Seismic phases from the Moho and its implication on the ultraslow spreading ridge   总被引：1，自引：0，他引：1  

ZHANG Jiazheng  ZHAO Minghui  QIU Xuelin  LI Jiabiao  RUAN Aiguo 《海洋学报(英文版)》2013,32(12):75-86

The Moho interface provides critical evidence for crustal thickness and the mode of oceanic crust accretion. The seismic Moho interface has not been identified yet at the magma-rich segments （46°-52°E） of the ultra- slow spreading Southwestern Indian Ridge （SWIR）. This paper firstly deduces the characteristics and do- mains of seismic phases based on a theoretical oceanic crust model. Then, topographic correction is carried out for the OBS record sections along Profile Y3Y4 using the latest OBS data acquired from the detailed 3D seismic survey at the SWIR in 2010. Seismic phases are identified and analyzed, especially for the reflected and refracted seismic phases from the Moho. A 2D crustal model is finally established using the ray tracing and travel-time simulation method. The presence of reflected seismic phases at Segment 28 shows that the crustal rocks have been separated from the mantle by cooling and the Moho interface has already formed at zero age. The 2D seismic velocity structure across the axis of Segment 28 indicates that detachment faults play a key role during the processes of asymmetric oceanic crust accretion.  相似文献   

Dependence of sediment sorting on bedload transport phase in a river meander          下载免费PDF全文

Albert Rovira  Francisco Núñez‐González  Carles Ibañez 《地球表面变化过程与地形》2018,43(10):2077-2088

It is widely recognized nowadays that there are at least two different phases of bedload sediment transport in gravel‐bed rivers. However, the transition between these phases is still poorly or subjectively defined, especially at bends in rivers, where cross‐stream sediment transport can strongly influence changes in the texture of the transported sediment. In this paper, we use piecewise models to identify objectively, at two points in the cross‐section of a river bend, the discharge at which the transition between bedload transport phases occurs. Piecewise models were applied to a new bedload data set collected during a wide range of discharges while analysing the associated changes in sediment texture. Results allowed the identification of two well‐differentiated phases of sediment transport (phase I and phase II), with a breakpoint located around bankfull discharge. Associated with each phase there was a change in bedload texture. In phase I there was non‐dominance in the transport of fine or coarse fractions at a particular sampling point; but in phase II bedload texture was strongly linked to the position of the sampling point across the channel. In this phase, fine particles tended to be transported to the inner bank, while coarse sizes were transferred throughout the middle parts of the channel. Moreover, bedload texture at the inner sampling point became bimodal while the transport of pebble‐sized particles was increasing in the central parts of the river channel. It is suggested that this general pattern may be related both to secondary currents, which transfer finer particles from the outer to the inner bank, and to the progressive dismantling of the riverbed surface layer. Copyright © 2018 John Wiley & Sons, Ltd.  相似文献   

四川省生态旅游发展的层次与阶段   总被引：3，自引：0，他引：3  

陈国阶  王青  涂建军 《地理科学》2006,26(2):151-155

生态旅游是一项新的旅游活动、一项新的产业,是社会经济发展到一定阶段的产物。生态旅游的开发是一个循序渐进的过程,产业的发展存在着初级阶段、发展阶段和成熟阶段。结合四川社会经济发展水平和生态旅游资源分布规律,四川生态旅游形式应具有一定的时空特征,表现为时间上的阶段性和空间上的差异性,即在同一时期的不同地区或同一地区的不同发展阶段同时存在三种形式的生态旅游:泛生态旅游、准生态旅游、纯生态旅游。  相似文献   

南亚和东亚热带夏季风强弱不同配置及其对中国夏季降水的影响北大核心          下载免费PDF全文

顾元华  郭品文  胡景高  郭栋 《气象科学》2023,43(1):15-24

利用NOAA向外长波辐射(OLR)、NCEP/NCAR再分析资料和CN05.1降水资料,研究了南亚和东亚热带夏季风强度年际变化关系,及其强弱不同配置对中国夏季降水的影响。结果表明:南亚和东亚热带夏季风强度变化之间存在同相和反相两种配置,定义的强度同相和反相变化指数可以很好地表征该关系。同相变化模态可能与海温异常时的强El Nino(La Nina)影响有关,其反相变化模态受El Nino(La Nina)以及印度洋海盆一致模的影响,同时西太平洋副热带高压和伊朗高压位置东西偏移和强度变化也影响着不同配置的出现。两者不同配置时,对中国夏季降水的影响不同。当变化呈同相偏强时,夏季中国东部地区降水为“中间少南北多”的雨型。当变化呈反相,东亚热带夏季风偏强南亚夏季风偏弱时,夏季中国东部地区降水为“一致偏少”雨型。  相似文献