A western boundary current east of New Caledonia: Observed characteristics     

Florent Gasparin  Alexandre Ganachaud  Christophe Maes 《Deep Sea Research Part I: Oceanographic Research Papers》2011,58(9):956-969

Waters from the South Equatorial Current (SEC), the northern branch of the South Pacific subtropical gyre, are a major supply of heat to the equatorial warm pool, and have an important contribution to climate variability and ENSO which motivated the Southwest Pacific Ocean and Climate Experiment (SPICE, CLIVAR/WCRP). Initially a broad westward current extending from the equator to 30°S, the SEC splits upon arriving at the major islands and archipelagoes of Fiji (18°S, 180°E), Vanuatu (16°S, 168°E), and New Caledonia (22°S, 165°E), resulting in a complex system of western boundary currents and zonal jets that feed the Coral and Solomon Seas. We focus here on the formation of one specific jet feeding the Coral Sea, the North Caledonian Jet (NCJ). Using a combination of recent oceanographic cruises, we describe the ocean circulation to the northeast of New Caledonia, where the SEC forms a western boundary current that ultimately becomes the NCJ. This current, which we document for the first time and propose to refer to as the East Caledonian Current (ECC), has its core located 10-100 km off the east coast of New Caledonia, and extends vertically to at least 1000 m depth. Water mass properties show continuous westward transports through the ECC, from the SEC to the NCJ in both the South Pacific Tropical Waters in the thermocline and Antarctic Intermediate Waters near 700 m depth. The ECC extends about 100 km horizontally; its average 0-1000 m transport was estimated at 14.5±3 Sv off the north tip of the New Caledonian reef, with a maximum of 20 Sv in May 2010. South of that the upstream branch of the ECC east of the Loyalty is close to 8 Sv suggesting an important additional contribution from central Pacific waters carried by the SEC at 16°S and diverted to our region through the western boundary current system east of Vanuatu.  相似文献   

影响XX带水凝析气田气油比变化因素分析     

王继立 《海洋地质译丛》2011,(2):72-74

气油比是已投入开发凝析气藏的一项重要开发指标。气油比的变化可反应气井、气藏生产状态,凝析气藏压力变化以及带水气藏边底水的推进程度。油藏工程研究人员还可据气油比变化对气井、气藏将来的生产形势做初步分析。因此,分析带水凝析气藏气油比变化规律以及对其影响因素进行深入剖析,对于凝析气藏生产具有重要的指导意义。  相似文献   

渤海浅层油田储层预测研究——以B2油田为例     

闫涛  苏进昌  高磊  王军  李宾 《海洋地质译丛》2011,(3):23-26,88

针对新近系明化镇组的油田地层较浅、地层反射结构相对简单的地质特点,如何充分挖掘地震资料中蕴含的丰富信息,并加以综合分析和利用,以满足不断增长的对于储层预测及含油气性预测的需求。通过一个储层预测实例表明,利用地震属性综合分析技术,可以较好地解决沉积相划分、储层预测、含油气判别等方面的地质问题。  相似文献   

Seismic random noise attenuation and signal-preserving by multiple directional time-frequency peak filtering     

《Comptes Rendus Geoscience》2015,347(1):2-12

Time-frequency peak filtering (TFPF) is an effective method for seismic random noise attenuation. The linearity of the signal has a significant influence on the accuracy of the TFPF method. The higher the linearity of the signal to be filtered is, the better the denoising result is. With this in mind, and taking the lateral coherence of reflected events into account, we do TFPF along the reflected events to improve the degree of linearity and enhance the continuity of these events. The key factor to realize this idea is to find the traces of the reflected events. However, the traces of the events are too hard to obtain in the complicated field seismic data. In this paper, we propose a Multiple Directional TFPF (MD–TFPF), in which the filtering is performed in certain direction components of the seismic data. These components are obtained by a directional filter bank. In each direction component, we do TFPF along these decomposed reflected events (the local direction of the events) instead of the channel direction. The final result is achieved by adding up the filtering results of all decomposition directions of seismic data. In this way, filtering along the reflected events is implemented without accurately finding the directions. The effectiveness of the proposed method is tested on synthetic and field seismic data. The experimental results demonstrate that MD–TFPF can more effectively eliminate random noise and enhance the continuity of the reflected events with better preservation than the conventional TFPF, curvelet denoising method and F–X deconvolution method.  相似文献   

黄海、东海区域漫衰减系数光谱遥感反演及激光测深性能评估     

李凯  童晓冲  张永生  哈长亮  申二华 《遥感学报》2015,19(5):761-769

本文在总结和比较中国现有黄海、东海海域漫衰减系数反演算法的基础上,利用水色测量数据分析得到漫衰减系数Kd(532)与Kd(490)之间的关系,为激光测深系统(以CZMIL为例)的性能评估提供了基础。利用MODIS二级数据产品评估了中国黄海、东海海域在CZMIL海道测量模式下最大可测水深的空间分布。研究结果表明CZMIL在黄海、东海海域可测水深基本在0—50 m,该区域的面积占研究区域面积的比例为76.2%,为浅海海域开展激光测深作业提供了测深能力评估的依据和方法。  相似文献   

东营凹陷八面河北部斜坡带构造特征及形成机制     

张蕾 《山东国土资源》2015,31(6)

研究了东营凹陷八面河北部斜坡带的断裂特征、构造演化特征及其形成机制,明确了该区的断裂展布特点和断层活动性,弄清了北部斜坡带的演化规律,同时分析该区的构造变形特征。结果表明：中生代以后,八面河地区存在2种独立的构造变形系统：一是板块边缘相互作用力;二是到后期由于板块的持续俯冲,地幔底辟作用在岩石圈底面产生的牵引力。八面河北部地区在这2种构造力的综合作用下,不同时期表现出不同的构造变形特征。  相似文献   

小牛煤矿晚二叠世含煤地层沉积环境与聚煤规律          下载免费PDF全文

李磊  谢兴友  王盼盼  赵蕻 《山东国土资源》2015,31(9)

小牛煤矿位于贵州省内水城矿区的格目底向斜东段北翼,含煤地层为晚二叠世龙潭组,含煤性好。通过对小牛煤矿含煤地层及其含煤性的研究,确定了研究区的沉积环境是海陆过渡相中的三角洲沉积类型,并初步建立了沉积模式,龙潭早期和晚期均有较好的聚煤作用发生并叠加,是聚煤的最佳场所,含煤性最好。  相似文献   

海底电缆多次波压制方法研究   总被引：2，自引：1，他引：1       下载免费PDF全文

马继涛  Sen K. Mrinal  陈小宏  姚逢昌 《地球物理学报》2011,54(11):2960-2966

多次波一直是影响地震处理与解释的主要因素之一.本文基于表层相关多次波衰减(Surface Related Multiple Elimination,SRME)理论,对其进行一定的改造,使其可以预测出海底电缆(Ocean Bottom Cable,OBC)数据中所有与表层相关的多次波,而后将预测出的多次波自适应减去.本文...  相似文献   

Hysteretic shear–flexure interaction model of reinforced concrete columns for seismic response assessment of bridges     

Jian Zhang 《地震工程与结构动力学》2011,40(3):315-337

  相似文献   

川滇及其邻区中强地震烈度衰减关系适用性研究   总被引：6，自引：0，他引：6  

孙继浩  帅向华 《地震工程与工程振动》2011,31(1):11-18

本文选取川滇及邻区作为研究区域,根据地震构造环境和震害分布特点,将该地区分为西南地区和盆地地区,选取该地区6级以上的典型历史震例,将其数字化得到等震线数据,通过对这些数据的统计回归分析,分别建立两个区域的地震烈度沿长轴与短轴的衰减关系、各烈度面积与地震震级的关系、破裂长度与震级的关系.同时,综合利用上述关系建立不同的地...  相似文献