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与岩浆成因相关的钼矿床成岩-成矿时差是确定矿床与岩浆岩成因关系的重要基础.本文根据收集的中国东部中生代典型钼矿床的成矿及相关岩体的同位素测年数据,详细讨论并定量厘定了钼矿的成岩-成矿时差分布特征.结果表明,钼矿成矿同步或略滞后于同源岩浆活动,中国东部整个钼矿成矿高峰的两个阶段时差介于0~10.0 Ma和0~15.0 Ma;对于单个钼矿床,其成岩-成矿时差集中在0~14.0 Ma,均值为3.9 Ma;从斑岩型钼矿床→斑岩-矽卡岩型钼矿床→矽卡岩型钼矿床→石英脉型钼矿床,成岩-成矿时差呈逐渐增加趋势,这与岩浆热液成矿过程的地质事实吻合. 相似文献
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安昌岘钼矿为隐伏矿床.矿体产于夕卡岩中,呈似层状、透镜体状大致平行分布.钼矿石中的金属矿物主要有辉钼矿,其次为黄铁矿、磁铁矿、黄铜矿、方铅矿、闪锌矿等.非金属矿物主要有石榴石、透辉石、符山石、透闪石、阳起石、石英.围岩蚀变类型主要有夕卡岩化、硅化、绿泥石化、绿帘石化、阳起石化.与成矿有关的蚀变主要为夕卡岩化.侏罗纪钢屯超单元花岗岩是主要含钼矿源岩.安昌岘钼矿属夕卡岩型钼矿床. 相似文献
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论金矿成矿与CO2相关性的实质 总被引:7,自引:0,他引:7
根据CO2的形成条件及其与Au的配合能力,金成矿系统矿物流体包裹体的气相成分,有代表性的金矿物的化学成分,具成因意义的共、伴生矿物,认为金成矿与CO2相关性的实质是CO与成矿物质形成羰基配合物、羰基氢配合物迁移至地壳浅部,由于温度、压力骤降,fo2剧增,上述配合物分解(CO、H2逃逸,氧化)形成金矿物沉淀富集成金矿床。 相似文献
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河北省丰宁撒岱沟门斑岩型钼矿,处于华北地台北缘的东段,是河北省内最大的钼矿床,撒岱沟门斑岩型钼矿主要与吕粱—五台期的中酸性岩、海西期的二长花岗岩和燕山期中酸性岩有关,钼矿主要产于二长花岗岩、石英正长斑岩中,一般呈岩株、岩墙状产出(黄典豪等,1996;范羽等,2014)。在结合华北板块北缘钼-铜矿床的成矿背景(黄典豪等,1996;代军治等,2008;魏然等,2013),通过对承德市丰宁县撒岱沟门钼矿区地质特征和矿体的流体包裹体特征(代军治等,2007)的研究,对其成矿环境(吕古贤,2015)和成因(骆文娟等,2010)进行了分析探讨。撒岱沟门钼矿床,在成矿前期和成矿阶段包裹体主要是以气液两相为主,同时存在含CO2的三相,和CO2相的包裹体。成矿流体以岩浆水为主,晚期有大气水的混入。主成矿流体总体属于H2O-NaCl-CO2体系,主成矿期成矿包裹体的均一温度介于160~300℃、盐度介于2%~13.38%,成矿期流体的不混溶作用对辉钼矿的沉淀成矿产生了积极的影响。 相似文献
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准噶尔北部希勒库都克斑岩钼铜矿床地质与成矿流体 总被引:2,自引:7,他引:2
希勒库都克斑岩铜钼矿床铜钼矿化与安山玢岩脉、英安玢岩脉有关,蚀变有钾长石化、绢云母化、绿帘石化等,向外发育绿泥石化、深部发育夕卡岩型蚀变。浅部以钼矿化为主,向深部铜钼矿化并存。与典型的斑岩型矿床相比,其石英中流体包裹体少而小,气体包裹体少,含CO2包裹体及含子矿物包裹体发育,子矿物以NaCl为主,基本不出现KCl子矿物。钼富集处出现了富CO2流体的沸腾,铜富集处出现了成群分布的含大子矿物包裹体,沸腾消失。钼的成矿主要与富CO2成矿流体沸腾及斑岩型蚀变和夕卡岩蚀变有关,钼主要源于地壳,成矿温度为280~530℃,集中在300~400℃左右。铜主要与直接从深源基性岩浆出溶的高盐度流体及夕卡岩型蚀变有关,铜主要源于上地幔,主要成矿温度低于350℃。晚期流体的成矿温度为180~300℃左右。希勒库都克矿床成矿流体特征反映了壳源与幔源流体混合、岩浆热液与天水混合的特征。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
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
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引:4,自引:0,他引:4
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
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozach Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003). 相似文献
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正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level 相似文献
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正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7), 相似文献
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正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci- 相似文献
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正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli- 相似文献
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正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.) 相似文献
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正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861 相似文献