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101.
东昆仑夏日哈木铜镍硫化物矿床辉石特征及地质意义 总被引:1,自引:0,他引:1
夏日哈木铜镍硫化物矿床的发现在矿床规模、成矿时代及成矿区带方面都有重要意义。辉石作为最主要的造岩矿物之一,广泛赋存于该矿床的各岩相中,在橄榄岩相中多为填隙相,而在辉石岩相及辉长岩相中多呈堆晶相;总体上,斜方辉石含量大于单斜辉石含量。辉石Cr_2O_3含量在橄榄岩相、辉石岩相、辉长岩相具有依次降低的趋势,说明从早到晚含矿的橄榄岩相、辉石岩相、辉长岩相先后结晶,并非所有辉长岩相的结晶均早于橄榄岩相和辉石岩相;单斜辉石SiO_2、TiO_2及Na_2O含量之间的关系显示夏日哈木矿床母岩浆属拉斑玄武质岩浆,较高的Al_2O_3含量(2.55%~10.61%)暗示岩体形成过程中与富铝围岩发生了同化混染作用。 相似文献
102.
中朝古大陆东部早前寒武纪变质岩系对比及其演化阶段划分 总被引:5,自引:0,他引:5
介绍了朝鲜半岛太古宙、古元古宙的表壳岩和花岗质岩石的岩石组合、岩石化学和地球化学特征;根据近几年来华北古大陆前寒武纪地质研究的新发现和同位素年代学的最新成果,对中朝古大陆东部吉-辽-鲁古陆同朝鲜半岛的狼林陆块、京畿陆块和冠帽陆块等进行对比,表明朝鲜北部的狼林、冠帽陆块同胶辽古陆为同一演化体系,而其南部的京畿、小白山陆块的对比,存在不少问题,有待今后深入对比研究。 相似文献
103.
滑坡预报的几个基本问题 总被引:19,自引:0,他引:19
在滑坡预报研究中,必须首先解决与预报密切相关的一些基本问题。否则,往往导致预报误差很大或者预报失败。根据作者的初步探索,本文重点讨论了滑坡预报的分类及定义、预报参数及其监测点的选取、变形突变现象的分析与处理以及斜坡变形阶段的定量判断等基本问题。 相似文献
104.
The accurate and timely estimates of crop physiological growth stages are essential for efficient crop management and precise modeling of agricultural systems. Satellite remote sensing has been widely used to retrieve vegetation phenology metrics at local to global scales. However, most of these phenology metrics (e.g., green-up) are different from crop growth stages (e.g., emergence) used in crop management and modeling. As such, an integrated framework referred to as PhenoCrop was developed to: 1) establish a connection between remote sensing-derived phenology metrics and key crop growth stages based on Wang and Engle plant phenology model and 2) use fused MODIS-Landsat 30 m 8-day reflectance data generated using Kalman Filter-based data fusion technique to produce onset dates of key growth stages of corn (Zea mays L.) and soybeans (Glycine max L.) at 30 m spatial resolution. In this paper, we described the PhenoCrop framework, and tested its performance for the State of Nebraska for 2012–2016 by comparison to observations of estimated key growth stages at four experimental sites, and state-level statistical data from Crop Progress Reports (CPRs) published by the United States Department of Agriculture’s (USDA) National Agricultural Statistical Services (NASS). In addition, to evaluate the suitability of using coarse or high spatial resolution satellite imagery, fused MODIS-Landsat-based estimates were compared with those produced using EOS MODIS 250 m (MOD9Q1) reflectance data.The PhenoCrop estimates captured the typical spatial trends of gradual delay in the progression of the growing season from southeast to northwest Nebraska. Also inter-annual differences due to factors such as weather fluctuations and change in management strategies (e.g., early season in 2012) were evident in the estimates. Validation results revealed that average root mean square error (RMSE) of the state-level estimates of corn and soybean growth stages ranged from 1.10 to 4.20 days and from 3.81 to 7.89 days, respectively, while pixel level estimates had a RMSE ranging from 3.72 to 8.51 days for corn and 4.76–9.51 days for soybean growth stages. Although MODIS 250 m based estimates showed similar general spatial patterns observed in the fused MODIS-Landsat based estimates, the accuracy and ability to capture field scale variations was improved with fused MODIS-Landsat data. Overall, results showed the ability of PhenoCrop framework to provide reliable estimates of crop growth stages that can be highly useful in crop modeling and crop management during the growing season. 相似文献
105.
卤虫休眠卵的若干生物学特性研究进展 总被引:2,自引:1,他引:1
王素凤 《中国海洋大学学报(自然科学版)》2009,39(1)
结合作者的研究工作对卤虫休眠卵的耐性、形态结构、胚胎发育及细胞(核)数目、以及卤虫休眠卵的生化适应性等方面的国内外研究成果及现状进行了综述,并提出应该在现有的研究基础上对Clegg的假设、卤虫卵内hsp70的分子结构特征、卤虫卵的卵壳结构及卤虫卵亚壳层的功能等方面进行深入研究,为卤虫休眠卵的基础生物学研究积累资料. 相似文献
106.
华北板块南缘自中元古代始,表现为沟弧盆体制的B型俯冲带,至中生代演化为大陆板块间碰撞挤压的A型俯冲带。这一大地构造格局及其演化决定着板缘成矿区带划分,并控制着区内不同矿产种类、不同矿床类型的成生规律和时空构型。板块南缘内生矿产丰富,矿床类型甚多,分布有序。它们是以燕山期构造-热事件为成矿动因的具有成生联系的有色金属-贵金属矿产成矿系列。板缘金矿类型甚多,主要有石英脉型、构造蚀变岩型、斑岩-接触交代型。各类矿床都具有成矿物质多来源、成矿溶液多来源和成矿作用多期次多阶段的特点。金的沉淀富集作用取决于有利的构造部位和成矿溶液性质的改变,而引起这一改变的原因是不同性质溶液的混合作用和热液运移过程中温压条件,及所遇围岩性质发生了根本转变。金的载体矿物主要为石英和黄铁矿,但随着不同矿化阶段和矿化环境常形成多样的矿石类型。 相似文献
107.
Ellen E. Deason 《Estuarine, Coastal and Shelf Science》1982,15(2):121-134
Surveys of the distribution, abundance and size of the ctenophore Mnemiopsis leidyi were carried out in Narragansett Bay, R.I. over a 5-year period, 1975–1979. Yearly variations were observed in time of initiation of the ctenophore increase and maximum abundance. Biomass maxima ranged from 0·2 to 3 g dry weight m?3 at Station 2 in lower Narragansett Bay while maximum abundance varied from 20 to 100 animals m?3. Ctenophores less than 1 cm in length generally composed up to 50% of the biomass and 95% of the numerical abundance during the peak of the M. leidyi pulse. During the 1978 maxima and the declining stages of the pulse each year, 100% of the population was composed of small animals. M. leidyi populations increased earlier, reached greater maximum abundances, and were more highly dominated by small animals in the upper bay than toward the mouth of the bay. The averageclearance rate of M. leidyi larvae feeding on A. tonsa at 22°C was 0·36 l mg?1 dry weight day?1, with apparent selection for nauplii relative to copepodites. Predation and excretion rates applied to ctenophore biomass estimated for Narragansett Bay indicated that M. leidyi excretion is minor but predation removed a bay-wide mean of 20% of the zooplankton standing stock daily during August of 1975 and 1976. Variation in M. leidyi predation at Station 2 was inversely related to mean zooplankton biomass during August and September, which increased 4-fold during the 5-year period. 相似文献
108.
Lars Clausen 《Natural Hazards》1992,6(2):181-190
To explain both origin and outcome of disasters (natural, technical, and war-borne), as well as social action during disasters proper, a macrosociological model of internal causation is introduced (PERDUE). It consists of six stages of possible, and of most likely paths of social change between these six (Peace is founded, Everyday routine, Rising class struggle, Disasters strike, Unconditional surrender of collective defence, and Evaporation of common values). The stages are developed by making use of three dimensions of social change (rapidity, radicality, and rituality), and described. 相似文献
109.
白庙地区是东濮凹陷勘探程度较高的含油气区,生气条件十分优越,已发现了Es2下,Es31,Es32,Es33-4 4套主要含油气层系。根据伊利石测年法和包裹体均一温度法综合分析了白庙地区天然气充注历史。研究表明白庙地区天然气主要分两次注入储层,一次为31.4~20.4 Ma,相当于东营组-馆陶组早期,另一次为2 Ma,相当于第四纪以来;第一阶段天然气成藏时期年龄绝大部分落入了剥蚀期年龄(27~17 Ma)段,是天然气藏的最主要形成时期,抬升剥蚀期压力下降,更有利于天然气成藏;第二阶段为2 Ma,相当于第四纪以来,馆陶组沉积以来白庙地区为欠补偿状态,无二次生气过程,一方面前梨园洼陷及葛岗集洼陷继续生气,生成的天然气向白庙构造运移,聚集成藏;另一方面是第一阶段形成气藏的重新调整。白庙地区天然气成藏期总体具有西早、东晚、北早、南晚的特点。 相似文献
110.
西藏尕尔穷铜金矿金矿物特征研究 总被引:7,自引:0,他引:7
尕尔穷铜金矿床是班公湖-怒江成矿带西段第一个达到详查程度的矽卡岩型铜金矿床。通过对矿床中金矿物的电子显微镜观察和扫描电镜能谱分析,查明了金矿物的类型及赋存状态,划分了成矿阶段。研究表明,金矿物有银-金矿物系列、铜-金矿物系列和少量碲化物类,主要有自然金、银金矿、金银矿、铜质金银矿、铜金矿、铜质银金矿和碲金银矿。金矿物主... 相似文献