排序方式： 共有15条查询结果，搜索用时 46 毫秒
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西秦岭地区晚二叠世—早三叠世沉积相分析和沉积古环境再造 总被引：6，自引：0，他引：6
青海省同仁地区处于祁连和秦岭造山带的接合部，构造演化历史悠久。本次工作在该地区隆务河一带发现较好的二叠—三叠系剖面。将该剖面从下而上划分为上二叠统石关组、下三叠统果木沟组和江里沟组，其中江里沟组又进一步划分为下部的浊积岩段和上部的风暴岩段，初步确定了二叠—三叠纪的界线。沉积序列、沉积相和沉积物表明上二叠统石关组和下三叠统果木沟组为一套陆源碎屑浊积岩，下三叠统江里沟组下部为一套不纯的内碎屑浊积岩，而下三叠统江里沟组上部为风暴岩沉积。根据沉积相和火山岩夹层的地球化学特征认为该地区上二叠统石关组和下三叠统果木沟组处于半深海的活动大陆边缘，下三叠统江里沟组早期的浊积岩段处于较稳定的半深海大陆边缘。根据沉积相和遗迹化石，恢复了晚二叠世—早三叠世的海平面变化特征。 相似文献
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Experimental study on the mechanism of non-synchronism of seismo-electromagnetic radiation precursors 总被引：1，自引：0，他引：1
ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｒｏｕｇｈ２０－ｏｄｄｙｅａｒｓ’ｏｂｓｅｒｖａｔｉｏｎａｎｄｓｔｕｄｙａｆｔｅｒｔｈｅ１９７６Ｔａｎｇｓｈａｎｇｒｅａｔｅａｒｔｈｑｕａｋｅ,ｔｈｅｓｅｉｓｍｏ－ｅｌｅｃｔｒｏｍａｇｎｅｔｉｃｒａｄｉａｔｉｏｎｐｒｅｃ... 相似文献
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Photoluminescence (PL) spectra of Si nanocrystals (NCs) prepared by 130 keV Si ions implantation onto SiO2 matrix were investigated as a function of annealing temperature and implanted ion dose. PL spectra consist of two PL peaks, originated from smaller Si NCs due to quantum confinement effect (QCE) and the interface states located at the surface of larger Si NCs. The evolution of number of dangling bonds (DBs) on Si NCs was also investigated. For hydrogen-passivated samples, a monotonic increase in PL peak intensity with the dose of implanted Si ions up to 3× 1017 ions /cm2 is observed. The number of DBs on individual Si NC, the interaction between DBs at the surface of neighbouring Si NCs and their effects on the efficiency of PL are discussed. 相似文献
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Xiao-Dong Liu Li-Guang Sun Zhong-Qi Cheng San-Ping Zhao Ke-Xin Liu Xiao-Hong Wu Zhou-Qing Xie Xue-Bin Yin Hong-Hao Luo Xing-Fang Ding Dong-Bo Fu Yu-Hong Wang 《Marine Geology》2008,247(1-2):1-16
The phosphatic cement in the bioclastic sediment sequence on the northeastern shore of Dongdao Island in the South China Sea was studied and its paleoenvironmental implications discussed. Petrological characteristics and major, trace, REE element data unequivocally supported the notion that phosphatization was closely associated with avian guano decomposition and leaching, whereas carbon and oxygen isotope results further revealed that meteoric water were involved in these processes. AMS 14C dates on the brown phosphate cements indicate that they were formed around 5700, 5000–5100 and 2900 yr BP, respectively. The multi-episodes of phosphatization very likely correspond to intermittent seabird occupation on this island — possibly reflecting Holocene sea-level oscillation and/or long term climate changes in the South China Sea that have controlled seabird habitat. The phosphate cementation, which occurs widely in tropical islands, may be another useful monitor for sea-level and/or paleoclimate changes. 相似文献
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中国海洋药物资源及其药用研究调查 总被引：3，自引：0，他引：3
对中国海洋药物资源状况进行了调查和评价.结果显示,历经3 600余年,中国海洋药物应用经验不断积累,特别是现代海洋药物的研究成果显著.截至2008年,中国近海已记录的海洋药物及已进行现代药理学、化学研究的潜在药物资源已达684味,其中植物药205味,动物药468味,矿物药11味;涉及海洋药用动植物1 667种(植物272种,动物1 395种),另有矿物18种.加强现代药学研究,保护现有药用生物资源,开拓新的资源领域,是未来海洋药物持续发展的保障. 相似文献
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构造活动是源-汇系统中形成古地貌和砂分散体系的重要影响因素。塔木察格盆地塔南凹陷在早白垩世是一个典型的断陷湖盆,经历了多期幕式断陷活动,但同沉积构造活动及其配置所产生的古地貌对层序结构特征、沉积体系及砂体分布的控制作用仍不明确。文中以地震、测井、岩心资料为基础,以层序地层学理论和古地貌控砂理论为指导,建立了塔南凹陷下白垩统层序地层格架;结合断层活动性分析,阐明了不同类型古地貌对沉积体系和砂体分布的控制作用和规律。构造演化和沉积充填的综合研究表明: 受控盆主断裂的幕式断陷活动及同沉积断裂的差异断陷活动影响,塔南凹陷发育横向凸起和走向斜坡2种类型的构造调节带,这些构造调节带是水系入盆的通道,控制着盆地的主体物源方向、沉积体系类型与分布特征;根据断层的几何形态及发育部位,共识别出4种类型构造坡折带,分别是陡坡断崖型坡折带、陡坡断阶型坡折带、缓坡反向断阶型坡折带和盆内坡折带,它们各自控制了不同类型沉积体系的形成与分布;沉积物入盆后,沉积物分散体系和砂体的分布特征受同沉积断裂的组合样式控制,研究区共发育梳状断裂系、叉状断裂系和平行断裂系3种同沉积断裂平面组合;与构造调节带相对应的断裂坡折带低部位是大型储层砂体,特别是低位扇三角洲或盆底扇砂体发育的有利部位,是寻找砂岩油气藏的有利区带。研究成果对于深化断陷湖盆源-汇系统理论、指导断陷湖盆砂体分布预测具有重要的理论意义和实际价值。 相似文献
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A type of relatively low frequency ULF magnetic disturbance has been generally observed by the magnetic induction-meter since
it’s operation at Baijiatuan observatory in Beijing. As the amplitudes and frequencies of such disturbance signals change
with time and are different from the disturbances produced by some man-made magnetic sources, therefore they are usually taken
as a kind of earthquake precursors for ULF electro-magnetic emission. However, a comparative analysis with magnetic storms
on the magnetogram obtained by variometerat the same station indicates that such signals always occur in the period of magnetic
storm occurrence and so far we have not found the cases where such signals occur with no magnetic storms, therefore this kind
of ULF magnetic disturbances should not be taken as a ULF earthquake precursors of the electromagnetic emission at present.
The main features of such signals are as follows: the signals occur discontinuously during storms and the duration of each
time section with such signals and the occurrence rates of the sections and the disturbance amplitudes are usually related
to the types and intensities of storms. The wave form characteristics of the ULF disturbance are also related to the types
of storms. Generally, the amplitudes and durations for SC storms are stronger and longer respectively than those for GC stroms,
and if a storm is with largerK index, then relatively large amplitudes and higher rates and longer durations as well as variable frequencies will be observed
andvice versa. Most of the start time and the time section with strongest disturbance recorded by the ULF unit and by the variometer are
not consistent with each other, and the same one is only about 44%. The periods and intensities of such disturbance signals
are in the ranges of few to several seconds and 0.04–8 nT respectively. The predominant frequency is about 0.06 Hz and certain
energies are also distributed on the harmonic frequencies.
Contribution No. 95A0063, Institute of Geophysics, SSB, China. 相似文献