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71.
黄海太平洋鲱受精前后卵膜的动态变化 总被引:1,自引:0,他引:1
本文使用透射电镜,细胞化学和扫描电镜等方法,在亚微水平上对黄海太平洋鲱鱼(ClupeapalasiCvv,&Vol.)卵黄膜和受精膜的结构以及皮层小泡在卵黄膜转化为受精膜过程中的作用,受精卵新质膜的形成及其细胞化学变化等进行了研究。观察到,太平洋鲱鱼卵黄膜由5层组成,皮层小泡参与了受精膜的形成,在卵黄膜转化为受精膜的过程中,5层都发生不同程度的形态和糖蛋白及PAS阳性物质的变化。另外发现太平洋鲱有3种皮层小泡存在。在皮层反应中,第一种皮层小泡在受精后3min内迅速破裂,未受精卵尚含有PTA染色的小颗粒从小泡中泌出,其界膜形成了质膜的一部份。受精后,此质膜与皮层小泡形成的质膜相同排列构成卵子新的质膜。另外,还发现第一小泡顶部,与卵子质膜相接触的卵子表面有富含糖蛋白的泡状结构。卵子质膜表面糖蛋白及PAS阳性物质,随时间推延而不断发生变化 相似文献
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川西北马脑壳金矿床流体包裹体研究与热液成矿机理探计 总被引:2,自引:0,他引:2
系统的流体包裹体研究表明,马脑壳金矿床物石英中发育有液相,纯液相,含CO3三相,纯CO2相及含有机质等五种主要类开型的原生流体包裹体,其均一温度为120~300℃,热液盐度为0.5~11.0wt%NaCl,密度为0.78~0.95g/cm^3,成矿压力为32.87~113.615MPa,主矿化阶段成矿认发生过明星的流体混合及相分离作用,由此导致含矿热液体纱T、pH、fo2及fs2等物化条件参数的降 相似文献
74.
Windows NT以其图形化操作界面和方便高效的管理方式 ,越来越成为组网的主流操作系统。甘肃省地震前兆局域网就是采用 Windows NT Sever4.0中文版作为自己的操作系统平台 ,使用 TCP/IP协议 ,通过甘肃省地震局网络中心与 Internet互联的。由于该网采用了TCP/IP协议 ,可以很方便地和 UNIX主机联接 ,从而与省局网络中心接轨。通常 ,一个Windows NT网络应该有一个主域控制器、一个备份域控制器、一个服务器、若干个客户端 ,从这个角度来说 ,甘肃省地震前兆局域网主体已基本建成。该网的主要任务是管理前兆资料 ,建立地震前兆数据库服… 相似文献
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Geochemistry, U-Pb Geochronology and Sr-Nd-Hf Isotopes of the Early Cretaceous Volcanic Rocks in the Northern Da Hinggan Mountains 总被引:1,自引:0,他引:1
Whole-rock geochemical, zircon U-Pb geochronological and Sr-Nd-Hf isotopic data are presented for the Early Cretaceous volcanic rocks from the northern Da Hinggan Mountains. The volcanic rocks generally display high SiO2(73.19–77.68 wt%) and Na2O+K2O(6.53–8.98 wt%) contents, with enrichment in Rb, Th, U, Pb and LREE, and depletion in Nb, Ta, P and Ti. Three rhyolite samples, one rhyolite porphyry sample, and one volcanic breccia sample yield weighted mean 206Pb/238 U ages of 135.1±1.2 Ma, 116.5±1.1 Ma, 121.9±1.0 Ma, 118.1±0.9 Ma and 116.9±1.4 Ma, respectively. All these rocks have moderate(87Sr/86Sr)i values of 0.704912 to 0.705896, slightly negative εNd(t) values of –1.4 to –0.1, and positive εHf(t) values of 3.7 to 8. Their zircon Hf and whole-rock Nd isotopic model ages range from 594 to 1024 Ma. These results suggest that the Early Cretaceous volcanic rocks were originated from melting of subducted oceanic crust and associated sediments during the closure of the Mongol-Okhotsk Ocean. 相似文献
77.
Suofei Xiong Mouchun He Shuzhen Yao Yubao Cui Guanzhong Shi Zhenju Ding Xinlu Hu 《Geological Journal》2015,50(6):720-738
The Chalukou giant Mo deposit in the Heilongjiang Province, northeastern China, is a porphyry deposit hosted in an intermediate‐felsic complex surrounded by Mesozoic volcano–sedimentary rocks. The mineralization process is composed of four stages, including quartz + K‐feldspar (Stage I), quartz + molybdenite (Stage II), pyrite + chalcopyrite + quartz ± other sulphides (Stage III) and carbonate ± fluorite ± quartz (Stage IV). The mineralization is generally associated with intense K‐feldspar‐, fluorite‐, phyllic‐ and propylitic alteration. Primary fluid inclusions (FIs) in quartz include four compositional types, i.e. pure carbonic (PC‐type), aqueous‐carbonic (C‐type), daughter mineral‐bearing (S‐type) and aqueous (W‐type) inclusions. Halite, sylvite and hematite are recognized as the daughter minerals in Stage I S‐type FIs, whereas molybdenite and chalcopyrite occur as daughter minerals in Stage II S‐type FIs. High‐salinity and high pressure (>220 MPa) FIs exist in Stage I quartz veins, characterized by homogenization through halite dissolution at temperatures of 324 to 517 °C. The paucity of coexisting vapour‐rich FIs with similar homogenization temperatures at this stage indicates that the initial S‐type inclusions have directly exsolved from the magma rather than boiling off of a low‐salinity vapour. Stage I quartz has captured the C‐ and W‐type FIs, which have totally homogenized at 270–530 °C with salinities of 1.6–17.0 wt.% NaCl equiv. At Stage II, the coexistence of all FI types were only observed at pressures of 150–218 MPa and temperatures of 352–375 °C, with two salinity clusters of 0.9–16.6 wt.% NaCl equiv. and 37–56 wt.% NaCl equiv. Stage III quartz contains W‐type FIs with homogenization temperatures of 158–365 °C, salinities of 0.5–9.0 wt.% NaCl equiv., and minimum pressures of 12–116 MPa; whilst Stage IV fluorite or calcite only contains W‐type FIs with homogenization temperatures of 121–287 °C, salinities of 0.5–5.3 wt.% NaCl equiv., and minimum pressures of 10–98 MPa. The estimated trapping pressure from Stages II to III suggests an alternating lithostatic–hydrostatic fluid‐system caused by fluid boiling. Ore fluids at the Chalukou Mo deposit may have been evolved from a CO2‐rich, high‐salinity, and high‐oxygen fugacity (fO2) magma system, to a CO2‐poor, low‐salinity, and low‐fO2 epithermal system. Two key points may have contributed to the formation of the Chalukou giant Mo deposit: The magmatic origin and fluid boiling that has resulted in decompression and rapid precipitation of metals. Copyright © 2014 John Wiley & Sons, Ltd. 相似文献
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Xinlu Hu Shuzhen Yao Mouchun He Zhenju Ding Yubao Cui Jun Shen Bin Chen Bopeng Zhu 《Resource Geology》2014,64(2):102-116
The Daheishan porphyry Mo deposit was recently discovered in the northern segment of the Great Xing'an Range, NE China. Three main types of granitoids are identified in this deposit: granodiorite, fine‐grained granite, and porphyritic granite. The orebodies are dominantly hosted within the granodiorite and in the contact zone between the granodiorite and tuff or hornfels, while no mineralization has been found in the fine‐grained granite or the porphyritic granite. We present in situ LA‐ICP‐MS zircon U‐Pb dates for the granodiorite, fine‐grained granite, and porphyritic granite, which yielded 146.9 ± 1.1 Ma (2σ), 146.6 ± 1.7 Ma (2σ), and 149.7 ± 4.2 Ma (2σ), respectively. Their εHf(t) values range from 3.9 to 12.2, associated with young crustal model ages (TDM2) ranging from 524 Ma to 849 Ma, indicating that their parental magmas may have been generated by partial melting of the Neoproterozoic–Cambrian crustal components. The formation of the Daheishan deposit was genetically related to the subduction of the Paleo‐Pacific Plate. 相似文献
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