OCEAN BOTTOM SEISMOMETER AND ONSHOREOFFSHORE SEISMIC EXPERIMENT IN NORTHEASTERN SOUTH CHINA SEA   总被引：7，自引：0，他引：7  

QIU Xuelin~ 《大地构造与成矿学(英文版)》2004,28(1):28-35

Three-component Ocean Bottom Seismometers, portable land stations and marine air gun seismic sources were used to carry out an onshore-offshore deep seismic profile in northeastern South China Sea. This profile, orientated in NNW-SSE, was as long as 500 km and perpendicular to the strike of regional tectonics. The offshore data were processed in Taiwan Ocean University using a number of available software and the onshore data were analyzed in South China Sea Institute of Oceanology by new-written programs and public software. Preliminary results show that the seismic data are in good quality and contain rich information of deep structure. Seismic phases, e.g. Pg, PmP and Pn, are identified in the offset range 5～220 km, which will provide an important dataset for the deep crustal structure and oil-gas basin evolution studies of this region.  相似文献   

EARTHQUAKE FOCAL MECHANISM AND ITS TECTONIC SIGNIFICANCE ALONG THE TWO SIDES OF THE RED RIVER FAULT ZONE   总被引：1，自引：0，他引：1  

ZHU Junjiang~*  ZHAN Wenhuan  QIU Xuelin  XU Huilong  TANG Cheng 《大地构造与成矿学(英文版)》2004,28(1):79-92

The Red River Fault Zone is a gigantic slide-slip fault zone extending up to 1000km from Tibet to South China Sea. It has been divided into the north, central and south segments according to the difference of the geometry, kinetics, and seismicity on the land, but according to the contacted relationship between the old pre-Cenozoic block in Indochina Peninsula and the South China block, the Red River Fault Zone was divided into two parts extending from land to ocean, the north and south segments. Since the Tertiary, the Red River Fault Zone suffered first the sinistral movement and then the dextral movement. The activities of the north and the south segments were different. Based on the analysis of earthquakes and focal mechanism solutions, earthquakes with the focus depths of 0-33km are distributed over the whole region and more deep earthquakes are distributed on the northeastern sides of the Red River fault. Types of faulting activities are the thrust in the northwest, the normal in the north and the  相似文献   

Sludge Bulking Property of Membrane Bio-reactor in Albumen Wqastewater Treatment     

ZHANG Ying~ 《地球科学进展》2004,(Z1)

Albumen wastewater was treated by Membrane Bio-reactor. Sludge bulking property of Membrane Bio-Reactor was investigated in this study through contrast research. When the sludge bulking appeared, the removal efficiency of COD in Membrane Bio-reactor increased slightly under the function of filamentous bacteria. However, the negative effects of the higher net water-head differential pressures,the higher block rate of membrane pore and the great quantity of filamentous bacteria at the externalsurface presented at the same time. Thus, plenty of methods should be performed to control sludge bulking once it happened in Membrane Bio-reactor.  相似文献   

The Cenozoic Volcanoes in Northeast China     

LIU Jiaqi  HAN Jingtai  GUO Zhengfu 《东北亚地学研究》2002,(2)

1　ＧｅｏｌｏｇｉｃａｌＢａｃｋｇｒｏｕｎｄＥｖｅｎｎｏｆａｓｃｉｎａｔｉｎｇｖｏｌｃａｎｉｃｅｒｕｐｔｉｏｎｏｃｃｕｒｒｅｄｉｎＣｈｉｎａｉｎｍｏｄｅｒｎｔｉｍｅｓ ,ｔｈｅｒｅａｒｅｍａｎｙＣｅｎｏｚｏｉｃｖｏｌｃａ ｎｏｅｓａｎｄｖｏｌｃａｎｉｃｒｏｃｋｓｄｉｓｔｒｉｂｕｔｅｄｉｎｔｈｅｅａｓｔｅｒｎｃｏｎｔｉ ｎｅｎｔｍａｒｇｉｎａｎｄｔｈｅｎｏｒｔｈｅｒｎＴｉｂｅｔａｎｐｌａｔｅａｕ .Ｅｓｐｅｃｉａｌｌｙｔｈｅｆｒｅｑｕｅｎｔｖｏｌｃａｎｉｃａｃｔｉｖｉｔｉｅｓｏｃｃｕｒｒｅｄｉｎｎｏｒｔ…  相似文献   

Monitoring the anthropogenic impact on the muddy coast by means of topographic and bathymetric surveys north of the Yellow River Mouth,China     

HU Guanghai )  *  YAN Tong )  WANG Xiuqin )  ZHONG Delin )) First Institute of Oceanography  S.O.A.  Qingdao  P..R.China) Ocean University of China  Qingdao  P..R.China 《中国海洋大学学报(英文版)》2004,3(2):195-200

1　Introduction　Manhasmodifiedmanyoftheworld’scoastlines ,eitherdirectlybyconstructionordredging ,orindi rectlyasaresultofenvironmentalchangesthatinflu encesedimentsupply ,runoff,orclimate (Johns ,1995 ) .HumanactivityhasalsoproducedthemostprofoundeffectsonthecoastalenvironmentinChina .Forex ample,damconstructions ,whichrestrictpeakflowsintheupstreamoftheYellowRiver ,couldgreatlyre ducethenaturalsupplyofsedimentintotherivermouthandresultintheerosionofbeaches .　Inrecentyears,manystudiescon…  相似文献   

三维交流电测井的有限元方法     

杨 《地球物理学报》2002,45(Z1):410-417

为了模拟三维地层中交流电测井的响应,本文考虑位移电流的影响,导出了用位函数A-Ф描述此问题的矩阵算子方程;证明了该矩阵算子是自伴算子;并由自伴算子的具势性得到了矩阵算子方程的泛函.最后用基于A-Ф的有限元方法计算了一维、二维及三维地层模型的交流电测井的响应.  相似文献   

烟台市环境气象预报服务系统     

黄少军  薛 《山东气象》2002,22(1):39-40,42

概述了烟台市环境气象预报服务系统的特点及主要功能，简要介绍了服务产品的主要内容及应用情况。该系统以T106产品、常规大气观测资料、公益及专业天气预报、空气污染浓度观测值等为基本资料，集信息采集、产品制作与分发及工作管理于一体，可以制作10种城市环境气象预报服务产品，并自动编写空气质量日报、预报报文。投入业务使用后，取得了较高的业务及社会经济效益。  相似文献   

AN EXPERIMENTAL STUDY ON BEDMAKING AND CATASTROPHIC PROCESSES IN ISLAND BRAIDED CHANNEL     

Desheng JIN  Project 《国际泥沙研究》1997,(3)

LINTRODUCTIONAstudyonevolutionandpredictionofthefluvialgeomorphicsystemhasdevelopedinthe1970's(Scheideggef,1975),andisstillapplied.Fromthemiddleofthe1980'son,researchofcatastrophicprocessesinthefluvialgeomorphicSystem(catatrophism,hazards)hasbeenfocusedon(SchummandChorley,1983,ShenandSchumm,1981,Chorley,SchununandSugden,1985).WhenafluvialgeomorphicSystemislocatedatthelinearregionofanollequilibriumstatebutveryclosetoequilibriumone,theboundaryconditionprotectstheSystemfromequilibrium,an…  相似文献   

Unconformity-like Reflection Pattern under the Moho in the Sulu Area   总被引：1，自引：0，他引：1  

YANG Wencai 《Continental Dynamics》1997,(1)

1.IntroductionSincethediscoveryofcoesiteandndcrodiamond,theDabie-Suluultra-highPressure(UHP)meta-morphicbelthasbeenattractingworldwideattentionsofgeoscientists.Studyingthisoutstandinggeologicalregionmaygreatlyenhanceourunderstandingofmetamorphism,deepeffectsofcontinentalcollisionandgeodynandcsinconvergentplateboundaries.Thestudymayalsobeveryhelpfultoprovideevidencetorevealinteractionbetweenthecrustandthemantle,andtheformationofnewtypesofdiamonddeposits.EncouragedbytheinternationalContinenta…  相似文献   

地洼学说在世界级超大型铀矿研究中得到应用     

据俄罗斯《矿床地质学》年第卷第期刊登的В.Ч.卡赞斯基等人的文章《额尔康斯克铀矿区形成历史及地质特征》中  在进行区域成矿对比时  把它与东南地洼区赣杭铀矿带进行对比。赣杭铀矿一带呈北东°～°方向延伸达km  宽～km  由余个矿床组成  在空间上产于扬子准地台 《大地构造与成矿学》2001,25(1):108

据俄罗斯《矿床地质学》2000年第42卷第3期刊登的В.Ч.卡赞斯基等人的文章《额尔康斯克铀矿区形成历史及地质特征》中，在进行区域成矿对比时，把它与东南地洼区赣杭铀矿带进行对比。赣杭铀矿一带呈北东45°～60°方向延伸达600km，宽50～80 km，由40余个矿床组成，在空间上产于扬子准地台(江南地洼区)和华南加里东褶皱带(东南地洼区)的结合处。从晚元古代开始，该带发育深大断裂，而且其位置随时间而变，从泥盆系中期到三叠纪为活化的地台体制，然后进入地洼体制或者构造岩浆活化体制[1988，陈国达]。侏罗纪在其范围内或周边地区产生火山构造或者喷发中心，充填了酸性或中性火山岩。赣杭铀矿带成为巨型鄂霍次克—楚科奇—闽浙大陆边缘火山带的旁侧分枝，是太平洋矿带的内带和外带的分界线；在白垩纪，赣杭带轴部又被红色沉积碎屑岩充填，它具有陆内裂谷构造的最终形态特点。 谭克仁供稿 2001.1.19  相似文献