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Valentina G. Klochkova Eugene L. Chentsov Tonu Kipper Vladimir E. Panchuk Nonna S. Tavolganskaya Maxim V. Yushkin 《Astrophysics and Space Science》2011,335(1):83-89
We present a spectral atlas of 4 B and A stars containing spectra in a poorly studied spectral range of 305–452 nm. The atlas
is based on high resolution (R=60 000) spectra obtained with the 6 meter telescope (SAO, Russia) combined with the NES-spectrograph. The procedure of spectral
lines identification and compilation of the atlas is discussed in detail. Using the spectral data we thoroughly investigated
the velocity field in expanding atmospheres and envelopes of hot evolved stars β Ori, α Cyg and supergiant KS Per with the extreme hydrogen deficiency. The complete atlas and list of the identified spectral lines
will be available via the astronomical database SIMBAD. 相似文献
2.
海南岛屯昌晨星地区变基性岩体变质特征及构造意义 总被引：1，自引：2，他引：1
海南岛屯昌晨星地区变基性岩体原岩可能包括辉长岩(粗粒的斜长角闪岩)、辉长-辉绿岩(中细粒和中粗粒的斜长角闪岩)和枕状熔岩(细粒或块状斜长角闪岩)。由于受多期变质和蚀变作用的影响,组成这些岩石的多数矿物如角闪石、斜长石和绿泥石等常表现两个或两个以上的世代。角闪石环带矿物化学分析表明,从核到边,钛、铝、(钠 钾)含量增长,反映了压力和温度同时升高的进变质演化过程;相反,角闪石环带从核部到边部钛、铝和钾 钠含量降低,则暗示温度和压力同时降低而进入另一个退变质演化阶段。所获得的 Sm-Nd 全岩及角闪石的内部等时线年龄为128±12 Ma、Rb-Sr 全岩等时线年龄分别为131.8±6.2 Ma和344±11Ma。根据角闪石环带、矿物共生组合、微结构以及变质温压条件的半定量计算和同位素定年,屯昌晨星地区变基性岩体的变质作用可能经历了三个演化阶段。第一阶段(～527～450 Ma)可能记录了与洋底变质作用有关的(亚)绿片岩相至角闪岩相条件,早期的阳起石、钙质角闪石及镁铁质角闪石残余核为该阶段的产物;第二阶段(～330～240 Ma)进变质作用达到高峰的P=～0.9 GPa、T=～700℃,显示了过渡的高角闪石相-麻粒岩相变质条件。广泛的剪切变形及韭闪质普通角闪石-韭闪石边是该阶段的产物;第三阶段(～130 Ma～90 Ma)显示一个绿片岩相变质条件(P=～0.1～0.3 GPa、7=～300～400℃),可能与区域/热接触变质有关。因而屯昌晨星地区变基性岩体的变质作用演化显示了一个逆时针 P-T-t 轨迹,最可能与古太平洋板块俯冲导致的大陆边缘裂解及洋壳化和随后的年轻洋壳消亡、陆(华南大陆)-陆(印支板块)碰撞事件有关。 相似文献
3.
海南岛北西部邦溪地区奥陶纪火山-碎屑沉积岩岩石学、矿物学和地球化学:源区及构造环境暗示 总被引：5，自引：0，他引：5
海南岛奥陶纪火山-碎屑沉积岩矿物、地球化学成分与源区岩性质和沉积构造环境密切相关.岩相学观察和矿物化学分析表明,所研究的岩石主要碎屑矿物由石英、绿泥石(Si:5.8～6.2 a.p.f.u.、Mg/(Mg Fe):～0.45)和自色云母(Si:6.2～6.8 a.p.f.u.、Al:4.5～5.7 a.p.f.u.)组成,含少量的长石(主要为钾长石)、黑云母(Mg/(Mg Fe)=0.43、TiO2=0.01%)和磷灰石等矿物.地球化学特征上,这些岩石普遍具有高SiO2含量(Al2O3/SiO2=0.07～0.19)、相对高的K2O/Na2O比值(1.25～14.71)和高的FeOtotal MgO含量(普遍大于5%,最高达11.5%),但微量元素(含REE)含量普遍低于PAAS(NASC),且REE分布模式显示LREE富集((La/Yb)N=6.1～12.5)、Eu负异常或弱负异常(δEu=0.57～0.86).高的前交代CIA(～84)和PIA(～85)指数、A-CN-K分布模式以及可变的Th/U(2.9～25)比值还说明源区已经历强烈的化学和机械风化作用.低的Ce/Pb比值(2.1～2.8)则反映海南岛早古生代地壳已经历过Pb的富集事件.结合矿物化学成分和区域地质对比,研究区奥陶纪火山-碎屑沉积岩源区主要由变质的岩浆弧花岗闪长岩和弧长英质火山岩组成,少量的铁镁质成分不能排除,因而暗示一个从活动大陆边缘到被动大陆边缘的过渡性沉积构造环境.同时,推测海南岛在早古生代和晚古生代-早中生代可能分别存在一次俯冲增生-碰撞造山事件;海南岛(可能包括华夏地块)应于晚奥陶世后才脱离东冈瓦纳大陆的澳大利亚边缘. 相似文献
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Monika A. Kusiak Kazuhiro Suzuki Daniel J. Dunkley Janusz Lekki Nonna Bakun-Czubarow Mariusz Paszkowski Bartosz Budzy&#x; 《Gondwana Research》2008,14(4):675
Chemical Th–U–total Pb (CHIME) dating of monazite by electron probe microanalyzer (EPMA) and proton microprobe (PIXE) was carried out on felsic granulites from Stary Gierałtów, Poland, which represent part of the Orlica-Śnieżnik Dome in the NE Bohemian Massif. Analyzed monazite is characterized by mosaic zoning rather than simple core-to-rim growth, and strontium contents of up to 750ppm. An isochron age of 347 ± 13Ma represents timing of amphibolite-facies metamorphism, in agreement with previously published estimates. 相似文献
5.
The Shilu iron ore deposit, located in the western Hainan Province, South China, is one of the most important iron-ore mining districts in China not only for its huge reserves of hematite- rich ores, but also for its potentially economic significance of associated metals of copper, cobalt, nickel, silver, lead and zinc, and of non-metals of dolomite, quartzite,barite,gypsum and sulfur. 相似文献
6.
D. Xu B. Xia N. Bakun-Czubarow R. Bachlinski P. Li G. Chen T. Chen 《Mineralogy and Petrology》2008,92(3-4):361-391
Summary The metabasites in Tunchang area, East-central Hainan Island, South China generally display strongly LREE-depleted patterns,
extremely low HFSE concentrations and relatively high LILE contents; a few boninite-like samples have a concave-up, slightly
LREE-enriched pattern. The low but variable Ti/V ratios between 6 and 20, and the high mg-numbers and Cr, Co, Ni contents,
are indicative of plume-influenced intraoceanic arc magmas. It accord with this model are moderately high ɛNd(t) values ranging from +2.16 to +6.75, and 87Sr/86Sri values ranging from 0.70239 to 0.70824. These geochemical features imply that the protoliths for the Tunchang area metabasites
are relics of an intra-oceanic island arc and the parental melts of these rocks were generated from a depleted, primitive
mantle arc source rather than from a N-MORB source in a supra-subduction zone-like setting. The minor geochemical differences
between the two identified groups of metabasites are due to a combined result of the variable degree of partial melting and
the crystal fractionation of clinoproxene ± olivine ± plagioclase.
The Tunchang area metabasites are distinctive in geochemical and isotopic compositions, and likely also in age from the Bangxi
area metabasites in the northwestern part of Hainan Island. We assume that the NE–SW trending Baisha Fault Zone likely marks
an early suture zone due to the collision of an Early Paleozoic intra-oceanic arc with the South China continent. In contrast,
the Bangxi area metabasites more likely are formed in an extensional back-arc basin due to subduction of the Paleo-Tethys
beneath the South China continental margin during the Late Paleozoic.
Present address: Chinese Academy of Sciences, Guangzhou Institute of Geochemistry, Guangzhou, Guangdong Province 510640, People’s
Republic of China
Authors’ addresses: Deru Xu, Bin xia, Pengchun Li, Guanghao Chen, Tao Chen, Key Lab of Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou Institute of Geochemistry, Guangzhou, Guangdong
Province 510640, People’s Republic of China; Bakun-Czubarow Nonna, Bachlinski Robert, Polish Academy of Sciences, Institute of Geological Sciences, Institute of Geological Sciences, ul. Twarda 51/55, 00-818
Warszawa, Poland 相似文献
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