This research was jointly granted by the Key Scientific Research Project of Inner Mongolia Geological Survey(2004-05);the National Natural Science Foundation of China(Grant No.40272088).
The Dajing Cu-Sn-polymetallic ore deposit is famous for its large scale, abundant associated elements, narrow and closely-spaced development of ore veins and high grade, but exploration within the mining district and ...
the National Natural Science Foundation of China (No. 40272088).
The Zhangjiakou-Xuanhua area is a mineral resource-concentrated area for gold-silver polymetallic ore deposits. The temporal and spatial distribution and origin of mineral resources have been argued for a long time. B...
This research is jointly granted by the National Natural Science Foundation of China (Grant No. 40272088).
The Longquanzhan gold deposit hosted in granitic cataclasites with mylontization of the foot wall of the main Yishui-Tangtou fault. 3He/4He ratios in fluid inclusions range from 0. 14 to 0. 24 R/Ra,close to those of t...
This research project was financially supported jointly by the NationaNatural Science Foundation of China (Grant No. 40272088), theLarge-scale Geological Survey in China (No. 2000110100038) and theCentral Mining Funds (2003-20).
This work deals with the characteristics of mantle branch structure in western Shandong Province, China, with respect to the distribution characteristics and ages of the regional strata, the development of ring-like a...
This work was supported by the Chinese Academy of Sciences(Grant No.KZCX3-SW-139);the National Natural Science Foundation of China(Grant Nos.40231001 and 40272088);the'973'Project(Grant No.2004CB720203).
In this study, grain-size of 507 bulk samples from the QA-I Mioceneloess-soil sequence at Qinan were analyzed, and the grain-size features are compared with those oftypical Quaternary loess and soil samples, represent...