期刊文献+
共找到2篇文章
< 1 >
每页显示 20 50 100
2015年4-5月尼泊尔地震的地震构造:基于余震样式、地表效应及形变特征的分析评估
1
作者 Revathy M.Parameswaran thulasiraman natarajan +8 位作者 Kusala Rajendran C.P.Rajendran Rishav Mallick Matthew Wood Harish C.Lekhak 胡亚轩(译) 宋尚武(译) 李煜航(校) 白志明(复校) 《世界地震译丛》 2016年第2期111-129,共19页
2015年4月25日尼泊尔中部的廓尔喀发生了M_W7.8地震,随后的5月12日,在距此震震中以东约140km处又发生了M_W7.3地震。这两次地震的发生为我们理解喜马拉雅山的地震提供了新的视角和机遇。本文试图基于这两次事件所产生的形变场以及它们... 2015年4月25日尼泊尔中部的廓尔喀发生了M_W7.8地震,随后的5月12日,在距此震震中以东约140km处又发生了M_W7.3地震。这两次地震的发生为我们理解喜马拉雅山的地震提供了新的视角和机遇。本文试图基于这两次事件所产生的形变场以及它们余震的时空特征分析这些地震的地震构造。结合震后对当地的破坏和地表形变等的实地考察可明显看出,尽管主震滑动主要局限于主喜马拉雅逆冲断裂(MHT),但破裂并没有扩展至主前缘逆冲断裂(MFT)。由形变场现有的合成孔径雷达干涉测量图像支持的野外证据表明,滑动分量可能在先前识别出的失序逆冲/活动逆冲区出现,该区域平行于主中央逆冲断裂(MCT),即文献中描述的与地形一致的地理转换带PT_2。第一次破裂终止后触发了第二次大地震,余震的分布在空间上仍局限在PT_2最东端。2015年发震序列的机理表明,失序逆冲断层吸收了部分滑移量,依据当前对地震机理的理解,此次地震始于主喜马拉雅逆冲断裂。 展开更多
关键词 地震活动性 尼泊尔喜马拉雅 震群 地表形变 余震 自然地理转换带 失序逆冲断层
下载PDF
Short-term desalination of Pulicat lagoon(Southeast India)due to the 2015 extreme flood event:insights from Land-Ocean Interactions in Coastal Zone(LOICZ)models
2
作者 Harini Santhanam thulasiraman natarajan 《Ecological Processes》 SCIE EI 2018年第1期93-105,共13页
Introduction:We investigated the magnitude and duration of desalination of Pulicat—a coastal lagoon ecosystem connected to the Bay of Bengal on the South-eastern coast of India—during the 2015 South India flood even... Introduction:We investigated the magnitude and duration of desalination of Pulicat—a coastal lagoon ecosystem connected to the Bay of Bengal on the South-eastern coast of India—during the 2015 South India flood event which was a period of high-magnitude precipitation and riverine flooding.Methods:We estimated freshwater runoff into the lagoon using flow accumulation models for a period of 55 days(November 1 to December 25,2015)using daily gridded precipitation data from the Global Precipitation Measurement and a digital elevation model.Using the estimates of freshwater runoff,direct precipitation and observed salinities,we simulated water and salinity fluxes of the lagoon using the Land-Ocean Interactions in the Coastal Zone model.Further,we also used Monte Carlo simulation to estimate the uncertainty in system salinity,the residual salinity at the boundary and the freshwater residence times in the lagoon.Results:We estimated that a high volume(~760×10^(6) m^(3))of relatively low salinity waters(residual salinity=23.47 psu)had been exported from the lagoon to the Bay of Bengal during the period which is likely to have caused a strong dip in the daily salinity profile of the coastal sea.We contend that the lagoon experienced~40%desalination due to the 2015 event with a freshwater residence time of 18.5 days.Conclusions:The study highlighted the short-term,high-magnitude desalination undergone by Pulicat lagoon during the 2015 South India floods.Considering the high residual and exchange volumes obtained from the study,we conclude that Pulicat could be a major exporter of relatively low salinity waters to the Bay of Bengal during monsoons. 展开更多
关键词 Pulicat lagoon 2015 South India floods LOICZ model Flow accumulation model Bay of Bengal
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部