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排序方式: 共有995条查询结果,搜索用时 234 毫秒
71.
就目前锚索抗滑桩的研究现状来看,基本上都是将锚索和抗滑桩分开计算,忽略了锚索与抗滑桩之间存在的相互作用关系。针对这一问题,对锚索-抗滑桩-岩土体相互作用系统的计算方法进行了研究。提出了在锚索抗滑桩设计计算中,除了应考虑锚索的强度外。还应该考虑锚索的伸长量,使其与桩的变形相协调。在此基础上,建立了新的锚索抗滑桩计算理论。本文用该方法进行了工程实例分析,并与其他计算方法所得结果进行了对比。 相似文献
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Magmatic History of Somma-Vesuvius on the Basis of New Geochemical and Isotopic Data from a Deep Borehole (Camaldoli della Torre) 总被引:3,自引:0,他引:3
Di Renzo V.; Di Vito M. A.; Arienzo I.; Carandente A.; Civetta L.; D'antonio M.; Giordano F.; Orsi G.; Tonarini S. 《Journal of Petrology》2007,48(4):753-784
A continuous-coring borehole recently drilled at Camaldoli dellaTorre on the southern slopes of SommaVesuvius providesconstraints on the volcanic and magmatic history of the Vesuvianvolcanic area since c. 126 ka BP. The cored sequence includesvolcanic units, defined on stratigraphical, sedimentological,petrological and geochemical grounds, emitted from both localand distal vents. Some of these units are of known age, suchas one Phlegraean pre-Campanian Ignimbrite, Campanian Ignimbrite(39 ka), Neapolitan Yellow Tuff (14· 9 ka) and VesuvianPlinian deposits, which helps to constrain the relative ageof the other units. The main rock types encountered are shoshonite,phonotephrite, latite, trachyte and phonolite. The sequenceincludes, from the base upwards: a thick succession of pyroclasticunits emplaced between 126 and 39 ka, most of them attributedto eruptions that occurred in the Phlegraean area; the CampanianIgnimbrite; the products of a local tuff cone formed between39 ka and the deposition of the products of the earliest activityof the Mt. Somma volcano; the products of the SommaVesuviusvolcano, which include from the base upwards a thick sequenceof lavas, pyroclastic rocks and the products of a local spattercone dated between 3· 7 ka and AD 79. The data obtainedfrom the study of the borehole show that, before the CampanianIgnimbrite eruption, low-energy explosive volcanism took placein the Vesuvian area, whereas mostly high-energy explosive eruptionscharacterized the Campi Flegrei activity. In the Vesuvian area,Campanian Ignimbrite deposition was followed by the eruptionof a local tuff cone and a long repose time, which predatedthe formation of the Mt. Somma edifice. Since 18· 3 ka(Pomici di Base eruption) the activity of SommaVesuviusbecame mostly explosive with rare lava effusions. The shallowestcored deposits belong to the Camaldoli della Torre cone, formedbetween the Pomici di Avellino and Pomici di Pompei eruptions(3· 7 kaAD 79). New geochemical and SrNdPbB-isotopicdata on samples from the drilled core, together with those availablefrom the literature, allow us to further distinguish the volcanicrocks as a function of both their provenance (i.e. Phlegraeanor Vesuvian areas) and age, and to identify different magmaticprocesses acting through time in the Vesuvian mantle source(s)and during magma ascent towards the surface. Isotopically distinctmagmas, rising from a mantle source variably contaminated byslab-derived components, stagnated at mid-crustal depths (810km below sea level) where magmas differentiated and were probablycontaminated. Contamination occurred either with Hercynian continentalcrust, mostly during the oldest stages of Vesuvian activity(from 39 to 16 ka), or with Mesozoic limestone, mostly duringrecent Vesuvian activity. Energy constrained assimilation andfractional crystallization (EC-AFC) modelling results show thatcontamination with Hercynian crust probably occurred duringdifferentiation from shoshonite to latite. Contamination withlimestone, which is not well constrained with the availabledata, might have occurred only during the transition from shoshoniteto tephrite. From the deep reservoir, magmas rosetowards a series of shallow reservoirs, in which they differentiatedfurther, mixed, and fed volcanic activity. KEY WORDS: SommaVesuvius; crustal contamination; source heterogeneity; radiogenic and stable isotopes; magmatic system 相似文献
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Johnson Simon P.; de Waele Bert; Tembo Francis; Katongo Crispin; Tani Kenichiro; Chang Qing; Iizuka Tsuyoshi; Dunkley Daniel 《Journal of Petrology》2007,48(7):1411-1441
The southern Irumide Belt (SIB) is an ENEWSW-trending,late Mesoproterozoic orogenic belt located between the CongoTanzaniaBangweulu(CTB) and Kalahari cratons in central southern Africa. It isseparated from the late Mesoproterozoic Irumide Belt (IB) tothe north by Permo-Triassic graben, raising the possibilitythat the younger rifts reactivated a suture between the twobelts that has been rendered cryptic as a result of youngerKaroo cover. Both belts are dominated by calc-alkaline gneisses,but in addition the SIB contains abundant metavolcanic and metasedimentaryrocks. In this study we present detailed geochemical, isotopicand geochronological data for volcanic and plutonic lithologiesfrom the southernmost part of the SIB, the CheworeRufunsaTerrane. This terrane comprises a wide variety of supracrustalto mid-crustal rocks that have major- and trace-element compositionssimilar to magmas formed in present-day subduction zones. Chondrite-normalizedrare earth element (REE) profiles and whole-rock SmNdisotope compositions indicate that the parental supra-subductionmelts interacted with, and were contaminated by sialic continentalcrust, implying a continental-margin-arc setting. Secondaryionization mass spectrometry dating of magmatic zircon has yieldedcrystallization ages between c. 1095 and 1040 Ma, similar toelsewhere in the SIB. UPb dating and in situ LuHfisotopic analyses of abundant xenocrystic zircon extracted fromthe late Mesoproterozoic granitoids indicate that the contaminantcontinental basement was principally Palaeoproterozoic in ageand had a juvenile isotopic signature at the time of its formation.These data are in contrast to those for the IB, which is characterizedby younger, c. 1020 Ma, calc-alkaline gneisses that formed bythe direct recycling of Archaean crust without significant additionof any juvenile material. We suggest that the SIB developedby the subduction of oceanic crust under the margin of an unnamedcontinental mass until ocean closure at c. 1040 Ma. Subsequentcollision between the SIB and the CTB margin led to the cessationof magmatism in the SIB and the initiation of compression andcrustal melting in the IB. KEY WORDS: geochemistry; Mesoproterozoic; SHRIMP zircon UPb dating; SmNd isotopes; Southern Irumide Belt 相似文献
76.
压力分散型锚索性能研究 总被引:1,自引:0,他引:1
赵世华 《中国地质灾害与防治学报》2007,(Z1)
文章在考察研究了国内应用压力分散型锚索治理不稳定边坡的工程实例的基础上,参考其它有关该方面的研究成果,分析了压力分散型锚索的作用机理、结构构造、破坏模式、承载力影响因素、耐久性能等,总结了压力分散型锚索的工程应用优势与不足,为引入该类锚索结构在湖南省滑坡及崩塌地质灾害治理工程中推广应用作了技术准备。 相似文献
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4地下连续墙施工技术方法4.1要点(1)导墙的修筑精度(宽度、平直度、垂直度和标高等)和强度对成槽施工质量有直接影响,高质量的导墙是高质量槽段的基础,常用的导墙形式如图2所示。图2导墙断面形式示意图(a)板型;(b)L型;(c)倒L型;(d)槽型导墙... 相似文献
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Processes of the deposition and vicissitude of Mu Us Desert, China since 150 ka B.P. 总被引:1,自引:0,他引:1
Li Baosheng Jin Heling Lü Haiyan Zhu Yizhi Dong Guangrong Sun Donghuai Zhang Jiashen Gao Quanzhou Yan Mancun 《中国科学D辑(英文版)》1998,41(3):248-254
“Milanggouwan stratigraphical section” named lately takes down 27 cycles of alternately evolutionary histories of desert depositions
in the Mu Us area with the fluviolacustrine facies and palaeosols since 150 ka B. P. Studies show that the sedimentary form
was induced by the growth and decline and confrontation each other between the winter monsoon and the summer monsoon of East
Asia in the past 150 ka.
Project supported by the National Natural Science Foundation of China (Grant No. 49473192). 相似文献
80.
深基坑锚杆护坡桩支护结构稳定性评价 总被引:3,自引:0,他引:3
锚杆护坡桩是深基坑工程常用的一种支护结构。文中对设计中所涉及到的结构稳定性评价问题进行了探讨,利用Kranz理论一些假设和条分法原理,提出了深基坑锚杆抗护坡桩稳定性评价的方法。该方法克服了Kranz理论中的一些不足,简化了条分法的计算并通过支护工程验证,具有一定的实用价值。 相似文献