Submarine canyons on the north of Chiwei Island:influenced by recent extension of the southern Okinawa Trough     

ZHAO Yuexi  LIU Baohu  LI Xishuang  LIU Chenguang  WU Jinlong  WANG Kuiyang 《海洋学报(英文版)》2008,27(4):63-72

Based on new multibeam bathymetric data and about 300 km long single seismic profiles, three topographic units were identified： the canyons, fractural valley and submarine terrace on the north of Chiwei Island where is a structural transition zone between the southern trough and the middle trough. The Chiwei Canyon and the North Chiwei Canyon are two of the largest canyons in the East China Sea （ECS） slope. Topographic features and architectures of them are described. The study shows that both of them are originated along faults. The evolution and spatial distribution of topographic units in the study area are controlled mainly by three groups of faults which were formed and reactive in the recent extensional phase of Okinawa Trough. The Chiwei Canyon was initia- ted during the middle Pleistocene and guided by F4 that is a N--S trending fault on the slope and F1, a large NW--SE trending fault on the trough. The pathway migration from the remnant channel to the present one of Chiwei Canyon is the result of uplift of tilted fault block that is coupled to the recent extension movements of the southern trough. The submarine terrace is detached from the ECS slope by the NEE -trending fault. The North Chiwei Canyon, developing during the late Pleistocene, is guided by FS, a N-S trending fault, diverted and blocked by the submarine terrace.  相似文献   

Site fidelity and movements of gilthead sea bream (Sparus aurata) in a coastal lagoon (Ria Formosa, Portugal)     

David Abecasis  Karim Erzini 《Estuarine, Coastal and Shelf Science》2008,79(4):758-763

Short-time site fidelity and movements of gilthead sea bream (Sparus aurata) in a coastal lagoon were determined using passive acoustic telemetry. Nine fish, ranging from 20.1 to 32.5 cm total length, were surgically implanted with acoustic transmitters and monitored for up to 179 days. Minimum convex polygon areas ranged from 18,698.6 m² to 352,711.9 m². Home range sizes were small, with individuals using core areas on a daily basis. However, these core areas shifted within the study site over time towards the opening to the sea. Two different diel behaviors were recorded, with some individuals more active at night and others during day time. Some individuals also demonstrated homing abilities, returning to the capture site after being released more than 4 km away.  相似文献   

On tectonic movement in the South China Sea during the Cenozoic   总被引：1，自引：1，他引：0  

LIN Changsong  CHU Fengyou  GAO Jinyao  TAN Yonghua 《海洋学报(英文版)》2009,28(1):25-36

The tectonic movement taking place at the end of Cretaceous and the beginning of Cenozoic had opened the Cenozoic phase of polycyclic tectonic movements, then the whole crust of the South China Sea had been mainly subjected to the regional stress field of tectonic tension, which was characterized by rifting depression. Seven times of regional tectonic movement and sedimentation had been assembled into a geological development history of polycyclic oscillation. Especially, the tectonic movements were strongly intensified at the end of Cretacious and the beginning of Paleagene, between Late Eocene and MidOligocene, during Mid and Late Miocene. These three times of tectonic movement had built the most important regional tectonic interfaces in the South China Sea. Crust movements of the South China Sea were the result and epitome of interaction of the Eurasia, Pacific and IndoAustralia plates, that is, they were introduced by polycyclic changes of directions, rates and strengths of lithospheric movements and asthenospheric flows across the Pacific and IndoAustralia plates.  相似文献   

近年来长江河口北支水沙特性与河槽稳定性分析   总被引：3，自引：0，他引：3  

冯凌旋  李九发  戴志军  闫虹  赵建春 《海洋学研究》2009,27(3):40-47

根据崇头、青龙港、三条港和连兴港1950～2001年潮汐潮流观测资料和2005年6～7月的大、中、小潮及2007年5月5～10日沿北支河槽进行的两个连续潮周期水、沙、盐的现场观测数据并结合参考2005年的实测地形图.通过对长时间序列(1950～2001年)的分流比、年均流量、潮位、潮历时等数据的整理分析并与近期(1998～2005年)的水文特征值比较,发现随着北支分流量逐渐减少,河槽内强烈的潮波已成为影响北支河槽不稳定的主要因素;青龙港近年来(1998～2005年)平均高、低潮位出现增高,比多年(1950～2001年)平均高、低潮位分别高出15和17cm,是北支河床近年来持续性淤浅的体现;大潮期间北支河槽涨潮含沙量无论量值还是扩散强度均大于落潮,明显表现出河口涨潮槽具有的泥沙运动规律.自2001年以来除少数年份的小潮汛外,均表现出明显的涨潮优势,其中2002年3月大潮的潮量优势流仅为9.42%,显示出涨潮优势十分明显,说明北支河槽近几年来正朝着衰退的过程发展;2005年北支河槽-2、-4和-6 m等深线均呈喇叭状,闭合端指向上游,符合涨潮槽的几何形态;再从河槽类型系数(λ)看,大潮期间λ值均大于1,最大值为31.1,涨潮槽特征显著;而洪季中、小潮各测站λ值均小于1,最小值为0.000 3,A、B两测站在大潮时λ值均大于1,而小潮时又都小于1,显示北支河槽虽主要表现为涨潮槽的特征,但洪季受径流和潮汛影响,其涨潮槽特性不稳定.总体而言,目前北支河槽为一条不稳定的废弃型涨潮槽.  相似文献   

南海及其周缘地区全新世海平面遗迹的构造含义     

孙桂华  邱燕  朱本铎 《海洋学报》2009,31(5):58-68

通过对海南岛海岸带野外考察,在文昌市铜鼓岭石头公园观察到高程为30m的海平面遗迹,在东方市黄流镇观察到高程为25~35m的海平面遗迹,在三亚市鹿回头观察到高程为2.5m的海平面遗迹。综合研究前人在该区关于海平面变化的研究成果,得出如下几点初步认识:(1)南海及其周缘地区中全新世以来海平面呈下降趋势,海平面最高位置出现在7000a左右、高于现代海平面3m左右的位置;(2)南海中全新世以来海平面遗迹所揭示的古海平面高程的差异性是古海平面本身持续下降和该区地壳差异性垂直运动共同作用的结果;(3)南海及其周缘地区中全新世期间中央海盆及其西缘的珠江口、红河、湄公河和昭披耶河4个河流三角洲地区为构造沉降区,而南海周缘的台湾岛、雷州半岛、印支半岛、南马来半岛、爪哇岛和苏拉威西岛6个地区为构造抬升区,抬升幅度最大的地方在台湾岛。  相似文献   

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单斌  傅容珊  郑勇 《大地测量与地球动力学》2009,29(1):46-51

???????????????????????????鹹????????????μ?????????????????????????????????????μ??????????????????1?????????????????????????????2???????????????μ????????????γ???????￡???80??????????????????????????????????????????μ???????????????60???????3??????????????????????????????????????????????????????????????????????С??????????????????μ????????????????????????4???????????????????й?????γ??????????????????????????  相似文献   

耿达短水准异常与汶川8.0级地震   总被引：2，自引：1，他引：1  

苏琴  朱航  杨永林 《大地测量与地球动力学》2009,29(Z1):103-105

结合龙门山断裂带其他跨断层资料,对耿达短水准在汶川8.0级地震前后的观测资料进行了重新分析,发现耿达短水准在汶川地震前后的异常为当地居民修建生活小区所致,不应视为地震前兆异常。  相似文献   

Spatial Variability of Mass Movements in the Satluj Valley,Himachal Pradesh during 1990～2006     

Vikram Gupta  M. P. Sah 《山地科学学报》2008,5(1):38-51

Satluj Valley is known to have a history of landslides and related mass movement activities since the geological times. Geological and geomorphological settings combined with anthropogenic activities constitute a propensity towards slope failure. During the last two decades,the area witnessed substantial increase in athropogenic pressure,mainly due to the exploitation of hydropower potential,changing landuse pattern and population growth. In addition,a shift of the climatic patterns in the form of larger area falling under the influence of rains was observed. These natural as well as anthropogenic changes in the area have resulted in increased spatial coverage of landslide in the area. This paper documents these changes during 1990～2006.  相似文献   

Submarine canyons on the north of Chiwei Island: influenced by recent extension of the southern Okinawa Trough     

ZHAO Yuexi  LIU Baohu  LI Xishuang  LIU Chenguang  WU Jinlong  WANG Kuiyang 《海洋学报(英文版)》2008,27(4):63-72

Based on new multibeam bathymetric data and about 300 km long single seismic profiles, three topographic units were identified:the canyons, fractural valley and submarine terrace on the north of Chiwei Island where is a structural transition zone between the southern trough and the middle trough. The Chiwei Canyon and the North Chiwei Canyon are two of the largest canyons in the East China Sea (ECS) slope. Topographic features and architectures of them are described. The study shows that both of them are originated along faults. The evolution and spatial distribution of topographic units in the study area are controlled mainly by three groups of faults which were formed and reactive in the recent extensional phase of Okinawa Trough. The Chiwei Canyon was initiated during the middle Pleistocene and guided by F4 that is a N-S trending fault on the slope and F1, a large NW-SE trending fault on the trough. The pathway migration from the remnant channel to the present one of Chiwei Canyon is the result of uplift of tilted fault block that is coupled to the recent extension movements of the southern trough. The submarine terrace is detached from the ECS slope by the NEE-trending fault. The North Chiwei Canyon, developing during the late Pleistocene, is guided by F5, a N-S trending fault, diverted and blocked by the submarine terrace.  相似文献   

青岛近海大型水母漂移集合预测方法研究   总被引：1，自引：0，他引：1  

吴玲娟  高松  刘桂艳  白涛 《海洋预报》2015,32(2):62-71

考虑水母垂直运动等自主运动,基于集合预报和拉格朗日粒子追踪方法,建立青岛近海大型水母的集合漂移预测模型。并利用2012—2013年青岛近海水母实时监测数据和集合漂移预测模型,快速预测水母集合漂移轨迹、速度、趋势和可能影响范围等要素。通过分析水母监测数据和数值模拟结果,在水母如何自主运动及其机理尚不十分清楚的情况下,多轨迹漂移预测结果比单轨迹的更合理、科学、可信,能够传达更多的信息量,对水母灾害的应急处置更具有指导意义。  相似文献