INTRODUCTION Gold placer deposits are generally divided into two classes based on the distance between the place of deposition and the auriferous lodes from which they are derived. The first is called eluvial deposits which are usually found in the vicinity of their parent lodes. Such phacers are
Abstract:
INTRODUCTION Gold placer deposits are generally divided into two classes based on the distance between the place of deposition and the auriferous lodes from which they are derived. The first is called eluvial deposits which are usually found in the vicinity of their parent lodes. Such phacers are
[8]Li Junjian,Shen Baofeng,Mao Debao,Li Shuangbao,Zhou Huifang and Cheng Yuming Tianjin Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,Tianjin Nonferrous Metal Geological Exploration Bureau,Changchun,Jilin.Mineralization Ages of the Jiapigou Gold Deposits,Jilin[J].《地质学报》英文版,1997,71(2):180-188.
[12]DENG Jun,YANG Liqiang,SUN Zhongshi,WANG Jianping,WANG QingfeiXIN Hongbo and LI Xinjun Key Laboratory of Lithospheric Tectonics and Exploration. China University of Geosciences,Ministry of Education,Beijing,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,Faculty of Earth Sciences,Jilin University,Changchun,Jilin.A Metallogenic Model of Gold Deposits of the Jiaodong Granite-Greenstone Belt[J].《地质学报》英文版,2003,77(4):537-546.
.1943. A Proposed Classification of Alluvial Placer Gold Deposits of W Szechuan and the Border Region of N Szechuan and S Kansu[J].地质学报,(Z1):118-123. .1943.[J]. Acta Geologica Sinica,(Z1):118-123.
