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- 其他发明人请求不公开姓名
- 李军
- 李明
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- 刘勇
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- 王辉
- 李涛
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- 刘杰
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- 王健
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Joice Dias de Moraes;
Pedro Cordeiro;
Eduardo Abrahão Filho;
Juliana Rezende Oliveira;
Carlos Victor Rios da Silva Filho
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摘要:
Iron formations are valuable archives of sedimentary conditions and post-depositional events.However,geochemical proxies commonly used to determine genetic characteristics can be variably modified during metamorphism and deformation,hampering their use as records of regional geological events.This work focuses on strongly reworked magnetite-quartz-rich rocks from the São Josédo Campestre Massif,one of the oldest fragments of preserved crust in South America.The genetic classification of these magnetite-quartz-rich rocks is not straightforward because primary assemblages and textures were variably modified by granulite facies metamorphism during a regional Paleoproterozoic migmatization event.To address genetic ambiguities,we analyzed their magnetite and pyroxene chemistry,wholerock geochemistry,and Sm-Nd isotopes.Magnetite chemistry indicates that pyroxene-poor iron formations(Type B)are low in trace elements such as Ti,Al,V,and Mn,suggesting a chemical similarity to iron formations elsewhere.In contrast,magnetites from pyroxene-enriched Type A iron formations are rich in trace elements and more akin to magnetite crystallized from higher temperature systems,such as skarn and IOCG.The^(147)Sm/^(144)Nd of these rocks show substantial variation even at the outcrop scale,indicating a locally-controlled,highly heterogeneous mixture of Archean,Paleoproterozoic,and Neoproterozoic sources.Therefore,our geochemical tools point out to heterogenous signatures of these magnetitequartz rocks and proxies compatible with both low and high-temperature conditions and age of deposition spanning sources from the Archean to the Neoproterozoic.We interpret that the studied São Josédo Campestre magnetite-quartz rocks represent Archean iron formations with original magnetite chemistry and isotopic signatures variably modified by metamorphism and by at least one deformation-related hydrothermal event.These results contrast with similar examples from China and Greenland where iron formations either preserved the magnetite chemistry or the primary isotopic signatures.Our study indicates that metamorphism can selectively affect chemical proxies used to study iron formations and undermine the genetic classification of iron ores.Thus,these proxies should be carefully applied in the interpretation of syn-depositional environments of polydeformed belts.
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摘要:
【夏日阳光】夏日的阳光,叶子微微被风吹着。zkx,能成为你的白扁豆,是我的幸运,和你坐在一起很开心,和你待在一起感到很放松愉悦。春天再美也比不上你的笑,没见过你的人自然不会明了。希望友谊99!From xzq(158****7178)。
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HE Sheng;
LI Ziying;
GUO Dongfa;
WANG Yongjian;
ZHANG Chuang;
GUO Jian;
FAN Zengwei
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摘要:
Objective The Hengjian uranium deposit is a typical hydrothermal deposit in the Xiangshan uranium ore field.The uranium mineralization ages of the Xiangshan deposits are poorly constrained,and only a few mineralization ages using the pitchblende U–Pb method have been published.These ages are commonly discordant and dispersed for abundant inclusions and an open U–Pb system.Zircon grains after strong hydrothermal alteration are usually characterized by high common Pb contents,and their U–Pb isochron ages recorded the hydrothermal alteration event without interference of common Pb components.The Hengjian gray/grayish-green granite porphyry experienced strong alteration by hydrothermal fluids during the pervasive uranium mineralization in the Xiangshan uranium ore field.Uranium mineralization in the Hengjian deposit may had different stages,and strong hydromicatization alteration occurred at a relatively early stage.Their altered zircon U–Pb isochron ages possibly represent relatively early mineralization age of the Xiangshan uranium deposits.Altered zircon grains from the Hengjian granite porphyry were analyzed using the secondary ion mass spectrometry(SIMS)U-Pb method in this study,and U–Pb isochron ages were measured to constrain the relatively early mineralization age of the Hengjian uranium deposit.
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MA Xu;
CHEN Bin;
CHEN Jiafu
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摘要:
Objective Though the Central Asian Orogenic Belt (CAOB) is characterized by widespread Phanerozoic crustal growth,there is little juvenile crust documented in its southeastern segment,northern margin of the North China Craton(NCC)(Zhang et al,2007,2009).Late Carboniferous Dongwanzi ultramafic-mafic cumulate complex occurs in northern margin of the NCC and is intruded by a syenite with depleted Sr-Nd isotopes (Ma et al.,2014).However,the age and petrogenesis of this syenite is poorly constrained.In this study,we present new petrological,zircon U-Pb and Hf isotopic data of the Dongwanzi syenite,in order to put insights on its formation age and petrogenetic relationship with cumulates.
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SUN Lei;
WANG Chenglong;
BIAN Xiongfei
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摘要:
Objective The Dayangshu Basin located in eastern Inner Mongolia,is one of the key areas for oil and gas exploration in the periphery of Songliao Basin.So far,this basin has been poorly explored,and the basic geological research is still weak,due to the lack of high-quality paleontologic and stratigraphic data.The previous oil and gas investigations were mainly focused on the Early Cretaceous strata.However,the Late Cretaceous Nenjiang Formation in the basin also has hydrocarbon potential according to the latest research.In recent oil and gas geological survey,palynological fossils have been discovered from the Nenjiang Formation in the Dayangshu Basin,providing new evidence for biostratigraphic division and correlation.
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LIU Siqi;
ZHENG Yuanchuan;
SHEN Yang;
HOU Zengqian;
WANG Lu;
WANG Zixuan
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摘要:
Objective The Beiya super-large Au-rich porphyry deposit(304 t Au,2.4 g/t Au)is located within the western Yangtze craton,to the southeast of the Sanjiang Tethyan Orogen(Fig.1).The ore-forming porphyry is adakitic,characterized by high Sr/Y and La/Yb ratios coupled with low Y and Yb contents,and is generally thought to be derived from partial melting of thickened mafic lower crust.The lower crust underneath the western Yangtze craton is mainly composed of ancient crust with Archean ages,juvenile crust resulting from the Neoproterozoic subduction(740–1000 Ma),and late Permian juvenile crust related to the Emeishan mantle plume.Which lower crustal end-member has played a critical role in genesis of the Beiya ore-forming porphyry can be constrained by zircon U-Pb ages of amphibolite xenoliths hosted in the ore-forming porphyry,because these xenoliths represent direct samples of the source.In this study,we present new zircon U-Pb ages of these amphibolite xenoliths to have insight into the nature of the Beiya adakitic porphyry source.
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摘要:
日前,2019 年劳伦斯·奥利弗奖(Laurence Olivier Awards)在伦敦皇家阿尔伯特音乐厅隆重举行。史蒂芬·达尔德里执导的戏剧《继承》(The Inheritance ),以及音乐剧《来自远方》(Come from Away )、《伙伴们》(Company)成为2019 年奥利弗奖的最大赢家。斩获4 项奥利弗奖的音乐剧《来自远方》,是一部由真实故事改编的音乐剧,讲述了加拿大纽芬兰省默默无闻的小镇甘德在“9·11”事件后,庇护了数千名滞留的航空公司乘客的故事。剧本和词曲皆由艾琳·桑科芙(IreneSankoff)和大卫·海恩(David Hein)夫妇操刀创作。
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钟翟1
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摘要:
盛夏未至,来自南太平洋的海风已经徐徐吹入。正在上海博物馆举行的"浮槎于海:法国凯布朗利博物馆藏太平洋艺术珍品展",是国内引进的首个较为完整地呈现大洋洲艺术的展览,以150件精彩纷呈的艺术品向人们讲述了来自太平洋波涛深处的美和往事。在澳大利亚大陆的北部,美拉尼西亚、密克罗尼西亚和波利尼西亚群岛如同千百颗珍珠穿成三层项链.
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- 长春理工大学
- 公开公告日期:2023.01.03
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摘要:
本发明涉及光纤耦合技术领域,尤其涉及一种高效率的叠阵型半导体激光器,包括激光源、光束整形组件、会聚透镜、鲍威尔棱镜组件和光纤;所述激光源发出的光束经过光束整形组件进行整形;整形后的光束经会聚透镜会聚,会聚后光束经过鲍威尔棱镜组件进行光束整形可以耦合进光纤的光束。本发明系统结构简单,便于操作,减少了操作步骤,光纤耦合效率达到84.3%。
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