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乌兰布和沙漠东海子湖全新世湖相沉积结构分析及其环境意义 被引量:20
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作者 贾铁飞 银山 +2 位作者 何雨 赵明 包桂兰 《中国沙漠》 CSCD 北大核心 2003年第2期165-170,共6页
根据乌兰布和沙漠北部东海子湖沉积纪录,对146cm的连续沉积进行146个样品的沉积结构分析,并运用沉积结构直方图对比、平均粒径值(Mz值)、沉积物标准离差(σ1值)、风力降尘作用指标(Kd值)等方法对沉积物代表的环境进行分析研究。依据东... 根据乌兰布和沙漠北部东海子湖沉积纪录,对146cm的连续沉积进行146个样品的沉积结构分析,并运用沉积结构直方图对比、平均粒径值(Mz值)、沉积物标准离差(σ1值)、风力降尘作用指标(Kd值)等方法对沉积物代表的环境进行分析研究。依据东海子湖沉积剖面的沉积结构特征,可以将乌兰布和沙漠北部地区中全新世以来划分为4个环境变化阶段:①中全新世湖泊(河流 湖泊)沉积阶段,沉积纪录年龄为6550~2550aBP,是环境普遍温暖、湿润的阶段。②晚全新世风力作用渐强阶段,沉积纪录年龄为2550~1211aBP,是一个风力作用不断加强的环境变化时期。③晚全新世强风力作用阶段,沉积纪录年龄为1211~275aBP,也是乌兰布和沙漠风成沙堆积最旺盛的阶段。④近代强风力作用阶段,沉积纪录年龄为275aBP以来。这样的环境变化过程表明,乌兰布和沙漠的形成、演化与中国北方环境演变的总体规律是相一致的。 展开更多
关键词 乌兰布和沙漠 湖泊沉积 沉积结构分析 环境演变 风力降尘作用指标 沉积物标准离差 风力作用 全新世
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NUMERICAL SIMULATION OF THE STRUCTURAL STRESS FIELD OF BEIYA GOLD DEPOSIT
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作者 MA Deyun and GAO Zhenmin(Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China Department of Earth Science, Kunming University of Scienceand Technology, Kunming 650093, China) 《Geotectonica et Metallogenia》 2003年第1期91-103,共13页
Based on the study about the geological background of Beiya Gold Deposit, numerical simulation was conducted about the three-dimensional structural stress field for Beiya Gold Deposit by applying finite element theory... Based on the study about the geological background of Beiya Gold Deposit, numerical simulation was conducted about the three-dimensional structural stress field for Beiya Gold Deposit by applying finite element theory and by employing a linear elasticity model. Results of the simulation indicate that the Beiya syncline is a faulted basin, and a hidden fracture occurs in the west wing of the syncline.Under the action of the EW-trending compressive force, four nearly NS-trending fractures (groups) were generated in the stress stretching areas of the two wings of the syncline, and these fractures constitute favorable tectonic positions for the upward intrusion of porphyry magma and the occurrence of Au-Pb-Zn polymetallic deposits. 展开更多
关键词 Beiya gold deposit structural stress field numerical simulation
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Ultrastructure analysis reveals sporopollenin deposition and nexine formation at early stage of pollen wall development in Arabidopsis 被引量:2
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作者 周鹊 朱骏 +1 位作者 崔永兰 杨仲南 《Science Bulletin》 SCIE EI CAS CSCD 2015年第2期273-276,I0003,共5页
In angiosperm, pollen wall formation is a critical step for male gametophyte development. Pollen wall constitutes of the outer layer exine and the inner layer intine. Exine is further divided into sexine and nexine. I... In angiosperm, pollen wall formation is a critical step for male gametophyte development. Pollen wall constitutes of the outer layer exine and the inner layer intine. Exine is further divided into sexine and nexine. In Arabidopsis, the general process of pollen wall formation has been reported. However, the nexine formation has not been revealed. Here, we observed the process of pollen wall formation in Arabidopsis thaliana using transmission electron microscope. After callose wall is formed, the primexine is present between plasma membrane and the callose layer in the tetrad. With plasma membrane undulation, sporopollenin precursors accumulated on the peak of undulated membrane which is further developed into probacula. The primexine determines plasma membrane undulation and sporopollenin accumulation based on previous analysis of an undulation-deficient mutant. Some materials obviously different from sporopollenin are filled between the primexine and plasma membrane. These materials cover all the surface of plasma membrane and gradually develop into nexine. After microspore is released from tetrad, the nexine layer is formed and the probacula is further developed into sexine with continued accumulation of sporopollenin. Based on these observations, we proposed a developmental model of early pollen wall formation. 展开更多
关键词 Arabidopsis thaliana Pollen wall formation Exine patterning Primexine Male gametophyte
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