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231.
232.
利用重力资料研究地壳分层结构的遗传反演方法 总被引:2,自引:0,他引:2
根据模型分解思想,采用变密度多层地壳密度模型,据此推导了相应的重力异常正演计算公式。以遗传算法为基础,结合上述重力异常正演公式,形成了地壳多层密度结构的遗传反演方法。 相似文献
233.
Limestone and clay samples were collected from Darukhula and adjoining areas of the Nizampur District Nowshera, N.W.EE, Pakistan, and analyzed for different parameters in order to search for new reserves of suitable material for the manufacture of different types of cements in N.W.F.P. It was found that the area under study contains three types of limestones, including high grade limestone, Darukhula limestone and siliceous limestone, which contain 53%, 49.03% and 45.19% CaO, respectively, and three types of clay, including maroon color, yellow to yel- lowish-green color and green color clay containing 57.76%, 65.47% and 61.24% SiO2, respectively. Chemical analysis of the limestone and clay samples collected from the deposits in the area under study showed that all the elements found in these samples are within the range of permissible limits for the production of high-strength Portland cement, sulphate resisting cement and white cement. This paper covers the detailed version of the potential raw material deposits at Darukhula and adjoining areas of the Nizampur District. 相似文献
234.
Post-orogenic and anorogenic A-type fluorite-bearing granitoids, Eastern Desert, Egypt: Petrogenetic and geotectonic implications 总被引:1,自引:1,他引:0
Fathy H. Mohamed 《Chemie der Erde / Geochemistry》2008,68(4):431-450
The present study focuses on four A-type fluorite-bearing granitic plutons in the Eastern Desert of Egypt which are classified into post-orogenic subsolvus (Homrit Waggat, 535 Ma; Homer Akarem, 541 Ma and Ineigi, 571 Ma) and anorogenic hypersolvus (Gabal Gharib, 476 Ma) granites. All the granites are Si- and alkali-rich and MgCaTi poor. Whereas both granite types appear relatively homogeneous in terms of most of their major and trace elements, they differ in that the subsolvus granites are depleted in TiO2, FeO*, Ba, Sr and Zr and enriched in Rb and Y with respect to the hypersolvus granites. The two granite types, however, can be distinguished more easily by their rare-earth element (REE) patterns. Chondrite-normalized REE patterns of the hypersolvus granite display a gull-wing shape, characterized by a large negative Eu anomaly and moderate-to-high LREE contents. Relative to the hypersolvus granite, subsolvus granite is depleted in LREE and more enriched in HREE contents. The increase of HREE in the subsolvus granite is presumably caused by F complexing during the late stage of its evolution. This is supported by the abundance of fluorite veins cross-cutting the subsolvus granite. The negative Eu anomalies in the subsolvus granite point to the role of feldspars as residual phase in the source, and as a crystallizing phase during magmatic differentiation.Field relations, textural, mineralogical and geochemical data of the post-orogenic subsolvus granite are consistent with its derivation from a parental basic magma through crystal-liquid fractionation of alkali feldspar, plagioclase, amphibole, FeTi oxides, titanite, zircon, monazite and allanite. Crystallization occurred in a water-enriched and rather oxidizing environment, as a result of which the entire suite has a transitional character between that of a post-orogenic and an anorogenic setting. On the other hand, the most credible mechanism for the origin of the anorogenic hypersolvus granite is partial melting of I-type granodiorite-monzogranite source rocks in the study area. 相似文献
235.
236.
以2014年构建的壳金长牡蛎(Crassostrea gigas)全同胞家系为亲本,通过近交和设置对照组的方法,研究了近交对壳金长牡蛎家系幼虫期与稚贝期生长和存活的影响。结果表明,在整个实验期间,壳金F1家系的壳高、壳长和存活率均小于对照组。壳金F1家系的壳高和壳长仅在1日龄、190日龄与对照组差异不显著(P0.05),存活率仅在20日龄时与对照组差异显著(P0.05)。幼虫期,壳金F1家系壳高的近交衰退率范围为0.85%—13.70%,壳长的近交衰退率范围为0.75%—10.83%,存活率的近交衰退范围为4.24%—27.44%。稚贝期,壳金F1家系壳高的近交衰退率范围为6.16%—9.90%,壳长的近交衰退率范围为1.76%—14.21%,存活率的近交衰退范围为1.92%—4.18%。 相似文献
237.
238.
R. J. Wilman A. C. Fabian R. M. Cutri C. S. Crawford & W. N. Brandt 《Monthly notices of the Royal Astronomical Society》1998,300(1):L7-L10
We report long, pointed ROSAT HRI observations of the hyperluminous galaxies IRAS F00235+1024, F12514+1027, F14481+4454 and F14537+1950. Two of them are optically classified as Seyfert-like. No X-ray sources are detected at the positions of any of the objects, with a mean upper limit L X / L Bol ≃ 2.3 × 10−4 . This indicates that any active nuclei are either atypically weak at X-ray wavelengths or obscured by column densities N H > 1023 cm−2 . They differ markedly from 'ordinary' Seyfert 2 galaxies, bearing a closer resemblance in the soft X-ray band to composite Seyfert 2 galaxies or to some types of starburst. 相似文献
239.
本文利用电离层数字测高仪 (DPS - 4)所测的f0 F2和从美国NOAA和DMSP卫星观测估算的半球功率指数和午夜极光区赤道侧边界纬度等资料 ,考察中山站电离层的极区特征。结果表明 ,冬季中山站电离层内的电离生成主要取决于从磁层沉降的粒子。在太阳活动和地磁变化宁静环境下 ,磁正午极隙区内的软粒子是最主要的电离源 ,它能使f0 F2达全天的最大值 ;上、下午各有数小时处于极光带内时 ,高能粒子的电离作用也很重要 ;夜间进入极盖区后 ,电子密度则很低。夏季太阳辐射电离效应使f0 F2值比冬季增加 1- 1 .5MHz,而其日变化的最大值时间也提前了 1- 2hr。发生很大扰动时 ,极隙区和极光带的位置均向低纬方向移动。若中山站日间也处于极盖区内时 ,电子密度会大幅度下降 ,并常接收不到电离层回波的信号。在中等扰动环境下情况更加复杂。由于高纬电离层对流速度很高 ,离子 /中性分子间的碰撞复合系数就很大。热层中性大气全球经向环流对高纬电离层电子密度的增加无显著作用。磁暴期间中午从极隙区向南的等离子体对流对中山站f0 F2的增高也无明显影响。 相似文献
240.
利用动态平差原理,处理了克孜尔水库水准监测网的14期跨断层流动水准资料,对穿过库区主坝、副坝之间F2断层的形变机制进行了初步研究。结果表明F2断层的活动属继承性活动,其活动方式为小幅度蠕变。这种活动方式对库区应力集中起到了解除的作用。 相似文献