ORE DEPOSITS OF CHINCHUANTANG,CHENHSIEN,HUNAN

I.INTRODUCTION The ore deposits of Chinchuantang were known to geologists sincethe publication of the report by Mr.H.C.Wang~1 and others in theyear of 1930.In this region a great number of different ores includingzinc,lead,arsenic,sulphur,manganese,tungsten and bismuth have been     

与王炳章先生讨论广西铀矿问题

近读王炳章先生“对南延宗吴磊伯二氏所记广西几种铀矿物之我见”一文,深感本文能引起王先生之注意,加以精辟之讨论,赐教甚多,实为荣幸钦佩之至,兹就王先生所提两点,分别讨论如下:     

答郝钊先生

(一) 武汉大学郝剑先生在上文里,对于作者等所记广西铀矿物的种名及成因等,提出几点意见商讨,值得注意,现在拟作一简单的答覆:     

地質和鑛產的關係

調查地質同時調查鑛產,這本是地質界的天經地義,再沒有提示的必要。現在所要說的,是我們調查地質時候,一定要進一步抱有一種野心和希望:有了這種野心和希望,便覺得乾     

MICROSCOPICAL STUDY OF THE SHUIKOUSHAN LEAD-ZINC DEPOSIT IN CHANGNING DISTRICT, S. HUNAN

INTRODUCTION Shuikoushan is the most important and well known mining district for production of silver, lead, zinc and pyrite in China. It is situated at about 65 li N. E. of Changning, 90 li S. of Hengyang and 620 li from Changsha, the Capital of Hunan.     

地質圖上火成岩花紋(Pattern)用法之商討

地質圖上各類岩石,可以用兩種方法來表示牠,一種是用顔色的,一種是用花纹(Pattern)的。世界上的一般地質學家,對於地質圖的繪畫,在水成岩,因牠本身間,有層次和結構的顯著不同,而種類又不多,比較的容易表示,大家用起来,並無背謬     

广西省富贺锺区铀矿之发现

吾国自有地质事业以来,对於稀有矿物,少有注意,唯民国二十年,何作霖先生在丁道衡先生所采绥远铁矿内,发现两种含Ce,La,Yt之Beiyinite与Oborite,二十三年张定钊氏曾用分光分析方法,检定赣南钨锡铋钼等矿内,含有V,Re(?)U(?),Ta,Nb(?),Cr,Te,Ag,Au等元素,最近Morris氏来广     

赣南之锡矿

赣南锡矿除大庾之洪水寨、漂塘,下龙、生龙口以外,其他各处产量均微,若以赣南总锡产量与钨矿产量比较之,相去甚远。历年纪录,锡钨相比,总觉瞠乎其後,依宗等调查研究     

MICROSCOPICAL STUDY OF THE SHUIKOUSHAN LEAD-ZINC DEPOSIT IN CHANGNING DISTRICT, S. HUNAN

INTRODUCTION Shuikoushan is the most important and well known mining district for production of silver, lead, zinc and pyrite in China. It is situated at about 65 li N. E. of Changning, 90 li S. of Hengyang and 620 li from Changsha, the Capital of Hunan. It has been visited by many geologists and mining