Zircon U–Pb Ages and Lu–Hf Isotope of the Dongchuan Group in Central Yunnan, China, and their Geological Significance     

HAN Kunying  ZHANG Heng  DING Xiaozhong  REN Liudong  SHI Chenglong  PANG Jianfeng 《《地质学报》英文版》2020,94(4):1093-1116

On the southwestern margin of the Yangtze Block, the Dongchuan Group consists of slightly metamorphosed sedimentary rocks, including silty slate, argillaceous slate, clayey slate, arkose, dolomite, and minor volcanic rocks. To date, it is still a controversy over the depositional age and stratigraphic sequence of the Dongchuan Group. In this study, we analyzed five samples of meta-sedimentary rocks and one sample of meta-tuff from the Yinmin, Luoxue and Etouchang Formations of the Dongchuan Group in the Yuxi region for detrital zircon U-Pb ages and Lu-Hf isotope. The detrital zircon ages of the meta-sediments vary from 3073 to 1703 Ma, mainly clustered at three periods, from 1889 to 1840, 2490 to 2008 and 2878 to 2844 Ma. The youngest age peak of all the samples is ～1859 Ma, with the εHf(t) values of the zircons ranging from-20.3 to +4.3 and more than 90% being negative, indicating that the Paleoproterozoic crustal accretion on the southwestern margin of the Yangtze Block was dominated by reworking of the ancient crustal materials involved in the assembly and breakup of the Columbia supercontinent. Another important age range is between 2490 Ma and 2008 Ma, with εHf(t) values from-14.7 to +8.9 and 70% of them are negative, suggesting that the magmatism in the source area was also dominated by reworking and recycling of the ancient crustal materials, with minor juvenile mantle substances added. The detritus was probably derived from the Paleoproterozoic crystalline basement in the southern Yuxi region. The oldest peak age is ～2847 Ma and the εHf(t) values are from-7.7 to +7.0 with 50% of both positive and negative values, demonstrating a possible ～2.85 Ga ancient continental nucleus on the southwestern margin of the Yangtze Block and substantial growth in juvenile crust materials during this period. Besides, the weighted average age of the zircons from the meta-tuff of the Etouchang Formation is 1677 ± 14 Ma. Combining the previous research data and this study, we can constrain the depositional age of the Dongchuan Group in central Yunnan Province to the period from the late Paleoproterozoic to early Mesoproterozoic, slightly earlier than that of the Dongchuan Group in the Dongchuan area near to the southwestern Sichuan Province. The depositional age of the Dongchuan Group is older than that of the Kunyang Group.  相似文献   

HST UV measurements of wind structure and velocities in Local Group OB stars     

Raman K. Prinja  & Paul A. Crowther 《Monthly notices of the Royal Astronomical Society》1998,300(3):828-836

Archival HST FOS and GHRS data sets have been used to collect ultraviolet evidence for large- and small-scale stellar wind structure in extragalactic Local Group OB stars (i.e. SMC, LMC including R136, M31, M33 and NGC 6822). By comparison with previous studies of Galactic OB stars, wind activity is principally diagnosed in individual spectrograms via the presence of 'narrow absorption components' and saturated 'black' absorption troughs in the resonance line doublets. Their characteristics broadly suggest that these stars share the same physical mechanisms for perturbing the winds as those that act in Galactic stars. Both of these spectral indicators are also used to provide reliable measures of wind terminal velocities. These velocities are directly compared with previously published Galactic values, without reliance on model profile fitting. Relative to Galactic OB stars, the most discrepant terminal velocities (and wind line profiles) result from main-sequence early O-type stars in the SMC.  相似文献   

湘东北—桂北中元古界岩石地球化学特征     

金文山  赵风清  王祖伟  甘晓春 《南方国土资源》1998,(1)

湘东北—桂北中元古代冷家溪群和四堡群的变玄武岩类显示过渡型拉斑玄武岩类的地球化学特征,变砂岩类和变泥岩类（绢云板岩类）显示大陆边缘的砂岩类和泥岩类的地球化学特征。根据岩石地球化学和沉积相（低密度流复理石建造）特征,推测湘东北冷家溪群和桂北四堡群主要形成于大陆边缘深水环境。  相似文献   

集团异化与亚太区域经济合作   总被引：2，自引：1，他引：1  

文云朝 《世界地理研究》1998,(1)

集团异化现象是集团化进程中的一种逆反行为,集中反映在经互会的解体和围绕“赫一伯法”而导致的北美集团成员国之间制裁与反制裁的公开对抗。冷战结束后这种现象异常活跃,而且具有广泛的世界意义。文章阐述了集团异化的概念和当代的集团异化现象和异化效应;分析了集团异化产生的国际背景与内因。作者进而指出,在新的国际形势下,集团异化构成为集团化进程中的一种新现象和新问题,并非偶然;最后探讨了它对于发展亚太区域经济合作的理论意义和现实意义。  相似文献   

内蒙古温都尔庙群变质基性火山岩Sm-Nd、Rb-Sr同位素年代研究   总被引：32，自引：1，他引：31       下载免费PDF全文

张臣  吴泰然 《地质科学》1998,33(1):25-30

温都尔庙群主要分布在内蒙古温都尔庙地区,该套地层是白乃庙-温都尔庙构造岩浆带的重要组成部分。长期以来,由于缺少古生物化石和可信的年龄数据,一般认为温都尔庙群属早古生代。本文对温都尔庙群变基性火山岩进行了Sm-Nd和Rb-Sr同位素研究,5件变基性火山岩全岩样品Sm-Nd和Rb-Sr等时线年龄分别为961±66Ma和624±110Ma,并对其形成时代和成因提出了一些新看法。  相似文献   

碧口岩群硅质岩成因及地质意义   总被引：1，自引：0，他引：1  

丁振举  姚书振 《矿物学报》1998,18(3):331-336

碧口块状硫化物矿床直接赋矿主岩硅质岩地质特征及常量、微量、稀土元素组成表明,碧口岩群硅质岩为同火山岩喷流热水沉积成因。碧口岩群硅质岩常量元素富Fe、贫Si,为典型热水沉积成因;其微量元素、稀土元素特征均与现代大洋热水沉积物相似。热水硅质岩Eu异常与古流体温度存在密切关系,Eu／Eu特征显示筏子坝、铜矿坡为较高温度喷流产物,而大茅坪、黑窝子、铜矿梁、周家坡则为较低温度下的产物。  相似文献   

扬子地块西南缘下震旦系火成岩系研究   总被引：9，自引：0，他引：9  

周朝宪  魏春生 《矿物学报》1998,18(4):401-410

研究区的天宝山组和苏雄组、开建桥组酸性、中酸性火山岩、火山碎屑岩同属下震旦系。它们及同期形成的花岗岩形成于后造山构造环境中,并非与裂谷活动有关。它们皆为S型,其源岩为太古界。  相似文献   

浙江景宁鹤溪群斜长角闪岩变质新生锆石特征、离子探针(SHRIMP)U-Pb年龄及地质意义   总被引：10，自引：0，他引：10  

陈多福  李献华  潘晶铭  董维权  陈光谦  陈先沛 《矿物学报》1998,(4)

景宁鹤溪群斜长角闪岩变质新生锆石特征是粒度均匀（约70μm）,晶体结晶和透明度极好,色调一致的淡粉红色,呈金刚光泽．未见裂隙、表面熔蚀、环带和核心构造。离子探针质谱GHRIMPⅡ）的206Pb／238U、207Pb／235U两组年龄在误差范围内基本谐和,206Pb／238U年龄的加权平均值（252±5Ma）为变质新生铁石的结晶年龄。锆石的精确定年（252±5Ma）为丽水—余姚断裂以东地区呈“天窗式”零星出露于中生代火山岩系中的鹤溪群提供了一个变质作用的确切年龄,也为印支运动在丽水—余姚断裂以东地区的存在提供了重要的年代学佐证。  相似文献   

通化集安群石榴子石和黑云母微区化学成分特征及其对变质作用p-T-t轨迹的指示意义     

卢良兆  靳是琴  胡大千  董永胜 《矿物学报》1998,(1)

集安群片麻岩中石榴子石和黑云母接触带两侧边缘广泛发育Fe－Mg交换反应所形成的扩散环带,但晶体内部各自保持变质峰期的成分,中温带石榴子石可保留生长环带。经微区化学成分详细研究后,正确运用Grt－Bt温度计获得进变质阶段,变质高峰期和修期后Fe－Mg交换反应停止时的温度条件。按石榴子石和斜长石的微区钙含量变化确定了峰期和退变质阶段压力。据此建立起逆时针形式的变质作用p－T－t轨迹,反映该区早元古代陆壳内裂陷带的闭合过程。  相似文献   

Upper Silurian–Middle Devonian radiolarian zones of the Yokokurayama and Konomori areas in the Kurosegawa Belt, Southwest Japan     

M. Umeda 《Island Arc》1998,7(4):637-646

Five radiolarian zones, from the Upper Silurian to Middle Devonian, are discriminated from the tuffaceous successions of the Joryu and Nakahata Formations of the Yokokurayama Group of the Yokokurayama area and the Konomori area in the Kurosegawa Belt, Southwest Japan. The definition of the zones is based on the first appearance biohorizon of the characteristic species. The zones are the Pseudospongoprunum sagittatum, Futobari solidus, Trilonche (?) sp. A, Glanta fragilis and Protoholoeciscus hindea zones, in ascending order. The preliminary age assignments for the zones are discussed on the basis of the comparison with other previous documented faunas. The age determination of the formations suggests the presence of unconformities and the episodic sedimentation of the tuffaceous strata in the Yokokurayama Group.  相似文献