Mesozoic Intrusive Rocks Characteristics and Comparative between the West Hubei-Jiangxi and the East Jiangsu-Anhui

2012 ◽  
Vol 524-527 ◽  
pp. 144-147
Author(s):  
Cui Xia Qu ◽  
Xing Ke Yang ◽  
Hu Jun He ◽  
Hong Ye Song

This paper relies on "The base structure and guide the middle and lower Yangtze River mine - re-controlling factors of research project" in order to study the Mesozoic intrusive rocks in the characteristics of the middle and lower Yangtze River area and distribute-on of the western part of Hubei - Jiangxi and eastern Jiangsu - Anhui comparative study of eastern and western areas. On the basis of the full collection and comprehensive study of previous data, with the actual project work and research, through comprehensive research and analysis, bounded on the east and west of Jiujiang area controlled by different tectonic framework of characteristics of intrusive rock, mainly from the petrology, rock chemistry, magma sources and diagenetic characteristics such as age were compared with paper.

2015 ◽  
Vol 41 (4) ◽  
pp. 613
Author(s):  
Zhong-Wei TIAN ◽  
Yong-Hui FAN ◽  
Mei YIN ◽  
Fang-Rui WANG ◽  
Jian CAI ◽  
...  

Ecosphere ◽  
2017 ◽  
Vol 8 (10) ◽  
pp. e01967 ◽  
Author(s):  
Ming-Hong Lu ◽  
Xiao Chen ◽  
Wan-Cai Liu ◽  
Feng Zhu ◽  
Ka-Sing Lim ◽  
...  

2013 ◽  
Vol 17 (5) ◽  
pp. 1985-2000 ◽  
Author(s):  
Y. Huang ◽  
M. S. Salama ◽  
M. S. Krol ◽  
R. van der Velde ◽  
A. Y. Hoekstra ◽  
...  

Abstract. In this study, we analyze 32 yr of terrestrial water storage (TWS) data obtained from the Interim Reanalysis Data (ERA-Interim) and Noah model from the Global Land Data Assimilation System (GLDAS-Noah) for the period 1979 to 2010. The accuracy of these datasets is validated using 26 yr (1979–2004) of runoff data from the Yichang gauging station and comparing them with 32 yr of independent precipitation data obtained from the Global Precipitation Climatology Centre Full Data Reanalysis Version 6 (GPCC) and NOAA's PRECipitation REConstruction over Land (PREC/L). Spatial and temporal analysis of the TWS data shows that TWS in the Yangtze River basin has decreased significantly since the year 1998. The driest period in the basin occurred between 2005 and 2010, and particularly in the middle and lower Yangtze reaches. The TWS figures changed abruptly to persistently high negative anomalies in the middle and lower Yangtze reaches in 2004. The year 2006 is identified as major inflection point, at which the system starts exhibiting a persistent decrease in TWS. Comparing these TWS trends with independent precipitation datasets shows that the recent decrease in TWS can be attributed mainly to a decrease in the amount of precipitation. Our findings are based on observations and modeling datasets and confirm previous results based on gauging station datasets.


Sign in / Sign up

Export Citation Format

Share Document