Glass inclusions in volcanic rocks in the Okinawa Trough back-arc basin:constraints on magma genesis and evolution   总被引：1，自引：0，他引：1  

Yu Zenghui  Zhai Shikui  Li Xianzhong 《海洋学报(英文版)》2001,20(3):383-390

INTROOUcr1ONThe Okinawa Trough is a typical marginal back-arc basin, where its oPening began in rela-tively recent years* There is a great controversy about the origin of its initial magYna. haltand acid volcanic pumice make up the bimedal volcanism in the Okinawa Trough. MOSt of geol-ogists believed that the acid pumice was the preduct of extremely crystal fractionation of baseltInagTna, but the others argued that it should com from the melting of lower-crust. Som de-tailed petrolOgic…  相似文献   

Elemental geochemical records of seafloor hydrothermal activities in the sediments from the Okinawa Trough     

ZHAI Shikui  YU Zenghui  DU Tongjun 《海洋学报(英文版)》2007,26(4):53-62

The major and minor element contents in the sediment core H9 from the hydrothermal fields of the Okinawa Trough show a sharp change at the depth of 80 cm. The elements enriched in the upper 80 cm core are those enriched in the hydrothermal deposits and in the surface sediments recovered from the hydrothermal fields in the trough, which indicates the input of hydrothermal materials. Comparing with other hydrothermal sediments from Mid-ocean Ridges or the Lau Basin, the degree of the enrichment of elements iron, copper,cobalt, and nickel is relatively low. However, the enrichment of elements manganese, lead, arsenic, antimony and mercury is remarkable. The average contents of these elements in the upper 80 cm core sediments are three to six times those in the lower section, and 3~12 times those in the surface sediments which are not influenced by hydrothermal activities. Hydrothermal activities have contributed significant manganese, lead, arsenic, antimony and mercury to the sediments, and these elements are distinct indicators for the hydrothermal activity in the Okinawa Trough. The significant enrichment of these elements in Core H9 upward from the depth 80 cm indicates the start or the significant enhancing of the hydrothermal activity in this area at about 5 740 aB.P. The average accumulation rate of manganese during this period is about 40 461 μg/(cm2·ka), which is similar to the hydrothermal sediments in the Lau Basin or the East Pacific Rise.  相似文献   

小浪底水库溯源冲刷效率评估试验          下载免费PDF全文

李涛  张俊华  夏军强  马怀宝  郜国明  王增辉 《水科学进展》2016,27(5):716-725

水库溯源冲刷试验是评估在水库速降水位过程中,结合工程控制条件、水沙条件、冲刷时机和初始水库蓄水条件等因素,研究支流拦门沙坎破坏程度对干流溯源冲刷的影响。采用按照水库高含沙模型相似律建立的小浪底水库实体模型开展了4个组次的水库降水库区发生溯源冲刷的试验,第1~4组次库容恢复率依次为11.6%、6.8%、12.2%和6.6%。拦门沙坎破坏越严重,水量越大,库区溯源冲刷量越大,库容恢复率大;侵蚀基准面越低,库区溯源冲刷量大,库容恢复率大;库区淤积量42.00亿m3时采用降低水位引起库区发生溯源冲刷优于库区淤积量32.00亿m3。对原有的陕西水利科学研究所与清华大学的逐日溯源冲刷公式在考虑支流促因的基础上进行了改进,说明支流蓄水量进入干流越多,引起支流口以下的干流河段冲刷量越大,其计算结果与实测值满足生产实践精度,可作为多沙河流水库调水调沙方案制定参考。  相似文献   

宇宙尘似文象结构的图像分析和成因探讨   总被引：2，自引：0，他引：2  

李增慧  李先宜 《矿物学报》1989,9(3):241-244

宇宙尘较广泛地分布于各地质时代和各种岩石中,它形成在不同的物理化学环境下,因此具有比较复杂的结构构造。本文对产于不同时代、不同岩性岩石中具有似文象结构的宇宙尘进行了广泛的研究,一方面研究Si、Al等元素的赋存状态,另一方面研究这些元素与似文象结构的关系,进一步为它们的成因提供信息。  相似文献   

Applying the Dynamic Two-Step Method to Forecast Remaining Oil Distribution of Lower Series, Xiaermen Oilfield     

周红汤传意  李增辉 《中国地质大学学报(英文版)》2006,17(1):65-70

INTRODUCTIONThe distribution of remaining oil is often de-scribed qualitatively .The remaining oil distributedinthe whole reservoir is calculated according to thecharacteristics of the space distribution of the satura-tion of remaining oil . Logging data are required toaccomplish this . However , many such projects can-not be completed.This method of studyingremainingoil distribution cannot be quantified efficiently and isunable to provide an effective quantitative forecast ofthe distribu…  相似文献   

鲁西南地区地下水锰的分布特征及其成因          下载免费PDF全文

朱恒华  徐建国  王玮  王增辉  徐华  刘治政 《山东国土资源》2015,31(3)

为了解鲁西南地区地下水中锰的含量及其成因,采集并分析了276组地下水样和18组地表水样,结果表明,鲁西南平原区浅层地下水中锰含量在未检出至2.84mg/L之间,平均浓度为0.35mg/L,超标率达41%。鲁西南地区地下水中锰含量的分布与该区的工业化程度以及所处的补、径、排条件密切相关。影响地下水中锰含量分布的因素主要有表层土壤、地下水径流条件及含水层介质和地下水矿化度等。  相似文献   

遥感影像专题图制作研究     

韩金芳  张华平  王增辉  刘丽 《山东地质》2010,(10):48-51

遥感软件有强大的影像处理功能,地理信息软件有强大的矢量功能;由于遥感软件以国外进口软件为主,与国内常用的地理信息基础不适应。通过对遥感影像专题图的制作的研究,有效地解决了遥感软件和国产地理信息软件不匹配的问题,为各类遥感专题图制作提供了有效的技术方法。  相似文献   

水库异重流一维水沙耦合模型          下载免费PDF全文

王增辉  夏军强  李涛  郜国明  张俊华 《水科学进展》2015,26(1):74-82

建立了基于库区不规则断面的一维非恒定异重流数学模型,并采用明流与异重流水沙输移模型交替运算的两步模式,即用潜入条件动态判别异重流计算的上游边界位置,将潜入点上游的明流浑水段与下游异重流段计算连接起来。水流运动、泥沙输移与河床变形过程完全耦合,采用TVD(Total Variation Diminishing)形式的MUSCL-Hancock格式进行数值求解。将该模型应用于恒定流量与释放定量悬沙两种条件下的异重流水槽实验模拟,比较了有无水面梯度项对模拟精度的影响,计算结果表明该模型能较为准确地预测异重流的厚度、含沙量分布及传播过程。  相似文献   

用聚类分析模糊综合评判评价地质环境质量   总被引：12，自引：0，他引：12  

付延玲  骆祖江  王增辉 《煤田地质与勘探》1999,27(6):47-50

讨论了应用聚类分析、模糊综合评判进行地质环境质量评价的原理、方法和步骤,并将其应用于陕西省地质环境质量评价。根据陕西省地质环境复杂多变,受多因素制约的特征,将全省剖分成３５０ 个样品单元,选取地下水资源、地表水资源、水质、土地资源、地形地貌、岩土体特征、植被、气候、地震、滑坡、泥石流、地方病、水土流失、沙漠化、地面沉降、地裂缝、盐碱化、沼泽化等１５ 个变量作为评价因子,采用Ｑ 型聚类分析方法,将全省分成３７ 个地质环境质量分区,并通过模糊综合评判,将其划分成７ 个地质环境质量等级,客观地反映了陕西省地质环境质量的宏观分布特征。  相似文献   

Mineralogical characteristics of polymetallic sulfides from the Deyin-1 hydrothermal field near 15°S,southern Mid-Atlantic Ridge   总被引：1，自引：0，他引：1  

王淑杰  李怀明  翟世奎  于增慧  邵宗泽  蔡宗伟 《海洋学报(英文版)》2017,36(2):22-34

A seafloor hydrothermal field, named Deyin-1 later, near 15°S southern Mid-Atlantic Ridge(SMAR) was newly found during the 22 nd cruise carried out by the China Ocean Mineral Resources Research Development Association(COMRA). Sulfide samples were collected at three stations from the hydrothermal field during the26 th cruise in 2012. In this paper, mineralogical characteristics of the sulfides were analyzed with optical microscope, X-ray diffractometer, scanning electron microscope and electron microprobe to study the crystallization sequence of minerals and the process of hydrothermal mineralization. According to the difference of the ore-forming metal elements, the sulfide samples can be divided into three types:(1) the Ferich sulfide, which contains mainly pyrite and chalcopyrite;(2) the Fe-Cu-rich sulfide consisting predominantly of pyrite, chalcopyrite and isocubanite, with lesser amount of sphalerite, marmatite and pyrrhotine; and(3) the Fe-Zn-rich sulfide dominated by pyrite, sphalerite and marmatite, with variable amounts of chalcopyrite, isocubanite, pyrrhotine, marcasite, galena and gratonite. Mineral precipitations in these sulfides are in the sequence of chalcopyrite(isocubanite and possible coarse pyrite), fine pyrite,sphalerite(marmatite), galena, gratonite and then the minerals out of the dissolution. Two morphologically distinct generations(Py-I and Py-II) of pyrite are identified in each of the samples; inclusions of marmatite tend to exist in the coarse pyrite crystals(Py-I). Sphalerite in the Fe-Zn-rich sulfide is characterized by a"chalcopyrite disease" phenomenon. Mineral paragenetic relationships and a wide range of chemical compositions suggest that the environment of hydrothermal mineralization was largely changing. By comparison, the Fe-rich sulfide was formed in a relatively stable environment with a high temperature, but the conditions for the formation of the Fe-Cu-rich sulfide were variable. The Fe-Zn-rich sulfide was precipitated during the hydrothermal venting at relatively low temperature.  相似文献