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1.
王一先  包志伟 《地球化学》1999,28(4):367-373
赣东北蛇绿混杂岩带中的西湾斜长花岗岩富Al2O3和Na2O,贫K2O;Sr、Ba和Th含量高,而Rb和高场强元素含量很低;LREE富集、无Eu异常;δNd(t)值高,为5.39。(^87Sr/^86Sr)i低,为0.7027。这些特征表明西湾斜长花岗岩是大洋斜长花岗岩。在La/Sm-La图中,该斜长花岗岩与超基性岩和基性岩的分离结晶趋势不一致,所以它不是岩浆分离结晶的产物,而可能是基性岩石小比例部  相似文献   

2.
山西吕梁群早元古代双峰式火山岩地球化学特征及成因   总被引:10,自引:10,他引:10  
山西吕梁山区中部的吕梁群形成于早元古代(~2.1Ga),其上部由变质玄武岩和变质流纹岩组成。流纹岩富集LIL和HFS元素且具高的Rb/Sr和Ga/Al比值,显示出与A型花岗质岩石的相似性。玄武岩具有低TiO2和P2O5含量且富集LIL和LREE元素。地球化学研究表明吕梁群玄武岩和流纹岩形成于大陆边缘的裂谷环境。玄武岩的母岩浆起源于亏损程度较低的地幔,并经历了结晶分异和地壳混染作用。流纹岩是由下地壳麻粒岩相正变质岩受到裂谷区高温热流和基性岩浆的影响部分熔融而形成  相似文献   

3.
嵩山A型花岗岩的地质地球化学特征和构造环境   总被引:8,自引:0,他引:8  
薛良伟  尉向东 《岩石学报》1996,12(1):137-144
从岩石学、岩石化学、微量元素、REE等方面讨论了嵩山古元古代钾长花岗岩体的地质地球化学特征,结果表明这些岩体属于A型花岗岩,其SiO2、K2O、K2O/Na2O、F、Ga、Hf、Rb、Y、Co、Ga/Al、REE高,Al2O3、MgO、CaO、Na2O、Ba、Sr、V、Th低,Eu为0.15~0.27,A/CNKM<1.10,这些岩体是与古元古代熊耳群火山岩相伴生的钾质侵入岩,两者均形成于非造山的大陆裂谷环境,表明华北陆台南缘在古元古代晚期处于拉张的非造山构造环境。  相似文献   

4.
晋南中条山北峪奥长花岗岩的岩石地球化学   总被引:3,自引:0,他引:3  
野外工作发现,北峪奥长花岗岩侵入于绛县群变富钾流纹岩之中,结合其2107±59Ma的全岩Rb-Sr等时线年龄,应为早元古代岩浆侵入的产物。北峪岩体具高的Al2O3含量和高的δ^18OSMOW(‰)比值,表明为铝过饱和的S型花岗岩。其高的Al2O3含量和低的Yb含量及强烈分异的稀土图谱,表明形成于大陆环境。在LILE元素特点上,北峪奥长花岗岩亏损U,Th,K,Rb,具低的Rb/Sr比值和高的K/Rb  相似文献   

5.
进贤早官岭侵入体是作者近年来从事1:5万进贤图组区域地质调查所发现的。该侵入体主体岩性为黑云角闪闪长岩,全岩Rb-Sr等时线年龄为1240±10Ma,( ̄(87)Sr/ ̄(86)Sr)=0.7034,具有高Al_2O_3、TiO_2、CaO含量,低SiO_2含量的成分特征,其微量元素的MORB标准化曲线与阿卓热斯碱性玄武岩极为相似,稀土总量较高,弱的负Eu异常。地球化学特征反映其岩浆为亏损地幔经低的部分融熔后,发生极低的结晶分异且未受地壳混染,固结后经构造运动拾升至地表。  相似文献   

6.
吉乃县塔斯特岩体地质地球化学特征及含矿性评价   总被引:5,自引:0,他引:5  
周刚 《新疆地质》2000,18(1):79-84
塔斯特岩体由石英闪长岩、英云闪长岩、二长花岗岩和钾长花岗岩组成。岩石均具有高Na低K,Na2O、Fe2O3、Hf、K/Rb偏高,K2O、CaO、FeO、Rb、Sr、Nb、∑REE、δ^18O、Rb/Sr明显偏低的特点。岩石化学和地球化学特征表明该岩体为形成于火山弧环境的“I”型花岗岩。岩体中Au、Ag、As、Bi、Cu等成矿元素明显富集,并与该岩体中金矿床、矿点的元素组合一致,说明该岩体与Au的成  相似文献   

7.
赣南寨背A型花岗岩体的地球化学特征及其构造地质意义   总被引:86,自引:9,他引:77  
陈培荣 《岩石学报》1998,14(3):289-298
赣南寨背岩体主要为黑云母钾长花岗岩,黑云母结晶晚于长石和石英,锆石群型地温测量标尺显示其结晶温度为800℃~900℃,表明寨背岩体形成于一种高温贫水的花岗质岩浆。岩石的化学成分特点为准铝质(Al2O3为12.21%~12.62%),富硅(SiO2为75.66%~76.74%),偏碱(Na2O+K2O为7.93%~8.90%),FeOT/MgO值高(59~148),CaO和MgO含量低(分别为0.10%~0.65%和0.01%~0.02%),富含REE(Eu除外,ΣREE平均为500μg/g),Y、Ga、Nb等高场强元素(HFSE)以及F,Sr和Ba较低。这些特点与本区的I型和S型花岗岩有明显差别,是一种典型的A2型花岗岩。寨背岩体Rb-Sr等时线年龄为176Ma,与辉长岩、双峰式火山岩有密切的时空关系,表明赣南地区在燕山早期即进入拉张裂解阶段。  相似文献   

8.
王笃昭 《广东地质》1996,11(3):17-24
南岭及邻区花岗岩的稀土元素主要地球化学特征:(1)稀土元素特征值的变化,主要受同源同期岩浆的不断熔离,连续分异演化过程中,岩石化学成分,(如∑R^2+,Na/Ca)变化的制约。(2)源自沉积陆壳的花岗岩的稀土元素总量,总体上高于幔源为主陆壳混合型花岗岩。(3)花岗岩的δEu值与(^86Sr/^86Sr)i值之间,没有内在联系,(4)同源同斯的花岗质岩浆,由中酸性岩向碱性岩演化时,稀土元素总量递增,  相似文献   

9.
银山火山岩次火山岩属于高钾钙碱性系列。化学成分以低Ti、Na,高K和相对富Al为特征。微量元素∑REE较低,K、Rb、Th、U、La、Ce富集和Ti、Ta、Sr、P、Yb相对贫化。从第一旋回到第三旋回,随着SiO2含量降低,Al2O3、FeO、MgO、CaO、Na2O含量以及∑REE、∑Ce/∑Y、(La/Yb)N逐渐升高,岩性由流纹岩流纹英安斑岩英安质熔岩和英安斑岩粗面安山斑岩,表现连续的反序演化。起源于下部地壳的英安质母岩浆同化混染了部分上地壳的硅铝层物质并演化形成以英安质岩浆为主、顶部有一层富SiO2、K的流纹质岩浆、底部有少量粗面安山质岩浆的带状岩浆房。断裂构造诱发岩浆房自上而下逐层抽取喷发—侵位形成反序的火山岩次火山岩。  相似文献   

10.
薛良伟  周长命 《地球化学》1999,28(5):473-478
用石英流体包裹体Rb-Sr、^40Ar-^39Ar法测定了小秦岭303号石英脉的形成时代为石元古代。其流体包裹体属H2O+CO2+CaCl型,盐度为6.5%-12.98%,CO2含量高,Na^+〉K+。303号石英脉Rb-Sr等时线年龄为(2382±336)Ma-(2234±47)Ma,(^87sR/^86Sr)i为(0.7351±0.0019)-(0.7416±0.0004),^40Ar^^39  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

14.
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.  相似文献   

15.
PALEONTOLOGY     
正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)  相似文献   

16.
正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)  相似文献   

17.
正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)  相似文献   

18.
PETROLOGY     
正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,  相似文献   

19.
正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an  相似文献   

20.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

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