内蒙古银都银铅锌多金属矿床成矿流体特征及成矿年代学研究

内蒙古银都银铅锌多金属矿床属于特大型银矿床, 经研究, 确定成矿过程经历了早、中、晚 3 个阶段, 分别形成以闪锌矿-磁黄铁矿-黄铜矿、方铅矿-磁黄铁矿、萤石- 白云母-碳酸盐为代表的矿物组合。其中, 早阶段为锌、铜的主成矿阶段, 中阶段则是银铅锌的成矿阶段, 晚阶段矿化较弱。激光拉曼显微探针分析表明成矿流体为 H₂O-CO₂-CH₄-NaCl 体系。包裹体研究显示成矿流体具有低盐度( 2%～5% ) 、低密度( 0. 72 ～0. 88 g/ cm³ ) 的特点, 成矿温度随着成矿流体的演变, 逐渐降低, 早、中、晚阶段分别为 340. 5℃, 282. 4℃及260. 3℃, 成矿压力为37 ～74 MPa, 成矿深度为 3. 7 ～7. 0 km。经对萤石- 白云母-碳酸盐阶段白云母的激光探针 ⁴⁰Ar-³⁹Ar年代学测定, 确定成矿年代为 135±3 Ma, 为白垩纪早期。     

Evidence of Nd isotope for unhomogeneity and origin of upper mantle of North China platform

Based on isptopic age of Sm-Nd and its initial composition and its evolution obtained during the recent years of archean metamorphic magnesio-ferro the vocanics of upper mantle of the North China platform, it is concluded that the isotopic composition of Archean upper mantle of the North China platform is not homogeneous, and values of I_ND don not change regularly through the whole Archean; in contrast, they present obvious differences in different regions. All this demands that the unhomogeneity of Archean upper mantle of the North China platform inherits initial unhomogeneity of origin, and the origin of the North China platform should contribute to uneven accumulation of planetesimals.     

The evidence of Sm-Nd isochron age for the early Paleozoic ophiolite in Mangya area, Altun Mountains

The REE patterns of the basic volcanic rocks in Mangya area, Altun, are slight rich in LREE with (La/Ya)-N=1.69-3.20, (La/Sm)-N=1.37-1.87, other trace element ratios of the rocks are Th/Ta≈1 (for a few samples greater than 1.5), Nb/Y=0.34-0.62, Ti/Y=310-443 (on the average: 381), Ti/V=37-62, Zr/Nb=9.4-12.4, Sr/Rb=12-80 (on the average: 37), and Nb/Th=7.7-16.8. These features are similar to that of E-MORE or OIB. The ε Nd(t) value, being 3.95- 4.12, shows that the source of the volcanic rocks is derived from depleted asthenosphere mantle mixed with materials from enriched mantle. These, together with the information of geological setting and rock assemblages, indicate that the basic volcanic rocks are of ophiolite. The Sm-Nd isotope ages for the eight basic volcanic rock samples construct a straight line with good correlation, and the calculated isochron age is (481.3±53) Ma. Besides, the eight calculated ε Nd(t) and model ages are close to each other, which suggests that they are homologous, so the isochron is not a mixed line. In the meantime, the isochron age ((481.3±53) Ma) is lower than the model ages (T DM=1 004-1 534 Ma) of the samples, suggeting that the isochron age represents the formation age of the basic volcanic rocks and the ophiolite belt in Mangya area, Altun is formed in the early Paleozoic (Cambrian-Ordovician). In spite of the greater uncertainty of the age, it is still reliable because it is consistent with the age constrained by the regional strata.     

An Sm-Nd isotopic dating study of the Archean Kongling Complex in the Huangling area of the Yangtze Craton

Sm Nd isotopic compositions of associated amphibolites, TTG gneisses and granitic gneisses from the Archean Kongling Complex of the Yangtze Craton, South China are systematically analyzed. The results show that the amphibolites and TTG gneisses have a similar age of ca. 2 700 Ma, which well agrees with zircon U Pb dating of previous studies. However, their ε Nd ( t ) are different, suggestive of possible dissimilarity in source composition.     

浅议考古学中的相对年代与绝对年代

相对年代与绝对年代之间的区别,并不在于时间精确度的高低而在于所选参照点的不同。绝对年代必须以已知时间点或时间段为参照点,而相对年代的参照点则可能是未知时间点或时间段。     

两宋人物贬谪永州编年考

永州以其独特的地理位置,承接了一批又一批的流寓之人,而两宋时期尤为突出,此间贬于永者达47人之多。这一现象反映了两宋＂以文治特著＂的社会政治状况,同时也造就了永州独特的地方文化。     

试论古今字和通假字的区别

古今字和通假字，一直是传统语言文字学两个界限不清的术语。历代语言学家对两者的含义及区别曾作过一些有益探索，但至今尚未形成一个圆满而统一的答案。通过从字形、意义、时间三个角度来正确区分两者，澄清人们对两者的错误认识，从而使两个术语趋向科学化、标准化。     

商纣王的年代学研究——夏商周断代探索之二

商王征伐人方在十祀（１０年），联系３件其铜，证明帝辛（即商纣）十祀在公元前１１５４年或１０９２年。构建帝辛历谱的初步框架。     

Chronology and pattern of integration of tandem genomic islands associated with the tmRNA gene in <Emphasis Type="Italic">Escherichia coli</Emphasis> and <Emphasis Type="Italic">Salmonella enterica</Emphasis>

tmRNA,a combination of a tRNA-related fragment and a small mRNA fragment,was confirmed as the integration site of genomic islands(GIs).Using sequence alignment and comparative genomics,68 GIs associated with tmRNA genes were identified among 13 genera of Enterobacteriaceae.Among them,53 GIs were found in Escherichia coli and Salmonella enterica.Among these 53 GIs,tandem GIs were verified in eight S.enterica and two E.coli chromosomes.The downstream regions of the tmRNA genes in most of the E.coli and S.enterica chromosomes include one GI or tandem GIs region and a remnant variable region distal to the tmRNA.The chronology of integration of tandem GIs into the genome indicated that GIs farther from the tmRNA were incorporated into the genome earlier than those nearer from the tmRNA.The integrases of the tmRNA gene-associated GIs can be further categorized into three subtypes:HP1 integrases,PhiCTX integrases,and P4 integrases,which are the most predominant.The GIs were first integrated into the chromosome by the P4 integrase,subsequently by the PhiCTX integrase,and finally by the HP1 integrase.Thus,the tmRNA gene is an important site for investigating the genetics and evolution of tandem GIs.