Garnet and Zircon U-Pb Geochronology and Geochemistry Reveal Genesis of the Dafang Au-Pb-Zn-Ag Deposit, Southern Hunan     

JIANG Hu  KONG Hu  LIU Biao  TAN Fucheng  QIN Yixue  HUANG Jingang  ZHU Yu 《《地质学报》英文版》2024,98(3):717-735

Garnet is a primary mineral in skarn deposits and plays a significant role in recording copious mineralization and metallogenic information. This study systematically investigates the geochemistry and geochronology of garnet and zircon in the Dafang Au-Pb-Zn-Ag deposit, which represents prominent gold mineralization in southern Hunan, China. Garnet samples with distinct zoning patterns and compositional variations were identified using various analytical techniques, including Backscattered Electron (BSE) imaging, Cathodoluminescence (CL) response, textural characterization, and analysis of rare-earth elements (REE), major contents, and trace element compositions. The garnet was dated U-Pb dating, which yielded a lower intercept age of 161.06 ± 1.93 Ma. This age is older than the underlying granodiorite porphyry, which has a concordia age of 155.13 ± 0.95 Ma determined by zircon U-Pb dating. These results suggest that the gold mineralization may be related to the concealed granite. Two groups of garnet changed from depleted Al garnet to enriched Al garnet, and the rare earth element (REE) patterns of these groups were converted from light REE (LREE)-enriched and heavy REE (HREE)-depleted with positive europium (Eu) anomalies to medium REE (MREE)-enriched from core to rim zoning. The different REE patterns of garnet in various zones may be attributed to changes in the fluid environment and late superposition alteration. The development of distal skarn in the southern Hunan could be a significant indicator for identifying gold mineralization.  相似文献   

墨西哥湾扇贝稚贝对盐度的耐受力   总被引：18，自引：0，他引：18  

何义朝  张福绥  王萍  李宝泉 《海洋学报》1999,21(4):87-91

用壳高15～21mm的墨西哥湾扇贝(Argopecten irradians concentricus)稚贝作为实验材料,控制水温在16和24℃条件下进行对盐度的耐受力实验.实验结果表明,当温度在24℃时,稚贝存活的盐度范围为18.5～44.4,低盐度对稚贝的存活影响明显.稚贝可生长的盐度范围是21.2～41.0(日增长率r>4.0),适宜的生长盐度为24.0～32.0(日增长率r>8.0),其中26.0～28.0的盐度为最佳生长盐度.在16℃条件下,最初8h内,其生存盐度范围为17.4～46.4,但是48h后稚贝的存活盐度范围与24℃温度条件时无明显差别,显示出低温条件会使稚贝对极限盐度的反应速率减缓.当盐度处于接近极限范围时,盐度变化幅度过大易导致稚贝死亡.墨西哥湾扇贝对盐度的适应能力与原生境盐度有关,稚贝预先在盐度为19.5和44.9中适应9d后,再过度到14.3和48.5中,48h后,存活率为78.3%和100%,而若是从盐度为32中直接移到3和48.5中,48h后存活率分别为0和27.3%.显然,通过中间驯化或适应过程,稚贝会提高耐盐能力.此结果表明,在高温多雨的南方海域,应避免在易受淡水中冲击的河口、海湾区域开展墨西哥湾扇贝养殖.  相似文献   

南黄海及长江口附近海域绿潮暴发前期微观繁殖体的动态变化     

方松  王宗灵  李艳  傅明珠  范士亮  王晓  张晓红 《海洋学报(英文版)》2012,31(4):147-154

基于2011年3至5月对南黄海及长江口附近海域的水体与沉积物样品采集及实验室萌发培养实验,分析了绿潮暴发前期该海域微观繁殖体的时空分布特征。结果表明,在调查期间,南黄海水体中微观繁殖体空间分布趋势表现为近岸高远岸低,高值区主要集中在紫菜筏架养殖区附近海域,在122°30'E以东区域未发现有微观繁殖体存在。3,4,5月份该区域海水中平均微观繁殖体数分别为144 ,164和140株/dm³,最大值分别为278,426,和537株/dm³;南黄海沉积物中微观繁殖体数量分布范围介于19~127株/层,表层微观繁殖体数高于底层。长江口以北靠近江苏近岸区域有微观繁殖体存在,数量介于1~10株/dm³,31°N以南区域和河口内未发现有繁殖体分布,由此可排除黄海浒苔等绿藻微观繁殖体由长江水携带入海或来源于长江口南部海域。在春季绿潮暴发前开展该海域微观繁殖体的研究,可为查明绿潮发源地及早期发生发展过程提供基础资料,为预测和预警绿潮发生提供科技支撑。  相似文献   

A revised Palaeozoic apparent polar wander path for Southern Britain (Eastern Avalonia)     

Allan Trench  Trond H. Torsvik 《Geophysical Journal International》1991,104(1):227-233

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辽东半岛南部原生金刚石特征     

赵秀英 《国土资源》1988,(1)

辽东半岛南部金刚石在含矿程度不同的金伯利岩岩管中,其主要物理特征和包体成分等是不同的。富矿金伯利岩体中金刚石的特征是颜色种类较多,晶形复杂(以曲面菱形十二面体为主),颗粒粗大,蚀象发育;含包体成分复杂。贫矿金伯利岩体中的金刚石颜色种类少,晶形单一(以平面八面体为主),颗粒细小,蚀象不发育;包体成分简单。高温碱熔试验与热台测定结果表明金刚石晶体形态的演化过程,盆刚石从650℃开始熔解,即八面体晶棱和顶角出现钝化,在温度不断升高时八面体所有晶棱逐渐熔解变为晶面,进而形成曲面菱形十二面体。因此可以推断,金刚石曲面菱形十二面体的初始晶形应是八面体晶形。金刚石包体中的镁铝榴石与金伯利岩中斑晶镁铝榴石的化学成分是一致的,说明二者来自同一岩浆源。  相似文献   

Geochronology and geochemistry of early Paleozoic granitic and coeval mafic rocks from the Tannuola terrane (Tuva,Russia): Implications for transition from a subduction to post-collisional setting in the northern part of the Central Asian Orogenic Belt     

《Gondwana Research》2024

Early Paleozoic magmatism of the Tannuola terrane located in the northern Central Asian Orogenic Belt is important to understanding the transition from subduction to post-collision settings. In this study, we report in situ zircon U-Pb ages, whole rock geochemistry, and Sr-Nd isotopic data from the mafic and granitic rocks of the eastern Tannuola terrane to better characterize their petrogenesis and to investigate changing of the tectonic setting and geodynamic evolution. Zircon U-Pb ages reveal three magmatic episodes for about 60 Ma from ∼510 to ∼450 Ma, that can be divided into the late Cambrian (∼510–490 Ma), the Early Ordovician (∼480–470 Ma) and the Middle-Late Ordovician (∼460–450 Ma) stages. The late Cambrian episode emplaced the mafic, intermediate and granitic rocks with volcanic arc affinity. The late Cambrian mafic rocks of the Tannuola terrane may originate from melting of mantle source that contain asthenosphere and subarc enriched mantle metasomatized by melts derived from sinking oceanic slab. Geochemical and isotopic compositions indicate the late Cambrian intermediate-granitic rocks are most consistent with an origin from a mixed source including fractionation of mantle-derived magmas and crustal-derived components. The Early Ordovician episode reveal bimodal intrusions containing mafic rocks and adakite-like granitic rocks implying the transition from a thinner to a thicker lower crust. The Early Ordovician mafic rocks are formed as a result of high degree melting of mantle source including dominantly depleted mantle and subordinate mantle metasomatized by fluid components while coeval granitic rocks were derived from partial melting of the high Sr/Y mafic rocks. The latest Middle-Late Ordovician magmatic episode emplaced high-K calc-alkaline ferroan granitic rocks that were formed through the partial melting the juvenile Neoproterozoic sources.These three episodes of magmatism identified in the eastern Tannuola terrane are interpreted as reflecting the transition from subduction to post-collision settings during the early Paleozoic. The emplacement of voluminous magmatic rocks was induced by several stages of asthenospheric upwelling in various geodynamic settings. The late Cambrian episode of magmatism was triggered by the slab break-off while subsequent Early Ordovician episode followed the switch to a collisional setting with thickening of the lower crust and the intrusion of mantle-induced bimodal magmatism. During the post-collisional stage, the large-scale lithospheric delamination provides the magma generation for the Middle-Late Ordovician granitic rocks.  相似文献   

辽南金矿集中区卫星图像构造解译及构造控矿模型探讨   总被引：2，自引：0，他引：2  

吕贻峰  李江风  秦松贤 《国土资源遥感》1998,9(4):43-49

辽南地区是我国最重要的五大金矿床集中区之一,大、中、小型矿床、矿点众多,矿床类型复杂,控矿因素多样。与国内外大多数金矿一样,在诸多控矿因素中,构造变形因素最为重要,而且有其自身的变形特点和特殊的控矿类型。本文旨在着重讨论辽南这一特定的金矿集中产出地所具有的构造控矿特征和构造控矿模型,为研究大型金矿区或金矿群的形成条件提供借鉴。  相似文献   

Interannual variability in western US precipitation   总被引：6，自引：0，他引：6  

B. Rajagopalan  U. Lall 《Journal of Hydrology》1998,210(1-4):51-67

Low-frequency (interannual or longer period) climatic variability is of interest, because of its significance for the understanding and prediction of protracted climatic anomalies. Since precipitation is one of the key variables driving various hydrologic processes, it is useful to examine precipitation records to better understand long-term climate dynamics. Here, we use the multi-taper method of spectral analysis to analyze the monthly precipitation time series (both occurrence and amount) at a few stations along a meridional transect from Priest River, ID to Tucson, AZ. We also examine spectral coherence between monthly precipitation and widely used atmospheric indices, such as the central Northern Pacific (CNP) and southern oscillation index (SOI). This analysis reveals statistically significant ‘signals' in the time series in the 5–7 and 2–3 year bands. These interannual signals are consistent with those related to El-Niño southern oscillation (ENSO) and quasi-biennial variability identified by others.  相似文献   

The radiolarian assemblages of the Bonarelli Horizon in the Umbria-Marche Apennines and Southern Alps, Italy     

Giovanni Salvini  Marta Marcucci Passerini 《Cretaceous Research》1998,19(6):777-804

The Bonarelli Horizon is an important regional marker level in the Umbria-Marche Apennines. It is characterized by consisting of black bituminous shales that yield a distinctive radiolarian fauna. Black shales referable to the Bonarelli Horizon are also present in the Southern Alps. The horizon is of uniform lithology and contains radiolarian assemblages of late Cenomanian-early Turonian age throughout both the Umbria-Marche Apennines and Southern Alps. Several new radiolarian taxa have been recognised and described from the Bonarelli Horizon of both areas. Two new species are defined in this paper, namelySethocapsa bossoensisandXitus picenus.  相似文献   

Response of deep-sea ostracod assemblages to Late Cretaceous palaeoceanographical changes: ODP Site 689 in the Southern Ocean     

Stefan Majoran  Joen G.V. Widmark 《Cretaceous Research》1998,19(6):843-872

Twenty-six deep-sea ostracod species are described from the late Campanian to late Maastrichtian of ODP Site 689 in the Southern Ocean. Three are described as new:Cytherelloidea megaspirocostata,Agulhasina sudoceanicaandPennyella foveolata. Correspondence analysis identified three faunal sample groups. The first is mainly characterised byA. sudoceanica,Kirthesp. andCytherellasp. This is replaced, first temporarily (betweenc. 71 and 69 Ma) by a group mainly characterised byArgilloeciaspp. andC. megaspirocostata, possibly a consequence of a short-lived global palaeoceanographic event marked by increased ventilation and cooling of intermediate waters at site 689. It then reappears before finally being replaced by a third group largely characterised byEucytherecf.circumcostata,P. foveolataandDutoitella mimicaDingle. This final change is coeval with a marked increase in the faunal density of ostracods, probably owing to an increase in food supply. However, the oxygen isotopic records of benthonic foraminifera suggests that the replacement of the first ostracod group by the third is a result of the long term Maastrichtian cooling of intermediate waters at high latitudes. This replacement is also coeval with a gradual change in benthonic foraminiferal assemblages at site 689. It is suggested, therefore, thatPennyellaandDutoitellahad a greater potential of adapting to successively colder palaeoceanographical conditions thanAgulhasina. The former genera have a cosmopolitan deep-sea distribution today.  相似文献