辽北法库韧性剪切带变形及其区域构造意义     

王雷  刘俊来  滕超  常玉巧 《地质论评》2021,67(1):251-264

晚古生代—早中生代古亚洲洋板块俯冲华北板块在辽北法库地区形成大型产状近水平的韧性剪切带。剪切带发展伴随着多期幔源及壳源的岩浆侵入,侵入岩在韧性剪切作用下发生韧性变形,记录了韧性剪切带变形历史。详细的野外地质调查结合岩石的宏观变形、显微构造及石英c轴组构特征分析,揭示了法库韧性剪切带内五龙山杂岩、高丽沟杂岩、早期十间房超单元变形处于上盘向北的剪切作用之下,晚期十间房超单元岩石变形指示构造运动转变为上盘向南剪切。LA-ICP-MS锆石U-Pb分析结果显示高丽沟杂岩变形时间为264.7±3.6 Ma(MSWD=1.3),早期十间房超单变形时间为253.9±4.3 Ma(MSWD=3.3),晚期十间房超单元244.0±3.0 Ma(MSWD=1.9)。岩石地球化学特征表明早期十间房超单元及小房申岩体中部分岩石来源于部分熔融的岩石圈地幔。结合前人研究成果,我们认为华北板块北缘东段(辽北地区)晚二叠世(264.7~253.9 Ma)处于古亚洲洋板块俯冲华北板块作用之下;晚二叠世至早三叠世(253.9~244.0 Ma)构造体制转变为碰撞后伸展且逐渐停止,244.0±3.0 Ma碰撞后伸展逐渐结束;构造体制转变并逐渐结束的过程是壳幔共同作用的结果,暗示了古亚洲洋板块的俯冲板片断离、重力失衡,这标志着辽北地区古亚洲洋构造域演化结束。  相似文献   

Sex change and morphological transitions in a marine ectoparasite          下载免费PDF全文

Colt Cook  Pablo Munguia 《Marine Ecology》2015,36(3):337-346

The fitness of parasitic organisms is strongly driven by their ability to infect potential hosts. Although transmission to a host organism is a key component to the parasitic lifestyle, surviving and reproducing within a host poses additional challenges. Cymothoa excisa is a parasitic isopod that infects Atlantic croaker, Micropogonias undulatus, along the Texas coast and has evolved mechanisms to successfully survive and reproduce within its host. Cymothoa excisa is known to exhibit sex‐change strategies but limited information exists on morphological changes, reproductive output and the timing at which sex change becomes optimal. This study collected Atlantic croaker during a 22‐month survey period and identified parasite prevalence and intensity in the host fish population. Infection rates were constant throughout the year at 19.88% and intensity increased through the season up to a maximum of four parasites. Following collection, isopod morphological parameters were quantified for each life stage (including female, transitional, male and juvenile), identifying shape and size transitions through ontogeny and sex change. Transitional C. excisa isopods only occurred when only one isopod was present in a fish, suggesting that isopods change sex from male to female if they are the first to recruit to an uninfected host. As isopods transition to females they have a large increase in size, legs, and pleotelson (which influence fecundity and anchoring ability), whereas the gonopod, eyes and uropod show a reduction (which are no longer needed for swimming and finding hosts). Data suggest that C. excisa sex change is related to the timing of infection and brood size increases with female size and host size. Therefore, it would be advantageous to be the first isopod to infect a host, as it could change into a female and increase reproductive potential. We discuss hypotheses that could explain the mating behavior of parasitic isopods.  相似文献   

Five supernova survey galaxies in the southern hemisphere. I. Optical and near-infrared database     

A. A. Hakobyan  A. R. Petrosian  G. A. Mamon  B. McLean  D. Kunth  M. Turatto  E. Cappelaro  F. Mannucci  R. J. Allen  N. Panagia  M. Della Valle 《Astrophysics》2009,52(1):40-53

The determination of the supernova (SN) rate is based not only on the number of detected events, but also on the properties of the parent galaxy population. This is the first paper of a series aimed at obtaining new, refined, SN rates from a set of five SN surveys, by making use of a joint analysis of near-infrared (NIR) data. We describe the properties of the 3838 galaxies that were monitored for SNe events, including newly determined morphologies and their DENIS, and POSS-II/UKST I, 2MASS and DENIS J and K_s and 2MASS H magnitudes. We have compared 2MASS, DENIS and POSS-II/UKST IJK magnitudes in order to find possible systematic photometric shifts in the measurements. The DENIS and POSS-II/UKST I band magnitudes show large discrepancies (mean absolute difference of 0.4 mag.), mostly due to different spectral responses of the two instruments, with an important contribution (0.33 mag rms) from the large uncertainties in the photometric calibration of the POSS-II and UKST photographic plates. In the other wavebands, the limiting near infrared magnitude, morphology, and inclination of the galaxies are the most influential factors which affect the determination of photometry of the galaxies. Nevertheless, no significant systematic differences have been found between any pair of NIR magnitude measurements, except for a few percent of galaxies showing large discrepancies. This allows us to combine DENIS and 2MASS data for the J and K_s filters. Published in Astrofizika, Vol. 52, No. 1, pp. 47–62 (Februay 2009).  相似文献   

四川攀西地区几个小型镁铁-超镁铁岩体含矿性的铂族元素示踪   总被引：2，自引：0，他引：2  

官建祥  宋谢炎 《矿床地质》2010,29(2):207-217

峨眉山大火成岩省内带,四川攀西地区的杨合伍、黄草坪和清水河等镁铁-超镁铁岩体分布在南北向的安宁河断裂和磨盘山-元谋断裂之间。分析表明,这些岩体无矿岩石与金宝山、杨柳坪、力马河等含矿岩体无矿岩石具有相似的铂族元素组成,普遍较高的Cu/Pd比值暗示这些岩体的母岩浆在侵入到目前层位前经历过硫化物熔离作用。定量模拟计算表明,原始岩浆经过大约0.01%的硫化物熔离作用形成了杨合伍岩体母岩浆,经过0.035%硫化物熔离形成了黄草坪和清水河岩体的母岩浆。根据硫化物熔离情况,认为杨合伍等岩体底部可能形成Ni-Cu-(PGE)硫化物矿床,而黄草坪和清水河岩体之下及附近可能存在Ni-Cu硫化物矿化的岩体。  相似文献   

蒙古国额尔登特特大型铜-钼矿床年代学与成因研究   总被引：7，自引：0，他引：7  

江思宏  聂凤军  苏永江  白大明  刘翼飞 《地球学报》2010,31(3):289-306

额尔登特铜钼矿床是20世纪60年代蒙古国发现的一处特大型斑岩型矿床。本文对矿区内的含矿斑岩体-石英闪长岩开展了锆石SHRIMP和LA-MC-ICP-MS同位素测年。分析结果表明, 含矿岩体形成时代在240 Ma左右, 这与矿石中辉钼矿的Re-Os等时线年龄(241.0±3.1 Ma, MSWD值为1.02)大体一致, 表明成岩成矿作用均发生在早三叠世末至中三叠世初。矿区范围内侵入岩体岩石地球化学研究表明, 石英闪长岩、花岗闪长岩和安山岩以及煌斑岩均可能是同源岩浆演化产物, 形成于岛弧环境, 成岩物质来源较深, 可能来自地幔或者熔融的年轻下地壳。硫、铅同位素和锇同位素初始比值显示, 成矿物质主要来自含矿侵入岩体, 但是也有其它来源。额尔登特斑岩型铜-钼矿床的成矿作用与蒙古?鄂霍次克洋的闭合所导致的构造-岩浆活动有关。  相似文献   

Geochemical Characteristics of the Sandstone—type Uranium Deposits in Northern Sichuan Province     

王旺章  张筑凤 《中国地球化学学报》1995,14(2):152-159

Described in detail in this paper are the geochemical characteristics of the sandstone-type uranium deposits in northern Sichuan Province .Favorable and unfavor-able conditions for the enrichment of uranium are explored on the basis of the elemental abundances and ratios of U,Th and K determined by gamma-ray spectroscopy. Gamma-ray spectroscopic(U, Th and K) and XRF analyses(As, Ba) are helpful to distinguish U-bearing light-colored sandstones from U-barren light-colored ones and red sandstones (red claystone) from light-colored sandstones. Therefore, the favorable target area for prospecting the sandstone-type uranium deposits can be difined in northern Sichuan Province.  相似文献   

Geochemistry of cumulates from the Bjerkreim–Sokndal layered intrusion (S. Norway) Part II. REE and the trapped liquid fraction     

Bernard Charlier  Jacqueline Vander Auwera  Jean-Clair Duchesne 《Lithos》2005,83(3-4):255-276

Rare earth elements in bulk cumulates and in separated minerals (plagioclase, apatite, Ca-poor and Ca-rich pyroxenes, ilmenite and magnetite) from the Bjerkreim–Sokndal layered intrusion (Rogaland Anorthosite Province, SW Norway) are investigated to better define the proportion of trapped liquid and its influence on bulk cumulate composition. In leuconoritic rocks (made up of plagioclase, Ca-poor pyroxene, ilmenite, ±magnetite, ±olivine), where apatite is an intercumulus phase, even a small fraction of trapped liquid significantly affects the REE pattern of the bulk cumulate, together with cumulus minerals proportion and composition. Contrastingly, in gabbronoritic cumulates characterized by the presence of cumulus Ca-rich pyroxene and apatite, cumulus apatite buffers the REE content. La/Sm and Eu/Eu* vs. P₂O₅ variations in leuconorites display mixing trends between a pure adcumulate and the composition of the trapped liquid, assumed to be similar to the parental magma. Assessment of the trapped liquid fraction in leuconorites ranges from 2 to 25% and is systematically higher in the north-eastern part of the intrusion. The likely reason for this wide range of TLF is different cooling rates in different parts of the intrusion depending on the distance to the gneissic margins. The REE patterns of liquids in equilibrium with primitive cumulates are calculated with mass balance equations. Major elements modelling (Duchesne, J.C., Charlier, B., 2005. Geochemistry of cumulates from the Bjerkreim–Sokndal layered intrusion (S. Norway): Part I. Constraints from major elements on the mechanism of cumulate formation and on the jotunite liquid line of descent. Lithos. 83, 299–254) permits calculation of the REE content of melt in equilibrium with gabbronorites. Partition coefficients for REE between cumulus minerals and a jotunitic liquid are then calculated. Calculated liquids from the most primitive cumulates are similar to a primitive jotunite representing the parental magma of the intrusion, taking into account the trapped liquid fraction calculated from the P₂O₅ content. Consistent results demonstrate the reliability of liquid compositions calculated from bulk cumulates and confirm the hypothesis that the trapped liquid has crystallized as a closed-system without subsequent mobility of REE in a migrating interstitial liquid.  相似文献   

Age and petrogenesis of plagiogranite intrusions in the Ankara mélange, central Turkey     

Yildirim  Dilek  Peter  Thy 《Island Arc》2006,15(1):44-57

Abstract   The Ankara mélange within the Izmir–Ankara–Erzincan suture zone in north-central Turkey includes ophiolitic fragments that represent the remnants of an oceanic basement evolved between the Sakarya and Kirsehir continental blocks in the early Mesozoic. The serpentinized upper mantle peridotites and lower crustal rocks in these ophiolites are cross-cut by dolerite and plagiogranite dykes, which show mutually intrusive relations indicating their synchronous emplacement into the pre-existing oceanic lithosphere. Zircon dating (U–Pb) of a plagiogranite dyke has revealed a concordia age of ∼179 ± 15 Ma that is interpreted here as the crystallization age of this differentiated rock. A fourth fraction of the zircon separates from this rock has also shown an inherited component greater than 1.7 Ga, possibly derived from the Precambrian core of the Rhodope–Strandja Metamorphic Massif in the Balkan Peninsula. Models for plagiogranite formation were tested and it is concluded that a high extent (<70%) of anhydrous or water-undersaturated, early amphibole-free fractionation of a basaltic melt source may have readily produced the observed REE concentrations for the Ankara mélange plagiogranites. The trace element abundances and other geochemical features of the coeval dolerite dykes are similar to those of the plagiogranites, suggesting a common melt source. The Ta–Nb patterns shown by both the plagiogranite and dolerite dykes are typical of arc-related petrogenesis and can be explained by the addition of slab-derived components to a depleted mantle wedge. The Early Jurassic ophiolitic basement and the dyke intrusions were formed in a back-arc setting between the Paleo- and Neo-Tethyan domains in the eastern Mediterranean region. The Izmir–Ankara–Erzincan Sea developed in this back-arc environment and the related suture zone had a diachronous evolutionary history.  相似文献   

论玄武岩金矿的地质特征     

薛步高 《化工矿产地质》2006,28(4):202-208

滇黔桂金三角区内一些产于峨眉山玄武岩组(含底部大厂层)和龙潭组内的金矿,其含矿岩性主要是玄武熔岩、凝灰岩和含凝灰质、碳质的粉砂岩、页岩．一些学者将它们都归入“卡林型金矿”．但因为地幔柱成因的玄武岩,自有其独立的成矿系列,包含Cu、Fe、Mn、Au、Pt、Pd、Co、Pb、Zn、Sb、CaF2、FeS2等多种矿产,在不同地区,其矿化各有侧重．可以看到金的矿集区都在铜的矿集区之南,且以玄武岩喷溢早期(大厂层)更富金,应命名为玄武岩金矿．晚期(龙潭组)更富铜为特色(玄武岩铜矿)．在共同具备含金(P2β2-1)、含铜(P21)有利地层与有利构造区内,发现卡林型金矿后,应着重探索玄武岩金矿,反之亦然．  相似文献   

四川阿加隆洼金矿地质特征与找矿标志   总被引：3，自引：0，他引：3  

夏廷高  孙传敏  李亮  王跃忠  刘春  杨永鹏 《地质与勘探》2006,42(3):53-55

阿加隆洼金矿矿床为浅成低温微细浸染型金矿.该矿床受断裂构造控制,岩浆活动影响.区域性深大断裂是沟通天水和地热流体的主要通道,次级断裂是矿体的储矿构造,脆性粗碎屑岩和火山碎屑岩(沉积火山岩)构成的断裂构造岩是主要的容矿岩石.文章在详细研究矿床地质及地球化学特征基础上,总结了该矿床的主要控矿因素并归纳了主要找矿标志,为区内找矿提供了新的思路.  相似文献