) by major element discrimination method of Maniar.⁴⁰Ar/³⁹Ar dating indicates that its emplacement time is about 240—230 Ma and it is the result of the Indo-Sinian magmatism. In the early Yanshan period (about 193.8 Ma), a thermal event resulted in the partial opening of the argon isotope system of the biotite.

     

吉林夹皮沟金矿带的稀土元素地球化学研究

为了解吉林夹皮沟金矿带的成矿期次,利用稀土元素的示踪性,对夹皮沟金矿带含矿石英脉、花岗岩及变质地层斜长角闪岩等21个样品进行稀土元素含量测定。测定结果表明,石英脉ΣREE=19.12×10-6～147.57×10-6,δEu=0.61～1.22,平均值0.89,具弱的负Eu异常;太古代花岗岩ΣREE=121.40×10-6～157.32×10-6,δEu=0.87～1.09;中生代花岗岩ΣREE=69.78×10-6～90.95×10-6,δEu=0.94～1.02,LREE/HREE比值分别为11.51～14.12和14.16～16.73,后者轻重稀土分馏程度略高于前者;变质围岩ΣREE=22.40×10-6～275.86×10-6,δEu=0.75～5.79,平均值2.30,具明显的正Eu异常。三者都具有轻稀土富集的平滑稀土配分模型。结合其区域地质背景、流体包裹体和稀土元素特征,得出夹皮沟金矿存在两期成矿作用,分别对应于太古代成矿花岗岩岩浆作用及中生代燕山期花岗岩岩浆作用。太古代首次富集成矿,中生代燕山期叠加成矿并扩大成矿规模,成矿时代分别为2475～2469 Ma和170～160 Ma;结合稀土特征研究及包裹体研究,成矿流体以岩浆热液流体为主,遭受轻微地层变质热液混染,中生代成矿流体混染作用更强烈。     

C~6F~6^+→C~6F~5^++F气相单分子分解及碰撞诱导分解 反应研究

用质量分析离子动能谱(MIKES)研究了C~6F~6^+→C~6F~5^++F的气相单分子分解及其与Ar和He的碰撞诱导分解(CID)反应。实验结果表明,C~6F~6^+在电离室中获得足够能量而被激发到某一长效激发态,而CID是诱导其分解的必要步骤,且该分解过程有两条能量不同的反应途径。当碰撞气体为Ar时,两条途径所对应的能量变化分别为0eV和+9.8eV(将多余能量转化为动能),而当碰撞气体为He时,则分别为0eV和-17eV(将多余能量转化为内能)。CID/Ar诱导该长效激发态在C-F键断裂之前将多余能量转化为动能,而在CID/He中则将多余能量转化为内能。     

聚氧乙烯-高氯酸锂-水复合物体系的固体核磁共振研究

运用13C和7Li固体高分辨核磁共振(NMR)技术对一系列以水作溶剂制备的不同配比聚氧乙烯(PEO)-高氯酸锂(LiClO4)复合物样品的相态结构进行了研究.发现在样品中有一定量水存在的条件下,随着LiClO4含量的增加,复合物体系经历了PEO的结晶逐渐被破坏,PEO与LiClO4形成的新的晶型逐渐增加的过程,当PEO单体与LiClO4的摩尔比在6/1与8/1之间时,样品完全非晶,水的存在对PEO与Li+的相互作用起到了明显的阻碍作用.     

Quantitative analysis of original and powdered rocks and mineral inclusions by laser ablation inductively coupled plasma mass spectrometry

Direct analysis of rocks by laser ablation inductively coupled plasma mass spectrometry is described. Both powdered standard rocks and the original rocks were analysed and the results agreed with each other in spite of the difference in the surface states. Microprobe analysis of biotite in granite JG1 was also done directly with a focused laser beam and the results obtained were very close to the solution values given by the conventional aqueous method using biotite separated from an original rock. For quantitative analysis, the measured signal intensity was normalized either by the ablated weight or the barium signal intensity. Forty-two major and minor elements (two of them being used as internal standards) in twelve standard rocks fromt the igneous rock series of the Geological Survey of Japan were determined successfully.     

2,4-二酮-5-咪唑烷基尿的~(15)N和~(13)C核磁共振研究

本实验测定了2.4-二酮-5-咪唑烷基尿的~(15)N和~(13)C NMR谱并确认了谱线归属。根据化学位移及其在脱质子化过程中的变化,讨论了化合物的互变异构平衡及立体构型的转化问题。结果表明,在溶液中此化合物以酮式结构(A)为主要构型。     

桂北摩天岭花岗岩体的地质地球化学特征及其意义

为研究摩天岭花岗岩体的地质及地球化学特征,分别测定了该岩体的主量元素,微量元素和稀土元素含量,并作了图解分析。结果表明,摩天岭花岗岩体在主量元素特征上表现为富钾,低钠、较低的／7,（Na2O）／n（K2O）,贫钙镁,富铁,w（A）／w（CNK）〉1．1,为强过铝质,具有华南产铀花岗岩的基本特征。微量元素特征表现为：富集强不相容元素,尤其是Rb、Th元素;而贫弱不相容元素zr、Hf、Sm、Y和Yb。Sr元素呈强烈亏损。稀土总含量较低,具有较低的轻重稀土分异,略富集LREE,亏损HREE,具有较低的埘（La）／w（Yb）。岩体具有强烈的负8Eu异常。摩天岭花岗岩体的岩石类型及地球化学特征表明其是S型花岗岩,其形成的构造环境判别图解显示摩天岭岩体具有火山弧花岗岩和同碰撞花岗岩的双重属性。     

~(13)C NMR STUDIES ON DYNAMICS OF POLY (n - ALKYL METHACRYLATES)

The dynamics of a series of poly(n-alkyl methacrylates) is investigated by means of ~(13)C spin-lattice relaxation experiments. The results show that the dynamics has the polymer property dependence.     

Pt羰基簇合物在NaY内的合成机理

利用IR，EXAFS, ~(13)CO同位素交换反应及与NO作用等手段研究了Pt羰基簇合物[Pt_3(CO)_6]~(2-)_n(n＝3,4)在NaY分子筛超笼内的合成机理．在氧化样品Pt~(2+)/NaY上300－373 K的还愿羰基化过程中，首先Pt~(2+)与CO反应生成PtO(CO)物种(波数σ_(CO)＝2110 cm~(-1))，然后聚集成“Pt_3(CO)_6”(σ_(CO)＝2112，1896和1841 cm~(-1))，最后生成深绿色的Pt羰基簇合物Pt_(12)(CO)_(24)]~(2-)/NaY(σ_(CO)＝2080，1824 cm~(-1))．“Pt_3(CO)_6”的羰基在室温下能迅速地与~(13)CO发生交换，而[Pt_3(CO)_6]~(2-)_n(n＝3,4)的羰基与~(13)CO的同位素交换即使在343 K也进行得很慢，室温下，NO能逐步破坏Pt羰基簇合物的层间和层内Pt－Pt键，得到中间物种“Pt_3(CO)_6”和PtO(CO)，同时在气相产生CO_2和N_2O．而由上述两中间物种出发，300－353 K温度下，在CO气氛中的还原羰基化又能可逆地得到原羰基簇合物．     

含R_2dtc配体Mo-Cu化合物的动态~(95)Mo NMR

本实验利用动态~(95)Mo NMR监测Mo-Cu系列化合物的形成过程,对反应CuCl+NaR_2dtc+MoO_nS,摩尔比3:3:1,溶剂为DMF;R=Et,n=0(Ⅰ);R=Me,n=0(Ⅱ);R=Et,n=2(Ⅲ)进行了研究,观察到具有不同簇骼的多种中间产物的存在及随反应进程相互转化等现象。     

GEOCHRONOLOGY OF WANYANGSHAN-ZHUGUANGSHAN GRANITOID BATHOLITH:IMPLICATION FOR THE CRUST DEVELOPMENT

Single-grain zircon U-Pb analyses, combined with Sm--Nd, Rb--Sr, K--Ar and ~(40)Ar-~(39)Ar datingresults, suggest that there are four magmatic periods in Wanyangshan--Zhuguangshan granitoidbatholith, i.e. late Caledonian (414--434 Ma), Indosinian (220 Ma), middle Yanshanian (155 Ma)and late Yanshanian (105 Ma). The tectonic movement characterized by the unconformablecontact between Mid--Devonian and Pre--Devonian occurred about 380 Ma ago. Magmation istightly related to the regional crustal movement.     

NMR研究溶剂与碱金属离子竞争配位过程

本文研究了锂、铵、钠、铯等盐类在21种溶剂中的~7Li、~(14)N、~(23)Na、~(133)Cs/NMR谱。考察了溶剂对碱金属离子化学位移的影响,求出了浓度系数。并研究了上述离子在15种二元溶剂体系中竞争配位过程,基于NMR数据,测定了等溶剂化点,交换过程平衡常数K及自由能变化△G等热力学参数。     

~(29)Si MAS-NMR STUDIES ON DEALUMINATION OF MORDENITE

A series of different H-mordenites from acid leaching and steam calcination have beenmeasured with ~(29)Si NMR. Through analysis of these solid-state ~(29)Si NMR spectra, theresults related to dealumination process of mordenite are obtained. It is shown that mor-denite is combined by four kinds of non-equivalent Si (or Al) via oxygen bridges. The deal-umination order is T(1), T(2), T(4) and T(3). The dealuminated amount in the non-equivalentsites during different dealumination processes has also been discussed in detail.     

[~(188)Re(CO)_3(H_2O)_3]~+前体及标记药盒的制备

~(186,188)Re具有优良的核素性质,是放射性治疗药物的首选核素之一~([1]).~(186,188)Re广泛用于有机小分子化合物,单抗(McAb)、单抗片段(Fab)、受体配基和生物小分子肽,以达到靶向治疗的目的~([2-3]).铼的化学性质与锝极其相似,在标记前以~(188)ReO_4~-形式存在,在标记药物中呈低价态.制备时常规方法是将七价铼通过亚锡法还原到五价~([4-5]).     

~(14)N ENDOR Study on Bis(2-Hydroxylphenyl Ketoxime)-~(63)Cu(Ⅱ) Complex

The ENDOR spectrum of ~(14)N-~(63)Cu-HAP complex in DMSO/EtOH (5:1) freezing solution at 20 K has been studied using orientational selective method in this paper. The anisotropic superhyperfine coupling tensor and qusdrupole coupling tensor of ligand ~(14)N nucleus, and the superhyperfine coupling tensor of various ~1H nuclei have been measured precisely. Comparing the superhyperfine coupling tensor of ~(14)N-nucleus with previous work shows that the analytical method of spectrum is reasonable and the data are reliable in our previous work.