内蒙古温都尔庙地区温都尔庙群的形成环境和构造意义   总被引：7，自引：1，他引：6  

吴泰然  张臣 《高校地质学报》1998,4(2):168-176

内蒙古温都尔庙地区有一套统称为温都尔庙群的变质岩系,该岩系主要由两种不同的岩石组合组成：一套是出露于乌兰沟一带的浅变质岩系,主要由变玄武岩、硅质岩、火山碎屑岩、碎屑岩组成的基性火山岩－碎屑岩组合;另一套是出露于德言其庙一带的深变质岩系,主要由斜长角并岩、斜长片麻岩组成。这两套岩石组合在变形变质、岩石化学和形成环境等方面都有很大的差异,前者主要表面出弧后盆地的特征,后者则是拉张过程中板底垫托的产物,它们分别代表了华北板块北缘中元古代不同构造演化阶段的产物。  相似文献   

论赣西北中元古界双桥山群构造样式地层序列及地质意义     

章泽军  曾佐勋  张雄华 《地质通报》1998,(4)

赣西北地区双桥山群自上而下划分为修水组、安乐林组,共计１１个岩性段,其时代属中元古代蓟县纪,并以近东西向褶皱叠加早期近南北向褶皱为主要变形样式。就该群构造样式、地层序列、变质温压条件以及沉积环境等进行简要论述与综合分析,在此基础上对本区长期争议的“修水运动”作出了否定的回答。  相似文献   

The globular cluster system of the Sagittarius dwarf spheroidal galaxy: the age of Terzan 8     

Montegriffo  Bellazzini  Ferraro  Martins  Sarajedini  & Fusi Pecci 《Monthly notices of the Royal Astronomical Society》1998,294(2):315-326

We present deep V - and I -band CCD photometry of the globular cluster Terzan 8, recently found to be a member of the globular cluster system of the Sagittarius dwarf spheroidal galaxy. We accurately estimate the metallicity of Terzan 8, and provide the first direct determination of the colour excess toward this cluster. Our robust age estimate confirms that this cluster is indeed coeval with typical Galactic globulars of comparable metal content, and thus it is probably significantly older than at least two other Sagittarius clusters, Terzan 7 and Arp 2. The implications of this result on the star formation history of the Sagittarius galaxy are briefly discussed.  相似文献   

胶东早元古代荆山群变质作用演化样式及其构造环境探讨   总被引：1，自引：0，他引：1  

董永胜  王微 《世界地质》1998,17(3):1-8

胶东地区发育大面积的早无古代变质地层──荆山群。该套岩系经历了三期五个阶段的变质作用,峰期温压条件为T＝700～750℃,p＝0．50～0．60GPa,达角闪麻拉岩相。变质作用pTt轨迹为逆时针形式,反映早元古代陆缘壳内裂陷带的闭合过程。  相似文献   

Evolution of three unconformity‐bounded sandy carbonate successions in the McArthur River region of northern Australia: The Lawn,Wide and Doom Supersequences in a proximal part of the Isa Superbasin     

M. J. Jackson  P. N. Southgate 《Australian Journal of Earth Sciences》2013,60(3):625-635

Gamma‐ray curves from surface outcrops together with U–Pb SHRIMP zircon dating are used to redefine the evolution of a Palaeoproterozoic sandy dolostone succession from northern Australia. This case history indicates that gamma‐ray logging of surface sections should accompany lithostratigraphic logging or an inadequate interpretation of stratigraphic evolution is a likely outcome. The 1200 m‐thick Nathan Group from the McArthur River area had previously been interpreted as a more‐or‐less continuous package of carbonates deposited in lacustrine and associated shallow‐water environments. Now it is seen to comprise the preserved remnants of three truncated, second‐order supersequences—the Lawn, Wide and Doom Supersequences—each a few hundred metres thick and each deposited over a time period of a few million years. These supersequences are separated by major stratigraphic breaks each approaching probably 10 million years duration. Each supersequence comprises several third‐order sequences which themselves contain higher‐order cycles. These were deposited in a series of continental, shoreline, and inner to outer carbonate platform environments. Transgressive, high‐energy, fluvial to marginal marine, mixed clastic‐carbonate facies dominate most of the sequences. The middle, Wide Supersequence, however, preserves deeper water (mostly sub‐storm‐wave‐base) stromatolitic facies in one sequence, and storm‐reworked clastics in another. These are interpreted as condensed intervals deposited around their respective maximum flooding surfaces and are succeeded by regressive facies that probably represent highstand systems tracts. New correlations between these 1615–1575 Ma sandy carbonate successions of the McArthur Basin (Amos, Balbirini and Dungaminnie Formations) and time‐equivalent largely clastic successions in the Lawn Hill area (Lawn Hill and Doomadgee Formations), some 400 km to the southeast, are proposed.  相似文献   

Constrained simulations of the local universe – I. Mass and motion in the local volume     

Luis A. Martinez-Vaquero  Gustavo Yepes  Yehuda Hoffman 《Monthly notices of the Royal Astronomical Society》2007,378(4):1601-1608

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Reconstruction of protoliths of metamorphic rocks and tectonic setting of Wolegen Group     

Lizhi LUO  Wei JIN  Changqing ZHENG  Xianli YANG 《世界地质(英文版)》2007,10(1)

Parametamorphic rocks from Arong County in southeastern Inner Mongolia-Daxinganling district are regarded as Proterozoic in age,belonging to the Wolegen Group and composed of volcanoclastic and sandstone in origin,and have been disputed in tectonic setting.Because of the stability in metamorphism,the rare earth dements indicate the features of their protoliths.The authors integrated the petrologic methods with the geochemical parameters which include ∑REE,∑LREE/∑HREE,δCe,δEu,La/Yb,Sm/Nd,Th/Sc and the standard values of chondrite.The results show that the protoliths of Wolengen Group may be a group of voleanoclastic and continental margin elastic rocks,and their tectonic setting is the continent island arc.  相似文献   

辽南早元古宙变质热液型金矿床成矿机理探讨     

戴立军  樊秉鸿 《国土资源》1990,(2)

辽南早元古宙辽河群变质岩系中的金矿床为变质热液成因金矿床,矿床的形成与吕梁期变质变形作用关系密切。金矿化带的展布与金矿体的产出受韧性剪切带控制。剪切带内岩石具有明显的动态性组构特征,直接赋矿围岩为辽河群盖县组糜棱岩化千枚岩、变砂岩及云母石英糜棱岩等。韧性剪切带为含矿流体的运移提供通道。作者定义这类金矿床为变质热液型含金剪切带金矿床。  相似文献   

Metallicity and kinematical clues to the formation of the Local Group     

R.F.G. Wyse 《Astronomische Nachrichten》2010,331(5):526-534

The kinematics and elemental abundances of resolved stars in the nearby Universe can be used to infer conditions at high redshift, trace how galaxies evolve and constrain the nature of dark matter. This approach is complementary to direct study of systems at high redshift, but I will show that analysis of individual stars allows one to break degeneracies, such as between star formation rate and stellar Initial Mass Function, that complicate the analysis of unresolved, distant galaxies (© 2010 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

中祁连东段化隆群中斜长角闪岩地球化学特征及构造意义   总被引：2，自引：0，他引：2  

高晓峰  李文渊  叶美芳  郭周平 《岩石矿物学杂志》2010,29(5):507-515

中祁连东段化隆群中斜长角闪岩岩相学特征及主、微量元素地球化学分析结果显示,其原岩为碱性玄武岩。斜长角闪岩表现出轻稀土元素富集、Nb-Ta不亏损,与典型洋岛玄武岩(OIB)的微量元素分布模式和特征元素比值(Nb/La=1.24～1.48,Th/Ta=1.19～1.40)类似,但与典型OIB相对亏损高场强元素(如Th、Nb)不同,且在大地构造环境判别图上落入板内大陆玄武岩区,反映了化隆群斜长角闪岩原岩来源于软流圈地幔交代大陆岩石圈地幔熔融源区,为Rodinia超大陆在新元古代汇聚过程中局部裂解或Rodinia大陆整体上汇聚未完成局部地区就开始裂解的产物。  相似文献