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Temporal change of clustered distribution in vertical profiles of three nutritional groups of planktonic ciliates, e.g. heterotrophic
naked ciliates, mixotrophic naked ciliates and heterotrophic loricated ciliates, was investigated by following a drifting
buoy in Toyama Bay on the Japan Sea coast of central Japan in summers of 1989 and 1990. Clustered distribution, represented
as the mode of population density in the vertical plane, occurred mainly in the oligotrophic upper layer (0–50 m depth) above
the subsurface chlorophyll-a maximum layer. Its clustered degree was stronger when the mode of population density in the vertical plane was formed at
shallower depth, while its longevity was shorter as mentioned above. Vertical distribution of ciliates during summer in Toyama
Bay is characterized by ephemeral clustered distribution, or in other wards, by rapid alternations of appearance and disappearance
of the clustered distribution. 相似文献
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地堡那木岗铜(金)矿床位于西藏多龙矿集区,探明储量达大型规模;矿床的成矿过程分为岩浆作用阶段、钾长石-硫化物阶段、石英-多金属硫化物阶段、碳酸盐-黄铁矿阶段和氧化作用阶段,其中石英-多金属硫化物阶段和碳酸盐-黄铁矿阶段为主要成矿阶段;为查明成矿流体特征,确定矿床成因类型,对取自深部矿石中的碳酸盐脉(均为碳酸盐-黄铁矿成矿阶段含黄铁矿黄铜矿石英脉)开展流体包裹体的岩相学观察和显微测温分析。分析结果表明,上述矿物中主要发育富液相、富气相和含子矿物三相包裹体。其中,富液相包裹体的均一温度与盐度分别为:t=80~600℃、w(NaCl,eq)=4.48%~18.79%;富气相包裹体的均一温度和盐度分别为:t=240~560℃、w(NaCl,eq)=5.09%~9.73%;含子矿物三相包裹体的均一温度与盐度分别为:t=240~560℃、w(NaCl,eq)=36%~72%。综合分析认为,地堡那木岗铜(金)矿床成矿流体发生了强烈的沸腾作用,流体沸腾作用是该矿床的重要成矿机制。通过与国内外典型斑岩型矿床与高硫化型浅成低温热液矿床的流体包裹体特征进行对比,其与斑岩型矿床的中高温、高盐度流体特征相似。因此,推测地堡那木岗矿床的成因类型为斑岩型铜(金)矿床。 相似文献
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本文系统阐述了亚洲中部及邻区地球动力系统的演变进程及其所制约的区域地质和成矿特征,并提出了以下新认识和新观点:①在西伯利亚陆块与中朝—塔里木陆块之间的原"古亚洲洋"区域内是全球地史演化中具有双向侧向陆缘增生与垂向增生同时发展的"双向增生"独特地区。②"古中国陆块群"是位于劳亚古陆和冈瓦纳古陆之间独立存在的古陆。由于它的特殊位置而构成了古亚洲洋与特提斯洋的"分水岭"。③地球动力学的"内动力"归根到底来自地球自身的两个方面:一是地球自转和公转形成的离心力(拉张力)与挤压力,它是地球动力学的基础,二是地球内部永不衰败的"高热能库"。当今地震、火山等等,都是地下过饱和的高热能向地表释放的一瞬间转变为强动能的地质事件。④由地球动力系统演变打造的具有不同特征的断裂系统是控矿储矿的良好空间,因此"断裂系统找矿法"是简便有效的找矿方法之一。据此提出了4个理论指导找矿的试点和验证区。 相似文献
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青城子地区煌斑岩与成矿具有密切的关系。本文详细研究了青城子地区不同空间分布的煌斑岩，并且对蚀变煌斑岩和未明显蚀变煌斑岩进行了地球化学测试分析工作。结果表明：煌斑岩具有幔源源区特征，又有壳源物质的混染特征；蚀变过程中，流体带来成矿元素Pb、Zn、Mo，带走Ti、Fe、V、Co、Ni元素；煌斑岩主量元素氧化物哈克图解呈现线性分布，说明它们之间具有演化趋势。大量钻孔中煌斑岩数量统计反映煌斑岩大致以青城子镇为中心，分别向二道→新岭→桃源、甸南→大地→小佟家堡子线性分布，这种分布与矿床/矿体分布规律相同，因此可以利用煌斑岩的分布规律指示矿床/矿体潜力分布区。 相似文献
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图谱迭代反馈的自适应水体信息提取方法 总被引：1，自引：0，他引：1
提出图谱迭代反馈模型,结合空间聚合图特征和非线性谱映射结果的优点,设计图谱迭代反馈机制,并通过自适应信息计算方法自动地调整提取参数,逐步地计算逼近正确的专题区域边界。结合水体提取案例,在分析当前较为有效的水体提取方法基础上,选取ETM影像作为数据源,提出图谱迭代反馈的自适应水体信息提取（WERSTP）理论与方法。试验比较表明,该方法能充分结合基于指数和基于光谱分类提取方法的优势并成功融入水体空间分布特征,获得较好的提取效果。 相似文献
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正Qarhan Salt Lake is located in the eastern part of the Qaidam Basin,which is first discovered the large potash deposit in the late 1950s.The Bieletan section is located in the west of Qarhan Salt Lake,where saline sediment 相似文献
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基于认知聚类分区方法的边坡可靠度分析 总被引：1，自引：0，他引：1
提出了边坡可靠度分析的一种新的全局优化方法--认知聚类分区方法。该方法主要包括5个步骤：分区、随机抽样、计算极径L、回代、计算可靠指标及验算点。给出了相应的计算流程图,并编写了基于C语言的计算程序KCPREL。最后,以岩质边坡稳定可靠度问题为例证明了所提方法的有效性。结果表明,认知聚类分区方法能同时计算出可靠指标和验算点,并能获得全局最优解。该方法的计算精度和蒙特卡洛模拟方法相当,计算效率远远高于传统的蒙特卡洛模拟方法。此外,该方法在分析含有复杂的隐式及非线性功能函数的边坡稳定可靠度问题方面体现出明显的优越性。等步长认知聚类分区方法能全面且均匀地搜索角度,从而得到更准确的验算点。为了保证足够的计算精度及减小计算量,建议步长取10º以内。 相似文献
9.
A new network of permanently recording seismic stations in West Saxony has considerably improved detection threshold, location
accuracy and depth determination in this seismically active region. Between 2001 and 2007 more than 900 events have been located.
Seismicity mainly occurred along a band stretching north-south between Leipzig and Vogtland/NW Bohemia area with local magnitudes
ranging between −0.8 and 2.8. Seismicity clearly delineates the Leipzig-Regensburg (L-R) fault zone striking N-S, and the
Gera-Jachymov (G-J) fault zone striking roughly NNW-SSE. The hypocentral depths can be divided into two depth ranges, one
at depths below 10 km, and a second at less than 10 km depth that only extends S-N from the Vogtland until the crossing between
L-R and G-J fault zones. A small earthquake sequence that occurred near Werdau/Zwickau in August 2006 at almost the same epicenters
as an earlier sequence 1997/98 seems to confirm this finding: a relative localization of 15 events with the double-difference
technique clearly reveals two distinct subclusters at about 6 and 12–14 km depth. With the improved station coverage 33 new
fault plane solutions from events along the L-R fault zone north of the swarmquake area could be determined from P-polarities
and P/S ratios. They do not differ significantly from solutions in the Vogtland/NW-Bohemia area and are mostly compatible
with a N-S oriented fault plane. Strike slip mechanisms with or without a dip slip component dominate. 相似文献
10.