Petrogenesis of Paleoproterozoic Luyashan charnockitic rocks in Shanxi Province: Constraints from Geochemistry and Nd isotope

Luyashan charnockite pluton mainly consists of monzonite, adamellite, charnockite and syenogranite, which are characterized by the enrichment of TiO2, P2O5, K2O, Zr, Nb, Y, Pb, La, Ce, Ba and a higher K2O/Na2O and depletion of MgO, CaO, Mg#, Th, U and lower Sr/Ba and Rb/Ba. The negative correlations between Zr, Nb, Ce and SiO2 are distinct from I-type granites. Iso-topically Luyashan charnockite plutons are relatively uniform in Nd isotope, displaying initial εNd(t) (-5.93 to -6.97) and Nd depleted mantle model ages (2.67 Ga to 2.78Ga). These features indicate that Luyashan charnockitic magma derived from pre-existing late Archean crustal sources and the partial melting of mafic granulites probably under exceptionally high temperature with CO2-rich fluid. The garnet is a main residual phase during the partial melting. The original dry charnockitic magma experienced crystal fractionation of pyroxene, plagioclase, apatite and ilmenite during early crystallization. The geochemical evidence suggests that the Luyashan charnockitic magma was probably generated in the post-collision thermal relaxation and uplift tectonic setting after the main collision ( - 1850 Ma) between the Eastern and Western continental blocks.     

Variations of organic carbon isotopic composition and its environmental significance during the last glacial on western Chinese Loess Plateau

The last glacial period is characterized by a cold and dry climate with low atmospheric CO2 concentration. The relatively arid climate and low CO2 concentration are favorable to the growth of C4 plants, but the low temperature limits the development of th…     

He and Ar isotope geochemistry of pyroxene megacrysts and mantle xenoliths in Cenozoic basalt from the Changle–Linqu area in western Shandong

We performed a combined study of He–Ar isotopes and element geochemistry for pyroxene megacrysts and mantle xenoliths from Cenozoic basalt in the Changle–Linqu area in western Shandong.The results are used to trace the evolution of subcontinental lithospheric mantle after destruction of the North China Craton.The3He/4He ratios of pyroxene megacrysts,websterite,and dunites are 7.0–7.7 Ra,7.4 Ra,and 7.0–7.7 Ra,respectively.They are related to the origin of host basalts,and are slightly lower than that of mid-ocean ridge basalts(MORB).Their40Ar/36Ar ratios are much lower than that of MORB and close to that of air.The lherzolites and wehrlites represent the fragments of the newly accreted lithospheric mantle,and their REE and trace elements indicate that they experienced melt metasomatism and partial melting.The3He/4He ratios of their olivine are slightly lower than that of MORB,but3He/4He ratios of their clinopyroxene are low(2.3–7.1 Ra)and display an inverse correlation with(La/Yb)N.The40Ar/36Ar ratios of these clinopyroxene are much lower than that of MORB and close to the air ratio.Combining existing studies of petrology,Sr–Nd–Pb isotopes,O isotopes,trace elements,and Mg isotopes,we infer that the juvenile lithospheric mantle in the Changle–Linqu area was metasomatized by oceanic crust-derived melts,which transfer the supracrustal Ar isotope signatures to the mantle sources.The low4He abundance and low3He/4He ratios of clinopyroxene in the lherzolites and wehrlites are ascribed to metasomatism by crustal melts from the subducted Pacific plate.     

Laserprobe oxygen isotope analysis of minerals from mantle-derived rocks in eastern China

Oxygen isotope analyses were carried out by the laserprobe technique for mineral separates from mantle xenolith and megacryst in Cenozoic basalts, East China. The results not only give the δ I8O range consistent with that reported for peridotites in the world, but also yield oxygen isotope equilibrium between coexisting minerals.     

几种获取1.8 K超流氦方案的对比分析

针对如何获得1．8K的超流氦提出了直接节流、预冷与节流相结合、抽真空以及抽真空与节流过程相结合的4种方案,同时针对各个方案给出了过程进行的温-熵图、流程简图以及实现过程的主要设备,借助于各个方案进行过程的温-熵图,对这4种方案进行了详细的对比分析和计算,确定了各个方案最终可以获得的超流氦液体率．抽真空及抽真空与节流过程相结合的方案最终获得的超流氦液体率分别约为100％、90．3％,但这两种方案所需要的设备比较复杂,成本较高,直接节流方案和节流与预冷相结合的方案要求的设备相对比较简单,但直接节流方案没有利用低温饱和超流氦蒸汽的冷量,而节流与预冷相结合的方案利用低温饱和超流氦蒸汽的冷量进行预冷,使其最终的超流氦液体率与直接节流方案相比提高了近12％。     

自引力反应扩散系统的涨落

根据非平衡态统计理论,获得了描述自引力反应扩散系统密度涨落的广义Master方程,通过分析红巨星中心氦核反应扩散系统的涨落,认为尺度大于临界波入区域内的氦核反应从引力上讲是不稳定的,一系列大小长涨落波将随时间指数增长。     

浮空器副气囊体积对环境适应性的影响分析

副气囊是浮空器的重要组成部分,其内部填充空气,通过充气或放气维持浮空器气囊内外压差在安全范围内,从而保证浮空器在空中长时间连续安全地工作。本文通过理论推导,建立了浮空器副气囊体积的数学模型,并对浮空器副气囊体积对环境适应性的影响进行了仿真分析。结果表明,本文方法对浮空器副气囊的设计有一定参考价值。     

Different climatic controls of soil δ 13Corg in three mid-latitude regions of the Northern Hemisphere since the Last Glacial period

Paleoecological records of soil δ^13Corg from three regions in the middle latitudes of the Northern Hemisphere, including the Chinese Loess Plateau （CLP）, the Great Plains and adjacent areas of North America and northwestern Europe, showed different variations since the Last Glacial period. An attempt was made to evaluate the causes for the difference in δ^13Corg on the basis of the modern climatic data collected in these regions and of the modern C3 and C4 plant distributions. The analysis indicates that temperature, especially the growing season temperature, has a dominant control on the growth of C4 plants. When the mean annual or growing season temperatures are below the ＂threshold value＂, the growth of C4 plants is limited. When the temperature is above the ＂threshold value＂, C4 plants can grow under a wide range of precipitation. However, when the precipitation is high enough to favor the growth of trees, the proportions of C4 plants in local biomass will decline. The implicit control factor recovered by sedimentary records is consistent with the control factor on modern C3/C4 distribution. Pure C3 plants have been dominating the local biomass since the Last Glacial period in European loess region, mainly owing to the low local temperature. The increases in C4 plants from the late Pleistocene to the Holocene in the Chinese Loess Plateau, the Great Plains and adjacent areas, mainly reflect the influence of increasing temperature.     

Stable isotopic compositions of precipitation events from Kathmandu,southern slope of the Himalayas

Investigation of temporal variations in the stable δ^18O and δD isotopes from Kathmandu＇s precipitation events shows that the relatively enriched δ^18O and δD values in the winter （the dry season, dominated by the westerlies） were positively correlated with temperature, indicating a temperature effect controlling the changes of δ^18O and δD. However, the δ^18O and δD values were depleted in the summer （the wet season, dominated by the Indian monsoon）, which were negatively correlated with precipitation amount, indicating an amount effect. In addition, the comparison of stable isotopes in precipitation from Kathmandu and Mawlong （near the Bay of Bengal） shows that the overall trends of δ^18O and δD values at Kathmandu generally approximate those at Mawlong. However, there remain many differences between the details of the isotopic changes at Kathmandu versus those at Mawlong. Compared with those at Mawlong, the further rainout effect and the more intense lift effect of the oceanic moisture by the high mountains resulted in the more depleted δ^18O and δD values in summer precipitation at Kathmandu. A deuterium excess and the local meteoric water lines reveal that evaporation at Kathmandu exceeds that at Mawlong. The data also show that the Indian monsoon activities at Mawlong are more intense than those at Kathmandu.     

相山矿田斑岩型铀矿床地球化学特征及成矿机制探讨

相山矿田北部多数铀矿床在时空和成因上与超浅成侵入相的花岗斑岩密切相关,可归属为斑岩型铀矿床.以横涧—岗上英、沙洲矿床为例,通过稀土元素、微量元素及C,O同位素地球化学特征研究,探讨铀成矿物质来源、成矿流体演化及成矿机制.研究表明,相山矿田火山岩系具同源性,是陆壳物质熔融的产物,火山岩浆在通向地表途中受到高度分馏的结晶作...